diff --git a/Makefile b/Makefile
index 3c2227a..76f33e8 100644
--- a/Makefile
+++ b/Makefile
@@ -13,16 +13,24 @@ setup-git-hooks:
lint:
ruff check soil_id
+ ruff format soil_id --diff
format:
+ ruff check soil_id --fix
ruff format soil_id
lock:
CUSTOM_COMPILE_COMMAND="make lock" uv pip compile --upgrade --generate-hashes requirements/base.in -o requirements.txt
+lock-package:
+ CUSTOM_COMPILE_COMMAND="make lock" uv pip compile --upgrade-package $(PACKAGE) --generate-hashes --emit-build-options requirements/base.in requirements/deploy.in -o requirements.txt
+
lock-dev:
CUSTOM_COMPILE_COMMAND="make lock-dev" uv pip compile --upgrade --generate-hashes requirements/dev.in -o requirements-dev.txt
+lock-dev-package:
+ CUSTOM_COMPILE_COMMAND="make lock-dev" uv pip compile --upgrade-package $(PACKAGE) --generate-hashes requirements/dev.in -o requirements-dev.txt
+
build:
echo "Building TK..."
@@ -35,9 +43,16 @@ clean:
test: clean check_rebuild
if [ -z "$(PATTERN)" ]; then \
- $(DC_RUN_CMD) pytest soil_id; \
+ $(DC_RUN_CMD) pytest soil_id -vv; \
+ else \
+ $(DC_RUN_CMD) pytest soil_id -vv -k $(PATTERN); \
+ fi
+
+test_update_snapshots: clean check_rebuild
+ if [ -z "$(PATTERN)" ]; then \
+ $(DC_RUN_CMD) pytest soil_id --snapshot-update; \
else \
- $(DC_RUN_CMD) pytest soil_id -k $(PATTERN); \
+ $(DC_RUN_CMD) pytest soil_id --snapshot-update -k $(PATTERN); \
fi
test-verbose:
diff --git a/requirements-dev.txt b/requirements-dev.txt
index 2ec54e4..31b0a7e 100644
--- a/requirements-dev.txt
+++ b/requirements-dev.txt
@@ -161,6 +161,7 @@ pytest==8.4.2 \
# via
# -r requirements/dev.in
# pytest-profiling
+ # syrupy
pytest-profiling==1.8.1 \
--hash=sha256:3dd8713a96298b42d83de8f5951df3ada3e61b3e5d2a06956684175529e17aea \
--hash=sha256:3f171fa69d5c82fa9aab76d66abd5f59da69135c37d6ae5bf7557f1b154cb08d
@@ -253,6 +254,10 @@ soupsieve==2.8 \
--hash=sha256:0cc76456a30e20f5d7f2e14a98a4ae2ee4e5abdc7c5ea0aafe795f344bc7984c \
--hash=sha256:e2dd4a40a628cb5f28f6d4b0db8800b8f581b65bb380b97de22ba5ca8d72572f
# via beautifulsoup4
+syrupy==4.9.1 \
+ --hash=sha256:b7d0fcadad80a7d2f6c4c71917918e8ebe2483e8c703dfc8d49cdbb01081f9a4 \
+ --hash=sha256:b94cc12ed0e5e75b448255430af642516842a2374a46936dd2650cfb6dd20eda
+ # via -r requirements/dev.in
tqdm==4.67.1 \
--hash=sha256:26445eca388f82e72884e0d580d5464cd801a3ea01e63e5601bdff9ba6a48de2 \
--hash=sha256:f8aef9c52c08c13a65f30ea34f4e5aac3fd1a34959879d7e59e63027286627f2
diff --git a/requirements/dev.in b/requirements/dev.in
index e351014..b993bd4 100644
--- a/requirements/dev.in
+++ b/requirements/dev.in
@@ -4,3 +4,4 @@ ruff
pre-commit
pytest
pytest-profiling
+syrupy
diff --git a/soil_id/config.py b/soil_id/config.py
index f228a46..4ec83b3 100644
--- a/soil_id/config.py
+++ b/soil_id/config.py
@@ -15,12 +15,17 @@
import os
import tempfile
+from dotenv import load_dotenv
from platformdirs import user_cache_dir
+# Load environment variables from .env file
+load_dotenv()
+
+
DATA_PATH = os.environ.get("DATA_PATH", "Data")
# Numpy seeding
-RANDOM_SEED = os.environ.get("RANDOM_SEED", 19)
+RANDOM_SEED = int(os.environ.get("RANDOM_SEED", 19))
# Output
APP_NAME = os.environ.get("APP_NAME", "org.terraso.soilid")
@@ -41,5 +46,6 @@
# Database
DB_NAME = os.environ.get("DB_NAME", "terraso_backend")
DB_HOST = os.environ.get("DB_HOST")
+DB_PORT = int(os.environ.get("DB_PORT", 5432))
DB_USERNAME = os.environ.get("DB_USERNAME")
DB_PASSWORD = os.environ.get("DB_PASSWORD")
diff --git a/soil_id/db.py b/soil_id/db.py
index a8f99be..a602a3b 100644
--- a/soil_id/db.py
+++ b/soil_id/db.py
@@ -39,6 +39,7 @@ def get_datastore_connection():
user=soil_id.config.DB_USERNAME,
password=soil_id.config.DB_PASSWORD,
dbname=soil_id.config.DB_NAME,
+ port=soil_id.config.DB_PORT,
)
return conn
except Exception as err:
@@ -185,6 +186,7 @@ def get_hwsd2_profile_data(connection, hwsd2_mu_select):
ph_water, elec_cond, fao90_name
FROM hwsd2_data
WHERE hwsd2_smu_id IN ({placeholders})
+ ORDER BY hwsd2_smu_id, compid, sequence, layer
"""
cur.execute(sql_query, tuple(hwsd2_mu_select))
results = cur.fetchall()
@@ -352,7 +354,8 @@ def extract_hwsd2_data(connection, lon, lat, buffer_dist, table_name):
BOOL_OR(ST_Intersects(shape, {point})) AS pt_intersect
FROM hwsd2_segment
WHERE ST_DWithin(shape, {point}, {buffer_dist})
- GROUP BY hwsd2_id;
+ GROUP BY hwsd2_id
+ ORDER BY hwsd2_id;
"""
# Use GeoPandas to execute the main query and load results into a GeoDataFrame.
@@ -398,7 +401,8 @@ def get_WRB_descriptions(connection, WRB_Comp_List):
sql = f"""SELECT WRB_tax, Description_en, Management_en, Description_es, Management_es,
Description_ks, Management_ks, Description_fr, Management_fr
FROM wrb_fao90_desc
- WHERE WRB_tax IN ({placeholders})"""
+ WHERE WRB_tax IN ({placeholders})
+ ORDER BY WRB_tax"""
# Execute the query with the parameters
cur.execute(sql, tuple(WRB_Comp_List))
@@ -455,6 +459,7 @@ def execute_query(query, params):
SELECT lu.WRB_1984_Full
FROM wrb2006_to_fao90 AS lu
WHERE lu.WRB_2006_Full = ANY(%s)
+ ORDER BY lu.WRB_1984_Full
"""
names = execute_query(sql1, ([WRB_Comp_List],))
@@ -491,6 +496,7 @@ def execute_query(query, params):
Management_fr
FROM wrb_fao90_desc
WHERE WRB_tax = ANY(%s)
+ ORDER BY WRB_tax
"""
results = execute_query(sql2, ([WRB_Comp_List_mapped],))
diff --git a/soil_id/global_soil.py b/soil_id/global_soil.py
index 09f96d0..fcbd418 100644
--- a/soil_id/global_soil.py
+++ b/soil_id/global_soil.py
@@ -31,8 +31,8 @@
from .utils import (
adjust_depth_interval,
agg_data_layer,
- assign_max_distance_scores,
- calculate_location_score,
+ # assign_max_distance_scores,
+ # calculate_location_score,
drop_cokey_horz,
getCF_fromClass,
getClay,
@@ -42,6 +42,7 @@
gower_distances,
max_comp_depth,
pedon_color,
+ process_distance_scores,
silt_calc,
)
@@ -71,7 +72,7 @@ class SoilListOutputData:
##################################################################################################
# getSoilLocationBasedGlobal #
##################################################################################################
-def list_soils_global(connection, lon, lat, buffer_dist=100000):
+def list_soils_global(connection, lon, lat, buffer_dist=30000):
# Extract HWSD2 Data
try:
hwsd2_data = extract_hwsd2_data(
@@ -89,9 +90,9 @@ def list_soils_global(connection, lon, lat, buffer_dist=100000):
# Component Data
mucompdata_pd = hwsd2_data[["hwsd2", "fao90_name", "distance", "share", "compid"]]
- mucompdata_pd.columns = ["mukey", "compname", "distance", "share", "cokey"]
+ mucompdata_pd.columns = ["mukey", "compname", "distance", "comppct_r", "cokey"]
mucompdata_pd["distance"] = pd.to_numeric(mucompdata_pd["distance"])
- mucompdata_pd["share"] = pd.to_numeric(mucompdata_pd["share"])
+ mucompdata_pd["comppct_r"] = pd.to_numeric(mucompdata_pd["comppct_r"])
mucompdata_pd = mucompdata_pd.drop_duplicates().reset_index(drop=True)
##############################################################################################
@@ -104,35 +105,12 @@ def list_soils_global(connection, lon, lat, buffer_dist=100000):
# instances.
##############################################################################################
ExpCoeff = -0.00036888 # Decays to 0.25 @ 10km
- loc_scores = []
- mucompdata_grouped = mucompdata_pd.groupby(["mukey", "cokey"], sort=False)
-
- for (mukey, cokey), group in mucompdata_grouped:
- loc_score = calculate_location_score(group, ExpCoeff)
- loc_scores.append({"cokey": cokey, "mukey": mukey, "distance_score": round(loc_score, 3)})
-
- loc_top_pd = pd.DataFrame(loc_scores)
- loc_top_comp_prob = loc_top_pd.groupby("cokey").distance_score.sum()
- loc_bot_prob_sum = loc_top_pd.distance_score.sum()
- cond_prob = (loc_top_comp_prob / loc_bot_prob_sum).reset_index(name="distance_score")
-
- mucompdata_pd = pd.merge(mucompdata_pd, cond_prob, on="cokey", how="left")
- mucompdata_pd = mucompdata_pd.sort_values("distance_score", ascending=False)
-
- mucompdata_pd = mucompdata_pd.reset_index(drop=True)
- mucompdata_pd["distance"] = mucompdata_pd["distance"].round(4)
- mucompdata_pd["Index"] = mucompdata_pd.index
-
- # Group by component name
- mucompdata_grouped = mucompdata_pd.groupby("compname", sort=False)
-
- # Take at most 12 groups
- mucompdata_comp_grps = [group for _, group in mucompdata_grouped][:12]
-
- # Assign max distance scores to all members within each group
- soilIDList_out = [assign_max_distance_scores(group) for group in mucompdata_comp_grps]
+ mucompdata_pd = process_distance_scores(
+ mucompdata_pd,
+ ExpCoeff,
+ compkind_filter=False, # Disable compkind filtering for global data
+ )
- mucompdata_pd = pd.concat(soilIDList_out).reset_index(drop=True)
comp_key = mucompdata_pd["cokey"].tolist()
# -----------------------------------------------------------------------------------------------------------------
@@ -181,6 +159,11 @@ def list_soils_global(connection, lon, lat, buffer_dist=100000):
lambda x: str(x) if isinstance(x, np.ndarray) else x
)
+ # Add distance column from mucompdata_pd using cokey link
+ muhorzdata_pd = pd.merge(
+ muhorzdata_pd, mucompdata_pd[["cokey", "distance"]], on="cokey", how="left"
+ )
+
# Check for duplicate component instances
hz_drop = drop_cokey_horz(muhorzdata_pd)
if hz_drop is not None:
@@ -192,8 +175,10 @@ def list_soils_global(connection, lon, lat, buffer_dist=100000):
comp_key = muhorzdata_pd["cokey"].unique().tolist()
mucompdata_pd = mucompdata_pd[mucompdata_pd["cokey"].isin(comp_key)]
- # Sort mucompdata_pd based on 'distance_score' and 'distance'
- mucompdata_pd.sort_values(["distance_score", "distance"], ascending=[False, True], inplace=True)
+ # Sort mucompdata_pd based on 'cond_prob' and 'distance'
+ mucompdata_pd.sort_values(
+ ["cond_prob", "distance", "compname"], ascending=[False, True, True], inplace=True
+ )
mucompdata_pd.reset_index(drop=True, inplace=True)
# Duplicate the 'compname' column for grouping purposes
@@ -217,14 +202,17 @@ def list_soils_global(connection, lon, lat, buffer_dist=100000):
component_names = mucompdata_pd["compname"].tolist()
name_counts = collections.Counter(component_names)
- for name, count in name_counts.items():
+ for name, count in sorted(name_counts.items()): # Sort for deterministic order
if count > 1: # If a component name is duplicated
- suffixes = range(1, count + 1) # Generate suffixes for the duplicate names
- for suffix in suffixes:
- index = component_names.index(
- name
- ) # Find the index of the first occurrence of the duplicate name
- component_names[index] = name + str(suffix) # Append the suffix
+ # Find all indices for this name
+ indices = [i for i, comp_name in enumerate(component_names) if comp_name == name]
+ # Sort indices for deterministic order
+ indices.sort()
+
+ # Add suffixes to all occurrences except the first
+ for i, idx in enumerate(indices):
+ if i > 0: # Skip the first occurrence (keep original name)
+ component_names[idx] = name + str(i + 1) # Append suffix starting from 2
mucompdata_pd["compname"] = component_names
muhorzdata_pd.rename(columns={"compname": "compname_grp"}, inplace=True)
@@ -282,9 +270,9 @@ def list_soils_global(connection, lon, lat, buffer_dist=100000):
sand_pct_intpl[["c_sandpct_intpl_grp"]],
clay_pct_intpl[["c_claypct_intpl_grp"]],
cf_pct_intpl[["c_cfpct_intpl_grp"]],
- pd.DataFrame({"compname": [profile.compname.unique()[0]] * n_rows}),
- pd.DataFrame({"cokey": [profile.cokey.unique()[0]] * n_rows}),
- pd.DataFrame({"comppct": [profile.comppct_r.unique()[0]] * n_rows}),
+ pd.DataFrame({"compname": [sorted(profile.compname.unique())[0]] * n_rows}),
+ pd.DataFrame({"cokey": [sorted(profile.cokey.unique())[0]] * n_rows}),
+ pd.DataFrame({"comppct": [sorted(profile.comppct_r.unique())[0]] * n_rows}),
],
axis=1,
)
@@ -367,10 +355,10 @@ def list_soils_global(connection, lon, lat, buffer_dist=100000):
# Create index for component instance display
mucompdata_comp_grps_list = []
- mucompdata_comp_grps = [group for _, group in mucompdata_pd.groupby("compname_grp", sort=False)]
+ mucompdata_comp_grps = [group for _, group in mucompdata_pd.groupby("compname_grp", sort=True)]
for group in mucompdata_comp_grps:
- group = group.sort_values("distance").reset_index(drop=True)
+ group = group.sort_values(["distance", "compname"]).reset_index(drop=True)
soilID_rank = [True if idx == 0 else False for idx in range(len(group))]
group["soilID_rank"] = soilID_rank
@@ -391,9 +379,9 @@ def list_soils_global(connection, lon, lat, buffer_dist=100000):
]
soilIDRank_output_pd = pd.concat(soilIDRank_output, axis=0).reset_index(drop=True)
- mucompdata_cond_prob = mucompdata_pd.sort_values("distance_score", ascending=False).reset_index(
- drop=True
- )
+ mucompdata_cond_prob = mucompdata_pd.sort_values(
+ ["cond_prob", "compname"], ascending=[False, True]
+ ).reset_index(drop=True)
# Generate the Rank_Loc column values
rank_id = 1
@@ -413,9 +401,9 @@ def list_soils_global(connection, lon, lat, buffer_dist=100000):
# Handle NaN values
mucompdata_cond_prob.replace([np.nan, "nan", "None", [None]], "", inplace=True)
- # Sort mucompdata_cond_prob by soilID_rank and distance_score
+ # Sort mucompdata_cond_prob by soilID_rank, cond_prob, and compname for deterministic tie-breaking
mucompdata_cond_prob = mucompdata_cond_prob.sort_values(
- ["soilID_rank", "distance_score"], ascending=[False, False]
+ ["soilID_rank", "cond_prob", "compname"], ascending=[False, False, True]
)
# Generate the ID list
@@ -429,7 +417,7 @@ def list_soils_global(connection, lon, lat, buffer_dist=100000):
for site, comp, sc, rank in zip(
mucompdata_cond_prob["compname"],
mucompdata_cond_prob["compname_grp"],
- mucompdata_cond_prob["distance_score"].round(3),
+ mucompdata_cond_prob["cond_prob"].round(3),
mucompdata_cond_prob["Rank_Loc"],
)
]
@@ -455,7 +443,7 @@ def list_soils_global(connection, lon, lat, buffer_dist=100000):
"siteData": {
"mapunitID": row.mukey,
"componentID": row.cokey,
- "share": row.share,
+ "share": row.comppct_r,
"distance": round(row.distance, 3),
"minCompDistance": row.min_dist,
"soilDepth": row.c_very_bottom,
@@ -771,7 +759,7 @@ def rank_soils_global(
# Horizon Data Similarity
if soilIDRank_output_pd is not None:
- cokey_groups = [group for _, group in soilIDRank_output_pd.groupby("compname", sort=False)]
+ cokey_groups = [group for _, group in soilIDRank_output_pd.groupby("compname", sort=True)]
# Create lists to store component statuses
Comp_Rank_Status, Comp_Missing_Status, Comp_name = [], [], []
@@ -787,7 +775,7 @@ def rank_soils_global(
Comp_Missing_Status.append(
"Missing Data" if subset_group.isnull().values.any() else "Data Complete"
)
- Comp_name.append(group["compname"].unique()[0])
+ Comp_name.append(sorted(group["compname"].unique())[0])
Rank_Filter = pd.DataFrame(
{
@@ -896,7 +884,7 @@ def rank_soils_global(
D_final_horz.columns = ["compname", "compname_grp", "horz_score", "weight"]
D_final_horz = pd.merge(
D_final_horz,
- mucompdata_pd[["compname", "mukey", "cokey", "distance_score", "Rank_Loc"]],
+ mucompdata_pd[["compname", "mukey", "cokey", "cond_prob", "Rank_Loc"]],
on="compname",
how="left",
)
@@ -912,7 +900,7 @@ def rank_soils_global(
D_final_horz.columns = ["compname", "compname_grp", "horz_score", "weight"]
D_final_horz = pd.merge(
D_final_horz,
- mucompdata_pd[["compname", "mukey", "cokey", "distance_score", "Rank_Loc"]],
+ mucompdata_pd[["compname", "mukey", "cokey", "cond_prob", "Rank_Loc"]],
on="compname",
how="left",
)
@@ -1088,12 +1076,12 @@ def normalize(arr):
# Sorting and reindexing of Data-only score
soilIDList_data = []
- D_final_comp_grps = [g for _, g in D_final_horz.groupby("compname_grp", sort=False)]
+ D_final_comp_grps = [g for _, g in D_final_horz.groupby("compname_grp", sort=True)]
for comp_grps_temp in D_final_comp_grps:
- comp_grps_temp = comp_grps_temp.sort_values("Score_Data", ascending=False).reset_index(
- drop=True
- )
+ comp_grps_temp = comp_grps_temp.sort_values(
+ ["Score_Data", "compname"], ascending=[False, True]
+ ).reset_index(drop=True)
SID_data = [True] + [False] * (len(comp_grps_temp) - 1)
comp_grps_temp["soilID_rank_data"] = SID_data
soilIDList_data.append(comp_grps_temp)
@@ -1131,7 +1119,7 @@ def normalize(arr):
location_weight = 1
# Calculate the combined score
- Score_Data_Loc = (D_final_loc[["Score_Data", "distance_score"]].sum(axis=1)) / (
+ Score_Data_Loc = (D_final_loc[["Score_Data", "cond_prob"]].sum(axis=1)) / (
D_final_loc.weight + location_weight
)
@@ -1158,16 +1146,16 @@ def normalize(arr):
D_final_loc["Score_Data_Loc"] = D_final_loc["Score_Data_Loc"] / np.nanmax(
D_final_loc["Score_Data_Loc"]
)
- D_final_loc = D_final_loc.sort_values("Score_Data_Loc", ascending=False)
+ D_final_loc = D_final_loc.sort_values(["Score_Data_Loc", "compname"], ascending=[False, True])
# Sorting and reindexing of final dataframe
soilIDList_out = []
- # Group by 'compname_grp'
- for _, comp_grps_temp in D_final_loc.groupby("compname_grp", sort=False):
- comp_grps_temp = comp_grps_temp.sort_values("Score_Data_Loc", ascending=False).reset_index(
- drop=True
- )
+ # Group by 'compname_grp' with deterministic sorting
+ for _, comp_grps_temp in D_final_loc.groupby("compname_grp", sort=True):
+ comp_grps_temp = comp_grps_temp.sort_values(
+ ["Score_Data_Loc", "compname"], ascending=[False, True]
+ ).reset_index(drop=True)
if len(comp_grps_temp) > 1:
# Mark the first entry as True, all others as False
@@ -1200,9 +1188,9 @@ def normalize(arr):
D_final_loc["Rank_Data_Loc"] = Rank_DataLoc
- # Sort dataframe based on soilID_rank_final and Score_Data_Loc
+ # Sort dataframe based on soilID_rank_final, Score_Data_Loc, and compname for deterministic tie-breaking
D_final_loc = D_final_loc.sort_values(
- ["soilID_rank_final", "Score_Data_Loc"], ascending=[False, False]
+ ["soilID_rank_final", "Score_Data_Loc", "compname"], ascending=[False, False, True]
).reset_index(drop=True)
# Replace NaN values in the specified columns with 0.0
@@ -1211,14 +1199,14 @@ def normalize(arr):
"Score_Data",
"horz_score",
"Score_Data_Loc",
- "distance_score",
+ "cond_prob",
]
] = D_final_loc[
[
"Score_Data",
"horz_score",
"Score_Data_Loc",
- "distance_score",
+ "cond_prob",
]
].fillna(0.0)
@@ -1238,7 +1226,7 @@ def normalize(arr):
"" if row.missing_status == "Location data only" else round(row.Score_Data, 3)
),
"rank_data": "" if row.missing_status == "Location data only" else row.Rank_Data,
- "score_loc": round(row.distance_score, 3),
+ "score_loc": round(row.cond_prob, 3),
"rank_loc": row.Rank_Loc,
"componentData": row.missing_status,
}
@@ -1393,7 +1381,7 @@ def sg_list(connection, lon, lat):
if sg_tax:
try:
sg_tax_prob = pd.DataFrame(sg_tax["wrb_class_probability"], columns=["WRB_tax", "Prob"])
- sg_tax_prob.sort_values("Prob", ascending=False, inplace=True)
+ sg_tax_prob.sort_values(["Prob", "WRB_tax"], ascending=[False, True], inplace=True)
# Merge with descriptive info
WRB_Comp_Desc = getSG_descriptions(connection, sg_tax_prob["WRB_tax"].tolist())
diff --git a/soil_id/soil_sim.py b/soil_id/soil_sim.py
index 1e3afa0..9ffe149 100644
--- a/soil_id/soil_sim.py
+++ b/soil_id/soil_sim.py
@@ -66,7 +66,7 @@ def soil_sim(muhorzdata_pd):
sim_columns = [
"compname_grp",
"hzname",
- "distance_score",
+ "cond_prob",
"hzdept_r",
"hzdepb_r",
"sandtotal_l",
@@ -129,12 +129,12 @@ def soil_sim(muhorzdata_pd):
agg_data = []
# Group data by compname_grp
- sim_group_compname = [group for _, group in sim.groupby("compname_grp", sort=False)]
+ sim_group_compname = [group for _, group in sim.groupby("compname_grp", sort=True)]
for index, group in enumerate(sim_group_compname):
# aggregate data into 0-30 and 30-100 or bottom depth
group_ag = slice_and_aggregate_soil_data(group[sim_data_columns])
- group_ag["compname_grp"] = group["compname_grp"].unique()[0]
- group_ag["distance_score"] = group["distance_score"].unique()[0]
+ group_ag["compname_grp"] = sorted(group["compname_grp"].unique())[0]
+ group_ag["cond_prob"] = sorted(group["cond_prob"].unique())[0]
group_ag = group_ag.drop("Depth", axis=1)
# group_ag = group_ag.where(pd.notna(group_ag), 0.01)
group_ag = group_ag.reset_index(drop=True)
@@ -161,8 +161,20 @@ def soil_sim(muhorzdata_pd):
"wthirdbar_r",
"wfifteenbar_r",
]
- rep_columns["ilr1"] = pd.Series(ilr_site_txt[:, 0])
- rep_columns["ilr2"] = pd.Series(ilr_site_txt[:, 1])
+ # Handle both 1D and 2D array cases for ilr_site_txt
+ if ilr_site_txt.ndim == 1:
+ # If 1D, assume it's a single observation with 2 components
+ if len(ilr_site_txt) >= 2:
+ rep_columns["ilr1"] = pd.Series([ilr_site_txt[0]])
+ rep_columns["ilr2"] = pd.Series([ilr_site_txt[1]])
+ else:
+ # Fallback if insufficient data
+ rep_columns["ilr1"] = pd.Series([0.0])
+ rep_columns["ilr2"] = pd.Series([0.0])
+ else:
+ # Normal 2D case
+ rep_columns["ilr1"] = pd.Series(ilr_site_txt[:, 0])
+ rep_columns["ilr2"] = pd.Series(ilr_site_txt[:, 1])
rep_columns[cor_cols] = rep_columns[cor_cols].replace(0, 0.01)
is_constant = rep_columns["rfv_r"].nunique() == 1
if is_constant:
@@ -238,7 +250,7 @@ def soil_sim(muhorzdata_pd):
"""
Step 2. Simulate data for each row, with the number of simulations equal
- to the (distance_score*100)*10
+ to the (cond_prob*100)*10
"""
# Global soil texture correlation matrix (used for initial simulation)
texture_correlation_matrix = np.array(
@@ -270,7 +282,7 @@ def soil_sim(muhorzdata_pd):
simulated_txt = acomp(
simulate_correlated_triangular(
- (int(row["distance_score"] * 1000)), params_txt, texture_correlation_matrix
+ (int(row["cond_prob"] * 1000)), params_txt, texture_correlation_matrix
)
)
simulated_txt_ilr = ilr(simulated_txt)
@@ -279,8 +291,20 @@ def soil_sim(muhorzdata_pd):
Step 2c. Extract l,r,h values (min, median, max for ilr1 and ilr2) and format into a
params object for simiulation
"""
- ilr1_values = simulated_txt_ilr[:, 0]
- ilr2_values = simulated_txt_ilr[:, 1]
+ # Handle both 1D and 2D array cases for simulated_txt_ilr
+ if simulated_txt_ilr.ndim == 1:
+ # If 1D, assume it's a single observation with 2 components
+ if len(simulated_txt_ilr) >= 2:
+ ilr1_values = np.array([simulated_txt_ilr[0]])
+ ilr2_values = np.array([simulated_txt_ilr[1]])
+ else:
+ # Fallback if insufficient data
+ ilr1_values = np.array([0.0])
+ ilr2_values = np.array([0.0])
+ else:
+ # Normal 2D case
+ ilr1_values = simulated_txt_ilr[:, 0]
+ ilr2_values = simulated_txt_ilr[:, 1]
ilr1_l, ilr1_r, ilr1_h = (
ilr1_values.min(),
@@ -348,7 +372,7 @@ def soil_sim(muhorzdata_pd):
)
local_correlation_matrix = regularize_matrix(local_correlation_matrix)
- n_sim = max(int(row["distance_score"] * 1000), 20)
+ n_sim = max(int(row["cond_prob"] * 1000), 20)
sim_data = simulate_correlated_triangular(
n=n_sim,
params=params,
@@ -376,7 +400,7 @@ def soil_sim(muhorzdata_pd):
"water_retention_15_bar",
],
)
- rfv_unique = rep_columns["rfv_r"].unique()[0]
+ rfv_unique = sorted(rep_columns["rfv_r"].unique())[0]
sim_data["rfv"] = rfv_unique
else:
sim_data = pd.DataFrame(
@@ -522,10 +546,13 @@ def soil_sim(muhorzdata_pd):
groups1 = df1.groupby("compname_grp")
groups2 = df2.groupby("compname_grp")
+ # Use only groups that exist in df1 (depth 0 data is required)
+ grp_list_filtered = [grp for grp in grp_list if grp in groups1.groups]
+
# Concatenating corresponding groups
concatenated_groups = []
- for group_label in grp_list:
+ for group_label in grp_list_filtered:
group_df1 = groups1.get_group(group_label).reset_index(drop=True)
if group_label in groups2.groups:
group_df2 = groups2.get_group(group_label).reset_index(drop=True)
@@ -535,6 +562,7 @@ def soil_sim(muhorzdata_pd):
group_df2["compname_grp"] = group_df1["compname_grp"]
group_df2 = group_df2.fillna(0)
group_df2 = group_df2.reset_index(drop=True)
+
concatenated_group = pd.concat(
[group_df1, group_df2.drop("compname_grp", axis=1)], axis=1
)
diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-1.75,13.6].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-1.75,13.6].json
new file mode 100644
index 0000000..d17932a
--- /dev/null
+++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-1.75,13.6].json
@@ -0,0 +1,811 @@
+{
+ "list": {
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 3.0,
+ "sl2": 3.0,
+ "sl3": 3.0,
+ "sl4": 2.4,
+ "sl5": 2.29,
+ "sl6": 2.2,
+ "sl7": 2.0
+ },
+ "clay": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 6.2,
+ "sl5": 6.43,
+ "sl6": 6.8,
+ "sl7": 7.0
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Ferralic arenosols",
+ "name": "Ferralic arenosols",
+ "rank_loc": "1",
+ "score_loc": 0.433
+ },
+ "ph": {
+ "sl1": 5.3,
+ "sl2": 5.3,
+ "sl3": 5.3,
+ "sl4": 5.32,
+ "sl5": 5.34,
+ "sl6": 5.36,
+ "sl7": 5.37
+ },
+ "rock_fragments": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 4.2,
+ "sl5": 4.43,
+ "sl6": 4.6,
+ "sl7": 4.5
+ },
+ "sand": {
+ "sl1": 87.0,
+ "sl2": 87.0,
+ "sl3": 87.0,
+ "sl4": 86.8,
+ "sl5": 86.57,
+ "sl6": 86.2,
+ "sl7": 86.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 156032,
+ "distance": 0.0,
+ "mapunitID": 918,
+ "minCompDistance": 0.0,
+ "share": 60,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.",
+ "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.",
+ "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.",
+ "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.",
+ "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ",
+ "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.",
+ "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ",
+ "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. "
+ }
+ },
+ "texture": {
+ "sl1": "Loamy sand",
+ "sl2": "Loamy sand",
+ "sl3": "Loamy sand",
+ "sl4": "Loamy sand",
+ "sl5": "Loamy sand",
+ "sl6": "Loamy sand",
+ "sl7": "Loamy sand"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 10.0,
+ "sl2": 10.0,
+ "sl3": 10.0,
+ "sl4": 8.0,
+ "sl5": 7.43,
+ "sl6": 7.0,
+ "sl7": 6.83
+ },
+ "clay": {
+ "sl1": 43.0,
+ "sl2": 43.0,
+ "sl3": 43.0,
+ "sl4": 46.4,
+ "sl5": 47.43,
+ "sl6": 48.2,
+ "sl7": 48.33
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Haplic ferralsols",
+ "name": "Haplic ferralsols",
+ "rank_loc": "2",
+ "score_loc": 0.3
+ },
+ "ph": {
+ "sl1": 4.9,
+ "sl2": 4.9,
+ "sl3": 4.9,
+ "sl4": 4.92,
+ "sl5": 4.96,
+ "sl6": 5.0,
+ "sl7": 5.02
+ },
+ "rock_fragments": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 4.6,
+ "sl5": 4.71,
+ "sl6": 5.0,
+ "sl7": 5.0
+ },
+ "sand": {
+ "sl1": 40.0,
+ "sl2": 40.0,
+ "sl3": 40.0,
+ "sl4": 37.4,
+ "sl5": 36.57,
+ "sl6": 35.8,
+ "sl7": 35.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 156034,
+ "distance": 0.0,
+ "mapunitID": 918,
+ "minCompDistance": 0.0,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.",
+ "Description_es": "Los Ferralsoles Háplicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada de retener nutrientes. ",
+ "Description_fr": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.",
+ "Description_ks": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.",
+ "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_es": "Estos suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.",
+ "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used."
+ }
+ },
+ "texture": {
+ "sl1": "Unknown",
+ "sl2": "Unknown",
+ "sl3": "Unknown",
+ "sl4": "Unknown",
+ "sl5": "Unknown",
+ "sl6": "Unknown",
+ "sl7": "Unknown"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 7.0,
+ "sl2": 7.0,
+ "sl3": 7.0,
+ "sl4": 5.6,
+ "sl5": 5.14,
+ "sl6": 4.6,
+ "sl7": 4.33
+ },
+ "clay": {
+ "sl1": 35.0,
+ "sl2": 35.0,
+ "sl3": 35.0,
+ "sl4": 39.2,
+ "sl5": 40.71,
+ "sl6": 42.0,
+ "sl7": 42.5
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Xanthic ferralsols",
+ "name": "Xanthic ferralsols",
+ "rank_loc": "3",
+ "score_loc": 0.133
+ },
+ "ph": {
+ "sl1": 4.5,
+ "sl2": 4.5,
+ "sl3": 4.5,
+ "sl4": 4.58,
+ "sl5": 4.63,
+ "sl6": 4.68,
+ "sl7": 4.72
+ },
+ "rock_fragments": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 3.2,
+ "sl5": 3.57,
+ "sl6": 4.0,
+ "sl7": 5.0
+ },
+ "sand": {
+ "sl1": 53.0,
+ "sl2": 53.0,
+ "sl3": 53.0,
+ "sl4": 50.0,
+ "sl5": 48.71,
+ "sl6": 47.6,
+ "sl7": 47.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 156033,
+ "distance": 0.0,
+ "mapunitID": 918,
+ "minCompDistance": 0.0,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ",
+ "Description_es": "Los Ferralsoles Xánticos son suelos bien desarrollados en climas húmedos y cálidos que están dominados por minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos xánticos tienen subsuelos de color amarillo que indican una retención de humedad ligeramente superior. ",
+ "Description_fr": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ",
+ "Description_ks": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ",
+ "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos. *Prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.",
+ "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy clay",
+ "sl2": "Sandy clay",
+ "sl3": "Sandy clay",
+ "sl4": "Sandy clay",
+ "sl5": "Sandy clay",
+ "sl6": "Sandy clay",
+ "sl7": "Sandy clay"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 9.0,
+ "sl2": 9.0,
+ "sl3": 9.0,
+ "sl4": 7.6,
+ "sl5": 7.14,
+ "sl6": 6.8,
+ "sl7": 6.67
+ },
+ "clay": {
+ "sl1": 31.0,
+ "sl2": 31.0,
+ "sl3": 31.0,
+ "sl4": 33.4,
+ "sl5": 33.86,
+ "sl6": 34.0,
+ "sl7": 33.83
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 0.86,
+ "sl6": 0.6,
+ "sl7": 0.5
+ },
+ "id": {
+ "component": "Ferralic cambisols",
+ "name": "Ferralic cambisols",
+ "rank_loc": "4",
+ "score_loc": 0.083
+ },
+ "ph": {
+ "sl1": 5.1,
+ "sl2": 5.1,
+ "sl3": 5.1,
+ "sl4": 5.12,
+ "sl5": 5.14,
+ "sl6": 5.14,
+ "sl7": 5.13
+ },
+ "rock_fragments": {
+ "sl1": 9.0,
+ "sl2": 9.0,
+ "sl3": 9.0,
+ "sl4": 10.2,
+ "sl5": 11.43,
+ "sl6": 12.6,
+ "sl7": 12.83
+ },
+ "sand": {
+ "sl1": 45.0,
+ "sl2": 45.0,
+ "sl3": 45.0,
+ "sl4": 43.0,
+ "sl5": 42.43,
+ "sl6": 42.0,
+ "sl7": 42.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 144042,
+ "distance": 29708.866,
+ "mapunitID": 463,
+ "minCompDistance": 29708.86642894,
+ "share": 50,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.",
+ "Description_es": "Los Cambisoles Ferrálicos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos tienen una escasa capacidad para retener nutrientes debido a su baja capacidad de intercambio catiónico. Como retienen menos nutrientes, suelen ser menos productivos. ",
+ "Description_fr": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.",
+ "Description_ks": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.",
+ "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ",
+ "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
El tipo de arcilla de este suelo está extremadamente erosionado, y como tal tendrá una baja capacidad de suministro de nutrientes.
La fertilización será necesaria para mejorar la productividad.",
+ "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ",
+ "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. "
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 9.4,
+ "sl5": 8.57,
+ "sl6": 7.8,
+ "sl7": 8.17
+ },
+ "clay": {
+ "sl1": 23.0,
+ "sl2": 23.0,
+ "sl3": 23.0,
+ "sl4": 24.2,
+ "sl5": 24.29,
+ "sl6": 24.2,
+ "sl7": 24.5
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 1.4,
+ "sl5": 1.43,
+ "sl6": 1.6,
+ "sl7": 1.67
+ },
+ "id": {
+ "component": "Dystric fluvisols",
+ "name": "Dystric fluvisols",
+ "rank_loc": "5",
+ "score_loc": 0.017
+ },
+ "ph": {
+ "sl1": 4.9,
+ "sl2": 4.9,
+ "sl3": 4.9,
+ "sl4": 4.96,
+ "sl5": 4.99,
+ "sl6": 5.04,
+ "sl7": 5.08
+ },
+ "rock_fragments": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 4.8,
+ "sl5": 7.0,
+ "sl6": 9.4,
+ "sl7": 9.67
+ },
+ "sand": {
+ "sl1": 49.0,
+ "sl2": 49.0,
+ "sl3": 49.0,
+ "sl4": 49.2,
+ "sl5": 49.71,
+ "sl6": 50.8,
+ "sl7": 50.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 148190,
+ "distance": 5397.735,
+ "mapunitID": 546,
+ "minCompDistance": 5397.73450719,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_es": "Los Fluvisoles Dístricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los Fluvisoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.",
+ "Description_fr": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_ks": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.",
+ "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ",
+ "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (acolchados, cultivos de cobertura), que mejoren la infiltración del agua o que proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).
Una baja saturación de bases (presencia de Ca, Mg, K) indica que el pH del suelo puede ser bajo, y puede estar justificado el encalado.",
+ "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ",
+ "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 13.0,
+ "sl2": 13.0,
+ "sl3": 13.0,
+ "sl4": 11.2,
+ "sl5": 10.57,
+ "sl6": 10.2,
+ "sl7": 10.5
+ },
+ "clay": {
+ "sl1": 27.0,
+ "sl2": 27.0,
+ "sl3": 27.0,
+ "sl4": 30.0,
+ "sl5": 31.57,
+ "sl6": 33.0,
+ "sl7": 33.67
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 0.8,
+ "sl5": 0.57,
+ "sl6": 0.4,
+ "sl7": 0.33
+ },
+ "id": {
+ "component": "Dystric gleysols",
+ "name": "Dystric gleysols",
+ "rank_loc": "6",
+ "score_loc": 0.017
+ },
+ "ph": {
+ "sl1": 4.8,
+ "sl2": 4.8,
+ "sl3": 4.8,
+ "sl4": 4.94,
+ "sl5": 5.0,
+ "sl6": 5.06,
+ "sl7": 5.08
+ },
+ "rock_fragments": {
+ "sl1": 7.0,
+ "sl2": 7.0,
+ "sl3": 7.0,
+ "sl4": 4.8,
+ "sl5": 4.86,
+ "sl6": 5.4,
+ "sl7": 5.33
+ },
+ "sand": {
+ "sl1": 43.0,
+ "sl2": 43.0,
+ "sl3": 43.0,
+ "sl4": 41.2,
+ "sl5": 40.71,
+ "sl6": 40.6,
+ "sl7": 40.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 148189,
+ "distance": 5397.735,
+ "mapunitID": 546,
+ "minCompDistance": 5397.73450719,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_es": "Los Gleysoles Dístricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
Es necesario un drenaje profundo para su cultivo.
Los Gleysoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.",
+ "Description_fr": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_ks": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.",
+ "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. ",
+ "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.
Estos suelos tienen poco calcio, magnesio u otras bases disponibles en el suelo, y pueden requerir fertilización suplementaria.
Si es necesario, el encalado aportará el calcio, y posiblemente el magnesio (cal dolomítica)..",
+ "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. ",
+ "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 8.0,
+ "sl2": 8.0,
+ "sl3": 8.0,
+ "sl4": 7.4,
+ "sl5": 7.43,
+ "sl6": 7.6,
+ "sl7": 7.67
+ },
+ "clay": {
+ "sl1": 23.0,
+ "sl2": 23.0,
+ "sl3": 23.0,
+ "sl4": 28.2,
+ "sl5": 30.57,
+ "sl6": 32.8,
+ "sl7": 34.0
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Gleyic acrisols",
+ "name": "Gleyic acrisols",
+ "rank_loc": "7",
+ "score_loc": 0.017
+ },
+ "ph": {
+ "sl1": 4.8,
+ "sl2": 4.8,
+ "sl3": 4.8,
+ "sl4": 4.88,
+ "sl5": 4.93,
+ "sl6": 4.98,
+ "sl7": 4.98
+ },
+ "rock_fragments": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 3.6,
+ "sl5": 4.86,
+ "sl6": 5.4,
+ "sl7": 5.83
+ },
+ "sand": {
+ "sl1": 45.0,
+ "sl2": 45.0,
+ "sl3": 45.0,
+ "sl4": 42.0,
+ "sl5": 40.57,
+ "sl6": 39.2,
+ "sl7": 37.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 144045,
+ "distance": 29708.866,
+ "mapunitID": 463,
+ "minCompDistance": 29708.86642894,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Gleyic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Gleyic Acrisols have a seasonal high-water table resulting in saturation during some time of the year.",
+ "Description_es": "Los Acrisoles Gleyicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Los acrisoles gleyicos tienen un nivel freático alto estacional que provoca la saturación durante algunas épocas del año. ",
+ "Description_fr": "Gleyic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Gleyic Acrisols have a seasonal high-water table resulting in saturation during some time of the year.",
+ "Description_ks": "Gleyic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Gleyic Acrisols have a seasonal high-water table resulting in saturation during some time of the year.",
+ "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Periods of saturation limit root growth and increase nitrogen loss.
To prevent N loss from leaching anddenitrification consider use of slow-release N fertilizers (sulfur-coated urea (SCU), for example), if those slow-release products are available, or use manures or other organic wastes for their slow-release properties.
Drainage of these soils may be needed, but this can be problematic, as the wetness is due to the high water table. ",
+ "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.
Los períodos de saturación limitan el crecimiento de las raíces y aumentan la pérdida de nitrógeno.
Para evitar la pérdida de N por lixiviación y/o desnitrificación, considere el uso de fertilizantes de liberación lenta de N (urea recubierta de azufre (SCU), por ejemplo), si esos productos de liberación lenta están disponibles, o utilice estiércol u otros residuos orgánicos por sus propiedades de liberación lenta.
Puede ser necesario el drenaje de estos suelos, pero esto puede ser problemático, ya que la humedad se debe al alto nivel freático. ",
+ "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Periods of saturation limit root growth and increase nitrogen loss.
To prevent N loss from leaching anddenitrification consider use of slow-release N fertilizers (sulfur-coated urea (SCU), for example), if those slow-release products are available, or use manures or other organic wastes for their slow-release properties.
Drainage of these soils may be needed, but this can be problematic, as the wetness is due to the high water table. ",
+ "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Periods of saturation limit root growth and increase nitrogen loss.
To prevent N loss from leaching anddenitrification consider use of slow-release N fertilizers (sulfur-coated urea (SCU), for example), if those slow-release products are available, or use manures or other organic wastes for their slow-release properties.
Drainage of these soils may be needed, but this can be problematic, as the wetness is due to the high water table. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "global",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Haplic ferralsols",
+ "componentData": "No Data",
+ "componentID": 156034,
+ "name": "Haplic ferralsols",
+ "rank_data": "3",
+ "rank_data_loc": "1",
+ "rank_loc": 2,
+ "score_data": 0.571,
+ "score_data_loc": 1.0,
+ "score_loc": 0.3
+ },
+ {
+ "component": "Ferralic arenosols",
+ "componentData": "Data Complete",
+ "componentID": 156032,
+ "name": "Ferralic arenosols",
+ "rank_data": "6",
+ "rank_data_loc": "2",
+ "rank_loc": 1,
+ "score_data": 0.35,
+ "score_data_loc": 0.9,
+ "score_loc": 0.433
+ },
+ {
+ "component": "Ferralic cambisols",
+ "componentData": "Data Complete",
+ "componentID": 144042,
+ "name": "Ferralic cambisols",
+ "rank_data": "1",
+ "rank_data_loc": "3",
+ "rank_loc": 4,
+ "score_data": 0.621,
+ "score_data_loc": 0.809,
+ "score_loc": 0.083
+ },
+ {
+ "component": "Dystric fluvisols",
+ "componentData": "Data Complete",
+ "componentID": 148190,
+ "name": "Dystric fluvisols",
+ "rank_data": "2",
+ "rank_data_loc": "4",
+ "rank_loc": 5,
+ "score_data": 0.571,
+ "score_data_loc": 0.675,
+ "score_loc": 0.017
+ },
+ {
+ "component": "Dystric gleysols",
+ "componentData": "Missing Data",
+ "componentID": 148189,
+ "name": "Dystric gleysols",
+ "rank_data": "4",
+ "rank_data_loc": "5",
+ "rank_loc": 6,
+ "score_data": 0.519,
+ "score_data_loc": 0.615,
+ "score_loc": 0.017
+ },
+ {
+ "component": "Gleyic acrisols",
+ "componentData": "Missing Data",
+ "componentID": 144045,
+ "name": "Gleyic acrisols",
+ "rank_data": "5",
+ "rank_data_loc": "6",
+ "rank_loc": 7,
+ "score_data": 0.517,
+ "score_data_loc": 0.613,
+ "score_loc": 0.017
+ },
+ {
+ "component": "Xanthic ferralsols",
+ "componentData": "Missing Data",
+ "componentID": 156033,
+ "name": "Xanthic ferralsols",
+ "rank_data": "7",
+ "rank_data_loc": "7",
+ "rank_loc": 3,
+ "score_data": 0.0,
+ "score_data_loc": 0.153,
+ "score_loc": 0.133
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.07856,15.107436].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.07856,15.107436].json
new file mode 100644
index 0000000..b4be33e
--- /dev/null
+++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.07856,15.107436].json
@@ -0,0 +1,1515 @@
+{
+ "list": {
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 7.0,
+ "sl2": 7.0,
+ "sl3": 7.0,
+ "sl4": 5.6,
+ "sl5": 5.14,
+ "sl6": 4.6,
+ "sl7": 4.33
+ },
+ "clay": {
+ "sl1": 35.0,
+ "sl2": 35.0,
+ "sl3": 35.0,
+ "sl4": 39.2,
+ "sl5": 40.71,
+ "sl6": 42.0,
+ "sl7": 42.5
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Xanthic ferralsols",
+ "name": "Xanthic ferralsols",
+ "rank_loc": "1",
+ "score_loc": 0.269
+ },
+ "ph": {
+ "sl1": 4.5,
+ "sl2": 4.5,
+ "sl3": 4.5,
+ "sl4": 4.58,
+ "sl5": 4.63,
+ "sl6": 4.68,
+ "sl7": 4.72
+ },
+ "rock_fragments": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 3.2,
+ "sl5": 3.57,
+ "sl6": 4.0,
+ "sl7": 5.0
+ },
+ "sand": {
+ "sl1": 53.0,
+ "sl2": 53.0,
+ "sl3": 53.0,
+ "sl4": 50.0,
+ "sl5": 48.71,
+ "sl6": 47.6,
+ "sl7": 47.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 105422,
+ "distance": 0.0,
+ "mapunitID": 12214,
+ "minCompDistance": 0.0,
+ "share": 40,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ",
+ "Description_es": "Los Ferralsoles Xánticos son suelos bien desarrollados en climas húmedos y cálidos que están dominados por minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos xánticos tienen subsuelos de color amarillo que indican una retención de humedad ligeramente superior. ",
+ "Description_fr": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ",
+ "Description_ks": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ",
+ "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos. *Prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.",
+ "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy clay",
+ "sl2": "Sandy clay",
+ "sl3": "Sandy clay",
+ "sl4": "Sandy clay",
+ "sl5": "Sandy clay",
+ "sl6": "Sandy clay",
+ "sl7": "Sandy clay"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 7.0,
+ "sl2": 7.0,
+ "sl3": 7.0,
+ "sl4": 6.4,
+ "sl5": 6.14,
+ "sl6": 5.8,
+ "sl7": 5.33
+ },
+ "clay": {
+ "sl1": 22.0,
+ "sl2": 22.0,
+ "sl3": 22.0,
+ "sl4": 25.8,
+ "sl5": 27.14,
+ "sl6": 28.6,
+ "sl7": 31.17
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Haplic ferralsols",
+ "name": "Haplic ferralsols",
+ "rank_loc": "2",
+ "score_loc": 0.181
+ },
+ "ph": {
+ "sl1": 4.5,
+ "sl2": 4.5,
+ "sl3": 4.5,
+ "sl4": 4.58,
+ "sl5": 4.63,
+ "sl6": 4.68,
+ "sl7": 4.72
+ },
+ "rock_fragments": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 3.2,
+ "sl5": 3.57,
+ "sl6": 4.0,
+ "sl7": 5.0
+ },
+ "sand": {
+ "sl1": 66.0,
+ "sl2": 66.0,
+ "sl3": 66.0,
+ "sl4": 62.8,
+ "sl5": 61.71,
+ "sl6": 61.0,
+ "sl7": 58.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 105423,
+ "distance": 0.0,
+ "mapunitID": 12214,
+ "minCompDistance": 0.0,
+ "share": 25,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.",
+ "Description_es": "Los Ferralsoles Háplicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada de retener nutrientes. ",
+ "Description_fr": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.",
+ "Description_ks": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.",
+ "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_es": "Estos suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.",
+ "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy clay loam",
+ "sl2": "Sandy clay loam",
+ "sl3": "Sandy clay loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 10.0,
+ "sl2": 10.0,
+ "sl3": 10.0,
+ "sl4": 8.0,
+ "sl5": 7.43,
+ "sl6": 7.0,
+ "sl7": 6.83
+ },
+ "clay": {
+ "sl1": 43.0,
+ "sl2": 43.0,
+ "sl3": 43.0,
+ "sl4": 46.4,
+ "sl5": 47.43,
+ "sl6": 48.2,
+ "sl7": 48.33
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Eutric leptosols",
+ "name": "Eutric leptosols",
+ "rank_loc": "3",
+ "score_loc": 0.144
+ },
+ "ph": {
+ "sl1": 4.9,
+ "sl2": 4.9,
+ "sl3": 4.9,
+ "sl4": 4.92,
+ "sl5": 4.96,
+ "sl6": 5.0,
+ "sl7": 5.02
+ },
+ "rock_fragments": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 4.6,
+ "sl5": 4.71,
+ "sl6": 5.0,
+ "sl7": 5.0
+ },
+ "sand": {
+ "sl1": 40.0,
+ "sl2": 40.0,
+ "sl3": 40.0,
+ "sl4": 37.4,
+ "sl5": 36.57,
+ "sl6": 35.8,
+ "sl7": 35.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 105424,
+ "distance": 0.0,
+ "mapunitID": 12214,
+ "minCompDistance": 0.0,
+ "share": 20,
+ "soilDepth": 40
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ",
+ "Description_es": "Los Leptosoles Eútricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles eútricos tienen una alta saturación de la base sobre la capa limitante de las raíces poco profundas. ",
+ "Description_fr": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ",
+ "Description_ks": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ",
+ "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ",
+ "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Se debe considerar el uso exclusivo para el pastoreo o la agroforestería.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Estos suelos pueden ser productivos para la agricultura, pero el enfoque debe ser el uso para el pastoreo.
Cualquier uso para el cultivo debe limitarse y combinarse con prácticas de conservación del suelo.",
+ "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ",
+ "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. "
+ }
+ },
+ "texture": {
+ "sl1": "Unknown",
+ "sl2": "Unknown",
+ "sl3": "Unknown",
+ "sl4": "Unknown",
+ "sl5": "Unknown",
+ "sl6": "Unknown",
+ "sl7": "Unknown"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 8.0,
+ "sl2": 8.0,
+ "sl3": 8.0,
+ "sl4": 6.6,
+ "sl5": 6.14,
+ "sl6": 5.8,
+ "sl7": 5.67
+ },
+ "clay": {
+ "sl1": 36.0,
+ "sl2": 36.0,
+ "sl3": 36.0,
+ "sl4": 38.8,
+ "sl5": 39.86,
+ "sl6": 40.8,
+ "sl7": 41.5
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Lithic leptosols",
+ "name": "Lithic leptosols",
+ "rank_loc": "4",
+ "score_loc": 0.138
+ },
+ "ph": {
+ "sl1": 5.1,
+ "sl2": 5.1,
+ "sl3": 5.1,
+ "sl4": 5.16,
+ "sl5": 5.19,
+ "sl6": 5.24,
+ "sl7": 5.28
+ },
+ "rock_fragments": {
+ "sl1": 3.0,
+ "sl2": 3.0,
+ "sl3": 3.0,
+ "sl4": 3.4,
+ "sl5": 3.29,
+ "sl6": 3.2,
+ "sl7": 5.17
+ },
+ "sand": {
+ "sl1": 41.0,
+ "sl2": 41.0,
+ "sl3": 41.0,
+ "sl4": 38.8,
+ "sl5": 37.86,
+ "sl6": 36.8,
+ "sl7": 36.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 105416,
+ "distance": 13359.43,
+ "mapunitID": 12212,
+ "minCompDistance": 13359.43009493,
+ "share": 100,
+ "soilDepth": 20
+ },
+ "siteDescription": {
+ "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ",
+ "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ",
+ "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.",
+ "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ",
+ "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. "
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Unknown",
+ "sl7": "Unknown"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 40
+ },
+ "cec": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 13.0
+ },
+ "clay": {
+ "sl1": 26.0,
+ "sl2": 26.0,
+ "sl3": 26.0,
+ "sl4": 27.0
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0
+ },
+ "id": {
+ "component": "Rhodic ferralsols",
+ "name": "Rhodic ferralsols",
+ "rank_loc": "5",
+ "score_loc": 0.1
+ },
+ "ph": {
+ "sl1": 6.5,
+ "sl2": 6.5,
+ "sl3": 6.5,
+ "sl4": 6.55
+ },
+ "rock_fragments": {
+ "sl1": 22.0,
+ "sl2": 22.0,
+ "sl3": 22.0,
+ "sl4": 30.5
+ },
+ "sand": {
+ "sl1": 45.0,
+ "sl2": 45.0,
+ "sl3": 45.0,
+ "sl4": 44.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 105425,
+ "distance": 0.0,
+ "mapunitID": 12214,
+ "minCompDistance": 0.0,
+ "share": 15,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ",
+ "Description_es": "Los Ferralsoles Ródicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas, pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos ródicos tienen subsuelos de color rojo oscuro con una buena estructura de suelo. ",
+ "Description_fr": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ",
+ "Description_ks": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ",
+ "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.",
+ "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used."
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 40
+ },
+ "cec": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 21.5
+ },
+ "clay": {
+ "sl1": 27.0,
+ "sl2": 27.0,
+ "sl3": 27.0,
+ "sl4": 34.5
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0
+ },
+ "id": {
+ "component": "Ferralic cambisols",
+ "name": "Ferralic cambisols",
+ "rank_loc": "6",
+ "score_loc": 0.069
+ },
+ "ph": {
+ "sl1": 6.7,
+ "sl2": 6.7,
+ "sl3": 6.7,
+ "sl4": 6.55
+ },
+ "rock_fragments": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 40.5
+ },
+ "sand": {
+ "sl1": 41.0,
+ "sl2": 41.0,
+ "sl3": 41.0,
+ "sl4": 36.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 105395,
+ "distance": 4468.846,
+ "mapunitID": 12207,
+ "minCompDistance": 4468.84592815,
+ "share": 40,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.",
+ "Description_es": "Los Cambisoles Ferrálicos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos tienen una escasa capacidad para retener nutrientes debido a su baja capacidad de intercambio catiónico. Como retienen menos nutrientes, suelen ser menos productivos. ",
+ "Description_fr": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.",
+ "Description_ks": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.",
+ "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ",
+ "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
El tipo de arcilla de este suelo está extremadamente erosionado, y como tal tendrá una baja capacidad de suministro de nutrientes.
La fertilización será necesaria para mejorar la productividad.",
+ "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ",
+ "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20
+ },
+ "cec": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0
+ },
+ "clay": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0
+ },
+ "id": {
+ "component": "Chromic luvisols",
+ "name": "Chromic luvisols",
+ "rank_loc": "7",
+ "score_loc": 0.05
+ },
+ "ph": {
+ "sl1": 6.7,
+ "sl2": 6.7,
+ "sl3": 6.7
+ },
+ "rock_fragments": {
+ "sl1": 22.0,
+ "sl2": 22.0,
+ "sl3": 22.0
+ },
+ "sand": {
+ "sl1": 51.0,
+ "sl2": 51.0,
+ "sl3": 51.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 105244,
+ "distance": 28892.433,
+ "mapunitID": 12167,
+ "minCompDistance": 28892.43320808,
+ "share": 40,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.",
+ "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.",
+ "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops."
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 10.0,
+ "sl2": 10.0,
+ "sl3": 10.0,
+ "sl4": 8.4,
+ "sl5": 7.71,
+ "sl6": 7.2,
+ "sl7": 7.0
+ },
+ "clay": {
+ "sl1": 48.0,
+ "sl2": 48.0,
+ "sl3": 48.0,
+ "sl4": 52.6,
+ "sl5": 53.86,
+ "sl6": 55.0,
+ "sl7": 55.67
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Haplic acrisols",
+ "name": "Haplic acrisols",
+ "rank_loc": "8",
+ "score_loc": 0.025
+ },
+ "ph": {
+ "sl1": 5.6,
+ "sl2": 5.6,
+ "sl3": 5.6,
+ "sl4": 5.62,
+ "sl5": 5.63,
+ "sl6": 5.64,
+ "sl7": 5.65
+ },
+ "rock_fragments": {
+ "sl1": 26.0,
+ "sl2": 26.0,
+ "sl3": 26.0,
+ "sl4": 17.0,
+ "sl5": 12.71,
+ "sl6": 10.0,
+ "sl7": 8.83
+ },
+ "sand": {
+ "sl1": 35.0,
+ "sl2": 35.0,
+ "sl3": 35.0,
+ "sl4": 32.2,
+ "sl5": 31.29,
+ "sl6": 30.4,
+ "sl7": 29.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 105396,
+ "distance": 4468.846,
+ "mapunitID": 12207,
+ "minCompDistance": 4468.84592815,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.",
+ "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ",
+ "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.",
+ "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.",
+ "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ",
+ "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ",
+ "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ",
+ "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. "
+ }
+ },
+ "texture": {
+ "sl1": "Unknown",
+ "sl2": "Unknown",
+ "sl3": "Unknown",
+ "sl4": "Unknown",
+ "sl5": "Unknown",
+ "sl6": "Unknown",
+ "sl7": "Unknown"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 9.0,
+ "sl2": 9.0,
+ "sl3": 9.0,
+ "sl4": 7.6,
+ "sl5": 7.14,
+ "sl6": 6.6,
+ "sl7": 6.33
+ },
+ "clay": {
+ "sl1": 46.0,
+ "sl2": 46.0,
+ "sl3": 46.0,
+ "sl4": 49.8,
+ "sl5": 50.71,
+ "sl6": 51.4,
+ "sl7": 51.67
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Haplic lixisols",
+ "name": "Haplic lixisols",
+ "rank_loc": "9",
+ "score_loc": 0.025
+ },
+ "ph": {
+ "sl1": 5.5,
+ "sl2": 5.5,
+ "sl3": 5.5,
+ "sl4": 5.44,
+ "sl5": 5.44,
+ "sl6": 5.46,
+ "sl7": 5.48
+ },
+ "rock_fragments": {
+ "sl1": 15.0,
+ "sl2": 15.0,
+ "sl3": 15.0,
+ "sl4": 7.0,
+ "sl5": 5.29,
+ "sl6": 4.2,
+ "sl7": 4.67
+ },
+ "sand": {
+ "sl1": 37.0,
+ "sl2": 37.0,
+ "sl3": 37.0,
+ "sl4": 34.4,
+ "sl5": 33.57,
+ "sl6": 32.8,
+ "sl7": 32.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 105245,
+ "distance": 28892.433,
+ "mapunitID": 12167,
+ "minCompDistance": 28892.43320808,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ",
+ "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ",
+ "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ",
+ "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ",
+ "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ",
+ "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.",
+ "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ",
+ "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. "
+ }
+ },
+ "texture": {
+ "sl1": "Unknown",
+ "sl2": "Unknown",
+ "sl3": "Unknown",
+ "sl4": "Unknown",
+ "sl5": "Unknown",
+ "sl6": "Unknown",
+ "sl7": "Unknown"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 8.0,
+ "sl2": 8.0,
+ "sl3": 8.0,
+ "sl4": 6.6,
+ "sl5": 6.14,
+ "sl6": 5.8,
+ "sl7": 5.67
+ },
+ "clay": {
+ "sl1": 30.0,
+ "sl2": 30.0,
+ "sl3": 30.0,
+ "sl4": 31.4,
+ "sl5": 32.0,
+ "sl6": 32.6,
+ "sl7": 33.0
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 0.4,
+ "sl5": 0.29,
+ "sl6": 0.2,
+ "sl7": 0.17
+ },
+ "id": {
+ "component": "Xanthic ferralsols",
+ "name": "Xanthic ferralsols2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.269
+ },
+ "ph": {
+ "sl1": 5.2,
+ "sl2": 5.2,
+ "sl3": 5.2,
+ "sl4": 5.2,
+ "sl5": 5.2,
+ "sl6": 5.2,
+ "sl7": 5.18
+ },
+ "rock_fragments": {
+ "sl1": 12.0,
+ "sl2": 12.0,
+ "sl3": 12.0,
+ "sl4": 9.4,
+ "sl5": 9.86,
+ "sl6": 10.6,
+ "sl7": 10.5
+ },
+ "sand": {
+ "sl1": 45.0,
+ "sl2": 45.0,
+ "sl3": 45.0,
+ "sl4": 43.0,
+ "sl5": 42.29,
+ "sl6": 41.4,
+ "sl7": 41.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 105399,
+ "distance": 4468.846,
+ "mapunitID": 12207,
+ "minCompDistance": 0.0,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ",
+ "Description_es": "Los Ferralsoles Xánticos son suelos bien desarrollados en climas húmedos y cálidos que están dominados por minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos xánticos tienen subsuelos de color amarillo que indican una retención de humedad ligeramente superior. ",
+ "Description_fr": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ",
+ "Description_ks": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ",
+ "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos. *Prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.",
+ "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used."
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 9.0,
+ "sl2": 9.0,
+ "sl3": 9.0,
+ "sl4": 7.6,
+ "sl5": 7.14,
+ "sl6": 6.8,
+ "sl7": 6.67
+ },
+ "clay": {
+ "sl1": 31.0,
+ "sl2": 31.0,
+ "sl3": 31.0,
+ "sl4": 33.4,
+ "sl5": 33.86,
+ "sl6": 34.0,
+ "sl7": 33.83
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 0.86,
+ "sl6": 0.6,
+ "sl7": 0.5
+ },
+ "id": {
+ "component": "Haplic ferralsols",
+ "name": "Haplic ferralsols2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.181
+ },
+ "ph": {
+ "sl1": 5.1,
+ "sl2": 5.1,
+ "sl3": 5.1,
+ "sl4": 5.12,
+ "sl5": 5.14,
+ "sl6": 5.14,
+ "sl7": 5.13
+ },
+ "rock_fragments": {
+ "sl1": 9.0,
+ "sl2": 9.0,
+ "sl3": 9.0,
+ "sl4": 10.2,
+ "sl5": 11.43,
+ "sl6": 12.6,
+ "sl7": 12.83
+ },
+ "sand": {
+ "sl1": 45.0,
+ "sl2": 45.0,
+ "sl3": 45.0,
+ "sl4": 43.0,
+ "sl5": 42.43,
+ "sl6": 42.0,
+ "sl7": 42.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 105398,
+ "distance": 4468.846,
+ "mapunitID": 12207,
+ "minCompDistance": 0.0,
+ "share": 15,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.",
+ "Description_es": "Los Ferralsoles Háplicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada de retener nutrientes. ",
+ "Description_fr": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.",
+ "Description_ks": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.",
+ "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_es": "Estos suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.",
+ "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used."
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 14.6,
+ "sl5": 14.71,
+ "sl6": 15.0,
+ "sl7": 15.17
+ },
+ "clay": {
+ "sl1": 24.0,
+ "sl2": 24.0,
+ "sl3": 24.0,
+ "sl4": 28.6,
+ "sl5": 29.86,
+ "sl6": 30.6,
+ "sl7": 30.5
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.0,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Eutric leptosols",
+ "name": "Eutric leptosols2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.144
+ },
+ "ph": {
+ "sl1": 6.4,
+ "sl2": 6.4,
+ "sl3": 6.4,
+ "sl4": 6.42,
+ "sl5": 6.44,
+ "sl6": 6.44,
+ "sl7": 6.43
+ },
+ "rock_fragments": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 6.8,
+ "sl5": 9.29,
+ "sl6": 13.4,
+ "sl7": 12.5
+ },
+ "sand": {
+ "sl1": 53.0,
+ "sl2": 53.0,
+ "sl3": 53.0,
+ "sl4": 49.0,
+ "sl5": 47.71,
+ "sl6": 46.6,
+ "sl7": 46.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 105397,
+ "distance": 4468.846,
+ "mapunitID": 12207,
+ "minCompDistance": 0.0,
+ "share": 15,
+ "soilDepth": 40
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ",
+ "Description_es": "Los Leptosoles Eútricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles eútricos tienen una alta saturación de la base sobre la capa limitante de las raíces poco profundas. ",
+ "Description_fr": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ",
+ "Description_ks": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ",
+ "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ",
+ "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Se debe considerar el uso exclusivo para el pastoreo o la agroforestería.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Estos suelos pueden ser productivos para la agricultura, pero el enfoque debe ser el uso para el pastoreo.
Cualquier uso para el cultivo debe limitarse y combinarse con prácticas de conservación del suelo.",
+ "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ",
+ "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy clay loam",
+ "sl2": "Sandy clay loam",
+ "sl3": "Sandy clay loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 6.0,
+ "sl5": 6.0,
+ "sl6": 6.0,
+ "sl7": 6.0
+ },
+ "clay": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 25.6,
+ "sl5": 28.14,
+ "sl6": 30.0,
+ "sl7": 30.5
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Rhodic ferralsols",
+ "name": "Rhodic ferralsols2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.1
+ },
+ "ph": {
+ "sl1": 5.2,
+ "sl2": 5.2,
+ "sl3": 5.2,
+ "sl4": 5.2,
+ "sl5": 5.19,
+ "sl6": 5.16,
+ "sl7": 5.13
+ },
+ "rock_fragments": {
+ "sl1": 8.0,
+ "sl2": 8.0,
+ "sl3": 8.0,
+ "sl4": 6.8,
+ "sl5": 6.71,
+ "sl6": 6.2,
+ "sl7": 5.83
+ },
+ "sand": {
+ "sl1": 53.0,
+ "sl2": 53.0,
+ "sl3": 53.0,
+ "sl4": 47.8,
+ "sl5": 45.86,
+ "sl6": 44.8,
+ "sl7": 44.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 105419,
+ "distance": 21840.312,
+ "mapunitID": 12213,
+ "minCompDistance": 0.0,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ",
+ "Description_es": "Los Ferralsoles Ródicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas, pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos ródicos tienen subsuelos de color rojo oscuro con una buena estructura de suelo. ",
+ "Description_fr": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ",
+ "Description_ks": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ",
+ "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.",
+ "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 8.0,
+ "sl2": 8.0,
+ "sl3": 8.0,
+ "sl4": 6.8,
+ "sl5": 6.71,
+ "sl6": 6.8,
+ "sl7": 6.83
+ },
+ "clay": {
+ "sl1": 21.0,
+ "sl2": 21.0,
+ "sl3": 21.0,
+ "sl4": 27.2,
+ "sl5": 30.29,
+ "sl6": 33.2,
+ "sl7": 34.33
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Ferralic cambisols",
+ "name": "Ferralic cambisols2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.069
+ },
+ "ph": {
+ "sl1": 6.2,
+ "sl2": 6.2,
+ "sl3": 6.2,
+ "sl4": 6.12,
+ "sl5": 6.07,
+ "sl6": 6.02,
+ "sl7": 6.02
+ },
+ "rock_fragments": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 9.8,
+ "sl5": 10.43,
+ "sl6": 10.6,
+ "sl7": 10.5
+ },
+ "sand": {
+ "sl1": 65.0,
+ "sl2": 65.0,
+ "sl3": 65.0,
+ "sl4": 60.2,
+ "sl5": 57.57,
+ "sl6": 54.8,
+ "sl7": 53.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 105247,
+ "distance": 28892.433,
+ "mapunitID": 12167,
+ "minCompDistance": 4468.84592815,
+ "share": 15,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.",
+ "Description_es": "Los Cambisoles Ferrálicos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos tienen una escasa capacidad para retener nutrientes debido a su baja capacidad de intercambio catiónico. Como retienen menos nutrientes, suelen ser menos productivos. ",
+ "Description_fr": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.",
+ "Description_ks": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.",
+ "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ",
+ "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
El tipo de arcilla de este suelo está extremadamente erosionado, y como tal tendrá una baja capacidad de suministro de nutrientes.
La fertilización será necesaria para mejorar la productividad.",
+ "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ",
+ "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy clay loam",
+ "sl2": "Sandy clay loam",
+ "sl3": "Sandy clay loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "global",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Xanthic ferralsols",
+ "componentData": "Missing Data",
+ "componentID": 105399,
+ "name": "Xanthic ferralsols2",
+ "rank_data": "3",
+ "rank_data_loc": "1",
+ "rank_loc": "Not Displayed",
+ "score_data": 1.0,
+ "score_data_loc": 1.0,
+ "score_loc": 0.269
+ },
+ {
+ "component": "Haplic ferralsols",
+ "componentData": "No Data",
+ "componentID": 105423,
+ "name": "Haplic ferralsols",
+ "rank_data": "2",
+ "rank_data_loc": "2",
+ "rank_loc": "2",
+ "score_data": 1.0,
+ "score_data_loc": 0.931,
+ "score_loc": 0.181
+ },
+ {
+ "component": "Chromic luvisols",
+ "componentData": "Data Complete",
+ "componentID": 105244,
+ "name": "Chromic luvisols",
+ "rank_data": "4",
+ "rank_data_loc": "3",
+ "rank_loc": "7",
+ "score_data": 0.738,
+ "score_data_loc": 0.621,
+ "score_loc": 0.05
+ },
+ {
+ "component": "Rhodic ferralsols",
+ "componentData": "No Data",
+ "componentID": 105425,
+ "name": "Rhodic ferralsols",
+ "rank_data": "7",
+ "rank_data_loc": "4",
+ "rank_loc": "5",
+ "score_data": 0.681,
+ "score_data_loc": 0.616,
+ "score_loc": 0.1
+ },
+ {
+ "component": "Haplic acrisols",
+ "componentData": "Data Complete",
+ "componentID": 105396,
+ "name": "Haplic acrisols",
+ "rank_data": "5",
+ "rank_data_loc": "5",
+ "rank_loc": "8",
+ "score_data": 0.681,
+ "score_data_loc": 0.556,
+ "score_loc": 0.025
+ },
+ {
+ "component": "Ferralic cambisols",
+ "componentData": "Data Complete",
+ "componentID": 105395,
+ "name": "Ferralic cambisols",
+ "rank_data": "8",
+ "rank_data_loc": "6",
+ "rank_loc": "6",
+ "score_data": 0.5,
+ "score_data_loc": 0.448,
+ "score_loc": 0.069
+ },
+ {
+ "component": "Haplic lixisols",
+ "componentData": "Missing Data",
+ "componentID": 105245,
+ "name": "Haplic lixisols",
+ "rank_data": "9",
+ "rank_data_loc": "7",
+ "rank_loc": "9",
+ "score_data": 0.433,
+ "score_data_loc": 0.361,
+ "score_loc": 0.025
+ },
+ {
+ "component": "Eutric leptosols",
+ "componentData": "Missing Data",
+ "componentID": 105424,
+ "name": "Eutric leptosols",
+ "rank_data": "1",
+ "rank_data_loc": "8",
+ "rank_loc": "3",
+ "score_data": 1.0,
+ "score_data_loc": 0.002,
+ "score_loc": 0.144
+ },
+ {
+ "component": "Lithic leptosols",
+ "componentData": "Missing Data",
+ "componentID": 105416,
+ "name": "Lithic leptosols",
+ "rank_data": "6",
+ "rank_data_loc": "9",
+ "rank_loc": "4",
+ "score_data": 0.681,
+ "score_data_loc": 0.002,
+ "score_loc": 0.138
+ },
+ {
+ "component": "Haplic ferralsols",
+ "componentData": "Missing Data",
+ "componentID": 105398,
+ "name": "Haplic ferralsols2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.738,
+ "score_data_loc": 0.724,
+ "score_loc": 0.181
+ },
+ {
+ "component": "Xanthic ferralsols",
+ "componentData": "Missing Data",
+ "componentID": 105422,
+ "name": "Xanthic ferralsols",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "1",
+ "score_data": 0.433,
+ "score_data_loc": 0.553,
+ "score_loc": 0.269
+ },
+ {
+ "component": "Ferralic cambisols",
+ "componentData": "Data Complete",
+ "componentID": 105247,
+ "name": "Ferralic cambisols2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.433,
+ "score_data_loc": 0.396,
+ "score_loc": 0.069
+ },
+ {
+ "component": "Rhodic ferralsols",
+ "componentData": "No Data",
+ "componentID": 105419,
+ "name": "Rhodic ferralsols2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.308,
+ "score_data_loc": 0.322,
+ "score_loc": 0.1
+ },
+ {
+ "component": "Eutric leptosols",
+ "componentData": "Missing Data",
+ "componentID": 105397,
+ "name": "Eutric leptosols2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.738,
+ "score_data_loc": 0.002,
+ "score_loc": 0.144
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.950086,17.573093].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.950086,17.573093].json
new file mode 100644
index 0000000..899163e
--- /dev/null
+++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.950086,17.573093].json
@@ -0,0 +1,1235 @@
+{
+ "list": {
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 10.2,
+ "sl5": 10.43,
+ "sl6": 10.4,
+ "sl7": 10.33
+ },
+ "clay": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 19.4,
+ "sl5": 21.43,
+ "sl6": 22.2,
+ "sl7": 22.0
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Gleyic alisols",
+ "name": "Gleyic alisols",
+ "rank_loc": "1",
+ "score_loc": 0.4
+ },
+ "ph": {
+ "sl1": 5.0,
+ "sl2": 5.0,
+ "sl3": 5.0,
+ "sl4": 4.92,
+ "sl5": 4.89,
+ "sl6": 4.86,
+ "sl7": 4.83
+ },
+ "rock_fragments": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 4.8,
+ "sl5": 4.29,
+ "sl6": 3.6,
+ "sl7": 3.83
+ },
+ "sand": {
+ "sl1": 30.0,
+ "sl2": 30.0,
+ "sl3": 30.0,
+ "sl4": 28.0,
+ "sl5": 28.43,
+ "sl6": 31.4,
+ "sl7": 33.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 104790,
+ "distance": 0.0,
+ "mapunitID": 12044,
+ "minCompDistance": 0.0,
+ "share": 70,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Gleyic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover.
These soils experience prolonged saturation from shallow groundwater. ",
+ "Description_es": "Los Alisoles Gleyicos son suelos ácidos que suelen encontrarse en zonas de colinas, por lo que son propensos a la erosión.
También tienen altos niveles de aluminio soluble, que es tóxico para las plantas.
Son suelos poco profundos y, por lo general, poco productivos para el cultivo, por lo que su uso debe limitarse al pastoreo de bajo volumen o a otros usos con cobertura vegetal continua.
Estos suelos experimentan una saturación prolongada de las aguas subterráneas poco profundas. ",
+ "Description_fr": "Gleyic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover.
These soils experience prolonged saturation from shallow groundwater. ",
+ "Description_ks": "Gleyic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover.
These soils experience prolonged saturation from shallow groundwater. ",
+ "Management_en": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotation andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity.
Drainage of these soils may be needed. However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers. ",
+ "Management_es": "La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el Al de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. *Aunque no suele recomendarse, si el suelo se utiliza para cultivos, la fertilización debe combinarse con la rotación de cultivos y/o los cultivos de cobertura, u otros medios de adición de materia orgánica para el desarrollo de una mayor fertilidad y capacidad de retención de agua.
Puede ser necesario el drenaje de estos suelos. Sin embargo, dado que se trata de una saturación a través de aguas subterráneas, esto puede no ser posible, por lo que se debe considerar la posibilidad de realizar cultivos con raíces superficiales.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta.",
+ "Management_fr": "
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotation andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity.
Drainage of these soils may be needed. However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers. ",
+ "Management_ks": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotation andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity.
Drainage of these soils may be needed. However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers. "
+ }
+ },
+ "texture": {
+ "sl1": "Silt loam",
+ "sl2": "Silt loam",
+ "sl3": "Silt loam",
+ "sl4": "Silt loam",
+ "sl5": "Silt loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 8.0,
+ "sl2": 8.0,
+ "sl3": 8.0,
+ "sl4": 6.6,
+ "sl5": 6.14,
+ "sl6": 5.8,
+ "sl7": 5.67
+ },
+ "clay": {
+ "sl1": 36.0,
+ "sl2": 36.0,
+ "sl3": 36.0,
+ "sl4": 38.8,
+ "sl5": 39.86,
+ "sl6": 40.8,
+ "sl7": 41.5
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Haplic ferralsols",
+ "name": "Haplic ferralsols",
+ "rank_loc": "2",
+ "score_loc": 0.107
+ },
+ "ph": {
+ "sl1": 5.1,
+ "sl2": 5.1,
+ "sl3": 5.1,
+ "sl4": 5.16,
+ "sl5": 5.19,
+ "sl6": 5.24,
+ "sl7": 5.28
+ },
+ "rock_fragments": {
+ "sl1": 3.0,
+ "sl2": 3.0,
+ "sl3": 3.0,
+ "sl4": 3.4,
+ "sl5": 3.29,
+ "sl6": 3.2,
+ "sl7": 5.17
+ },
+ "sand": {
+ "sl1": 41.0,
+ "sl2": 41.0,
+ "sl3": 41.0,
+ "sl4": 38.8,
+ "sl5": 37.86,
+ "sl6": 36.8,
+ "sl7": 36.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 104788,
+ "distance": 15721.279,
+ "mapunitID": 12043,
+ "minCompDistance": 15721.27917076,
+ "share": 35,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.",
+ "Description_es": "Los Ferralsoles Háplicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada de retener nutrientes. ",
+ "Description_fr": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.",
+ "Description_ks": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.",
+ "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_es": "Estos suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.",
+ "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used."
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Unknown",
+ "sl7": "Unknown"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 26.0,
+ "sl2": 26.0,
+ "sl3": 26.0,
+ "sl4": 19.6,
+ "sl5": 17.14,
+ "sl6": 14.6,
+ "sl7": 13.5
+ },
+ "clay": {
+ "sl1": 27.0,
+ "sl2": 27.0,
+ "sl3": 27.0,
+ "sl4": 26.4,
+ "sl5": 26.29,
+ "sl6": 26.2,
+ "sl7": 25.5
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 0.8,
+ "sl5": 0.57,
+ "sl6": 0.4,
+ "sl7": 0.33
+ },
+ "id": {
+ "component": "Umbric gleysols",
+ "name": "Umbric gleysols",
+ "rank_loc": "3",
+ "score_loc": 0.1
+ },
+ "ph": {
+ "sl1": 4.7,
+ "sl2": 4.7,
+ "sl3": 4.7,
+ "sl4": 4.86,
+ "sl5": 4.94,
+ "sl6": 5.02,
+ "sl7": 5.07
+ },
+ "rock_fragments": {
+ "sl1": 10.0,
+ "sl2": 10.0,
+ "sl3": 10.0,
+ "sl4": 11.8,
+ "sl5": 11.86,
+ "sl6": 13.6,
+ "sl7": 14.67
+ },
+ "sand": {
+ "sl1": 39.0,
+ "sl2": 39.0,
+ "sl3": 39.0,
+ "sl4": 42.0,
+ "sl5": 43.43,
+ "sl6": 45.0,
+ "sl7": 47.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 104792,
+ "distance": 0.0,
+ "mapunitID": 12044,
+ "minCompDistance": 0.0,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.",
+ "Description_es": "Los Gleysoles Úmbricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles úmbricos tienen una materia orgánica relativamente alta, pero menos nutrientes en los horizontes superficiales. ",
+ "Description_fr": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.",
+ "Description_ks": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.",
+ "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. ",
+ "Management_es": "Estos suelos están saturados y, si se cultivan, se requiere un drenaje importante.
Una vez drenados, estos suelos pueden ser muy productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.
El pH superficial del suelo es bajo en estos suelos, y es probable que sea necesario el encalado.",
+ "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. ",
+ "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 9.0,
+ "sl2": 9.0,
+ "sl3": 9.0,
+ "sl4": 7.6,
+ "sl5": 7.14,
+ "sl6": 6.6,
+ "sl7": 6.33
+ },
+ "clay": {
+ "sl1": 46.0,
+ "sl2": 46.0,
+ "sl3": 46.0,
+ "sl4": 49.8,
+ "sl5": 50.71,
+ "sl6": 51.4,
+ "sl7": 51.67
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Rhodic ferralsols",
+ "name": "Rhodic ferralsols",
+ "rank_loc": "4",
+ "score_loc": 0.093
+ },
+ "ph": {
+ "sl1": 5.5,
+ "sl2": 5.5,
+ "sl3": 5.5,
+ "sl4": 5.44,
+ "sl5": 5.44,
+ "sl6": 5.46,
+ "sl7": 5.48
+ },
+ "rock_fragments": {
+ "sl1": 15.0,
+ "sl2": 15.0,
+ "sl3": 15.0,
+ "sl4": 7.0,
+ "sl5": 5.29,
+ "sl6": 4.2,
+ "sl7": 4.67
+ },
+ "sand": {
+ "sl1": 37.0,
+ "sl2": 37.0,
+ "sl3": 37.0,
+ "sl4": 34.4,
+ "sl5": 33.57,
+ "sl6": 32.8,
+ "sl7": 32.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 104787,
+ "distance": 15721.279,
+ "mapunitID": 12043,
+ "minCompDistance": 15721.27917076,
+ "share": 45,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ",
+ "Description_es": "Los Ferralsoles Ródicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas, pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos ródicos tienen subsuelos de color rojo oscuro con una buena estructura de suelo. ",
+ "Description_fr": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ",
+ "Description_ks": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ",
+ "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.",
+ "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used."
+ }
+ },
+ "texture": {
+ "sl1": "Unknown",
+ "sl2": "Unknown",
+ "sl3": "Unknown",
+ "sl4": "Unknown",
+ "sl5": "Unknown",
+ "sl6": "Unknown",
+ "sl7": "Unknown"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 5.0,
+ "sl2": 5.0,
+ "sl3": 5.0,
+ "sl4": 3.6,
+ "sl5": 3.14,
+ "sl6": 2.8,
+ "sl7": 2.67
+ },
+ "clay": {
+ "sl1": 5.0,
+ "sl2": 5.0,
+ "sl3": 5.0,
+ "sl4": 5.0,
+ "sl5": 5.14,
+ "sl6": 5.2,
+ "sl7": 5.33
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Gleyic arenosols",
+ "name": "Gleyic arenosols",
+ "rank_loc": "5",
+ "score_loc": 0.071
+ },
+ "ph": {
+ "sl1": 5.8,
+ "sl2": 5.8,
+ "sl3": 5.8,
+ "sl4": 5.8,
+ "sl5": 5.8,
+ "sl6": 5.8,
+ "sl7": 5.82
+ },
+ "rock_fragments": {
+ "sl1": 7.0,
+ "sl2": 7.0,
+ "sl3": 7.0,
+ "sl4": 10.4,
+ "sl5": 11.0,
+ "sl6": 10.0,
+ "sl7": 8.83
+ },
+ "sand": {
+ "sl1": 87.0,
+ "sl2": 87.0,
+ "sl3": 87.0,
+ "sl4": 87.2,
+ "sl5": 87.29,
+ "sl6": 87.4,
+ "sl7": 86.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 104793,
+ "distance": 0.0,
+ "mapunitID": 12044,
+ "minCompDistance": 0.0,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.",
+ "Description_es": "Los Arenosoles Gleyicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos están saturados con aguas subterráneas poco profundas por encima de un metro.",
+ "Description_fr": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.",
+ "Description_ks": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.",
+ "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ",
+ "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación por aguas subterráneas puede no ser posible la instalación de líneas de drenaje, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
En estos suelos se puede conseguir un uso más eficiente del N por parte de los cultivos mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).",
+ "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ",
+ "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). "
+ }
+ },
+ "texture": {
+ "sl1": "Loamy sand",
+ "sl2": "Loamy sand",
+ "sl3": "Loamy sand",
+ "sl4": "Loamy sand",
+ "sl5": "Loamy sand",
+ "sl6": "Loamy sand",
+ "sl7": "Loamy sand"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 40
+ },
+ "cec": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 21.5
+ },
+ "clay": {
+ "sl1": 27.0,
+ "sl2": 27.0,
+ "sl3": 27.0,
+ "sl4": 34.5
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0
+ },
+ "id": {
+ "component": "Eutric leptosols",
+ "name": "Eutric leptosols",
+ "rank_loc": "6",
+ "score_loc": 0.057
+ },
+ "ph": {
+ "sl1": 6.7,
+ "sl2": 6.7,
+ "sl3": 6.7,
+ "sl4": 6.55
+ },
+ "rock_fragments": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 40.5
+ },
+ "sand": {
+ "sl1": 41.0,
+ "sl2": 41.0,
+ "sl3": 41.0,
+ "sl4": 36.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 104791,
+ "distance": 0.0,
+ "mapunitID": 12044,
+ "minCompDistance": 0.0,
+ "share": 10,
+ "soilDepth": 40
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ",
+ "Description_es": "Los Leptosoles Eútricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles eútricos tienen una alta saturación de la base sobre la capa limitante de las raíces poco profundas. ",
+ "Description_fr": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ",
+ "Description_ks": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ",
+ "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ",
+ "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Se debe considerar el uso exclusivo para el pastoreo o la agroforestería.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Estos suelos pueden ser productivos para la agricultura, pero el enfoque debe ser el uso para el pastoreo.
Cualquier uso para el cultivo debe limitarse y combinarse con prácticas de conservación del suelo.",
+ "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ",
+ "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 7.0,
+ "sl2": 7.0,
+ "sl3": 7.0,
+ "sl4": 6.4,
+ "sl5": 6.14,
+ "sl6": 5.8,
+ "sl7": 5.33
+ },
+ "clay": {
+ "sl1": 22.0,
+ "sl2": 22.0,
+ "sl3": 22.0,
+ "sl4": 25.8,
+ "sl5": 27.14,
+ "sl6": 28.6,
+ "sl7": 31.17
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Xanthic ferralsols",
+ "name": "Xanthic ferralsols",
+ "rank_loc": "7",
+ "score_loc": 0.043
+ },
+ "ph": {
+ "sl1": 4.5,
+ "sl2": 4.5,
+ "sl3": 4.5,
+ "sl4": 4.58,
+ "sl5": 4.63,
+ "sl6": 4.68,
+ "sl7": 4.72
+ },
+ "rock_fragments": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 3.2,
+ "sl5": 3.57,
+ "sl6": 4.0,
+ "sl7": 5.0
+ },
+ "sand": {
+ "sl1": 66.0,
+ "sl2": 66.0,
+ "sl3": 66.0,
+ "sl4": 62.8,
+ "sl5": 61.71,
+ "sl6": 61.0,
+ "sl7": 58.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 104789,
+ "distance": 15721.279,
+ "mapunitID": 12043,
+ "minCompDistance": 15721.27917076,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ",
+ "Description_es": "Los Ferralsoles Xánticos son suelos bien desarrollados en climas húmedos y cálidos que están dominados por minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos xánticos tienen subsuelos de color amarillo que indican una retención de humedad ligeramente superior. ",
+ "Description_fr": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ",
+ "Description_ks": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ",
+ "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos. *Prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.",
+ "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy clay loam",
+ "sl2": "Sandy clay loam",
+ "sl3": "Sandy clay loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 7.0,
+ "sl2": 7.0,
+ "sl3": 7.0,
+ "sl4": 5.8,
+ "sl5": 5.71,
+ "sl6": 5.8,
+ "sl7": 6.0
+ },
+ "clay": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 12.6,
+ "sl5": 12.14,
+ "sl6": 12.2,
+ "sl7": 12.67
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 2.0,
+ "sl5": 2.29,
+ "sl6": 2.4,
+ "sl7": 2.33
+ },
+ "id": {
+ "component": "Dystric fluvisols",
+ "name": "Dystric fluvisols",
+ "rank_loc": "8",
+ "score_loc": 0.043
+ },
+ "ph": {
+ "sl1": 4.9,
+ "sl2": 4.9,
+ "sl3": 4.9,
+ "sl4": 4.98,
+ "sl5": 5.03,
+ "sl6": 5.08,
+ "sl7": 5.12
+ },
+ "rock_fragments": {
+ "sl1": 10.0,
+ "sl2": 10.0,
+ "sl3": 10.0,
+ "sl4": 11.2,
+ "sl5": 12.29,
+ "sl6": 14.0,
+ "sl7": 13.83
+ },
+ "sand": {
+ "sl1": 40.0,
+ "sl2": 40.0,
+ "sl3": 40.0,
+ "sl4": 47.2,
+ "sl5": 48.57,
+ "sl6": 48.8,
+ "sl7": 48.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 104796,
+ "distance": 26247.791,
+ "mapunitID": 12045,
+ "minCompDistance": 26247.79069505,
+ "share": 30,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_es": "Los Fluvisoles Dístricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los Fluvisoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.",
+ "Description_fr": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_ks": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.",
+ "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ",
+ "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (acolchados, cultivos de cobertura), que mejoren la infiltración del agua o que proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).
Una baja saturación de bases (presencia de Ca, Mg, K) indica que el pH del suelo puede ser bajo, y puede estar justificado el encalado.",
+ "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ",
+ "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 17.0,
+ "sl2": 17.0,
+ "sl3": 17.0,
+ "sl4": 16.4,
+ "sl5": 16.29,
+ "sl6": 16.4,
+ "sl7": 16.83
+ },
+ "clay": {
+ "sl1": 21.0,
+ "sl2": 21.0,
+ "sl3": 21.0,
+ "sl4": 21.6,
+ "sl5": 21.57,
+ "sl6": 21.6,
+ "sl7": 22.0
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 2.0,
+ "sl5": 2.29,
+ "sl6": 2.4,
+ "sl7": 2.33
+ },
+ "id": {
+ "component": "Eutric fluvisols",
+ "name": "Eutric fluvisols",
+ "rank_loc": "9",
+ "score_loc": 0.043
+ },
+ "ph": {
+ "sl1": 6.8,
+ "sl2": 6.8,
+ "sl3": 6.8,
+ "sl4": 7.0,
+ "sl5": 7.07,
+ "sl6": 7.16,
+ "sl7": 7.2
+ },
+ "rock_fragments": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 4.2,
+ "sl5": 4.0,
+ "sl6": 3.4,
+ "sl7": 4.83
+ },
+ "sand": {
+ "sl1": 37.0,
+ "sl2": 37.0,
+ "sl3": 37.0,
+ "sl4": 36.4,
+ "sl5": 36.43,
+ "sl6": 36.4,
+ "sl7": 35.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 104795,
+ "distance": 26247.791,
+ "mapunitID": 12045,
+ "minCompDistance": 26247.79069505,
+ "share": 30,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ",
+ "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).",
+ "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered."
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 3.0,
+ "sl2": 3.0,
+ "sl3": 3.0,
+ "sl4": 2.4,
+ "sl5": 2.14,
+ "sl6": 1.8,
+ "sl7": 1.67
+ },
+ "clay": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 6.6,
+ "sl5": 6.86,
+ "sl6": 7.2,
+ "sl7": 7.33
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Ferralic arenosols",
+ "name": "Ferralic arenosols",
+ "rank_loc": "10",
+ "score_loc": 0.029
+ },
+ "ph": {
+ "sl1": 5.5,
+ "sl2": 5.5,
+ "sl3": 5.5,
+ "sl4": 5.5,
+ "sl5": 5.5,
+ "sl6": 5.5,
+ "sl7": 5.48
+ },
+ "rock_fragments": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 3.2,
+ "sl5": 3.71,
+ "sl6": 4.4,
+ "sl7": 6.0
+ },
+ "sand": {
+ "sl1": 89.0,
+ "sl2": 89.0,
+ "sl3": 89.0,
+ "sl4": 89.0,
+ "sl5": 88.86,
+ "sl6": 88.4,
+ "sl7": 88.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 105472,
+ "distance": 19093.787,
+ "mapunitID": 12228,
+ "minCompDistance": 19093.78746931,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.",
+ "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.",
+ "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.",
+ "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.",
+ "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ",
+ "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.",
+ "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ",
+ "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. "
+ }
+ },
+ "texture": {
+ "sl1": "Sand",
+ "sl2": "Sand",
+ "sl3": "Sand",
+ "sl4": "Sand",
+ "sl5": "Sand",
+ "sl6": "Loamy sand",
+ "sl7": "Loamy sand"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 78.0,
+ "sl2": 78.0,
+ "sl3": 78.0,
+ "sl4": 77.2,
+ "sl5": 75.86,
+ "sl6": 73.8,
+ "sl7": 72.0
+ },
+ "clay": {
+ "sl1": 35.0,
+ "sl2": 35.0,
+ "sl3": 35.0,
+ "sl4": 34.4,
+ "sl5": 34.29,
+ "sl6": 33.4,
+ "sl7": 32.67
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.6,
+ "sl5": 0.71,
+ "sl6": 0.8,
+ "sl7": 0.83
+ },
+ "id": {
+ "component": "Fibric histosols",
+ "name": "Fibric histosols",
+ "rank_loc": "11",
+ "score_loc": 0.014
+ },
+ "ph": {
+ "sl1": 4.4,
+ "sl2": 4.4,
+ "sl3": 4.4,
+ "sl4": 4.3,
+ "sl5": 4.31,
+ "sl6": 4.34,
+ "sl7": 4.37
+ },
+ "rock_fragments": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 10.2,
+ "sl5": 11.29,
+ "sl6": 10.6,
+ "sl7": 10.67
+ },
+ "sand": {
+ "sl1": 27.0,
+ "sl2": 27.0,
+ "sl3": 27.0,
+ "sl4": 28.6,
+ "sl5": 29.0,
+ "sl6": 31.8,
+ "sl7": 33.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 104797,
+ "distance": 26247.791,
+ "mapunitID": 12045,
+ "minCompDistance": 26247.79069505,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Fibric Histosols are organic soils that typically form in wet environments.
Their properties are largely dependent on the type and degree of decomposition of the organic soil materials.
The soils can be productive with intensive management including soil drainage but their fragile nature and habitat suggests preservation of these soils is warranted where possible.
When cultivated, subsidence and sulfide oxidation present management challenges.
Fibric Histosols have relatively undecomposed organic soil materials.
Thus, they have a slightly lower bulk density and higher water content. ",
+ "Description_es": "Los Histosoles Fíbricos son suelos orgánicos que se forman típicamente en ambientes húmedos.
Sus propiedades dependen en gran medida del tipo y el grado de descomposición de los materiales orgánicos del suelo.
Los suelos pueden ser productivos con una gestión intensiva que incluya el drenaje del suelo, pero su naturaleza frágil y su hábitat sugieren que se garantice la preservación de estos suelos cuando sea posible.
Cuando se cultivan, el hundimiento y la oxidación de los sulfuros plantean problemas de gestión.
Los Histosoles Fíbricos tienen materiales orgánicos relativamente poco descompuestos.
Por lo tanto, tienen una densidad aparente ligeramente inferior y un mayor contenido de agua. ",
+ "Description_fr": "Fibric Histosols are organic soils that typically form in wet environments.
Their properties are largely dependent on the type and degree of decomposition of the organic soil materials.
The soils can be productive with intensive management including soil drainage but their fragile nature and habitat suggests preservation of these soils is warranted where possible.
When cultivated, subsidence and sulfide oxidation present management challenges.
Fibric Histosols have relatively undecomposed organic soil materials.
Thus, they have a slightly lower bulk density and higher water content. ",
+ "Description_ks": "Fibric Histosols are organic soils that typically form in wet environments.
Their properties are largely dependent on the type and degree of decomposition of the organic soil materials.
The soils can be productive with intensive management including soil drainage but their fragile nature and habitat suggests preservation of these soils is warranted where possible.
When cultivated, subsidence and sulfide oxidation present management challenges.
Fibric Histosols have relatively undecomposed organic soil materials.
Thus, they have a slightly lower bulk density and higher water content. ",
+ "Management_en": "These soils can be some of our most productive soils, especially for specialty crops such as vegetables.
However, they must be drained for use, and this will lead to subsidence of the soil, as exposed peat is rapidly mineralized, and organic matter content quickly drops.
This will lead to increasingly acid soils, and thus regularliming will be needed.
These organic soils must be managed differently from mineral soils, and techniques that minimize organic matter degradation are a priority. ",
+ "Management_es": "Estos suelos pueden ser algunos de los más productivos, especialmente para cultivos especiales como las hortalizas.
Sin embargo, deben ser drenados para su uso, y esto conducirá al hundimiento del suelo, ya que la turba expuesta se mineraliza rápidamente, y el contenido de materia orgánica disminuye rápidamente.
Esto hará que los suelos se vuelvan cada vez más ácidos, por lo que será necesario un tratamiento regular.
Estos suelos orgánicos deben gestionarse de forma diferente a los suelos minerales, y las técnicas que minimizan la degradación de la materia orgánica son una prioridad.",
+ "Management_fr": "These soils can be some of our most productive soils, especially for specialty crops such as vegetables.
However, they must be drained for use, and this will lead to subsidence of the soil, as exposed peat is rapidly mineralized, and organic matter content quickly drops.
This will lead to increasingly acid soils, and thus regularliming will be needed.
These organic soils must be managed differently from mineral soils, and techniques that minimize organic matter degradation are a priority. ",
+ "Management_ks": "These soils can be some of our most productive soils, especially for specialty crops such as vegetables.
However, they must be drained for use, and this will lead to subsidence of the soil, as exposed peat is rapidly mineralized, and organic matter content quickly drops.
This will lead to increasingly acid soils, and thus regularliming will be needed.
These organic soils must be managed differently from mineral soils, and techniques that minimize organic matter degradation are a priority. "
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "global",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Gleyic alisols",
+ "componentData": "Data Complete",
+ "componentID": 104790,
+ "name": "Gleyic alisols",
+ "rank_data": "2",
+ "rank_data_loc": "1",
+ "rank_loc": 1,
+ "score_data": 1.0,
+ "score_data_loc": 1.0,
+ "score_loc": 0.4
+ },
+ {
+ "component": "Haplic ferralsols",
+ "componentData": "Missing Data",
+ "componentID": 104788,
+ "name": "Haplic ferralsols",
+ "rank_data": "3",
+ "rank_data_loc": "2",
+ "rank_loc": 2,
+ "score_data": 1.0,
+ "score_data_loc": 0.791,
+ "score_loc": 0.107
+ },
+ {
+ "component": "Umbric gleysols",
+ "componentData": "Data Complete",
+ "componentID": 104792,
+ "name": "Umbric gleysols",
+ "rank_data": "4",
+ "rank_data_loc": "3",
+ "rank_loc": 3,
+ "score_data": 1.0,
+ "score_data_loc": 0.786,
+ "score_loc": 0.1
+ },
+ {
+ "component": "Ferralic arenosols",
+ "componentData": "Data Complete",
+ "componentID": 105472,
+ "name": "Ferralic arenosols",
+ "rank_data": "1",
+ "rank_data_loc": "4",
+ "rank_loc": 10,
+ "score_data": 1.0,
+ "score_data_loc": 0.735,
+ "score_loc": 0.029
+ },
+ {
+ "component": "Eutric fluvisols",
+ "componentData": "Data Complete",
+ "componentID": 104795,
+ "name": "Eutric fluvisols",
+ "rank_data": "5",
+ "rank_data_loc": "5",
+ "rank_loc": 9,
+ "score_data": 0.903,
+ "score_data_loc": 0.676,
+ "score_loc": 0.043
+ },
+ {
+ "component": "Gleyic arenosols",
+ "componentData": "Data Complete",
+ "componentID": 104793,
+ "name": "Gleyic arenosols",
+ "rank_data": "8",
+ "rank_data_loc": "6",
+ "rank_loc": 5,
+ "score_data": 0.673,
+ "score_data_loc": 0.532,
+ "score_loc": 0.071
+ },
+ {
+ "component": "Dystric fluvisols",
+ "componentData": "Data Complete",
+ "componentID": 104796,
+ "name": "Dystric fluvisols",
+ "rank_data": "7",
+ "rank_data_loc": "7",
+ "rank_loc": 8,
+ "score_data": 0.673,
+ "score_data_loc": 0.511,
+ "score_loc": 0.043
+ },
+ {
+ "component": "Fibric histosols",
+ "componentData": "Data Complete",
+ "componentID": 104797,
+ "name": "Fibric histosols",
+ "rank_data": "9",
+ "rank_data_loc": "8",
+ "rank_loc": 11,
+ "score_data": 0.629,
+ "score_data_loc": 0.46,
+ "score_loc": 0.014
+ },
+ {
+ "component": "Xanthic ferralsols",
+ "componentData": "Missing Data",
+ "componentID": 104789,
+ "name": "Xanthic ferralsols",
+ "rank_data": "10",
+ "rank_data_loc": "9",
+ "rank_loc": 7,
+ "score_data": 0.516,
+ "score_data_loc": 0.399,
+ "score_loc": 0.043
+ },
+ {
+ "component": "Rhodic ferralsols",
+ "componentData": "No Data",
+ "componentID": 104787,
+ "name": "Rhodic ferralsols",
+ "rank_data": "11",
+ "rank_data_loc": "10",
+ "rank_loc": 4,
+ "score_data": 0.383,
+ "score_data_loc": 0.34,
+ "score_loc": 0.093
+ },
+ {
+ "component": "Eutric leptosols",
+ "componentData": "Missing Data",
+ "componentID": 104791,
+ "name": "Eutric leptosols",
+ "rank_data": "6",
+ "rank_data_loc": "11",
+ "rank_loc": 6,
+ "score_data": 0.845,
+ "score_data_loc": 0.001,
+ "score_loc": 0.057
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-19.13333,145.5125].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-19.13333,145.5125].json
new file mode 100644
index 0000000..37a9eda
--- /dev/null
+++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-19.13333,145.5125].json
@@ -0,0 +1,2155 @@
+{
+ "list": {
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 18.0,
+ "sl2": 18.0,
+ "sl3": 18.0,
+ "sl4": 18.2,
+ "sl5": 18.43,
+ "sl6": 18.4,
+ "sl7": 17.83
+ },
+ "clay": {
+ "sl1": 30.0,
+ "sl2": 30.0,
+ "sl3": 30.0,
+ "sl4": 34.2,
+ "sl5": 35.86,
+ "sl6": 37.2,
+ "sl7": 37.5
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.0,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Chromic luvisols",
+ "name": "Chromic luvisols",
+ "rank_loc": "1",
+ "score_loc": 0.126
+ },
+ "ph": {
+ "sl1": 6.5,
+ "sl2": 6.5,
+ "sl3": 6.5,
+ "sl4": 6.56,
+ "sl5": 6.57,
+ "sl6": 6.58,
+ "sl7": 6.55
+ },
+ "rock_fragments": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 10.6,
+ "sl5": 10.14,
+ "sl6": 9.8,
+ "sl7": 11.33
+ },
+ "sand": {
+ "sl1": 37.0,
+ "sl2": 37.0,
+ "sl3": 37.0,
+ "sl4": 34.4,
+ "sl5": 33.43,
+ "sl6": 32.6,
+ "sl7": 33.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 149086,
+ "distance": 0.0,
+ "mapunitID": 6080,
+ "minCompDistance": 0.0,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.",
+ "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.",
+ "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops."
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 14.6,
+ "sl5": 14.71,
+ "sl6": 15.0,
+ "sl7": 15.17
+ },
+ "clay": {
+ "sl1": 24.0,
+ "sl2": 24.0,
+ "sl3": 24.0,
+ "sl4": 28.6,
+ "sl5": 29.86,
+ "sl6": 30.6,
+ "sl7": 30.5
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.0,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Eutric planosols",
+ "name": "Eutric planosols",
+ "rank_loc": "2",
+ "score_loc": 0.12
+ },
+ "ph": {
+ "sl1": 6.4,
+ "sl2": 6.4,
+ "sl3": 6.4,
+ "sl4": 6.42,
+ "sl5": 6.44,
+ "sl6": 6.44,
+ "sl7": 6.43
+ },
+ "rock_fragments": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 6.8,
+ "sl5": 9.29,
+ "sl6": 13.4,
+ "sl7": 12.5
+ },
+ "sand": {
+ "sl1": 53.0,
+ "sl2": 53.0,
+ "sl3": 53.0,
+ "sl4": 49.0,
+ "sl5": 47.71,
+ "sl6": 46.6,
+ "sl7": 46.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 149085,
+ "distance": 0.0,
+ "mapunitID": 6080,
+ "minCompDistance": 0.0,
+ "share": 30,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.",
+ "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.",
+ "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.",
+ "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.",
+ "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.",
+ "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.",
+ "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.",
+ "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy clay loam",
+ "sl2": "Sandy clay loam",
+ "sl3": "Sandy clay loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 10.0,
+ "sl2": 10.0,
+ "sl3": 10.0,
+ "sl4": 11.8,
+ "sl5": 12.14,
+ "sl6": 12.2,
+ "sl7": 12.17
+ },
+ "clay": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 24.2,
+ "sl5": 25.43,
+ "sl6": 26.2,
+ "sl7": 26.0
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.0,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Albic arenosols",
+ "name": "Albic arenosols",
+ "rank_loc": "3",
+ "score_loc": 0.094
+ },
+ "ph": {
+ "sl1": 6.5,
+ "sl2": 6.5,
+ "sl3": 6.5,
+ "sl4": 6.62,
+ "sl5": 6.66,
+ "sl6": 6.76,
+ "sl7": 6.83
+ },
+ "rock_fragments": {
+ "sl1": 12.0,
+ "sl2": 12.0,
+ "sl3": 12.0,
+ "sl4": 12.0,
+ "sl5": 12.71,
+ "sl6": 16.0,
+ "sl7": 18.0
+ },
+ "sand": {
+ "sl1": 67.0,
+ "sl2": 67.0,
+ "sl3": 67.0,
+ "sl4": 62.6,
+ "sl5": 61.71,
+ "sl6": 61.0,
+ "sl7": 61.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 148957,
+ "distance": 438.366,
+ "mapunitID": 6037,
+ "minCompDistance": 438.36624807,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.",
+ "Description_es": "Los Arenosoles Álbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos están muy lixiviados con pocos nutrientes y agua disponible.",
+ "Description_fr": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.",
+ "Description_ks": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.",
+ "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. ",
+ "Management_es": "Dado que estos suelos tienen poca retención de agua y nutrientes, deben ser fertilizados y regados para lograr una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
En estos suelos se debe prestar especial atención a minimizar la pérdida de nutrientes durante la fertilización.
Si se dispone de ellas, deben considerarse fuentes de N de liberación lenta, o una aplicación más frecuente de N a tasas más bajas.",
+ "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. ",
+ "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 13.6,
+ "sl5": 15.0,
+ "sl6": 16.4,
+ "sl7": 16.83
+ },
+ "clay": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0,
+ "sl4": 24.4,
+ "sl5": 26.86,
+ "sl6": 29.2,
+ "sl7": 30.0
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.0,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Cambic arenosols",
+ "name": "Cambic arenosols",
+ "rank_loc": "4",
+ "score_loc": 0.088
+ },
+ "ph": {
+ "sl1": 6.1,
+ "sl2": 6.1,
+ "sl3": 6.1,
+ "sl4": 6.26,
+ "sl5": 6.37,
+ "sl6": 6.52,
+ "sl7": 6.57
+ },
+ "rock_fragments": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 2.6,
+ "sl5": 2.57,
+ "sl6": 2.4,
+ "sl7": 2.33
+ },
+ "sand": {
+ "sl1": 49.0,
+ "sl2": 49.0,
+ "sl3": 49.0,
+ "sl4": 46.0,
+ "sl5": 44.14,
+ "sl6": 42.2,
+ "sl7": 42.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 148955,
+ "distance": 438.366,
+ "mapunitID": 6037,
+ "minCompDistance": 438.36624807,
+ "share": 30,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.",
+ "Description_es": "Los Arenosoles Cámbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles cámbicos tienen un horizonte del subsuelo mínimamente desarrollado que puede retener cantidades ligeramente superiores de nutrientes y agua.",
+ "Description_fr": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.",
+ "Description_ks": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.",
+ "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ",
+ "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.",
+ "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ",
+ "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 8.8,
+ "sl5": 10.0,
+ "sl6": 10.8,
+ "sl7": 11.33
+ },
+ "clay": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 18.4,
+ "sl5": 20.86,
+ "sl6": 22.2,
+ "sl7": 22.83
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.2,
+ "sl7": 1.33
+ },
+ "id": {
+ "component": "Haplic luvisols",
+ "name": "Haplic luvisols",
+ "rank_loc": "5",
+ "score_loc": 0.087
+ },
+ "ph": {
+ "sl1": 6.2,
+ "sl2": 6.2,
+ "sl3": 6.2,
+ "sl4": 6.36,
+ "sl5": 6.46,
+ "sl6": 6.64,
+ "sl7": 6.73
+ },
+ "rock_fragments": {
+ "sl1": 21.0,
+ "sl2": 21.0,
+ "sl3": 21.0,
+ "sl4": 13.6,
+ "sl5": 11.29,
+ "sl6": 9.6,
+ "sl7": 8.83
+ },
+ "sand": {
+ "sl1": 80.0,
+ "sl2": 80.0,
+ "sl3": 80.0,
+ "sl4": 72.0,
+ "sl5": 70.0,
+ "sl6": 69.0,
+ "sl7": 68.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 149088,
+ "distance": 0.0,
+ "mapunitID": 6080,
+ "minCompDistance": 0.0,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.",
+ "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.",
+ "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.",
+ "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.",
+ "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.",
+ "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops."
+ }
+ },
+ "texture": {
+ "sl1": "Loamy sand",
+ "sl2": "Loamy sand",
+ "sl3": "Loamy sand",
+ "sl4": "Sandy loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 3.0,
+ "sl2": 3.0,
+ "sl3": 3.0,
+ "sl4": 1.8,
+ "sl5": 1.57,
+ "sl6": 1.4,
+ "sl7": 1.33
+ },
+ "clay": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 4.0,
+ "sl5": 4.0,
+ "sl6": 4.0,
+ "sl7": 4.17
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Dystric regosols",
+ "name": "Dystric regosols",
+ "rank_loc": "6",
+ "score_loc": 0.054
+ },
+ "ph": {
+ "sl1": 5.3,
+ "sl2": 5.3,
+ "sl3": 5.3,
+ "sl4": 5.32,
+ "sl5": 5.36,
+ "sl6": 5.42,
+ "sl7": 5.43
+ },
+ "rock_fragments": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 3.2,
+ "sl5": 3.43,
+ "sl6": 3.6,
+ "sl7": 4.5
+ },
+ "sand": {
+ "sl1": 86.0,
+ "sl2": 86.0,
+ "sl3": 86.0,
+ "sl4": 86.8,
+ "sl5": 86.86,
+ "sl6": 86.6,
+ "sl7": 86.33
+ },
+ "site": {
+ "siteData": {
+ "componentID": 148956,
+ "distance": 438.366,
+ "mapunitID": 6037,
+ "minCompDistance": 438.36624807,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ",
+ "Description_es": "Los Regosoles Dístricos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.
Los Regosoles Dístricos tienen una baja saturación de base en el subsuelo. ",
+ "Description_fr": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ",
+ "Description_ks": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ",
+ "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ",
+ "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo. *Incluso cuando se utilizan para el pastoreo, el riego será necesario debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos. *Con una baja saturación de bases, estos suelos pueden responder a la adición de bases como el potasio, el calcio o el magnesio. ",
+ "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ",
+ "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. "
+ }
+ },
+ "texture": {
+ "sl1": "Loamy sand",
+ "sl2": "Loamy sand",
+ "sl3": "Loamy sand",
+ "sl4": "Loamy sand",
+ "sl5": "Loamy sand",
+ "sl6": "Loamy sand",
+ "sl7": "Loamy sand"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 3.0,
+ "sl2": 3.0,
+ "sl3": 3.0,
+ "sl4": 2.4,
+ "sl5": 2.14,
+ "sl6": 1.8,
+ "sl7": 1.67
+ },
+ "clay": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 4.0,
+ "sl5": 4.0,
+ "sl6": 4.0,
+ "sl7": 4.0
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Calcic luvisols",
+ "name": "Calcic luvisols",
+ "rank_loc": "7",
+ "score_loc": 0.039
+ },
+ "ph": {
+ "sl1": 5.5,
+ "sl2": 5.5,
+ "sl3": 5.5,
+ "sl4": 5.5,
+ "sl5": 5.53,
+ "sl6": 5.58,
+ "sl7": 5.6
+ },
+ "rock_fragments": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 3.0,
+ "sl5": 3.14,
+ "sl6": 3.4,
+ "sl7": 4.17
+ },
+ "sand": {
+ "sl1": 88.0,
+ "sl2": 88.0,
+ "sl3": 88.0,
+ "sl4": 88.6,
+ "sl5": 88.57,
+ "sl6": 88.4,
+ "sl7": 88.33
+ },
+ "site": {
+ "siteData": {
+ "componentID": 149087,
+ "distance": 0.0,
+ "mapunitID": 6080,
+ "minCompDistance": 0.0,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.",
+ "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.",
+ "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.",
+ "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.",
+ "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ",
+ "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.",
+ "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ",
+ "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. "
+ }
+ },
+ "texture": {
+ "sl1": "Sand",
+ "sl2": "Sand",
+ "sl3": "Sand",
+ "sl4": "Sand",
+ "sl5": "Sand",
+ "sl6": "Sand",
+ "sl7": "Sand"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 5.0,
+ "sl2": 5.0,
+ "sl3": 5.0,
+ "sl4": 3.8,
+ "sl5": 3.57,
+ "sl6": 3.8,
+ "sl7": 3.5
+ },
+ "clay": {
+ "sl1": 7.0,
+ "sl2": 7.0,
+ "sl3": 7.0,
+ "sl4": 7.0,
+ "sl5": 7.14,
+ "sl6": 7.6,
+ "sl7": 7.17
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Acrisols",
+ "name": "Acrisols",
+ "rank_loc": "8",
+ "score_loc": 0.037
+ },
+ "ph": {
+ "sl1": 6.4,
+ "sl2": 6.4,
+ "sl3": 6.4,
+ "sl4": 6.42,
+ "sl5": 6.46,
+ "sl6": 6.54,
+ "sl7": 6.55
+ },
+ "rock_fragments": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 2.4,
+ "sl5": 2.86,
+ "sl6": 2.8,
+ "sl7": 5.33
+ },
+ "sand": {
+ "sl1": 87.0,
+ "sl2": 87.0,
+ "sl3": 87.0,
+ "sl4": 86.8,
+ "sl5": 86.29,
+ "sl6": 85.2,
+ "sl7": 86.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 148960,
+ "distance": 438.366,
+ "mapunitID": 6037,
+ "minCompDistance": 438.36624807,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.",
+ "Description_es": "Los Acrisoles son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ",
+ "Description_fr": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.",
+ "Description_ks": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.",
+ "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ",
+ "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ",
+ "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ",
+ "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. "
+ }
+ },
+ "texture": {
+ "sl1": "Loamy sand",
+ "sl2": "Loamy sand",
+ "sl3": "Loamy sand",
+ "sl4": "Loamy sand",
+ "sl5": "Loamy sand",
+ "sl6": "Loamy sand",
+ "sl7": "Loamy sand"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 13.0,
+ "sl2": 13.0,
+ "sl3": 13.0,
+ "sl4": 14.0,
+ "sl5": 14.71,
+ "sl6": 15.2,
+ "sl7": 15.33
+ },
+ "clay": {
+ "sl1": 17.0,
+ "sl2": 17.0,
+ "sl3": 17.0,
+ "sl4": 22.8,
+ "sl5": 24.86,
+ "sl6": 26.2,
+ "sl7": 26.17
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.2,
+ "sl7": 1.33
+ },
+ "id": {
+ "component": "Ferralsols",
+ "name": "Ferralsols",
+ "rank_loc": "9",
+ "score_loc": 0.027
+ },
+ "ph": {
+ "sl1": 5.9,
+ "sl2": 5.9,
+ "sl3": 5.9,
+ "sl4": 5.96,
+ "sl5": 5.97,
+ "sl6": 6.0,
+ "sl7": 6.03
+ },
+ "rock_fragments": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 11.2,
+ "sl5": 11.71,
+ "sl6": 12.8,
+ "sl7": 13.33
+ },
+ "sand": {
+ "sl1": 41.0,
+ "sl2": 41.0,
+ "sl3": 41.0,
+ "sl4": 37.6,
+ "sl5": 36.57,
+ "sl6": 36.2,
+ "sl7": 36.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 148959,
+ "distance": 438.366,
+ "mapunitID": 6037,
+ "minCompDistance": 438.36624807,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients. ",
+ "Description_es": "Los Ferralisoles son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad, como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas, pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes. ",
+ "Description_fr": "Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients. ",
+ "Description_ks": "Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients. ",
+ "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_es": "suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por parte de los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.",
+ "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.",
+ "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used."
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 16.6,
+ "sl5": 16.71,
+ "sl6": 16.6,
+ "sl7": 16.5
+ },
+ "clay": {
+ "sl1": 25.0,
+ "sl2": 25.0,
+ "sl3": 25.0,
+ "sl4": 30.2,
+ "sl5": 31.57,
+ "sl6": 32.4,
+ "sl7": 32.33
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.0,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Haplic acrisols",
+ "name": "Haplic acrisols",
+ "rank_loc": "10",
+ "score_loc": 0.016
+ },
+ "ph": {
+ "sl1": 6.2,
+ "sl2": 6.2,
+ "sl3": 6.2,
+ "sl4": 6.22,
+ "sl5": 6.26,
+ "sl6": 6.32,
+ "sl7": 6.37
+ },
+ "rock_fragments": {
+ "sl1": 10.0,
+ "sl2": 10.0,
+ "sl3": 10.0,
+ "sl4": 14.8,
+ "sl5": 15.29,
+ "sl6": 15.2,
+ "sl7": 14.67
+ },
+ "sand": {
+ "sl1": 47.0,
+ "sl2": 47.0,
+ "sl3": 47.0,
+ "sl4": 43.6,
+ "sl5": 42.71,
+ "sl6": 42.4,
+ "sl7": 42.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 148400,
+ "distance": 29716.363,
+ "mapunitID": 5876,
+ "minCompDistance": 29716.36256981,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.",
+ "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ",
+ "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.",
+ "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.",
+ "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ",
+ "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ",
+ "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ",
+ "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 9.0,
+ "sl2": 9.0,
+ "sl3": 9.0,
+ "sl4": 7.6,
+ "sl5": 7.0,
+ "sl6": 6.4,
+ "sl7": 6.0
+ },
+ "clay": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0,
+ "sl4": 18.0,
+ "sl5": 17.14,
+ "sl6": 16.0,
+ "sl7": 15.67
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.14,
+ "sl6": 1.2,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Dystric planosols",
+ "name": "Dystric planosols",
+ "rank_loc": "11",
+ "score_loc": 0.008
+ },
+ "ph": {
+ "sl1": 5.1,
+ "sl2": 5.1,
+ "sl3": 5.1,
+ "sl4": 5.08,
+ "sl5": 5.13,
+ "sl6": 5.16,
+ "sl7": 5.18
+ },
+ "rock_fragments": {
+ "sl1": 24.0,
+ "sl2": 24.0,
+ "sl3": 24.0,
+ "sl4": 30.6,
+ "sl5": 31.14,
+ "sl6": 35.2,
+ "sl7": 36.67
+ },
+ "sand": {
+ "sl1": 55.0,
+ "sl2": 55.0,
+ "sl3": 55.0,
+ "sl4": 57.6,
+ "sl5": 58.71,
+ "sl6": 60.2,
+ "sl7": 60.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 148585,
+ "distance": 7539.61,
+ "mapunitID": 5933,
+ "minCompDistance": 7539.61019871,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.",
+ "Description_es": "Los Planosoles Dístricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren de drenaje para la producción de cultivos.
Los Planosoles Dístricos son suelos menos productivos con baja saturación de base en el subsuelo.",
+ "Description_fr": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.",
+ "Description_ks": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.",
+ "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed.",
+ "Management_es": "Situados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requerirán una fertilización adicional.
Los niveles de calcio son muy bajos en el perfil inferior de este suelo.
Se necesitará una fertilización suplementaria.",
+ "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed.",
+ "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy loam",
+ "sl5": "Sandy loam",
+ "sl6": "Sandy loam",
+ "sl7": "Sandy loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 20.2,
+ "sl5": 20.14,
+ "sl6": 19.8,
+ "sl7": 19.0
+ },
+ "clay": {
+ "sl1": 23.0,
+ "sl2": 23.0,
+ "sl3": 23.0,
+ "sl4": 26.8,
+ "sl5": 27.86,
+ "sl6": 29.2,
+ "sl7": 28.83
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.2,
+ "sl5": 0.43,
+ "sl6": 0.8,
+ "sl7": 0.83
+ },
+ "id": {
+ "component": "Eutric cambisols",
+ "name": "Eutric cambisols",
+ "rank_loc": "12",
+ "score_loc": 0.008
+ },
+ "ph": {
+ "sl1": 7.6,
+ "sl2": 7.6,
+ "sl3": 7.6,
+ "sl4": 7.68,
+ "sl5": 7.74,
+ "sl6": 7.82,
+ "sl7": 7.88
+ },
+ "rock_fragments": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 16.0,
+ "sl5": 18.0,
+ "sl6": 21.2,
+ "sl7": 21.67
+ },
+ "sand": {
+ "sl1": 42.0,
+ "sl2": 42.0,
+ "sl3": 42.0,
+ "sl4": 39.0,
+ "sl5": 38.29,
+ "sl6": 36.8,
+ "sl7": 36.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 148586,
+ "distance": 7539.61,
+ "mapunitID": 5933,
+ "minCompDistance": 7539.61019871,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ",
+ "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ",
+ "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ",
+ "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ",
+ "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ",
+ "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.",
+ "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ",
+ "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 15.0,
+ "sl2": 15.0,
+ "sl3": 15.0,
+ "sl4": 16.0,
+ "sl5": 16.0,
+ "sl6": 16.0,
+ "sl7": 15.83
+ },
+ "clay": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 22.2,
+ "sl5": 23.0,
+ "sl6": 23.6,
+ "sl7": 23.67
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.0,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Chromic luvisols",
+ "name": "Chromic luvisols2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.126
+ },
+ "ph": {
+ "sl1": 7.4,
+ "sl2": 7.4,
+ "sl3": 7.4,
+ "sl4": 7.56,
+ "sl5": 7.64,
+ "sl6": 7.74,
+ "sl7": 7.82
+ },
+ "rock_fragments": {
+ "sl1": 15.0,
+ "sl2": 15.0,
+ "sl3": 15.0,
+ "sl4": 19.0,
+ "sl5": 21.0,
+ "sl6": 22.6,
+ "sl7": 22.83
+ },
+ "sand": {
+ "sl1": 57.0,
+ "sl2": 57.0,
+ "sl3": 57.0,
+ "sl4": 55.0,
+ "sl5": 54.57,
+ "sl6": 54.2,
+ "sl7": 54.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 148550,
+ "distance": 11835.884,
+ "mapunitID": 5927,
+ "minCompDistance": 0.0,
+ "share": 70,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.",
+ "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.",
+ "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 8.0,
+ "sl2": 8.0,
+ "sl3": 8.0,
+ "sl4": 6.8,
+ "sl5": 6.57,
+ "sl6": 6.6,
+ "sl7": 6.67
+ },
+ "clay": {
+ "sl1": 25.0,
+ "sl2": 25.0,
+ "sl3": 25.0,
+ "sl4": 30.8,
+ "sl5": 33.14,
+ "sl6": 35.6,
+ "sl7": 36.67
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Chromic luvisols",
+ "name": "Chromic luvisols3",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.126
+ },
+ "ph": {
+ "sl1": 5.1,
+ "sl2": 5.1,
+ "sl3": 5.1,
+ "sl4": 5.04,
+ "sl5": 5.03,
+ "sl6": 5.02,
+ "sl7": 5.02
+ },
+ "rock_fragments": {
+ "sl1": 15.0,
+ "sl2": 15.0,
+ "sl3": 15.0,
+ "sl4": 17.8,
+ "sl5": 19.14,
+ "sl6": 19.6,
+ "sl7": 20.0
+ },
+ "sand": {
+ "sl1": 54.0,
+ "sl2": 54.0,
+ "sl3": 54.0,
+ "sl4": 49.6,
+ "sl5": 47.71,
+ "sl6": 45.6,
+ "sl7": 44.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 148831,
+ "distance": 27418.494,
+ "mapunitID": 6000,
+ "minCompDistance": 0.0,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.",
+ "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.",
+ "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy clay loam",
+ "sl2": "Sandy clay loam",
+ "sl3": "Sandy clay loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 3.0,
+ "sl2": 3.0,
+ "sl3": 3.0,
+ "sl4": 3.6,
+ "sl5": 3.71,
+ "sl6": 3.8,
+ "sl7": 3.83
+ },
+ "clay": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 15.4,
+ "sl5": 17.14,
+ "sl6": 18.6,
+ "sl7": 19.17
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Eutric planosols",
+ "name": "Eutric planosols2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.12
+ },
+ "ph": {
+ "sl1": 5.4,
+ "sl2": 5.4,
+ "sl3": 5.4,
+ "sl4": 5.22,
+ "sl5": 5.19,
+ "sl6": 5.16,
+ "sl7": 5.17
+ },
+ "rock_fragments": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 11.0,
+ "sl5": 9.14,
+ "sl6": 8.4,
+ "sl7": 9.17
+ },
+ "sand": {
+ "sl1": 77.0,
+ "sl2": 77.0,
+ "sl3": 77.0,
+ "sl4": 72.6,
+ "sl5": 71.0,
+ "sl6": 70.0,
+ "sl7": 69.33
+ },
+ "site": {
+ "siteData": {
+ "componentID": 148917,
+ "distance": 3068.563,
+ "mapunitID": 6024,
+ "minCompDistance": 0.0,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.",
+ "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.",
+ "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.",
+ "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.",
+ "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.",
+ "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.",
+ "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.",
+ "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization."
+ }
+ },
+ "texture": {
+ "sl1": "Loamy sand",
+ "sl2": "Loamy sand",
+ "sl3": "Loamy sand",
+ "sl4": "Sandy loam",
+ "sl5": "Sandy loam",
+ "sl6": "Sandy loam",
+ "sl7": "Sandy loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 9.0,
+ "sl2": 9.0,
+ "sl3": 9.0,
+ "sl4": 7.6,
+ "sl5": 7.0,
+ "sl6": 6.4,
+ "sl7": 6.17
+ },
+ "clay": {
+ "sl1": 43.0,
+ "sl2": 43.0,
+ "sl3": 43.0,
+ "sl4": 46.4,
+ "sl5": 47.43,
+ "sl6": 48.2,
+ "sl7": 48.67
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Albic arenosols",
+ "name": "Albic arenosols2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.094
+ },
+ "ph": {
+ "sl1": 4.9,
+ "sl2": 4.9,
+ "sl3": 4.9,
+ "sl4": 4.92,
+ "sl5": 4.94,
+ "sl6": 4.98,
+ "sl7": 5.0
+ },
+ "rock_fragments": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 4.2,
+ "sl5": 4.43,
+ "sl6": 4.8,
+ "sl7": 5.0
+ },
+ "sand": {
+ "sl1": 41.0,
+ "sl2": 41.0,
+ "sl3": 41.0,
+ "sl4": 38.8,
+ "sl5": 38.0,
+ "sl6": 37.4,
+ "sl7": 37.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 148914,
+ "distance": 3068.563,
+ "mapunitID": 6024,
+ "minCompDistance": 438.36624807,
+ "share": 40,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.",
+ "Description_es": "Los Arenosoles Álbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos están muy lixiviados con pocos nutrientes y agua disponible.",
+ "Description_fr": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.",
+ "Description_ks": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.",
+ "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. ",
+ "Management_es": "Dado que estos suelos tienen poca retención de agua y nutrientes, deben ser fertilizados y regados para lograr una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
En estos suelos se debe prestar especial atención a minimizar la pérdida de nutrientes durante la fertilización.
Si se dispone de ellas, deben considerarse fuentes de N de liberación lenta, o una aplicación más frecuente de N a tasas más bajas.",
+ "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. ",
+ "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. "
+ }
+ },
+ "texture": {
+ "sl1": "Unknown",
+ "sl2": "Unknown",
+ "sl3": "Unknown",
+ "sl4": "Unknown",
+ "sl5": "Unknown",
+ "sl6": "Unknown",
+ "sl7": "Unknown"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 7.0,
+ "sl2": 7.0,
+ "sl3": 7.0,
+ "sl4": 6.4,
+ "sl5": 6.29,
+ "sl6": 6.2,
+ "sl7": 6.17
+ },
+ "clay": {
+ "sl1": 23.0,
+ "sl2": 23.0,
+ "sl3": 23.0,
+ "sl4": 28.8,
+ "sl5": 31.14,
+ "sl6": 33.4,
+ "sl7": 34.33
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Haplic luvisols",
+ "name": "Haplic luvisols2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.087
+ },
+ "ph": {
+ "sl1": 5.1,
+ "sl2": 5.1,
+ "sl3": 5.1,
+ "sl4": 5.04,
+ "sl5": 5.03,
+ "sl6": 5.02,
+ "sl7": 5.02
+ },
+ "rock_fragments": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 12.4,
+ "sl5": 13.29,
+ "sl6": 13.0,
+ "sl7": 14.0
+ },
+ "sand": {
+ "sl1": 59.0,
+ "sl2": 59.0,
+ "sl3": 59.0,
+ "sl4": 54.4,
+ "sl5": 52.29,
+ "sl6": 50.2,
+ "sl7": 49.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 148551,
+ "distance": 11835.884,
+ "mapunitID": 5927,
+ "minCompDistance": 0.0,
+ "share": 30,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.",
+ "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.",
+ "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.",
+ "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.",
+ "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.",
+ "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy clay loam",
+ "sl2": "Sandy clay loam",
+ "sl3": "Sandy clay loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 12.0,
+ "sl2": 12.0,
+ "sl3": 12.0,
+ "sl4": 13.2,
+ "sl5": 14.71,
+ "sl6": 15.8,
+ "sl7": 15.67
+ },
+ "clay": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 25.6,
+ "sl5": 31.86,
+ "sl6": 36.2,
+ "sl7": 36.33
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Calcic luvisols",
+ "name": "Calcic luvisols2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.039
+ },
+ "ph": {
+ "sl1": 4.7,
+ "sl2": 4.7,
+ "sl3": 4.7,
+ "sl4": 4.78,
+ "sl5": 4.76,
+ "sl6": 4.74,
+ "sl7": 4.87
+ },
+ "rock_fragments": {
+ "sl1": 15.0,
+ "sl2": 15.0,
+ "sl3": 15.0,
+ "sl4": 13.2,
+ "sl5": 11.14,
+ "sl6": 10.2,
+ "sl7": 12.67
+ },
+ "sand": {
+ "sl1": 51.0,
+ "sl2": 51.0,
+ "sl3": 51.0,
+ "sl4": 43.0,
+ "sl5": 38.14,
+ "sl6": 35.2,
+ "sl7": 36.33
+ },
+ "site": {
+ "siteData": {
+ "componentID": 148402,
+ "distance": 29716.363,
+ "mapunitID": 5876,
+ "minCompDistance": 0.0,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.",
+ "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.",
+ "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.",
+ "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.",
+ "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ",
+ "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.",
+ "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ",
+ "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 14.8,
+ "sl5": 14.57,
+ "sl6": 14.2,
+ "sl7": 14.0
+ },
+ "clay": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0,
+ "sl4": 20.6,
+ "sl5": 20.86,
+ "sl6": 21.0,
+ "sl7": 20.83
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 0.8,
+ "sl5": 0.71,
+ "sl6": 0.8,
+ "sl7": 0.83
+ },
+ "id": {
+ "component": "Acrisols",
+ "name": "Acrisols2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.037
+ },
+ "ph": {
+ "sl1": 6.4,
+ "sl2": 6.4,
+ "sl3": 6.4,
+ "sl4": 6.54,
+ "sl5": 6.6,
+ "sl6": 6.66,
+ "sl7": 6.7
+ },
+ "rock_fragments": {
+ "sl1": 13.0,
+ "sl2": 13.0,
+ "sl3": 13.0,
+ "sl4": 15.0,
+ "sl5": 16.57,
+ "sl6": 18.8,
+ "sl7": 19.17
+ },
+ "sand": {
+ "sl1": 40.0,
+ "sl2": 40.0,
+ "sl3": 40.0,
+ "sl4": 40.8,
+ "sl5": 41.14,
+ "sl6": 41.8,
+ "sl7": 42.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 148918,
+ "distance": 3068.563,
+ "mapunitID": 6024,
+ "minCompDistance": 438.36624807,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.",
+ "Description_es": "Los Acrisoles son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ",
+ "Description_fr": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.",
+ "Description_ks": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.",
+ "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ",
+ "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ",
+ "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ",
+ "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "global",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Chromic luvisols",
+ "componentData": "Data Complete",
+ "componentID": 148550,
+ "name": "Chromic luvisols2",
+ "rank_data": "2",
+ "rank_data_loc": "1",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.919,
+ "score_data_loc": 1.0,
+ "score_loc": 0.126
+ },
+ {
+ "component": "Calcic luvisols",
+ "componentData": "Data Complete",
+ "componentID": 148402,
+ "name": "Calcic luvisols2",
+ "rank_data": "1",
+ "rank_data_loc": "2",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.919,
+ "score_data_loc": 0.917,
+ "score_loc": 0.039
+ },
+ {
+ "component": "Dystric planosols",
+ "componentData": "Missing Data",
+ "componentID": 148585,
+ "name": "Dystric planosols",
+ "rank_data": "3",
+ "rank_data_loc": "3",
+ "rank_loc": "11",
+ "score_data": 0.919,
+ "score_data_loc": 0.887,
+ "score_loc": 0.008
+ },
+ {
+ "component": "Albic arenosols",
+ "componentData": "Data Complete",
+ "componentID": 148914,
+ "name": "Albic arenosols2",
+ "rank_data": "4",
+ "rank_data_loc": "4",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.821,
+ "score_data_loc": 0.876,
+ "score_loc": 0.094
+ },
+ {
+ "component": "Haplic luvisols",
+ "componentData": "Data Complete",
+ "componentID": 149088,
+ "name": "Haplic luvisols",
+ "rank_data": "7",
+ "rank_data_loc": "5",
+ "rank_loc": "5",
+ "score_data": 0.753,
+ "score_data_loc": 0.804,
+ "score_loc": 0.087
+ },
+ {
+ "component": "Acrisols",
+ "componentData": "Data Complete",
+ "componentID": 148918,
+ "name": "Acrisols2",
+ "rank_data": "6",
+ "rank_data_loc": "6",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.753,
+ "score_data_loc": 0.756,
+ "score_loc": 0.037
+ },
+ {
+ "component": "Eutric planosols",
+ "componentData": "Data Complete",
+ "componentID": 149085,
+ "name": "Eutric planosols",
+ "rank_data": "10",
+ "rank_data_loc": "7",
+ "rank_loc": "2",
+ "score_data": 0.657,
+ "score_data_loc": 0.744,
+ "score_loc": 0.12
+ },
+ {
+ "component": "Dystric regosols",
+ "componentData": "Data Complete",
+ "componentID": 148956,
+ "name": "Dystric regosols",
+ "rank_data": "8",
+ "rank_data_loc": "8",
+ "rank_loc": "6",
+ "score_data": 0.722,
+ "score_data_loc": 0.742,
+ "score_loc": 0.054
+ },
+ {
+ "component": "Eutric cambisols",
+ "componentData": "Data Complete",
+ "componentID": 148586,
+ "name": "Eutric cambisols",
+ "rank_data": "5",
+ "rank_data_loc": "9",
+ "rank_loc": "12",
+ "score_data": 0.757,
+ "score_data_loc": 0.732,
+ "score_loc": 0.008
+ },
+ {
+ "component": "Haplic acrisols",
+ "componentData": "Data Complete",
+ "componentID": 148400,
+ "name": "Haplic acrisols",
+ "rank_data": "9",
+ "rank_data_loc": "10",
+ "rank_loc": "10",
+ "score_data": 0.722,
+ "score_data_loc": 0.706,
+ "score_loc": 0.016
+ },
+ {
+ "component": "Ferralsols",
+ "componentData": "No Data",
+ "componentID": 148959,
+ "name": "Ferralsols",
+ "rank_data": "11",
+ "rank_data_loc": "11",
+ "rank_loc": "9",
+ "score_data": 0.625,
+ "score_data_loc": 0.624,
+ "score_loc": 0.027
+ },
+ {
+ "component": "Cambic arenosols",
+ "componentData": "Data Complete",
+ "componentID": 148955,
+ "name": "Cambic arenosols",
+ "rank_data": "12",
+ "rank_data_loc": "12",
+ "rank_loc": "4",
+ "score_data": 0.413,
+ "score_data_loc": 0.479,
+ "score_loc": 0.088
+ },
+ {
+ "component": "Chromic luvisols",
+ "componentData": "Data Complete",
+ "componentID": 148831,
+ "name": "Chromic luvisols3",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.919,
+ "score_data_loc": 1.0,
+ "score_loc": 0.126
+ },
+ {
+ "component": "Chromic luvisols",
+ "componentData": "Missing Data",
+ "componentID": 149086,
+ "name": "Chromic luvisols",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "1",
+ "score_data": 0.625,
+ "score_data_loc": 0.719,
+ "score_loc": 0.126
+ },
+ {
+ "component": "Eutric planosols",
+ "componentData": "Data Complete",
+ "componentID": 148917,
+ "name": "Eutric planosols2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.622,
+ "score_data_loc": 0.711,
+ "score_loc": 0.12
+ },
+ {
+ "component": "Haplic luvisols",
+ "componentData": "Data Complete",
+ "componentID": 148551,
+ "name": "Haplic luvisols2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.625,
+ "score_data_loc": 0.681,
+ "score_loc": 0.087
+ },
+ {
+ "component": "Albic arenosols",
+ "componentData": "Data Complete",
+ "componentID": 148957,
+ "name": "Albic arenosols",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "3",
+ "score_data": 0.557,
+ "score_data_loc": 0.624,
+ "score_loc": 0.094
+ },
+ {
+ "component": "Acrisols",
+ "componentData": "Missing Data",
+ "componentID": 148960,
+ "name": "Acrisols",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "8",
+ "score_data": 0.587,
+ "score_data_loc": 0.597,
+ "score_loc": 0.037
+ },
+ {
+ "component": "Calcic luvisols",
+ "componentData": "Data Complete",
+ "componentID": 149087,
+ "name": "Calcic luvisols",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "7",
+ "score_data": 0.557,
+ "score_data_loc": 0.571,
+ "score_loc": 0.039
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-2.06972,37.29].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-2.06972,37.29].json
new file mode 100644
index 0000000..658e87b
--- /dev/null
+++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-2.06972,37.29].json
@@ -0,0 +1,1595 @@
+{
+ "list": {
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 3.0,
+ "sl2": 3.0,
+ "sl3": 3.0,
+ "sl4": 2.4,
+ "sl5": 2.29,
+ "sl6": 2.2,
+ "sl7": 2.0
+ },
+ "clay": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 6.2,
+ "sl5": 6.43,
+ "sl6": 6.8,
+ "sl7": 7.0
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Ferralic arenosols",
+ "name": "Ferralic arenosols",
+ "rank_loc": "1",
+ "score_loc": 0.107
+ },
+ "ph": {
+ "sl1": 5.3,
+ "sl2": 5.3,
+ "sl3": 5.3,
+ "sl4": 5.32,
+ "sl5": 5.34,
+ "sl6": 5.36,
+ "sl7": 5.37
+ },
+ "rock_fragments": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 4.2,
+ "sl5": 4.43,
+ "sl6": 4.6,
+ "sl7": 4.5
+ },
+ "sand": {
+ "sl1": 87.0,
+ "sl2": 87.0,
+ "sl3": 87.0,
+ "sl4": 86.8,
+ "sl5": 86.57,
+ "sl6": 86.2,
+ "sl7": 86.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 111274,
+ "distance": 337.622,
+ "mapunitID": 17482,
+ "minCompDistance": 337.62221932,
+ "share": 80,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.",
+ "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.",
+ "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.",
+ "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.",
+ "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ",
+ "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.",
+ "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ",
+ "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. "
+ }
+ },
+ "texture": {
+ "sl1": "Loamy sand",
+ "sl2": "Loamy sand",
+ "sl3": "Loamy sand",
+ "sl4": "Loamy sand",
+ "sl5": "Loamy sand",
+ "sl6": "Loamy sand",
+ "sl7": "Loamy sand"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 39.0,
+ "sl2": 39.0,
+ "sl3": 39.0,
+ "sl4": 39.8,
+ "sl5": 40.0,
+ "sl6": 39.8,
+ "sl7": 39.5
+ },
+ "clay": {
+ "sl1": 52.0,
+ "sl2": 52.0,
+ "sl3": 52.0,
+ "sl4": 54.6,
+ "sl5": 55.14,
+ "sl6": 55.4,
+ "sl7": 54.67
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.2,
+ "sl5": 0.43,
+ "sl6": 0.6,
+ "sl7": 0.83
+ },
+ "id": {
+ "component": "Eutric vertisols",
+ "name": "Eutric vertisols",
+ "rank_loc": "2",
+ "score_loc": 0.077
+ },
+ "ph": {
+ "sl1": 6.7,
+ "sl2": 6.7,
+ "sl3": 6.7,
+ "sl4": 6.78,
+ "sl5": 6.84,
+ "sl6": 6.94,
+ "sl7": 7.05
+ },
+ "rock_fragments": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 3.6,
+ "sl5": 3.71,
+ "sl6": 4.0,
+ "sl7": 4.0
+ },
+ "sand": {
+ "sl1": 21.0,
+ "sl2": 21.0,
+ "sl3": 21.0,
+ "sl4": 19.8,
+ "sl5": 19.71,
+ "sl6": 19.8,
+ "sl7": 20.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 111333,
+ "distance": 3522.833,
+ "mapunitID": 17516,
+ "minCompDistance": 3522.83287208,
+ "share": 50,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.",
+ "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ",
+ "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.",
+ "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.",
+ "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ",
+ "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.",
+ "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ",
+ "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. "
+ }
+ },
+ "texture": {
+ "sl1": "Unknown",
+ "sl2": "Unknown",
+ "sl3": "Unknown",
+ "sl4": "Unknown",
+ "sl5": "Unknown",
+ "sl6": "Unknown",
+ "sl7": "Unknown"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0,
+ "sl4": 18.2,
+ "sl5": 18.29,
+ "sl6": 18.2,
+ "sl7": 17.67
+ },
+ "clay": {
+ "sl1": 29.0,
+ "sl2": 29.0,
+ "sl3": 29.0,
+ "sl4": 31.4,
+ "sl5": 31.71,
+ "sl6": 31.4,
+ "sl7": 31.5
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 0.86,
+ "sl6": 0.6,
+ "sl7": 0.5
+ },
+ "id": {
+ "component": "Chromic cambisols",
+ "name": "Chromic cambisols",
+ "rank_loc": "3",
+ "score_loc": 0.07
+ },
+ "ph": {
+ "sl1": 6.6,
+ "sl2": 6.6,
+ "sl3": 6.6,
+ "sl4": 6.56,
+ "sl5": 6.6,
+ "sl6": 6.68,
+ "sl7": 6.77
+ },
+ "rock_fragments": {
+ "sl1": 5.0,
+ "sl2": 5.0,
+ "sl3": 5.0,
+ "sl4": 12.0,
+ "sl5": 14.14,
+ "sl6": 12.6,
+ "sl7": 10.83
+ },
+ "sand": {
+ "sl1": 43.0,
+ "sl2": 43.0,
+ "sl3": 43.0,
+ "sl4": 41.8,
+ "sl5": 41.57,
+ "sl6": 42.0,
+ "sl7": 42.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 111306,
+ "distance": 0.0,
+ "mapunitID": 17499,
+ "minCompDistance": 0.0,
+ "share": 30,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ",
+ "Description_es": "Los Cambisoles Crómicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos bien drenados, con un color intenso.
Cuando el clima y el paisaje son favorables, pueden ser suelos productivos. ",
+ "Description_fr": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ",
+ "Description_ks": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ",
+ "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ",
+ "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.",
+ "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ",
+ "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. "
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 9.0,
+ "sl2": 9.0,
+ "sl3": 9.0,
+ "sl4": 7.6,
+ "sl5": 7.0,
+ "sl6": 6.4,
+ "sl7": 6.0
+ },
+ "clay": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0,
+ "sl4": 18.0,
+ "sl5": 17.14,
+ "sl6": 16.0,
+ "sl7": 15.67
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.14,
+ "sl6": 1.2,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Dystric regosols",
+ "name": "Dystric regosols",
+ "rank_loc": "4",
+ "score_loc": 0.055
+ },
+ "ph": {
+ "sl1": 5.1,
+ "sl2": 5.1,
+ "sl3": 5.1,
+ "sl4": 5.08,
+ "sl5": 5.13,
+ "sl6": 5.16,
+ "sl7": 5.18
+ },
+ "rock_fragments": {
+ "sl1": 24.0,
+ "sl2": 24.0,
+ "sl3": 24.0,
+ "sl4": 30.6,
+ "sl5": 31.14,
+ "sl6": 35.2,
+ "sl7": 36.67
+ },
+ "sand": {
+ "sl1": 55.0,
+ "sl2": 55.0,
+ "sl3": 55.0,
+ "sl4": 57.6,
+ "sl5": 58.71,
+ "sl6": 60.2,
+ "sl7": 60.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 111300,
+ "distance": 3832.725,
+ "mapunitID": 17496,
+ "minCompDistance": 3832.72465414,
+ "share": 85,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ",
+ "Description_es": "Los Regosoles Dístricos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.
Los Regosoles Dístricos tienen una baja saturación de base en el subsuelo. ",
+ "Description_fr": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ",
+ "Description_ks": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ",
+ "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ",
+ "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo. *Incluso cuando se utilizan para el pastoreo, el riego será necesario debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos. *Con una baja saturación de bases, estos suelos pueden responder a la adición de bases como el potasio, el calcio o el magnesio. ",
+ "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ",
+ "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy loam",
+ "sl5": "Sandy loam",
+ "sl6": "Sandy loam",
+ "sl7": "Sandy loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 7.0,
+ "sl2": 7.0,
+ "sl3": 7.0,
+ "sl4": 6.4,
+ "sl5": 6.29,
+ "sl6": 6.2,
+ "sl7": 6.17
+ },
+ "clay": {
+ "sl1": 23.0,
+ "sl2": 23.0,
+ "sl3": 23.0,
+ "sl4": 28.8,
+ "sl5": 31.14,
+ "sl6": 33.4,
+ "sl7": 34.33
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Haplic acrisols",
+ "name": "Haplic acrisols",
+ "rank_loc": "5",
+ "score_loc": 0.047
+ },
+ "ph": {
+ "sl1": 5.1,
+ "sl2": 5.1,
+ "sl3": 5.1,
+ "sl4": 5.04,
+ "sl5": 5.03,
+ "sl6": 5.02,
+ "sl7": 5.02
+ },
+ "rock_fragments": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 12.4,
+ "sl5": 13.29,
+ "sl6": 13.0,
+ "sl7": 14.0
+ },
+ "sand": {
+ "sl1": 59.0,
+ "sl2": 59.0,
+ "sl3": 59.0,
+ "sl4": 54.4,
+ "sl5": 52.29,
+ "sl6": 50.2,
+ "sl7": 49.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 111239,
+ "distance": 9468.474,
+ "mapunitID": 17466,
+ "minCompDistance": 9468.47413229,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.",
+ "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ",
+ "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.",
+ "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.",
+ "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ",
+ "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ",
+ "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ",
+ "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy clay loam",
+ "sl2": "Sandy clay loam",
+ "sl3": "Sandy clay loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 52.0,
+ "sl2": 52.0,
+ "sl3": 52.0,
+ "sl4": 51.2,
+ "sl5": 50.86,
+ "sl6": 50.0,
+ "sl7": 49.17
+ },
+ "clay": {
+ "sl1": 53.0,
+ "sl2": 53.0,
+ "sl3": 53.0,
+ "sl4": 54.6,
+ "sl5": 55.0,
+ "sl6": 54.2,
+ "sl7": 53.67
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.2,
+ "sl7": 1.5
+ },
+ "id": {
+ "component": "Calcic vertisols",
+ "name": "Calcic vertisols",
+ "rank_loc": "6",
+ "score_loc": 0.04
+ },
+ "ph": {
+ "sl1": 7.5,
+ "sl2": 7.5,
+ "sl3": 7.5,
+ "sl4": 7.7,
+ "sl5": 7.8,
+ "sl6": 7.96,
+ "sl7": 8.05
+ },
+ "rock_fragments": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 6.0,
+ "sl5": 6.0,
+ "sl6": 7.8,
+ "sl7": 7.83
+ },
+ "sand": {
+ "sl1": 21.0,
+ "sl2": 21.0,
+ "sl3": 21.0,
+ "sl4": 20.2,
+ "sl5": 20.14,
+ "sl6": 20.8,
+ "sl7": 21.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 111275,
+ "distance": 337.622,
+ "mapunitID": 17482,
+ "minCompDistance": 337.62221932,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Calcic Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Calcic Vertisols are calcareous in a soil layer below the surface.",
+ "Description_es": "Los Vertisoles Cálcicos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles cálcicos son calcáreos en una capa del suelo por debajo de la superficie. ",
+ "Description_fr": "Calcic Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Calcic Vertisols are calcareous in a soil layer below the surface.",
+ "Description_ks": "Calcic Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Calcic Vertisols are calcareous in a soil layer below the surface.",
+ "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ",
+ "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, sin embargo las características de la arcilla en este suelo pueden hacer que el manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite el laboreo excesivo cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero se necesitará una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que favorezcan el drenaje y la infiltración del agua.",
+ "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ",
+ "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. "
+ }
+ },
+ "texture": {
+ "sl1": "Unknown",
+ "sl2": "Unknown",
+ "sl3": "Unknown",
+ "sl4": "Unknown",
+ "sl5": "Unknown",
+ "sl6": "Unknown",
+ "sl7": "Unknown"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 18.0,
+ "sl2": 18.0,
+ "sl3": 18.0,
+ "sl4": 18.2,
+ "sl5": 18.43,
+ "sl6": 18.4,
+ "sl7": 17.83
+ },
+ "clay": {
+ "sl1": 30.0,
+ "sl2": 30.0,
+ "sl3": 30.0,
+ "sl4": 34.2,
+ "sl5": 35.86,
+ "sl6": 37.2,
+ "sl7": 37.5
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.0,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Chromic luvisols",
+ "name": "Chromic luvisols",
+ "rank_loc": "7",
+ "score_loc": 0.036
+ },
+ "ph": {
+ "sl1": 6.5,
+ "sl2": 6.5,
+ "sl3": 6.5,
+ "sl4": 6.56,
+ "sl5": 6.57,
+ "sl6": 6.58,
+ "sl7": 6.55
+ },
+ "rock_fragments": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 10.6,
+ "sl5": 10.14,
+ "sl6": 9.8,
+ "sl7": 11.33
+ },
+ "sand": {
+ "sl1": 37.0,
+ "sl2": 37.0,
+ "sl3": 37.0,
+ "sl4": 34.4,
+ "sl5": 33.43,
+ "sl6": 32.6,
+ "sl7": 33.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 111210,
+ "distance": 4944.944,
+ "mapunitID": 17454,
+ "minCompDistance": 4944.94414068,
+ "share": 70,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.",
+ "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.",
+ "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops."
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 10.0,
+ "sl2": 10.0,
+ "sl3": 10.0,
+ "sl4": 11.8,
+ "sl5": 12.14,
+ "sl6": 12.2,
+ "sl7": 12.17
+ },
+ "clay": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 24.2,
+ "sl5": 25.43,
+ "sl6": 26.2,
+ "sl7": 26.0
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.0,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Dystric cambisols",
+ "name": "Dystric cambisols",
+ "rank_loc": "8",
+ "score_loc": 0.034
+ },
+ "ph": {
+ "sl1": 6.5,
+ "sl2": 6.5,
+ "sl3": 6.5,
+ "sl4": 6.62,
+ "sl5": 6.66,
+ "sl6": 6.76,
+ "sl7": 6.83
+ },
+ "rock_fragments": {
+ "sl1": 12.0,
+ "sl2": 12.0,
+ "sl3": 12.0,
+ "sl4": 12.0,
+ "sl5": 12.71,
+ "sl6": 16.0,
+ "sl7": 18.0
+ },
+ "sand": {
+ "sl1": 67.0,
+ "sl2": 67.0,
+ "sl3": 67.0,
+ "sl4": 62.6,
+ "sl5": 61.71,
+ "sl6": 61.0,
+ "sl7": 61.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 111211,
+ "distance": 4944.944,
+ "mapunitID": 17454,
+ "minCompDistance": 4944.94414068,
+ "share": 30,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_es": "Los Cambisoles Dístricos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos menos productivos con baja saturación de bases en la parte superior del suelo.",
+ "Description_fr": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_ks": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.",
+ "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ",
+ "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Debido a que este suelo tiene una baja saturación de bases, puede ser necesaria la aplicación de bases (a través de la fertlización) para un rendimiento más productivo del cultivo.
Si el pH del suelo es bajo, el calcio (y posiblemente el magnesio, si se utiliza cal dolomítica) puede ser suministrado a través de la adición de cal.
Si el pH del suelo es adecuado para la producción de cultivos, entonces el yeso (CaSO4) puede ser utilizado como fuente de Ca, si es necesario, u otras fuentes como MgSO4 podrían ser aplicadas (si la prueba del suelo indica una necesidad).
Una fertilización adecuada también aportará potasio, si el análisis del suelo indica que es necesario.",
+ "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ",
+ "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 18.0,
+ "sl2": 18.0,
+ "sl3": 18.0,
+ "sl4": 14.2,
+ "sl5": 13.14,
+ "sl6": 12.2,
+ "sl7": 11.83
+ },
+ "clay": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0,
+ "sl4": 20.4,
+ "sl5": 20.29,
+ "sl6": 20.2,
+ "sl7": 19.83
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 0.4,
+ "sl5": 0.29,
+ "sl6": 0.2,
+ "sl7": 0.17
+ },
+ "id": {
+ "component": "Calcaric cambisols",
+ "name": "Calcaric cambisols",
+ "rank_loc": "9",
+ "score_loc": 0.032
+ },
+ "ph": {
+ "sl1": 5.2,
+ "sl2": 5.2,
+ "sl3": 5.2,
+ "sl4": 5.26,
+ "sl5": 5.27,
+ "sl6": 5.3,
+ "sl7": 5.32
+ },
+ "rock_fragments": {
+ "sl1": 17.0,
+ "sl2": 17.0,
+ "sl3": 17.0,
+ "sl4": 20.0,
+ "sl5": 21.57,
+ "sl6": 23.4,
+ "sl7": 23.83
+ },
+ "sand": {
+ "sl1": 44.0,
+ "sl2": 44.0,
+ "sl3": 44.0,
+ "sl4": 44.0,
+ "sl5": 44.57,
+ "sl6": 45.0,
+ "sl7": 45.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 111282,
+ "distance": 9861.436,
+ "mapunitID": 17486,
+ "minCompDistance": 9861.43578287,
+ "share": 85,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.",
+ "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.",
+ "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.",
+ "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.",
+ "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ",
+ "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.",
+ "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ",
+ "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 17.0,
+ "sl5": 16.29,
+ "sl6": 15.6,
+ "sl7": 15.33
+ },
+ "clay": {
+ "sl1": 29.0,
+ "sl2": 29.0,
+ "sl3": 29.0,
+ "sl4": 29.8,
+ "sl5": 30.14,
+ "sl6": 30.0,
+ "sl7": 29.67
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 0.86,
+ "sl6": 0.6,
+ "sl7": 0.5
+ },
+ "id": {
+ "component": "Calcaric fluvisols",
+ "name": "Calcaric fluvisols",
+ "rank_loc": "10",
+ "score_loc": 0.028
+ },
+ "ph": {
+ "sl1": 5.0,
+ "sl2": 5.0,
+ "sl3": 5.0,
+ "sl4": 5.02,
+ "sl5": 5.06,
+ "sl6": 5.12,
+ "sl7": 5.13
+ },
+ "rock_fragments": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 14.4,
+ "sl5": 14.43,
+ "sl6": 15.2,
+ "sl7": 16.67
+ },
+ "sand": {
+ "sl1": 42.0,
+ "sl2": 42.0,
+ "sl3": 42.0,
+ "sl4": 42.6,
+ "sl5": 42.57,
+ "sl6": 42.6,
+ "sl7": 43.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 111096,
+ "distance": 14199.569,
+ "mapunitID": 17389,
+ "minCompDistance": 14199.56875094,
+ "share": 75,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.",
+ "Description_es": "Los Fluvisoles Calcáricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles calcáricos tienen carbonatos y un pH elevado en la parte superior del suelo.",
+ "Description_fr": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.",
+ "Description_ks": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.",
+ "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o el manejo de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Una vez en cultivo continuo se debe tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una vía para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).",
+ "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered."
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 39.0,
+ "sl2": 39.0,
+ "sl3": 39.0,
+ "sl4": 37.4,
+ "sl5": 36.0,
+ "sl6": 33.2,
+ "sl7": 32.0
+ },
+ "clay": {
+ "sl1": 43.0,
+ "sl2": 43.0,
+ "sl3": 43.0,
+ "sl4": 42.4,
+ "sl5": 40.14,
+ "sl6": 36.4,
+ "sl7": 34.33
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 0.86,
+ "sl6": 0.6,
+ "sl7": 0.67
+ },
+ "id": {
+ "component": "Calcic solonchaks",
+ "name": "Calcic solonchaks",
+ "rank_loc": "11",
+ "score_loc": 0.019
+ },
+ "ph": {
+ "sl1": 7.6,
+ "sl2": 7.6,
+ "sl3": 7.6,
+ "sl4": 7.76,
+ "sl5": 7.83,
+ "sl6": 7.94,
+ "sl7": 8.02
+ },
+ "rock_fragments": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 21.8,
+ "sl5": 24.0,
+ "sl6": 22.8,
+ "sl7": 22.83
+ },
+ "sand": {
+ "sl1": 30.0,
+ "sl2": 30.0,
+ "sl3": 30.0,
+ "sl4": 29.4,
+ "sl5": 30.43,
+ "sl6": 32.4,
+ "sl7": 33.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 111008,
+ "distance": 4355.807,
+ "mapunitID": 17338,
+ "minCompDistance": 4355.80730857,
+ "share": 50,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Calcic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
Calcic Solonchaks are calcareous in a soil layer below the surface.",
+ "Description_es": "Los Solonchaks Cálcicos son suelos que contienen sales en la superficie del suelo o cerca de ella y que se forman en los desiertos o cerca de las costas.
Los Solonchaks cálcicos son calcáreos en una capa del suelo por debajo de la superficie.",
+ "Description_fr": "Calcic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
Calcic Solonchaks are calcareous in a soil layer below the surface.",
+ "Description_ks": "Calcic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
Calcic Solonchaks are calcareous in a soil layer below the surface.",
+ "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.
The soil pH in the upper soil layer will be high (> 7.0) ",
+ "Management_es": "Estos suelos son típicamente altos en sales totales.
Tienen una productividad muy pobre, y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.
El pH del suelo en la capa superior será alto (> 7,0).",
+ "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.
The soil pH in the upper soil layer will be high (> 7.0) ",
+ "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.
The soil pH in the upper soil layer will be high (> 7.0) "
+ }
+ },
+ "texture": {
+ "sl1": "Unknown",
+ "sl2": "Unknown",
+ "sl3": "Unknown",
+ "sl4": "Unknown",
+ "sl5": "Unknown",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 16.4,
+ "sl5": 16.14,
+ "sl6": 16.0,
+ "sl7": 15.83
+ },
+ "clay": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0,
+ "sl4": 20.0,
+ "sl5": 20.0,
+ "sl6": 20.2,
+ "sl7": 20.17
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 1.4,
+ "sl5": 1.43,
+ "sl6": 1.6,
+ "sl7": 1.67
+ },
+ "id": {
+ "component": "Eutric fluvisols",
+ "name": "Eutric fluvisols",
+ "rank_loc": "12",
+ "score_loc": 0.015
+ },
+ "ph": {
+ "sl1": 8.2,
+ "sl2": 8.2,
+ "sl3": 8.2,
+ "sl4": 8.2,
+ "sl5": 8.2,
+ "sl6": 8.2,
+ "sl7": 8.2
+ },
+ "rock_fragments": {
+ "sl1": 3.0,
+ "sl2": 3.0,
+ "sl3": 3.0,
+ "sl4": 4.2,
+ "sl5": 5.0,
+ "sl6": 5.2,
+ "sl7": 5.33
+ },
+ "sand": {
+ "sl1": 40.0,
+ "sl2": 40.0,
+ "sl3": 40.0,
+ "sl4": 39.6,
+ "sl5": 39.86,
+ "sl6": 39.8,
+ "sl7": 39.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 111317,
+ "distance": 29220.538,
+ "mapunitID": 17506,
+ "minCompDistance": 29220.53821141,
+ "share": 40,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ",
+ "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).",
+ "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered."
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 13.4,
+ "sl5": 13.29,
+ "sl6": 13.0,
+ "sl7": 12.67
+ },
+ "clay": {
+ "sl1": 27.0,
+ "sl2": 27.0,
+ "sl3": 27.0,
+ "sl4": 28.4,
+ "sl5": 28.86,
+ "sl6": 28.6,
+ "sl7": 27.83
+ },
+ "ec": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 15.2,
+ "sl5": 16.14,
+ "sl6": 16.8,
+ "sl7": 16.67
+ },
+ "id": {
+ "component": "Chromic luvisols",
+ "name": "Chromic luvisols2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.036
+ },
+ "ph": {
+ "sl1": 8.3,
+ "sl2": 8.3,
+ "sl3": 8.3,
+ "sl4": 8.36,
+ "sl5": 8.37,
+ "sl6": 8.38,
+ "sl7": 8.38
+ },
+ "rock_fragments": {
+ "sl1": 17.0,
+ "sl2": 17.0,
+ "sl3": 17.0,
+ "sl4": 18.0,
+ "sl5": 21.29,
+ "sl6": 26.4,
+ "sl7": 28.17
+ },
+ "sand": {
+ "sl1": 41.0,
+ "sl2": 41.0,
+ "sl3": 41.0,
+ "sl4": 40.0,
+ "sl5": 40.0,
+ "sl6": 40.4,
+ "sl7": 41.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 111097,
+ "distance": 14199.569,
+ "mapunitID": 17389,
+ "minCompDistance": 4944.94414068,
+ "share": 25,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.",
+ "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.",
+ "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops."
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 18.4,
+ "sl5": 18.14,
+ "sl6": 17.6,
+ "sl7": 17.5
+ },
+ "clay": {
+ "sl1": 31.0,
+ "sl2": 31.0,
+ "sl3": 31.0,
+ "sl4": 32.2,
+ "sl5": 32.14,
+ "sl6": 31.6,
+ "sl7": 31.33
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 1.4,
+ "sl5": 1.43,
+ "sl6": 1.6,
+ "sl7": 1.67
+ },
+ "id": {
+ "component": "Dystric cambisols",
+ "name": "Dystric cambisols2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.034
+ },
+ "ph": {
+ "sl1": 6.1,
+ "sl2": 6.1,
+ "sl3": 6.1,
+ "sl4": 6.24,
+ "sl5": 6.3,
+ "sl6": 6.38,
+ "sl7": 6.43
+ },
+ "rock_fragments": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 11.6,
+ "sl5": 9.86,
+ "sl6": 10.2,
+ "sl7": 10.33
+ },
+ "sand": {
+ "sl1": 37.0,
+ "sl2": 37.0,
+ "sl3": 37.0,
+ "sl4": 36.2,
+ "sl5": 36.86,
+ "sl6": 38.4,
+ "sl7": 38.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 111624,
+ "distance": 18090.354,
+ "mapunitID": 17691,
+ "minCompDistance": 4944.94414068,
+ "share": 60,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_es": "Los Cambisoles Dístricos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos menos productivos con baja saturación de bases en la parte superior del suelo.",
+ "Description_fr": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_ks": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.",
+ "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ",
+ "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Debido a que este suelo tiene una baja saturación de bases, puede ser necesaria la aplicación de bases (a través de la fertlización) para un rendimiento más productivo del cultivo.
Si el pH del suelo es bajo, el calcio (y posiblemente el magnesio, si se utiliza cal dolomítica) puede ser suministrado a través de la adición de cal.
Si el pH del suelo es adecuado para la producción de cultivos, entonces el yeso (CaSO4) puede ser utilizado como fuente de Ca, si es necesario, u otras fuentes como MgSO4 podrían ser aplicadas (si la prueba del suelo indica una necesidad).
Una fertilización adecuada también aportará potasio, si el análisis del suelo indica que es necesario.",
+ "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ",
+ "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. "
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "global",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Ferralic arenosols",
+ "componentData": "Data Complete",
+ "componentID": 111274,
+ "name": "Ferralic arenosols",
+ "rank_data": "7",
+ "rank_data_loc": "1",
+ "rank_loc": "1",
+ "score_data": 0.649,
+ "score_data_loc": 1.0,
+ "score_loc": 0.107
+ },
+ {
+ "component": "Dystric regosols",
+ "componentData": "Data Complete",
+ "componentID": 111300,
+ "name": "Dystric regosols",
+ "rank_data": "1",
+ "rank_data_loc": "2",
+ "rank_loc": "4",
+ "score_data": 0.691,
+ "score_data_loc": 0.987,
+ "score_loc": 0.055
+ },
+ {
+ "component": "Haplic acrisols",
+ "componentData": "Data Complete",
+ "componentID": 111239,
+ "name": "Haplic acrisols",
+ "rank_data": "3",
+ "rank_data_loc": "3",
+ "rank_loc": "5",
+ "score_data": 0.683,
+ "score_data_loc": 0.966,
+ "score_loc": 0.047
+ },
+ {
+ "component": "Chromic cambisols",
+ "componentData": "Data Complete",
+ "componentID": 111306,
+ "name": "Chromic cambisols",
+ "rank_data": "6",
+ "rank_data_loc": "4",
+ "rank_loc": "3",
+ "score_data": 0.653,
+ "score_data_loc": 0.956,
+ "score_loc": 0.07
+ },
+ {
+ "component": "Eutric fluvisols",
+ "componentData": "Data Complete",
+ "componentID": 111317,
+ "name": "Eutric fluvisols",
+ "rank_data": "2",
+ "rank_data_loc": "5",
+ "rank_loc": "12",
+ "score_data": 0.691,
+ "score_data_loc": 0.935,
+ "score_loc": 0.015
+ },
+ {
+ "component": "Calcaric cambisols",
+ "componentData": "Missing Data",
+ "componentID": 111282,
+ "name": "Calcaric cambisols",
+ "rank_data": "4",
+ "rank_data_loc": "6",
+ "rank_loc": "9",
+ "score_data": 0.666,
+ "score_data_loc": 0.924,
+ "score_loc": 0.032
+ },
+ {
+ "component": "Calcic solonchaks",
+ "componentData": "Data Complete",
+ "componentID": 111008,
+ "name": "Calcic solonchaks",
+ "rank_data": "5",
+ "rank_data_loc": "7",
+ "rank_loc": "11",
+ "score_data": 0.666,
+ "score_data_loc": 0.906,
+ "score_loc": 0.019
+ },
+ {
+ "component": "Eutric vertisols",
+ "componentData": "No Data",
+ "componentID": 111333,
+ "name": "Eutric vertisols",
+ "rank_data": "10",
+ "rank_data_loc": "8",
+ "rank_loc": "2",
+ "score_data": 0.58,
+ "score_data_loc": 0.869,
+ "score_loc": 0.077
+ },
+ {
+ "component": "Dystric cambisols",
+ "componentData": "Data Complete",
+ "componentID": 111624,
+ "name": "Dystric cambisols2",
+ "rank_data": "8",
+ "rank_data_loc": "9",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.617,
+ "score_data_loc": 0.861,
+ "score_loc": 0.034
+ },
+ {
+ "component": "Calcic vertisols",
+ "componentData": "No Data",
+ "componentID": 111275,
+ "name": "Calcic vertisols",
+ "rank_data": "9",
+ "rank_data_loc": "10",
+ "rank_loc": "6",
+ "score_data": 0.602,
+ "score_data_loc": 0.85,
+ "score_loc": 0.04
+ },
+ {
+ "component": "Chromic luvisols",
+ "componentData": "Missing Data",
+ "componentID": 111210,
+ "name": "Chromic luvisols",
+ "rank_data": "11",
+ "rank_data_loc": "11",
+ "rank_loc": "7",
+ "score_data": 0.492,
+ "score_data_loc": 0.698,
+ "score_loc": 0.036
+ },
+ {
+ "component": "Calcaric fluvisols",
+ "componentData": "Data Complete",
+ "componentID": 111096,
+ "name": "Calcaric fluvisols",
+ "rank_data": "12",
+ "rank_data_loc": "12",
+ "rank_loc": "10",
+ "score_data": 0.326,
+ "score_data_loc": 0.469,
+ "score_loc": 0.028
+ },
+ {
+ "component": "Dystric cambisols",
+ "componentData": "Data Complete",
+ "componentID": 111211,
+ "name": "Dystric cambisols",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "8",
+ "score_data": 0.58,
+ "score_data_loc": 0.812,
+ "score_loc": 0.034
+ },
+ {
+ "component": "Chromic luvisols",
+ "componentData": "Data Complete",
+ "componentID": 111097,
+ "name": "Chromic luvisols2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.123,
+ "score_data_loc": 0.21,
+ "score_loc": 0.036
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-24.53333,33.36667].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-24.53333,33.36667].json
new file mode 100644
index 0000000..a72828e
--- /dev/null
+++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-24.53333,33.36667].json
@@ -0,0 +1,1371 @@
+{
+ "list": {
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 13.2,
+ "sl5": 12.71,
+ "sl6": 12.4,
+ "sl7": 12.5
+ },
+ "clay": {
+ "sl1": 26.0,
+ "sl2": 26.0,
+ "sl3": 26.0,
+ "sl4": 26.2,
+ "sl5": 25.57,
+ "sl6": 25.2,
+ "sl7": 25.0
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 1.4,
+ "sl5": 1.43,
+ "sl6": 1.6,
+ "sl7": 1.67
+ },
+ "id": {
+ "component": "Salic fluvisols",
+ "name": "Salic fluvisols",
+ "rank_loc": "1",
+ "score_loc": 0.182
+ },
+ "ph": {
+ "sl1": 8.4,
+ "sl2": 8.4,
+ "sl3": 8.4,
+ "sl4": 8.4,
+ "sl5": 8.41,
+ "sl6": 8.44,
+ "sl7": 8.45
+ },
+ "rock_fragments": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 6.0,
+ "sl5": 7.71,
+ "sl6": 10.4,
+ "sl7": 10.67
+ },
+ "sand": {
+ "sl1": 39.0,
+ "sl2": 39.0,
+ "sl3": 39.0,
+ "sl4": 39.4,
+ "sl5": 40.43,
+ "sl6": 41.0,
+ "sl7": 41.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 113476,
+ "distance": 0.5,
+ "mapunitID": 18586,
+ "minCompDistance": 0.50040511,
+ "share": 50,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Salic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Salic Fluvisols have high salinity in the upper portion of soil.",
+ "Description_es": "Los Fluvisoles Sálicos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles salinos tienen una alta salinidad en la parte superior del suelo.",
+ "Description_fr": "Salic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Salic Fluvisols have high salinity in the upper portion of soil.",
+ "Description_ks": "Salic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Salic Fluvisols have high salinity in the upper portion of soil.",
+ "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
Leaching with a high quality (low salinity) water source will be needed to move salts out of the rooting zone.
Use of salt tolerant crops and varieties is also recommended.
Last, management of fertilization programs to avoid overapplication and accumulation of salts is needed. ",
+ "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una vía para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).
La lixiviación con una fuente de agua de alta calidad (baja salinidad) será necesaria para desplazar las sales fuera de la zona de enraizamiento.
También se recomienda el uso de cultivos y variedades tolerantes a la sal.
Por último, es necesario gestionar los programas de fertilización para evitar la sobreaplicación y la acumulación de sales.",
+ "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
Leaching with a high quality (low salinity) water source will be needed to move salts out of the rooting zone.
Use of salt tolerant crops and varieties is also recommended.
Last, management of fertilization programs to avoid overapplication and accumulation of salts is needed. ",
+ "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
Leaching with a high quality (low salinity) water source will be needed to move salts out of the rooting zone.
Use of salt tolerant crops and varieties is also recommended.
Last, management of fertilization programs to avoid overapplication and accumulation of salts is needed. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 4.0,
+ "sl5": 4.0,
+ "sl6": 4.0,
+ "sl7": 4.0
+ },
+ "clay": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 5.8,
+ "sl5": 5.57,
+ "sl6": 5.4,
+ "sl7": 5.33
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Cambic arenosols",
+ "name": "Cambic arenosols",
+ "rank_loc": "2",
+ "score_loc": 0.178
+ },
+ "ph": {
+ "sl1": 6.9,
+ "sl2": 6.9,
+ "sl3": 6.9,
+ "sl4": 6.82,
+ "sl5": 6.8,
+ "sl6": 6.8,
+ "sl7": 6.82
+ },
+ "rock_fragments": {
+ "sl1": 7.0,
+ "sl2": 7.0,
+ "sl3": 7.0,
+ "sl4": 14.4,
+ "sl5": 16.57,
+ "sl6": 21.2,
+ "sl7": 20.67
+ },
+ "sand": {
+ "sl1": 89.0,
+ "sl2": 89.0,
+ "sl3": 89.0,
+ "sl4": 89.2,
+ "sl5": 89.29,
+ "sl6": 89.2,
+ "sl7": 89.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 113052,
+ "distance": 0.0,
+ "mapunitID": 18428,
+ "minCompDistance": 0.0,
+ "share": 30,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.",
+ "Description_es": "Los Arenosoles Cámbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles cámbicos tienen un horizonte del subsuelo mínimamente desarrollado que puede retener cantidades ligeramente superiores de nutrientes y agua.",
+ "Description_fr": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.",
+ "Description_ks": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.",
+ "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ",
+ "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.",
+ "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ",
+ "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. "
+ }
+ },
+ "texture": {
+ "sl1": "Sand",
+ "sl2": "Sand",
+ "sl3": "Sand",
+ "sl4": "Sand",
+ "sl5": "Sand",
+ "sl6": "Sand",
+ "sl7": "Sand"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 5.0,
+ "sl2": 5.0,
+ "sl3": 5.0,
+ "sl4": 3.8,
+ "sl5": 3.57,
+ "sl6": 3.8,
+ "sl7": 3.5
+ },
+ "clay": {
+ "sl1": 7.0,
+ "sl2": 7.0,
+ "sl3": 7.0,
+ "sl4": 7.0,
+ "sl5": 7.14,
+ "sl6": 7.6,
+ "sl7": 7.17
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Eutric fluvisols",
+ "name": "Eutric fluvisols",
+ "rank_loc": "3",
+ "score_loc": 0.127
+ },
+ "ph": {
+ "sl1": 6.4,
+ "sl2": 6.4,
+ "sl3": 6.4,
+ "sl4": 6.42,
+ "sl5": 6.46,
+ "sl6": 6.54,
+ "sl7": 6.55
+ },
+ "rock_fragments": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 2.4,
+ "sl5": 2.86,
+ "sl6": 2.8,
+ "sl7": 5.33
+ },
+ "sand": {
+ "sl1": 87.0,
+ "sl2": 87.0,
+ "sl3": 87.0,
+ "sl4": 86.8,
+ "sl5": 86.29,
+ "sl6": 85.2,
+ "sl7": 86.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 113479,
+ "distance": 0.5,
+ "mapunitID": 18586,
+ "minCompDistance": 0.50040511,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ",
+ "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).",
+ "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered."
+ }
+ },
+ "texture": {
+ "sl1": "Loamy sand",
+ "sl2": "Loamy sand",
+ "sl3": "Loamy sand",
+ "sl4": "Loamy sand",
+ "sl5": "Loamy sand",
+ "sl6": "Loamy sand",
+ "sl7": "Loamy sand"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 17.0,
+ "sl2": 17.0,
+ "sl3": 17.0,
+ "sl4": 19.2,
+ "sl5": 19.29,
+ "sl6": 19.0,
+ "sl7": 18.67
+ },
+ "clay": {
+ "sl1": 21.0,
+ "sl2": 21.0,
+ "sl3": 21.0,
+ "sl4": 26.0,
+ "sl5": 26.29,
+ "sl6": 25.6,
+ "sl7": 24.67
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.8,
+ "sl5": 2.57,
+ "sl6": 3.8,
+ "sl7": 3.83
+ },
+ "id": {
+ "component": "Haplic solonetz",
+ "name": "Haplic solonetz",
+ "rank_loc": "4",
+ "score_loc": 0.127
+ },
+ "ph": {
+ "sl1": 8.3,
+ "sl2": 8.3,
+ "sl3": 8.3,
+ "sl4": 8.56,
+ "sl5": 8.63,
+ "sl6": 8.66,
+ "sl7": 8.65
+ },
+ "rock_fragments": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 5.0,
+ "sl5": 5.29,
+ "sl6": 7.4,
+ "sl7": 9.0
+ },
+ "sand": {
+ "sl1": 49.0,
+ "sl2": 49.0,
+ "sl3": 49.0,
+ "sl4": 44.6,
+ "sl5": 44.57,
+ "sl6": 45.4,
+ "sl7": 46.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 113051,
+ "distance": 0.0,
+ "mapunitID": 18428,
+ "minCompDistance": 0.0,
+ "share": 35,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.",
+ "Description_es": "Los Solonetz Háplicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.",
+ "Description_fr": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.",
+ "Description_ks": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.",
+ "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ",
+ "Management_es": "Es probable que tengan un alto nivel de sodio en los horizontes subsuperficiales, lo que da lugar a una mala estructura del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Para mejorar el drenaje interno, debe aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.",
+ "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ",
+ "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 18.4,
+ "sl5": 18.14,
+ "sl6": 17.6,
+ "sl7": 17.5
+ },
+ "clay": {
+ "sl1": 31.0,
+ "sl2": 31.0,
+ "sl3": 31.0,
+ "sl4": 32.2,
+ "sl5": 32.14,
+ "sl6": 31.6,
+ "sl7": 31.33
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 1.4,
+ "sl5": 1.43,
+ "sl6": 1.6,
+ "sl7": 1.67
+ },
+ "id": {
+ "component": "Mollic fluvisols",
+ "name": "Mollic fluvisols",
+ "rank_loc": "5",
+ "score_loc": 0.109
+ },
+ "ph": {
+ "sl1": 6.1,
+ "sl2": 6.1,
+ "sl3": 6.1,
+ "sl4": 6.24,
+ "sl5": 6.3,
+ "sl6": 6.38,
+ "sl7": 6.43
+ },
+ "rock_fragments": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 11.6,
+ "sl5": 9.86,
+ "sl6": 10.2,
+ "sl7": 10.33
+ },
+ "sand": {
+ "sl1": 37.0,
+ "sl2": 37.0,
+ "sl3": 37.0,
+ "sl4": 36.2,
+ "sl5": 36.86,
+ "sl6": 38.4,
+ "sl7": 38.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 113477,
+ "distance": 0.5,
+ "mapunitID": 18586,
+ "minCompDistance": 0.50040511,
+ "share": 30,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Mollic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Mollic Fluvisols have relatively higher organic matter and nutrients in surface horizons.",
+ "Description_es": "Los Fluvisoles Mólicos se encuentran principalmente en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles móllicos tienen una materia orgánica y nutrientes relativamente altos en los horizontes superficiales.",
+ "Description_fr": "Mollic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Mollic Fluvisols have relatively higher organic matter and nutrients in surface horizons.",
+ "Description_ks": "Mollic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Mollic Fluvisols have relatively higher organic matter and nutrients in surface horizons.",
+ "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).",
+ "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered."
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 13.6,
+ "sl5": 13.57,
+ "sl6": 13.0,
+ "sl7": 13.17
+ },
+ "clay": {
+ "sl1": 18.0,
+ "sl2": 18.0,
+ "sl3": 18.0,
+ "sl4": 18.8,
+ "sl5": 18.86,
+ "sl6": 18.8,
+ "sl7": 18.83
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 1.4,
+ "sl5": 1.43,
+ "sl6": 1.6,
+ "sl7": 1.67
+ },
+ "id": {
+ "component": "Ferralic arenosols",
+ "name": "Ferralic arenosols",
+ "rank_loc": "6",
+ "score_loc": 0.1
+ },
+ "ph": {
+ "sl1": 7.5,
+ "sl2": 7.5,
+ "sl3": 7.5,
+ "sl4": 7.62,
+ "sl5": 7.66,
+ "sl6": 7.68,
+ "sl7": 7.7
+ },
+ "rock_fragments": {
+ "sl1": 3.0,
+ "sl2": 3.0,
+ "sl3": 3.0,
+ "sl4": 2.4,
+ "sl5": 2.57,
+ "sl6": 4.4,
+ "sl7": 5.5
+ },
+ "sand": {
+ "sl1": 55.0,
+ "sl2": 55.0,
+ "sl3": 55.0,
+ "sl4": 54.2,
+ "sl5": 54.14,
+ "sl6": 54.6,
+ "sl7": 55.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 112871,
+ "distance": 14598.857,
+ "mapunitID": 18373,
+ "minCompDistance": 14598.85741844,
+ "share": 85,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.",
+ "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.",
+ "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.",
+ "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.",
+ "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ",
+ "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.",
+ "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ",
+ "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy loam",
+ "sl5": "Sandy loam",
+ "sl6": "Sandy loam",
+ "sl7": "Sandy loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 23.0,
+ "sl2": 23.0,
+ "sl3": 23.0,
+ "sl4": 21.4,
+ "sl5": 21.0,
+ "sl6": 20.2,
+ "sl7": 18.67
+ },
+ "clay": {
+ "sl1": 32.0,
+ "sl2": 32.0,
+ "sl3": 32.0,
+ "sl4": 33.4,
+ "sl5": 32.86,
+ "sl6": 31.4,
+ "sl7": 29.83
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 1.4,
+ "sl5": 1.43,
+ "sl6": 1.6,
+ "sl7": 1.67
+ },
+ "id": {
+ "component": "Eutric planosols",
+ "name": "Eutric planosols",
+ "rank_loc": "7",
+ "score_loc": 0.073
+ },
+ "ph": {
+ "sl1": 6.5,
+ "sl2": 6.5,
+ "sl3": 6.5,
+ "sl4": 6.52,
+ "sl5": 6.56,
+ "sl6": 6.62,
+ "sl7": 6.7
+ },
+ "rock_fragments": {
+ "sl1": 18.0,
+ "sl2": 18.0,
+ "sl3": 18.0,
+ "sl4": 17.6,
+ "sl5": 16.43,
+ "sl6": 17.4,
+ "sl7": 18.0
+ },
+ "sand": {
+ "sl1": 39.0,
+ "sl2": 39.0,
+ "sl3": 39.0,
+ "sl4": 40.0,
+ "sl5": 41.29,
+ "sl6": 43.8,
+ "sl7": 45.33
+ },
+ "site": {
+ "siteData": {
+ "componentID": 113053,
+ "distance": 0.0,
+ "mapunitID": 18428,
+ "minCompDistance": 0.0,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.",
+ "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.",
+ "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.",
+ "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.",
+ "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.",
+ "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.",
+ "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.",
+ "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization."
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 3.0,
+ "sl2": 3.0,
+ "sl3": 3.0,
+ "sl4": 2.4,
+ "sl5": 2.29,
+ "sl6": 2.2,
+ "sl7": 2.0
+ },
+ "clay": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 6.2,
+ "sl5": 6.43,
+ "sl6": 6.8,
+ "sl7": 7.0
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Gleyic solonetz",
+ "name": "Gleyic solonetz",
+ "rank_loc": "8",
+ "score_loc": 0.055
+ },
+ "ph": {
+ "sl1": 5.3,
+ "sl2": 5.3,
+ "sl3": 5.3,
+ "sl4": 5.32,
+ "sl5": 5.34,
+ "sl6": 5.36,
+ "sl7": 5.37
+ },
+ "rock_fragments": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 4.2,
+ "sl5": 4.43,
+ "sl6": 4.6,
+ "sl7": 4.5
+ },
+ "sand": {
+ "sl1": 87.0,
+ "sl2": 87.0,
+ "sl3": 87.0,
+ "sl4": 86.8,
+ "sl5": 86.57,
+ "sl6": 86.2,
+ "sl7": 86.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 113054,
+ "distance": 0.0,
+ "mapunitID": 18428,
+ "minCompDistance": 0.0,
+ "share": 15,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Gleyic Solonetz have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.
Gleyic Solonetz are saturated with shallow groundwater within one meter of the soil surface.",
+ "Description_es": "Los Solonetz Gléyicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.
Los Solonetz gleyicos están saturados de aguas subterráneas poco profundas a menos de un metro de la superficie del suelo.",
+ "Description_fr": "Gleyic Solonetz have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.
Gleyic Solonetz are saturated with shallow groundwater within one meter of the soil surface.",
+ "Description_ks": "Gleyic Solonetz have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.
Gleyic Solonetz are saturated with shallow groundwater within one meter of the soil surface.",
+ "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
Drainage of these soils will be needed, both to eliminate standing water and remediate sodicity issues.
To further improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ",
+ "Management_es": "Es probable que tengan un alto contenido de sodio en los horizontes subsuperficiales, lo que da lugar a una estructura deficiente del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Será necesario drenar estos suelos, tanto para eliminar el agua estancada como para remediar los problemas de sodicidad.
Para mejorar aún más el drenaje interno, debería aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.",
+ "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
Drainage of these soils will be needed, both to eliminate standing water and remediate sodicity issues.
To further improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ",
+ "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
Drainage of these soils will be needed, both to eliminate standing water and remediate sodicity issues.
To further improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. "
+ }
+ },
+ "texture": {
+ "sl1": "Loamy sand",
+ "sl2": "Loamy sand",
+ "sl3": "Loamy sand",
+ "sl4": "Loamy sand",
+ "sl5": "Loamy sand",
+ "sl6": "Loamy sand",
+ "sl7": "Loamy sand"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 8.8,
+ "sl5": 10.0,
+ "sl6": 10.8,
+ "sl7": 11.33
+ },
+ "clay": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 18.4,
+ "sl5": 20.86,
+ "sl6": 22.2,
+ "sl7": 22.83
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.2,
+ "sl7": 1.33
+ },
+ "id": {
+ "component": "Umbric gleysols",
+ "name": "Umbric gleysols",
+ "rank_loc": "9",
+ "score_loc": 0.036
+ },
+ "ph": {
+ "sl1": 6.2,
+ "sl2": 6.2,
+ "sl3": 6.2,
+ "sl4": 6.36,
+ "sl5": 6.46,
+ "sl6": 6.64,
+ "sl7": 6.73
+ },
+ "rock_fragments": {
+ "sl1": 21.0,
+ "sl2": 21.0,
+ "sl3": 21.0,
+ "sl4": 13.6,
+ "sl5": 11.29,
+ "sl6": 9.6,
+ "sl7": 8.83
+ },
+ "sand": {
+ "sl1": 80.0,
+ "sl2": 80.0,
+ "sl3": 80.0,
+ "sl4": 72.0,
+ "sl5": 70.0,
+ "sl6": 69.0,
+ "sl7": 68.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 113478,
+ "distance": 0.5,
+ "mapunitID": 18586,
+ "minCompDistance": 0.50040511,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.",
+ "Description_es": "Los Gleysoles Úmbricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles úmbricos tienen una materia orgánica relativamente alta, pero menos nutrientes en los horizontes superficiales. ",
+ "Description_fr": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.",
+ "Description_ks": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.",
+ "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. ",
+ "Management_es": "Estos suelos están saturados y, si se cultivan, se requiere un drenaje importante.
Una vez drenados, estos suelos pueden ser muy productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.
El pH superficial del suelo es bajo en estos suelos, y es probable que sea necesario el encalado.",
+ "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. ",
+ "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. "
+ }
+ },
+ "texture": {
+ "sl1": "Loamy sand",
+ "sl2": "Loamy sand",
+ "sl3": "Loamy sand",
+ "sl4": "Sandy loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 16.0,
+ "sl5": 16.14,
+ "sl6": 16.6,
+ "sl7": 17.0
+ },
+ "clay": {
+ "sl1": 26.0,
+ "sl2": 26.0,
+ "sl3": 26.0,
+ "sl4": 29.2,
+ "sl5": 30.14,
+ "sl6": 30.8,
+ "sl7": 31.33
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 3.2,
+ "sl5": 3.86,
+ "sl6": 5.0,
+ "sl7": 5.17
+ },
+ "id": {
+ "component": "Gleyic arenosols",
+ "name": "Gleyic arenosols",
+ "rank_loc": "10",
+ "score_loc": 0.013
+ },
+ "ph": {
+ "sl1": 7.9,
+ "sl2": 7.9,
+ "sl3": 7.9,
+ "sl4": 8.26,
+ "sl5": 8.41,
+ "sl6": 8.6,
+ "sl7": 8.7
+ },
+ "rock_fragments": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 4.0,
+ "sl5": 4.0,
+ "sl6": 4.2,
+ "sl7": 4.5
+ },
+ "sand": {
+ "sl1": 42.0,
+ "sl2": 42.0,
+ "sl3": 42.0,
+ "sl4": 38.4,
+ "sl5": 37.14,
+ "sl6": 35.6,
+ "sl7": 35.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 112872,
+ "distance": 14598.857,
+ "mapunitID": 18373,
+ "minCompDistance": 14598.85741844,
+ "share": 15,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.",
+ "Description_es": "Los Arenosoles Gleyicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos están saturados con aguas subterráneas poco profundas por encima de un metro.",
+ "Description_fr": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.",
+ "Description_ks": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.",
+ "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ",
+ "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación por aguas subterráneas puede no ser posible la instalación de líneas de drenaje, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
En estos suelos se puede conseguir un uso más eficiente del N por parte de los cultivos mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).",
+ "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ",
+ "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 28.0,
+ "sl2": 28.0,
+ "sl3": 28.0,
+ "sl4": 26.2,
+ "sl5": 24.71,
+ "sl6": 23.0,
+ "sl7": 21.5
+ },
+ "clay": {
+ "sl1": 46.0,
+ "sl2": 46.0,
+ "sl3": 46.0,
+ "sl4": 49.0,
+ "sl5": 48.43,
+ "sl6": 46.8,
+ "sl7": 46.33
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 0.8,
+ "sl5": 0.57,
+ "sl6": 0.4,
+ "sl7": 0.33
+ },
+ "id": {
+ "component": "Cambic arenosols",
+ "name": "Cambic arenosols2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.178
+ },
+ "ph": {
+ "sl1": 5.0,
+ "sl2": 5.0,
+ "sl3": 5.0,
+ "sl4": 4.9,
+ "sl5": 4.91,
+ "sl6": 4.9,
+ "sl7": 4.9
+ },
+ "rock_fragments": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 10.0,
+ "sl5": 11.43,
+ "sl6": 13.4,
+ "sl7": 14.33
+ },
+ "sand": {
+ "sl1": 25.0,
+ "sl2": 25.0,
+ "sl3": 25.0,
+ "sl4": 25.0,
+ "sl5": 26.14,
+ "sl6": 27.6,
+ "sl7": 27.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 113348,
+ "distance": 26104.038,
+ "mapunitID": 18542,
+ "minCompDistance": 0.0,
+ "share": 75,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.",
+ "Description_es": "Los Arenosoles Cámbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles cámbicos tienen un horizonte del subsuelo mínimamente desarrollado que puede retener cantidades ligeramente superiores de nutrientes y agua.",
+ "Description_fr": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.",
+ "Description_ks": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.",
+ "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ",
+ "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.",
+ "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ",
+ "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. "
+ }
+ },
+ "texture": {
+ "sl1": "Unknown",
+ "sl2": "Unknown",
+ "sl3": "Unknown",
+ "sl4": "Unknown",
+ "sl5": "Unknown",
+ "sl6": "Unknown",
+ "sl7": "Unknown"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 3.2,
+ "sl5": 2.86,
+ "sl6": 2.6,
+ "sl7": 2.5
+ },
+ "clay": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 5.6,
+ "sl5": 5.71,
+ "sl6": 6.0,
+ "sl7": 6.67
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Eutric fluvisols",
+ "name": "Eutric fluvisols2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.127
+ },
+ "ph": {
+ "sl1": 5.7,
+ "sl2": 5.7,
+ "sl3": 5.7,
+ "sl4": 5.64,
+ "sl5": 5.63,
+ "sl6": 5.64,
+ "sl7": 5.63
+ },
+ "rock_fragments": {
+ "sl1": 7.0,
+ "sl2": 7.0,
+ "sl3": 7.0,
+ "sl4": 11.6,
+ "sl5": 11.86,
+ "sl6": 10.6,
+ "sl7": 9.33
+ },
+ "sand": {
+ "sl1": 84.0,
+ "sl2": 84.0,
+ "sl3": 84.0,
+ "sl4": 84.6,
+ "sl5": 84.71,
+ "sl6": 84.2,
+ "sl7": 82.33
+ },
+ "site": {
+ "siteData": {
+ "componentID": 113211,
+ "distance": 25925.864,
+ "mapunitID": 18484,
+ "minCompDistance": 0.50040511,
+ "share": 100,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ",
+ "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).",
+ "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered."
+ }
+ },
+ "texture": {
+ "sl1": "Loamy sand",
+ "sl2": "Loamy sand",
+ "sl3": "Loamy sand",
+ "sl4": "Loamy sand",
+ "sl5": "Loamy sand",
+ "sl6": "Loamy sand",
+ "sl7": "Loamy sand"
+ }
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "global",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Cambic arenosols",
+ "componentData": "Data Complete",
+ "componentID": 113052,
+ "name": "Cambic arenosols",
+ "rank_data": "1",
+ "rank_data_loc": "1",
+ "rank_loc": "2",
+ "score_data": 0.9,
+ "score_data_loc": 1.0,
+ "score_loc": 0.178
+ },
+ {
+ "component": "Haplic solonetz",
+ "componentData": "Data Complete",
+ "componentID": 113051,
+ "name": "Haplic solonetz",
+ "rank_data": "4",
+ "rank_data_loc": "2",
+ "rank_loc": "4",
+ "score_data": 0.9,
+ "score_data_loc": 0.953,
+ "score_loc": 0.127
+ },
+ {
+ "component": "Mollic fluvisols",
+ "componentData": "Data Complete",
+ "componentID": 113477,
+ "name": "Mollic fluvisols",
+ "rank_data": "5",
+ "rank_data_loc": "3",
+ "rank_loc": "5",
+ "score_data": 0.9,
+ "score_data_loc": 0.937,
+ "score_loc": 0.109
+ },
+ {
+ "component": "Ferralic arenosols",
+ "componentData": "Data Complete",
+ "componentID": 112871,
+ "name": "Ferralic arenosols",
+ "rank_data": "3",
+ "rank_data_loc": "4",
+ "rank_loc": "6",
+ "score_data": 0.9,
+ "score_data_loc": 0.928,
+ "score_loc": 0.1
+ },
+ {
+ "component": "Eutric planosols",
+ "componentData": "Data Complete",
+ "componentID": 113053,
+ "name": "Eutric planosols",
+ "rank_data": "2",
+ "rank_data_loc": "5",
+ "rank_loc": "7",
+ "score_data": 0.9,
+ "score_data_loc": 0.903,
+ "score_loc": 0.073
+ },
+ {
+ "component": "Eutric fluvisols",
+ "componentData": "Data Complete",
+ "componentID": 113211,
+ "name": "Eutric fluvisols2",
+ "rank_data": "6",
+ "rank_data_loc": "6",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.813,
+ "score_data_loc": 0.873,
+ "score_loc": 0.127
+ },
+ {
+ "component": "Salic fluvisols",
+ "componentData": "Data Complete",
+ "componentID": 113476,
+ "name": "Salic fluvisols",
+ "rank_data": "7",
+ "rank_data_loc": "7",
+ "rank_loc": "1",
+ "score_data": 0.756,
+ "score_data_loc": 0.87,
+ "score_loc": 0.182
+ },
+ {
+ "component": "Gleyic solonetz",
+ "componentData": "Data Complete",
+ "componentID": 113054,
+ "name": "Gleyic solonetz",
+ "rank_data": "8",
+ "rank_data_loc": "8",
+ "rank_loc": "8",
+ "score_data": 0.576,
+ "score_data_loc": 0.585,
+ "score_loc": 0.055
+ },
+ {
+ "component": "Umbric gleysols",
+ "componentData": "Missing Data",
+ "componentID": 113478,
+ "name": "Umbric gleysols",
+ "rank_data": "9",
+ "rank_data_loc": "9",
+ "rank_loc": "9",
+ "score_data": 0.576,
+ "score_data_loc": 0.568,
+ "score_loc": 0.036
+ },
+ {
+ "component": "Gleyic arenosols",
+ "componentData": "Data Complete",
+ "componentID": 112872,
+ "name": "Gleyic arenosols",
+ "rank_data": "10",
+ "rank_data_loc": "10",
+ "rank_loc": "10",
+ "score_data": 0.244,
+ "score_data_loc": 0.239,
+ "score_loc": 0.013
+ },
+ {
+ "component": "Cambic arenosols",
+ "componentData": "Data Complete",
+ "componentID": 113348,
+ "name": "Cambic arenosols2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.576,
+ "score_data_loc": 0.699,
+ "score_loc": 0.178
+ },
+ {
+ "component": "Eutric fluvisols",
+ "componentData": "Data Complete",
+ "componentID": 113479,
+ "name": "Eutric fluvisols",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "3",
+ "score_data": 0.244,
+ "score_data_loc": 0.345,
+ "score_loc": 0.127
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[15.73333,120.31667].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[15.73333,120.31667].json
new file mode 100644
index 0000000..23805e4
--- /dev/null
+++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[15.73333,120.31667].json
@@ -0,0 +1,1339 @@
+{
+ "list": {
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 11.0,
+ "sl5": 11.0,
+ "sl6": 11.0,
+ "sl7": 10.83
+ },
+ "clay": {
+ "sl1": 30.0,
+ "sl2": 30.0,
+ "sl3": 30.0,
+ "sl4": 37.6,
+ "sl5": 41.0,
+ "sl6": 44.2,
+ "sl7": 45.17
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Haplic nitisols",
+ "name": "Haplic nitisols",
+ "rank_loc": "1",
+ "score_loc": 0.17
+ },
+ "ph": {
+ "sl1": 5.5,
+ "sl2": 5.5,
+ "sl3": 5.5,
+ "sl4": 5.36,
+ "sl5": 5.31,
+ "sl6": 5.28,
+ "sl7": 5.27
+ },
+ "rock_fragments": {
+ "sl1": 10.0,
+ "sl2": 10.0,
+ "sl3": 10.0,
+ "sl4": 13.2,
+ "sl5": 14.14,
+ "sl6": 13.0,
+ "sl7": 11.5
+ },
+ "sand": {
+ "sl1": 46.0,
+ "sl2": 46.0,
+ "sl3": 46.0,
+ "sl4": 40.6,
+ "sl5": 38.0,
+ "sl6": 35.4,
+ "sl7": 34.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 141607,
+ "distance": 0.357,
+ "mapunitID": 4413,
+ "minCompDistance": 0.35725062,
+ "share": 40,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.",
+ "Description_es": "Los Nitisoles Háplicos son los suelos subtropicales y tropicales húmedos más productivos.
Tienen una estructura bien desarrollada con subsuelos relativamente arcillosos y enriquecidos en hierro que retienen agua y nutrientes.",
+ "Description_fr": "Haplic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.",
+ "Description_ks": "Haplic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.",
+ "Management_en": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.",
+ "Management_es": "Son suelos productivos y pueden utilizarse para la producción de cultivos.
Tienen un excelente drenaje interno y una buena capacidad de retención de agua.
Estos suelos tienen un alto grado de absorción de fósforo y fijan el fósforo, por lo que no está disponible para la planta durante la temporada de cultivo.
La fertilización con fósforo será necesaria para obtener la mejor productividad.
Las prácticas bien documentadas, como la aplicación de fertilizantes fosfatados en banda (directamente sobre la semilla o a un lado y abajo de la semilla), ayudarán a reducir la fijación de P.",
+ "Management_fr": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.",
+ "Management_ks": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy clay loam",
+ "sl2": "Sandy clay loam",
+ "sl3": "Sandy clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Unknown",
+ "sl6": "Unknown",
+ "sl7": "Unknown"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 22.0,
+ "sl2": 22.0,
+ "sl3": 22.0,
+ "sl4": 21.6,
+ "sl5": 21.86,
+ "sl6": 22.2,
+ "sl7": 22.67
+ },
+ "clay": {
+ "sl1": 29.0,
+ "sl2": 29.0,
+ "sl3": 29.0,
+ "sl4": 31.0,
+ "sl5": 31.43,
+ "sl6": 31.4,
+ "sl7": 31.33
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 1.4,
+ "sl5": 1.29,
+ "sl6": 1.2,
+ "sl7": 1.17
+ },
+ "id": {
+ "component": "Eutric cambisols",
+ "name": "Eutric cambisols",
+ "rank_loc": "2",
+ "score_loc": 0.12
+ },
+ "ph": {
+ "sl1": 6.4,
+ "sl2": 6.4,
+ "sl3": 6.4,
+ "sl4": 6.42,
+ "sl5": 6.47,
+ "sl6": 6.58,
+ "sl7": 6.65
+ },
+ "rock_fragments": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 15.8,
+ "sl5": 16.57,
+ "sl6": 17.8,
+ "sl7": 16.0
+ },
+ "sand": {
+ "sl1": 40.0,
+ "sl2": 40.0,
+ "sl3": 40.0,
+ "sl4": 39.2,
+ "sl5": 39.14,
+ "sl6": 39.6,
+ "sl7": 39.33
+ },
+ "site": {
+ "siteData": {
+ "componentID": 142290,
+ "distance": 0.0,
+ "mapunitID": 4478,
+ "minCompDistance": 0.0,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ",
+ "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ",
+ "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ",
+ "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ",
+ "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ",
+ "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.",
+ "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ",
+ "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. "
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 7.0,
+ "sl2": 7.0,
+ "sl3": 7.0,
+ "sl4": 6.4,
+ "sl5": 6.29,
+ "sl6": 6.2,
+ "sl7": 6.17
+ },
+ "clay": {
+ "sl1": 23.0,
+ "sl2": 23.0,
+ "sl3": 23.0,
+ "sl4": 28.8,
+ "sl5": 31.14,
+ "sl6": 33.4,
+ "sl7": 34.33
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Haplic acrisols",
+ "name": "Haplic acrisols",
+ "rank_loc": "3",
+ "score_loc": 0.12
+ },
+ "ph": {
+ "sl1": 5.1,
+ "sl2": 5.1,
+ "sl3": 5.1,
+ "sl4": 5.04,
+ "sl5": 5.03,
+ "sl6": 5.02,
+ "sl7": 5.02
+ },
+ "rock_fragments": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 12.4,
+ "sl5": 13.29,
+ "sl6": 13.0,
+ "sl7": 14.0
+ },
+ "sand": {
+ "sl1": 59.0,
+ "sl2": 59.0,
+ "sl3": 59.0,
+ "sl4": 54.4,
+ "sl5": 52.29,
+ "sl6": 50.2,
+ "sl7": 49.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 141609,
+ "distance": 0.357,
+ "mapunitID": 4413,
+ "minCompDistance": 0.35725062,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.",
+ "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ",
+ "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.",
+ "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.",
+ "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ",
+ "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ",
+ "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ",
+ "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy clay loam",
+ "sl2": "Sandy clay loam",
+ "sl3": "Sandy clay loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 16.0,
+ "sl5": 16.14,
+ "sl6": 16.6,
+ "sl7": 16.83
+ },
+ "clay": {
+ "sl1": 30.0,
+ "sl2": 30.0,
+ "sl3": 30.0,
+ "sl4": 33.8,
+ "sl5": 35.57,
+ "sl6": 37.4,
+ "sl7": 38.33
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 0.86,
+ "sl6": 0.6,
+ "sl7": 0.5
+ },
+ "id": {
+ "component": "Gleyic cambisols",
+ "name": "Gleyic cambisols",
+ "rank_loc": "4",
+ "score_loc": 0.12
+ },
+ "ph": {
+ "sl1": 5.7,
+ "sl2": 5.7,
+ "sl3": 5.7,
+ "sl4": 5.78,
+ "sl5": 5.83,
+ "sl6": 5.9,
+ "sl7": 5.93
+ },
+ "rock_fragments": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 7.6,
+ "sl5": 8.29,
+ "sl6": 8.0,
+ "sl7": 8.17
+ },
+ "sand": {
+ "sl1": 41.0,
+ "sl2": 41.0,
+ "sl3": 41.0,
+ "sl4": 39.0,
+ "sl5": 37.57,
+ "sl6": 35.8,
+ "sl7": 35.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 142288,
+ "distance": 0.0,
+ "mapunitID": 4478,
+ "minCompDistance": 0.0,
+ "share": 30,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Gleyic Cambisols are widely occurring soils with limited soil development.
These soils are saturated with shallow groundwater above one meter of soil depth.",
+ "Description_es": "Los Cambisoles Gleyicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Estos suelos están saturados con aguas subterráneas poco profundas por encima de un metro de profundidad.",
+ "Description_fr": "Gleyic Cambisols are widely occurring soils with limited soil development.
These soils are saturated with shallow groundwater above one meter of soil depth.",
+ "Description_ks": "Gleyic Cambisols are widely occurring soils with limited soil development.
These soils are saturated with shallow groundwater above one meter of soil depth.",
+ "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ",
+ "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación procedente de aguas subterráneas, puede que no sea posible la instalación de líneas de drenaje, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).",
+ "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ",
+ "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). "
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 17.0,
+ "sl5": 16.29,
+ "sl6": 15.6,
+ "sl7": 15.33
+ },
+ "clay": {
+ "sl1": 29.0,
+ "sl2": 29.0,
+ "sl3": 29.0,
+ "sl4": 29.8,
+ "sl5": 30.14,
+ "sl6": 30.0,
+ "sl7": 29.67
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 0.86,
+ "sl6": 0.6,
+ "sl7": 0.5
+ },
+ "id": {
+ "component": "Dystric cambisols",
+ "name": "Dystric cambisols",
+ "rank_loc": "5",
+ "score_loc": 0.1
+ },
+ "ph": {
+ "sl1": 5.0,
+ "sl2": 5.0,
+ "sl3": 5.0,
+ "sl4": 5.02,
+ "sl5": 5.06,
+ "sl6": 5.12,
+ "sl7": 5.13
+ },
+ "rock_fragments": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 14.4,
+ "sl5": 14.43,
+ "sl6": 15.2,
+ "sl7": 16.67
+ },
+ "sand": {
+ "sl1": 42.0,
+ "sl2": 42.0,
+ "sl3": 42.0,
+ "sl4": 42.6,
+ "sl5": 42.57,
+ "sl6": 42.6,
+ "sl7": 43.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 142291,
+ "distance": 0.0,
+ "mapunitID": 4478,
+ "minCompDistance": 0.0,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_es": "Los Cambisoles Dístricos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos menos productivos con baja saturación de bases en la parte superior del suelo.",
+ "Description_fr": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_ks": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.",
+ "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ",
+ "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Debido a que este suelo tiene una baja saturación de bases, puede ser necesaria la aplicación de bases (a través de la fertlización) para un rendimiento más productivo del cultivo.
Si el pH del suelo es bajo, el calcio (y posiblemente el magnesio, si se utiliza cal dolomítica) puede ser suministrado a través de la adición de cal.
Si el pH del suelo es adecuado para la producción de cultivos, entonces el yeso (CaSO4) puede ser utilizado como fuente de Ca, si es necesario, u otras fuentes como MgSO4 podrían ser aplicadas (si la prueba del suelo indica una necesidad).
Una fertilización adecuada también aportará potasio, si el análisis del suelo indica que es necesario.",
+ "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ",
+ "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. "
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 9.0,
+ "sl2": 9.0,
+ "sl3": 9.0,
+ "sl4": 10.8,
+ "sl5": 11.86,
+ "sl6": 13.0,
+ "sl7": 13.5
+ },
+ "clay": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 22.2,
+ "sl5": 25.57,
+ "sl6": 28.6,
+ "sl7": 29.83
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.14,
+ "sl6": 1.4,
+ "sl7": 1.67
+ },
+ "id": {
+ "component": "Gleyic luvisols",
+ "name": "Gleyic luvisols",
+ "rank_loc": "6",
+ "score_loc": 0.08
+ },
+ "ph": {
+ "sl1": 6.3,
+ "sl2": 6.3,
+ "sl3": 6.3,
+ "sl4": 6.34,
+ "sl5": 6.41,
+ "sl6": 6.54,
+ "sl7": 6.62
+ },
+ "rock_fragments": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 8.4,
+ "sl5": 13.14,
+ "sl6": 17.8,
+ "sl7": 15.67
+ },
+ "sand": {
+ "sl1": 62.0,
+ "sl2": 62.0,
+ "sl3": 62.0,
+ "sl4": 57.4,
+ "sl5": 54.57,
+ "sl6": 51.4,
+ "sl7": 49.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 142289,
+ "distance": 0.0,
+ "mapunitID": 4478,
+ "minCompDistance": 0.0,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.",
+ "Description_es": "Los Luvisoles Gleyicos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles Gleyicos están saturados con agua subterránea poco profunda en el metro superior del perfil del suelo.",
+ "Description_fr": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.",
+ "Description_ks": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.",
+ "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ",
+ "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación a través de las aguas subterráneas, esto puede no ser posible, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).",
+ "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ",
+ "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 18.4,
+ "sl5": 18.14,
+ "sl6": 17.6,
+ "sl7": 17.5
+ },
+ "clay": {
+ "sl1": 31.0,
+ "sl2": 31.0,
+ "sl3": 31.0,
+ "sl4": 32.2,
+ "sl5": 32.14,
+ "sl6": 31.6,
+ "sl7": 31.33
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 1.4,
+ "sl5": 1.43,
+ "sl6": 1.6,
+ "sl7": 1.67
+ },
+ "id": {
+ "component": "Eutric fluvisols",
+ "name": "Eutric fluvisols",
+ "rank_loc": "7",
+ "score_loc": 0.07
+ },
+ "ph": {
+ "sl1": 6.1,
+ "sl2": 6.1,
+ "sl3": 6.1,
+ "sl4": 6.24,
+ "sl5": 6.3,
+ "sl6": 6.38,
+ "sl7": 6.43
+ },
+ "rock_fragments": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 11.6,
+ "sl5": 9.86,
+ "sl6": 10.2,
+ "sl7": 10.33
+ },
+ "sand": {
+ "sl1": 37.0,
+ "sl2": 37.0,
+ "sl3": 37.0,
+ "sl4": 36.2,
+ "sl5": 36.86,
+ "sl6": 38.4,
+ "sl7": 38.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 142740,
+ "distance": 5134.803,
+ "mapunitID": 4517,
+ "minCompDistance": 5134.80309245,
+ "share": 70,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ",
+ "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).",
+ "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered."
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 16.6,
+ "sl5": 16.71,
+ "sl6": 16.6,
+ "sl7": 16.5
+ },
+ "clay": {
+ "sl1": 25.0,
+ "sl2": 25.0,
+ "sl3": 25.0,
+ "sl4": 30.2,
+ "sl5": 31.57,
+ "sl6": 32.4,
+ "sl7": 32.33
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.0,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Haplic luvisols",
+ "name": "Haplic luvisols",
+ "rank_loc": "8",
+ "score_loc": 0.04
+ },
+ "ph": {
+ "sl1": 6.2,
+ "sl2": 6.2,
+ "sl3": 6.2,
+ "sl4": 6.22,
+ "sl5": 6.26,
+ "sl6": 6.32,
+ "sl7": 6.37
+ },
+ "rock_fragments": {
+ "sl1": 10.0,
+ "sl2": 10.0,
+ "sl3": 10.0,
+ "sl4": 14.8,
+ "sl5": 15.29,
+ "sl6": 15.2,
+ "sl7": 14.67
+ },
+ "sand": {
+ "sl1": 47.0,
+ "sl2": 47.0,
+ "sl3": 47.0,
+ "sl4": 43.6,
+ "sl5": 42.71,
+ "sl6": 42.4,
+ "sl7": 42.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 141610,
+ "distance": 0.357,
+ "mapunitID": 4413,
+ "minCompDistance": 0.35725062,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.",
+ "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.",
+ "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.",
+ "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.",
+ "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.",
+ "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops."
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 18.0,
+ "sl2": 18.0,
+ "sl3": 18.0,
+ "sl4": 17.6,
+ "sl5": 17.86,
+ "sl6": 18.4,
+ "sl7": 18.83
+ },
+ "clay": {
+ "sl1": 33.0,
+ "sl2": 33.0,
+ "sl3": 33.0,
+ "sl4": 35.8,
+ "sl5": 36.71,
+ "sl6": 37.8,
+ "sl7": 38.5
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 0.8,
+ "sl5": 0.57,
+ "sl6": 0.6,
+ "sl7": 0.67
+ },
+ "id": {
+ "component": "Eutric gleysols",
+ "name": "Eutric gleysols",
+ "rank_loc": "9",
+ "score_loc": 0.03
+ },
+ "ph": {
+ "sl1": 5.9,
+ "sl2": 5.9,
+ "sl3": 5.9,
+ "sl4": 5.96,
+ "sl5": 5.97,
+ "sl6": 6.02,
+ "sl7": 6.05
+ },
+ "rock_fragments": {
+ "sl1": 13.0,
+ "sl2": 13.0,
+ "sl3": 13.0,
+ "sl4": 17.6,
+ "sl5": 17.14,
+ "sl6": 14.8,
+ "sl7": 15.83
+ },
+ "sand": {
+ "sl1": 35.0,
+ "sl2": 35.0,
+ "sl3": 35.0,
+ "sl4": 33.6,
+ "sl5": 33.29,
+ "sl6": 32.8,
+ "sl7": 31.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 142741,
+ "distance": 5134.803,
+ "mapunitID": 4517,
+ "minCompDistance": 5134.80309245,
+ "share": 30,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.",
+ "Description_es": "Los gleysoles Eútricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles Eutricos son suelos productivos con una alta saturación de la base en la parte superior del suelo.",
+ "Description_fr": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.",
+ "Description_ks": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.",
+ "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ",
+ "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.",
+ "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ",
+ "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. "
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 18.4,
+ "sl5": 18.29,
+ "sl6": 18.4,
+ "sl7": 18.5
+ },
+ "clay": {
+ "sl1": 34.0,
+ "sl2": 34.0,
+ "sl3": 34.0,
+ "sl4": 36.6,
+ "sl5": 37.29,
+ "sl6": 38.0,
+ "sl7": 38.33
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 0.8,
+ "sl5": 0.57,
+ "sl6": 0.4,
+ "sl7": 0.33
+ },
+ "id": {
+ "component": "Gleysols",
+ "name": "Gleysols",
+ "rank_loc": "10",
+ "score_loc": 0.02
+ },
+ "ph": {
+ "sl1": 5.6,
+ "sl2": 5.6,
+ "sl3": 5.6,
+ "sl4": 5.66,
+ "sl5": 5.69,
+ "sl6": 5.74,
+ "sl7": 5.77
+ },
+ "rock_fragments": {
+ "sl1": 10.0,
+ "sl2": 10.0,
+ "sl3": 10.0,
+ "sl4": 9.6,
+ "sl5": 10.43,
+ "sl6": 10.8,
+ "sl7": 11.83
+ },
+ "sand": {
+ "sl1": 35.0,
+ "sl2": 35.0,
+ "sl3": 35.0,
+ "sl4": 33.8,
+ "sl5": 33.71,
+ "sl6": 33.6,
+ "sl7": 33.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 142293,
+ "distance": 0.0,
+ "mapunitID": 4478,
+ "minCompDistance": 0.0,
+ "share": 5,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Gleysols are productive soils with high base saturation in the upper portion of soil.",
+ "Description_es": "Los Gleysoles tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los gleysoles son suelos productivos con una alta saturación de la base en la parte superior del suelo.",
+ "Description_fr": "Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Gleysols are productive soils with high base saturation in the upper portion of soil.",
+ "Description_ks": "Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Gleysols are productive soils with high base saturation in the upper portion of soil.",
+ "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ",
+ "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.",
+ "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ",
+ "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. "
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20
+ },
+ "cec": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0
+ },
+ "clay": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0
+ },
+ "id": {
+ "component": "Lithic leptosols",
+ "name": "Lithic leptosols",
+ "rank_loc": "11",
+ "score_loc": 0.02
+ },
+ "ph": {
+ "sl1": 6.7,
+ "sl2": 6.7,
+ "sl3": 6.7
+ },
+ "rock_fragments": {
+ "sl1": 36.0,
+ "sl2": 36.0,
+ "sl3": 36.0
+ },
+ "sand": {
+ "sl1": 51.0,
+ "sl2": 51.0,
+ "sl3": 51.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 142152,
+ "distance": 9267.434,
+ "mapunitID": 4465,
+ "minCompDistance": 9267.43362967,
+ "share": 20,
+ "soilDepth": 20
+ },
+ "siteDescription": {
+ "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ",
+ "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ",
+ "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.",
+ "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ",
+ "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 15.0,
+ "sl2": 15.0,
+ "sl3": 15.0,
+ "sl4": 12.4,
+ "sl5": 11.71,
+ "sl6": 11.2,
+ "sl7": 10.83
+ },
+ "clay": {
+ "sl1": 41.0,
+ "sl2": 41.0,
+ "sl3": 41.0,
+ "sl4": 45.4,
+ "sl5": 47.14,
+ "sl6": 48.4,
+ "sl7": 49.0
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Humic acrisols",
+ "name": "Humic acrisols",
+ "rank_loc": "12",
+ "score_loc": 0.01
+ },
+ "ph": {
+ "sl1": 4.9,
+ "sl2": 4.9,
+ "sl3": 4.9,
+ "sl4": 4.9,
+ "sl5": 4.91,
+ "sl6": 4.92,
+ "sl7": 4.93
+ },
+ "rock_fragments": {
+ "sl1": 15.0,
+ "sl2": 15.0,
+ "sl3": 15.0,
+ "sl4": 19.4,
+ "sl5": 21.0,
+ "sl6": 22.2,
+ "sl7": 23.0
+ },
+ "sand": {
+ "sl1": 36.0,
+ "sl2": 36.0,
+ "sl3": 36.0,
+ "sl4": 33.6,
+ "sl5": 32.43,
+ "sl6": 31.4,
+ "sl7": 31.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 142155,
+ "distance": 9267.434,
+ "mapunitID": 4465,
+ "minCompDistance": 9267.43362967,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Humic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Humic Acrisols contain large amounts of organic matter in the upper soil layer.
They often have poor structure, but will become more productive in systems that include crop rotations, cover crops or green manures. ",
+ "Description_es": "Los Acrisoles Húmicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Los acrisoles húmicos contienen grandes cantidades de materia orgánica en la capa superior del suelo.
Suelen tener una estructura pobre, pero se vuelven más productivos en sistemas que incluyen rotaciones de cultivos, cultivos de cobertura o abonos verdes. ",
+ "Description_fr": "Humic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Humic Acrisols contain large amounts of organic matter in the upper soil layer.
They often have poor structure, but will become more productive in systems that include crop rotations, cover crops or green manures. ",
+ "Description_ks": "Humic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Humic Acrisols contain large amounts of organic matter in the upper soil layer.
They often have poor structure, but will become more productive in systems that include crop rotations, cover crops or green manures. ",
+ "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ",
+ "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.",
+ "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ",
+ "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. "
+ }
+ },
+ "texture": {
+ "sl1": "Unknown",
+ "sl2": "Unknown",
+ "sl3": "Unknown",
+ "sl4": "Unknown",
+ "sl5": "Unknown",
+ "sl6": "Unknown",
+ "sl7": "Unknown"
+ }
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "global",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Haplic nitisols",
+ "componentData": "Missing Data",
+ "componentID": 141607,
+ "name": "Haplic nitisols",
+ "rank_data": "5",
+ "rank_data_loc": "1",
+ "rank_loc": 1,
+ "score_data": 0.475,
+ "score_data_loc": 1.0,
+ "score_loc": 0.17
+ },
+ {
+ "component": "Eutric cambisols",
+ "componentData": "Data Complete",
+ "componentID": 142290,
+ "name": "Eutric cambisols",
+ "rank_data": "3",
+ "rank_data_loc": "2",
+ "rank_loc": 2,
+ "score_data": 0.515,
+ "score_data_loc": 0.983,
+ "score_loc": 0.12
+ },
+ {
+ "component": "Gleyic cambisols",
+ "componentData": "Missing Data",
+ "componentID": 142288,
+ "name": "Gleyic cambisols",
+ "rank_data": "4",
+ "rank_data_loc": "3",
+ "rank_loc": 4,
+ "score_data": 0.515,
+ "score_data_loc": 0.983,
+ "score_loc": 0.12
+ },
+ {
+ "component": "Dystric cambisols",
+ "componentData": "Data Complete",
+ "componentID": 142291,
+ "name": "Dystric cambisols",
+ "rank_data": "2",
+ "rank_data_loc": "4",
+ "rank_loc": 5,
+ "score_data": 0.515,
+ "score_data_loc": 0.952,
+ "score_loc": 0.1
+ },
+ {
+ "component": "Gleysols",
+ "componentData": "Missing Data",
+ "componentID": 142293,
+ "name": "Gleysols",
+ "rank_data": "1",
+ "rank_data_loc": "5",
+ "rank_loc": 10,
+ "score_data": 0.566,
+ "score_data_loc": 0.908,
+ "score_loc": 0.02
+ },
+ {
+ "component": "Eutric fluvisols",
+ "componentData": "Data Complete",
+ "componentID": 142740,
+ "name": "Eutric fluvisols",
+ "rank_data": "7",
+ "rank_data_loc": "6",
+ "rank_loc": 7,
+ "score_data": 0.464,
+ "score_data_loc": 0.827,
+ "score_loc": 0.07
+ },
+ {
+ "component": "Haplic acrisols",
+ "componentData": "Data Complete",
+ "componentID": 141609,
+ "name": "Haplic acrisols",
+ "rank_data": "9",
+ "rank_data_loc": "7",
+ "rank_loc": 3,
+ "score_data": 0.402,
+ "score_data_loc": 0.809,
+ "score_loc": 0.12
+ },
+ {
+ "component": "Eutric gleysols",
+ "componentData": "Missing Data",
+ "componentID": 142741,
+ "name": "Eutric gleysols",
+ "rank_data": "8",
+ "rank_data_loc": "8",
+ "rank_loc": 9,
+ "score_data": 0.451,
+ "score_data_loc": 0.745,
+ "score_loc": 0.03
+ },
+ {
+ "component": "Humic acrisols",
+ "componentData": "No Data",
+ "componentID": 142155,
+ "name": "Humic acrisols",
+ "rank_data": "10",
+ "rank_data_loc": "9",
+ "rank_loc": 12,
+ "score_data": 0.337,
+ "score_data_loc": 0.538,
+ "score_loc": 0.01
+ },
+ {
+ "component": "Haplic luvisols",
+ "componentData": "Data Complete",
+ "componentID": 141610,
+ "name": "Haplic luvisols",
+ "rank_data": "11",
+ "rank_data_loc": "10",
+ "rank_loc": 8,
+ "score_data": 0.208,
+ "score_data_loc": 0.383,
+ "score_loc": 0.04
+ },
+ {
+ "component": "Gleyic luvisols",
+ "componentData": "Data Complete",
+ "componentID": 142289,
+ "name": "Gleyic luvisols",
+ "rank_data": "12",
+ "rank_data_loc": "11",
+ "rank_loc": 6,
+ "score_data": 0.157,
+ "score_data_loc": 0.367,
+ "score_loc": 0.08
+ },
+ {
+ "component": "Lithic leptosols",
+ "componentData": "Missing Data",
+ "componentID": 142152,
+ "name": "Lithic leptosols",
+ "rank_data": "6",
+ "rank_data_loc": "12",
+ "rank_loc": 11,
+ "score_data": 0.465,
+ "score_data_loc": 0.003,
+ "score_loc": 0.02
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[30.38333,35.53333].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[30.38333,35.53333].json
new file mode 100644
index 0000000..08e5ca8
--- /dev/null
+++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[30.38333,35.53333].json
@@ -0,0 +1,779 @@
+{
+ "list": {
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 13.8,
+ "sl5": 13.43,
+ "sl6": 13.0,
+ "sl7": 12.67
+ },
+ "clay": {
+ "sl1": 18.0,
+ "sl2": 18.0,
+ "sl3": 18.0,
+ "sl4": 20.0,
+ "sl5": 20.43,
+ "sl6": 20.4,
+ "sl7": 20.17
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.4,
+ "sl5": 1.71,
+ "sl6": 1.8,
+ "sl7": 1.83
+ },
+ "id": {
+ "component": "Haplic calcisols",
+ "name": "Haplic calcisols",
+ "rank_loc": "1",
+ "score_loc": 0.327
+ },
+ "ph": {
+ "sl1": 8.2,
+ "sl2": 8.2,
+ "sl3": 8.2,
+ "sl4": 8.28,
+ "sl5": 8.31,
+ "sl6": 8.34,
+ "sl7": 8.35
+ },
+ "rock_fragments": {
+ "sl1": 12.0,
+ "sl2": 12.0,
+ "sl3": 12.0,
+ "sl4": 14.2,
+ "sl5": 15.29,
+ "sl6": 16.6,
+ "sl7": 17.33
+ },
+ "sand": {
+ "sl1": 49.0,
+ "sl2": 49.0,
+ "sl3": 49.0,
+ "sl4": 46.8,
+ "sl5": 46.14,
+ "sl6": 46.0,
+ "sl7": 46.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 133143,
+ "distance": 0.0,
+ "mapunitID": 3571,
+ "minCompDistance": 0.0,
+ "share": 40,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Calcisols mostly occur in semiarid and arid climates. They are calcareous soils, with high base saturation, pH, and P fixation.
Many have gravelly surface horizons. ",
+ "Description_es": "Los Calcisoles Háplicos se dan principalmente en climas semiáridos y áridos. Son suelos calcáreos, con alta saturación de bases, pH y fijación de P.
Muchos tienen horizontes superficiales de grava. ",
+ "Description_fr": "Haplic Calcisols mostly occur in semiarid and arid climates. They are calcareous soils, with high base saturation, pH, and P fixation.
Many have gravelly surface horizons. ",
+ "Description_ks": "Haplic Calcisols mostly occur in semiarid and arid climates. They are calcareous soils, with high base saturation, pH, and P fixation.
Many have gravelly surface horizons. ",
+ "Management_en": "These soils have low organic matter content, are dry, and often stony.
They are calcareous, and will have high base saturation (Ca, Mg and K) and high soil pH.
If used, the soils are best suited for grazing or limited use with drought tolerant crops.
At best they could be cultivated every-other or every-third year, with fallow in the years in which the soils are not used for crops.
If irrigated, care must be taken so that the soils do not become high in salts (saline). High quality irrigation water that is low in salts would be needed to prevent salinization.",
+ "Management_es": "Estos suelos tienen un bajo contenido en materia orgánica, son secos y a menudo pedregosos.
Son calcáreos, y tendrán una alta saturación de bases (Ca, Mg y K) y un alto pH del suelo.
Si se utilizan, los suelos son más adecuados para el pastoreo o para un uso limitado con cultivos tolerantes a la sequía.
En el mejor de los casos, podrían cultivarse cada dos o tres años, con barbecho en los años en que no se utilicen los suelos para cultivos.
Si se riega, hay que tener cuidado para que los suelos no se vuelvan altos en sales (salinos). Para evitar la salinización sería necesario un agua de riego de alta calidad y bajo contenido en sales.",
+ "Management_fr": "These soils have low organic matter content, are dry, and often stony.
They are calcareous, and will have high base saturation (Ca, Mg and K) and high soil pH.
If used, the soils are best suited for grazing or limited use with drought tolerant crops.
At best they could be cultivated every-other or every-third year, with fallow in the years in which the soils are not used for crops.
If irrigated, care must be taken so that the soils do not become high in salts (saline). High quality irrigation water that is low in salts would be needed to prevent salinization.",
+ "Management_ks": "These soils have low organic matter content, are dry, and often stony.
They are calcareous, and will have high base saturation (Ca, Mg and K) and high soil pH.
If used, the soils are best suited for grazing or limited use with drought tolerant crops.
At best they could be cultivated every-other or every-third year, with fallow in the years in which the soils are not used for crops.
If irrigated, care must be taken so that the soils do not become high in salts (saline). High quality irrigation water that is low in salts would be needed to prevent salinization."
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20
+ },
+ "cec": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0
+ },
+ "clay": {
+ "sl1": 12.0,
+ "sl2": 12.0,
+ "sl3": 12.0
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0
+ },
+ "id": {
+ "component": "Lithic leptosols",
+ "name": "Lithic leptosols",
+ "rank_loc": "2",
+ "score_loc": 0.286
+ },
+ "ph": {
+ "sl1": 7.4,
+ "sl2": 7.4,
+ "sl3": 7.4
+ },
+ "rock_fragments": {
+ "sl1": 18.0,
+ "sl2": 18.0,
+ "sl3": 18.0
+ },
+ "sand": {
+ "sl1": 66.0,
+ "sl2": 66.0,
+ "sl3": 66.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 133145,
+ "distance": 0.0,
+ "mapunitID": 3571,
+ "minCompDistance": 0.0,
+ "share": 20,
+ "soilDepth": 20
+ },
+ "siteDescription": {
+ "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ",
+ "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ",
+ "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.",
+ "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ",
+ "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 13.4,
+ "sl5": 13.29,
+ "sl6": 13.0,
+ "sl7": 12.67
+ },
+ "clay": {
+ "sl1": 15.0,
+ "sl2": 15.0,
+ "sl3": 15.0,
+ "sl4": 15.4,
+ "sl5": 15.43,
+ "sl6": 15.8,
+ "sl7": 16.17
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.6,
+ "sl5": 1.71,
+ "sl6": 1.6,
+ "sl7": 1.83
+ },
+ "id": {
+ "component": "Calcaric regosols",
+ "name": "Calcaric regosols",
+ "rank_loc": "3",
+ "score_loc": 0.128
+ },
+ "ph": {
+ "sl1": 8.2,
+ "sl2": 8.2,
+ "sl3": 8.2,
+ "sl4": 8.26,
+ "sl5": 8.27,
+ "sl6": 8.28,
+ "sl7": 8.28
+ },
+ "rock_fragments": {
+ "sl1": 9.0,
+ "sl2": 9.0,
+ "sl3": 9.0,
+ "sl4": 9.4,
+ "sl5": 8.0,
+ "sl6": 7.4,
+ "sl7": 7.83
+ },
+ "sand": {
+ "sl1": 55.0,
+ "sl2": 55.0,
+ "sl3": 55.0,
+ "sl4": 54.0,
+ "sl5": 53.71,
+ "sl6": 52.8,
+ "sl7": 52.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 133144,
+ "distance": 0.0,
+ "mapunitID": 3571,
+ "minCompDistance": 0.0,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ",
+ "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ",
+ "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ",
+ "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ",
+ "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ",
+ "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.",
+ "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ",
+ "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy loam",
+ "sl5": "Sandy loam",
+ "sl6": "Sandy loam",
+ "sl7": "Sandy loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 13.0,
+ "sl2": 13.0,
+ "sl3": 13.0,
+ "sl4": 13.2,
+ "sl5": 13.43,
+ "sl6": 13.8,
+ "sl7": 14.0
+ },
+ "clay": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 16.6,
+ "sl5": 16.71,
+ "sl6": 17.0,
+ "sl7": 17.5
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.6,
+ "sl5": 1.71,
+ "sl6": 1.6,
+ "sl7": 1.83
+ },
+ "id": {
+ "component": "Regosols",
+ "name": "Regosols",
+ "rank_loc": "4",
+ "score_loc": 0.073
+ },
+ "ph": {
+ "sl1": 7.8,
+ "sl2": 7.8,
+ "sl3": 7.8,
+ "sl4": 7.86,
+ "sl5": 7.93,
+ "sl6": 7.98,
+ "sl7": 8.02
+ },
+ "rock_fragments": {
+ "sl1": 12.0,
+ "sl2": 12.0,
+ "sl3": 12.0,
+ "sl4": 15.6,
+ "sl5": 16.57,
+ "sl6": 17.0,
+ "sl7": 17.17
+ },
+ "sand": {
+ "sl1": 57.0,
+ "sl2": 57.0,
+ "sl3": 57.0,
+ "sl4": 56.2,
+ "sl5": 55.57,
+ "sl6": 54.4,
+ "sl7": 53.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 132625,
+ "distance": 3698.05,
+ "mapunitID": 3515,
+ "minCompDistance": 3698.04959689,
+ "share": 50,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity. ",
+ "Description_es": "Los Regosoles son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad. ",
+ "Description_fr": "Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity. ",
+ "Description_ks": "Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity. ",
+ "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ",
+ "Management_es": "Estos suelos tienen baja capacidad de retención de agua, y son muy sensibles a la sequía.
Estos suelos pueden ser productivos, si se les proporciona riego y fertilización.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.",
+ "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ",
+ "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy loam",
+ "sl5": "Sandy loam",
+ "sl6": "Sandy loam",
+ "sl7": "Sandy loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 12.0,
+ "sl2": 12.0,
+ "sl3": 12.0,
+ "sl4": 13.8,
+ "sl5": 14.0,
+ "sl6": 14.0,
+ "sl7": 13.83
+ },
+ "clay": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 19.6,
+ "sl5": 20.14,
+ "sl6": 20.2,
+ "sl7": 20.17
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.0,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Haplic luvisols",
+ "name": "Haplic luvisols",
+ "rank_loc": "5",
+ "score_loc": 0.071
+ },
+ "ph": {
+ "sl1": 7.0,
+ "sl2": 7.0,
+ "sl3": 7.0,
+ "sl4": 7.14,
+ "sl5": 7.21,
+ "sl6": 7.34,
+ "sl7": 7.42
+ },
+ "rock_fragments": {
+ "sl1": 15.0,
+ "sl2": 15.0,
+ "sl3": 15.0,
+ "sl4": 15.8,
+ "sl5": 16.71,
+ "sl6": 17.8,
+ "sl7": 17.83
+ },
+ "sand": {
+ "sl1": 64.0,
+ "sl2": 64.0,
+ "sl3": 64.0,
+ "sl4": 61.2,
+ "sl5": 60.86,
+ "sl6": 60.8,
+ "sl7": 60.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 133773,
+ "distance": 16922.699,
+ "mapunitID": 3612,
+ "minCompDistance": 16922.69933315,
+ "share": 50,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.",
+ "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.",
+ "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.",
+ "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.",
+ "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.",
+ "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 10.0,
+ "sl2": 10.0,
+ "sl3": 10.0,
+ "sl4": 11.8,
+ "sl5": 12.14,
+ "sl6": 12.2,
+ "sl7": 12.17
+ },
+ "clay": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 24.2,
+ "sl5": 25.43,
+ "sl6": 26.2,
+ "sl7": 26.0
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.0,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Chromic luvisols",
+ "name": "Chromic luvisols",
+ "rank_loc": "6",
+ "score_loc": 0.057
+ },
+ "ph": {
+ "sl1": 6.5,
+ "sl2": 6.5,
+ "sl3": 6.5,
+ "sl4": 6.62,
+ "sl5": 6.66,
+ "sl6": 6.76,
+ "sl7": 6.83
+ },
+ "rock_fragments": {
+ "sl1": 12.0,
+ "sl2": 12.0,
+ "sl3": 12.0,
+ "sl4": 12.0,
+ "sl5": 12.71,
+ "sl6": 16.0,
+ "sl7": 18.0
+ },
+ "sand": {
+ "sl1": 67.0,
+ "sl2": 67.0,
+ "sl3": 67.0,
+ "sl4": 62.6,
+ "sl5": 61.71,
+ "sl6": 61.0,
+ "sl7": 61.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 133147,
+ "distance": 0.0,
+ "mapunitID": 3571,
+ "minCompDistance": 0.0,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.",
+ "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.",
+ "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 13.0,
+ "sl2": 13.0,
+ "sl3": 13.0,
+ "sl4": 13.0,
+ "sl5": 12.86,
+ "sl6": 12.6,
+ "sl7": 12.17
+ },
+ "clay": {
+ "sl1": 23.0,
+ "sl2": 23.0,
+ "sl3": 23.0,
+ "sl4": 23.6,
+ "sl5": 23.71,
+ "sl6": 23.8,
+ "sl7": 23.67
+ },
+ "ec": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 15.2,
+ "sl5": 16.14,
+ "sl6": 16.8,
+ "sl7": 16.67
+ },
+ "id": {
+ "component": "Solonchaks",
+ "name": "Solonchaks",
+ "rank_loc": "7",
+ "score_loc": 0.057
+ },
+ "ph": {
+ "sl1": 8.3,
+ "sl2": 8.3,
+ "sl3": 8.3,
+ "sl4": 8.36,
+ "sl5": 8.37,
+ "sl6": 8.38,
+ "sl7": 8.38
+ },
+ "rock_fragments": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 19.0,
+ "sl5": 21.14,
+ "sl6": 22.8,
+ "sl7": 23.33
+ },
+ "sand": {
+ "sl1": 47.0,
+ "sl2": 47.0,
+ "sl3": 47.0,
+ "sl4": 47.6,
+ "sl5": 47.57,
+ "sl6": 47.6,
+ "sl7": 47.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 133146,
+ "distance": 0.0,
+ "mapunitID": 3571,
+ "minCompDistance": 0.0,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.",
+ "Description_es": "Los Solonchaks son suelos que contienen sales en la superficie del suelo o cerca de ella. Estos suelos se forman en los desiertos o cerca de las costas.",
+ "Description_fr": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.",
+ "Description_ks": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.",
+ "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ",
+ "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy pobre, y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.",
+ "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ",
+ "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "global",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Calcaric regosols",
+ "componentData": "Data Complete",
+ "componentID": 133144,
+ "name": "Calcaric regosols",
+ "rank_data": "1",
+ "rank_data_loc": "1",
+ "rank_loc": 3,
+ "score_data": 1.0,
+ "score_data_loc": 1.0,
+ "score_loc": 0.128
+ },
+ {
+ "component": "Solonchaks",
+ "componentData": "Data Complete",
+ "componentID": 133146,
+ "name": "Solonchaks",
+ "rank_data": "2",
+ "rank_data_loc": "2",
+ "rank_loc": 7,
+ "score_data": 1.0,
+ "score_data_loc": 0.937,
+ "score_loc": 0.057
+ },
+ {
+ "component": "Haplic calcisols",
+ "componentData": "Data Complete",
+ "componentID": 133143,
+ "name": "Haplic calcisols",
+ "rank_data": "4",
+ "rank_data_loc": "3",
+ "rank_loc": 1,
+ "score_data": 0.0,
+ "score_data_loc": 0.29,
+ "score_loc": 0.327
+ },
+ {
+ "component": "Regosols",
+ "componentData": "Data Complete",
+ "componentID": 132625,
+ "name": "Regosols",
+ "rank_data": "7",
+ "rank_data_loc": "4",
+ "rank_loc": 4,
+ "score_data": 0.0,
+ "score_data_loc": 0.065,
+ "score_loc": 0.073
+ },
+ {
+ "component": "Haplic luvisols",
+ "componentData": "Data Complete",
+ "componentID": 133773,
+ "name": "Haplic luvisols",
+ "rank_data": "5",
+ "rank_data_loc": "5",
+ "rank_loc": 5,
+ "score_data": 0.0,
+ "score_data_loc": 0.063,
+ "score_loc": 0.071
+ },
+ {
+ "component": "Chromic luvisols",
+ "componentData": "Data Complete",
+ "componentID": 133147,
+ "name": "Chromic luvisols",
+ "rank_data": "3",
+ "rank_data_loc": "6",
+ "rank_loc": 6,
+ "score_data": 0.0,
+ "score_data_loc": 0.05,
+ "score_loc": 0.057
+ },
+ {
+ "component": "Lithic leptosols",
+ "componentData": "Missing Data",
+ "componentID": 133145,
+ "name": "Lithic leptosols",
+ "rank_data": "6",
+ "rank_data_loc": "7",
+ "rank_loc": 2,
+ "score_data": 0.0,
+ "score_data_loc": 0.002,
+ "score_loc": 0.286
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[32.11667,20.08333].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[32.11667,20.08333].json
new file mode 100644
index 0000000..364500e
--- /dev/null
+++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[32.11667,20.08333].json
@@ -0,0 +1,667 @@
+{
+ "list": {
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 16.4,
+ "sl5": 16.14,
+ "sl6": 16.0,
+ "sl7": 15.83
+ },
+ "clay": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0,
+ "sl4": 20.0,
+ "sl5": 20.0,
+ "sl6": 20.2,
+ "sl7": 20.17
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 1.4,
+ "sl5": 1.43,
+ "sl6": 1.6,
+ "sl7": 1.67
+ },
+ "id": {
+ "component": "Calcaric fluvisols",
+ "name": "Calcaric fluvisols",
+ "rank_loc": "1",
+ "score_loc": 0.3
+ },
+ "ph": {
+ "sl1": 8.2,
+ "sl2": 8.2,
+ "sl3": 8.2,
+ "sl4": 8.2,
+ "sl5": 8.2,
+ "sl6": 8.2,
+ "sl7": 8.2
+ },
+ "rock_fragments": {
+ "sl1": 3.0,
+ "sl2": 3.0,
+ "sl3": 3.0,
+ "sl4": 4.2,
+ "sl5": 5.0,
+ "sl6": 5.2,
+ "sl7": 5.33
+ },
+ "sand": {
+ "sl1": 40.0,
+ "sl2": 40.0,
+ "sl3": 40.0,
+ "sl4": 39.6,
+ "sl5": 39.86,
+ "sl6": 39.8,
+ "sl7": 39.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 101342,
+ "distance": 0.0,
+ "mapunitID": 103,
+ "minCompDistance": 0.0,
+ "share": 30,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.",
+ "Description_es": "Los Fluvisoles Calcáricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles calcáricos tienen carbonatos y un pH elevado en la parte superior del suelo.",
+ "Description_fr": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.",
+ "Description_ks": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.",
+ "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o el manejo de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Una vez en cultivo continuo se debe tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una vía para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).",
+ "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered."
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 12.2,
+ "sl5": 12.43,
+ "sl6": 13.0,
+ "sl7": 13.33
+ },
+ "clay": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0,
+ "sl4": 22.8,
+ "sl5": 23.29,
+ "sl6": 23.4,
+ "sl7": 23.17
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.0,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Chromic cambisols",
+ "name": "Chromic cambisols",
+ "rank_loc": "2",
+ "score_loc": 0.2
+ },
+ "ph": {
+ "sl1": 6.7,
+ "sl2": 6.7,
+ "sl3": 6.7,
+ "sl4": 6.9,
+ "sl5": 6.96,
+ "sl6": 7.06,
+ "sl7": 7.13
+ },
+ "rock_fragments": {
+ "sl1": 9.0,
+ "sl2": 9.0,
+ "sl3": 9.0,
+ "sl4": 8.6,
+ "sl5": 10.14,
+ "sl6": 10.8,
+ "sl7": 12.17
+ },
+ "sand": {
+ "sl1": 61.0,
+ "sl2": 61.0,
+ "sl3": 61.0,
+ "sl4": 58.6,
+ "sl5": 58.43,
+ "sl6": 58.2,
+ "sl7": 58.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 101344,
+ "distance": 0.0,
+ "mapunitID": 103,
+ "minCompDistance": 0.0,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ",
+ "Description_es": "Los Cambisoles Crómicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos bien drenados, con un color intenso.
Cuando el clima y el paisaje son favorables, pueden ser suelos productivos. ",
+ "Description_fr": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ",
+ "Description_ks": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ",
+ "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ",
+ "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.",
+ "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ",
+ "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 13.8,
+ "sl5": 13.43,
+ "sl6": 13.0,
+ "sl7": 12.67
+ },
+ "clay": {
+ "sl1": 18.0,
+ "sl2": 18.0,
+ "sl3": 18.0,
+ "sl4": 20.0,
+ "sl5": 20.43,
+ "sl6": 20.4,
+ "sl7": 20.17
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.4,
+ "sl5": 1.71,
+ "sl6": 1.8,
+ "sl7": 1.83
+ },
+ "id": {
+ "component": "Haplic calcisols",
+ "name": "Haplic calcisols",
+ "rank_loc": "3",
+ "score_loc": 0.2
+ },
+ "ph": {
+ "sl1": 8.2,
+ "sl2": 8.2,
+ "sl3": 8.2,
+ "sl4": 8.28,
+ "sl5": 8.31,
+ "sl6": 8.34,
+ "sl7": 8.35
+ },
+ "rock_fragments": {
+ "sl1": 12.0,
+ "sl2": 12.0,
+ "sl3": 12.0,
+ "sl4": 14.2,
+ "sl5": 15.29,
+ "sl6": 16.6,
+ "sl7": 17.33
+ },
+ "sand": {
+ "sl1": 49.0,
+ "sl2": 49.0,
+ "sl3": 49.0,
+ "sl4": 46.8,
+ "sl5": 46.14,
+ "sl6": 46.0,
+ "sl7": 46.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 101345,
+ "distance": 0.0,
+ "mapunitID": 103,
+ "minCompDistance": 0.0,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Calcisols mostly occur in semiarid and arid climates. They are calcareous soils, with high base saturation, pH, and P fixation.
Many have gravelly surface horizons. ",
+ "Description_es": "Los Calcisoles Háplicos se dan principalmente en climas semiáridos y áridos. Son suelos calcáreos, con alta saturación de bases, pH y fijación de P.
Muchos tienen horizontes superficiales de grava. ",
+ "Description_fr": "Haplic Calcisols mostly occur in semiarid and arid climates. They are calcareous soils, with high base saturation, pH, and P fixation.
Many have gravelly surface horizons. ",
+ "Description_ks": "Haplic Calcisols mostly occur in semiarid and arid climates. They are calcareous soils, with high base saturation, pH, and P fixation.
Many have gravelly surface horizons. ",
+ "Management_en": "These soils have low organic matter content, are dry, and often stony.
They are calcareous, and will have high base saturation (Ca, Mg and K) and high soil pH.
If used, the soils are best suited for grazing or limited use with drought tolerant crops.
At best they could be cultivated every-other or every-third year, with fallow in the years in which the soils are not used for crops.
If irrigated, care must be taken so that the soils do not become high in salts (saline). High quality irrigation water that is low in salts would be needed to prevent salinization.",
+ "Management_es": "Estos suelos tienen un bajo contenido en materia orgánica, son secos y a menudo pedregosos.
Son calcáreos, y tendrán una alta saturación de bases (Ca, Mg y K) y un alto pH del suelo.
Si se utilizan, los suelos son más adecuados para el pastoreo o para un uso limitado con cultivos tolerantes a la sequía.
En el mejor de los casos, podrían cultivarse cada dos o tres años, con barbecho en los años en que no se utilicen los suelos para cultivos.
Si se riega, hay que tener cuidado para que los suelos no se vuelvan altos en sales (salinos). Para evitar la salinización sería necesario un agua de riego de alta calidad y bajo contenido en sales.",
+ "Management_fr": "These soils have low organic matter content, are dry, and often stony.
They are calcareous, and will have high base saturation (Ca, Mg and K) and high soil pH.
If used, the soils are best suited for grazing or limited use with drought tolerant crops.
At best they could be cultivated every-other or every-third year, with fallow in the years in which the soils are not used for crops.
If irrigated, care must be taken so that the soils do not become high in salts (saline). High quality irrigation water that is low in salts would be needed to prevent salinization.",
+ "Management_ks": "These soils have low organic matter content, are dry, and often stony.
They are calcareous, and will have high base saturation (Ca, Mg and K) and high soil pH.
If used, the soils are best suited for grazing or limited use with drought tolerant crops.
At best they could be cultivated every-other or every-third year, with fallow in the years in which the soils are not used for crops.
If irrigated, care must be taken so that the soils do not become high in salts (saline). High quality irrigation water that is low in salts would be needed to prevent salinization."
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 13.0,
+ "sl2": 13.0,
+ "sl3": 13.0,
+ "sl4": 13.0,
+ "sl5": 12.86,
+ "sl6": 12.6,
+ "sl7": 12.17
+ },
+ "clay": {
+ "sl1": 23.0,
+ "sl2": 23.0,
+ "sl3": 23.0,
+ "sl4": 23.6,
+ "sl5": 23.71,
+ "sl6": 23.8,
+ "sl7": 23.67
+ },
+ "ec": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 15.2,
+ "sl5": 16.14,
+ "sl6": 16.8,
+ "sl7": 16.67
+ },
+ "id": {
+ "component": "Solonchaks",
+ "name": "Solonchaks",
+ "rank_loc": "4",
+ "score_loc": 0.2
+ },
+ "ph": {
+ "sl1": 8.3,
+ "sl2": 8.3,
+ "sl3": 8.3,
+ "sl4": 8.36,
+ "sl5": 8.37,
+ "sl6": 8.38,
+ "sl7": 8.38
+ },
+ "rock_fragments": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 19.0,
+ "sl5": 21.14,
+ "sl6": 22.8,
+ "sl7": 23.33
+ },
+ "sand": {
+ "sl1": 47.0,
+ "sl2": 47.0,
+ "sl3": 47.0,
+ "sl4": 47.6,
+ "sl5": 47.57,
+ "sl6": 47.6,
+ "sl7": 47.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 101343,
+ "distance": 0.0,
+ "mapunitID": 103,
+ "minCompDistance": 0.0,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.",
+ "Description_es": "Los Solonchaks son suelos que contienen sales en la superficie del suelo o cerca de ella. Estos suelos se forman en los desiertos o cerca de las costas.",
+ "Description_fr": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.",
+ "Description_ks": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.",
+ "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ",
+ "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy pobre, y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.",
+ "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ",
+ "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 13.4,
+ "sl5": 13.29,
+ "sl6": 13.0,
+ "sl7": 12.67
+ },
+ "clay": {
+ "sl1": 15.0,
+ "sl2": 15.0,
+ "sl3": 15.0,
+ "sl4": 15.4,
+ "sl5": 15.43,
+ "sl6": 15.8,
+ "sl7": 16.17
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.6,
+ "sl5": 1.71,
+ "sl6": 1.6,
+ "sl7": 1.83
+ },
+ "id": {
+ "component": "Calcaric regosols",
+ "name": "Calcaric regosols",
+ "rank_loc": "5",
+ "score_loc": 0.05
+ },
+ "ph": {
+ "sl1": 8.2,
+ "sl2": 8.2,
+ "sl3": 8.2,
+ "sl4": 8.26,
+ "sl5": 8.27,
+ "sl6": 8.28,
+ "sl7": 8.28
+ },
+ "rock_fragments": {
+ "sl1": 9.0,
+ "sl2": 9.0,
+ "sl3": 9.0,
+ "sl4": 9.4,
+ "sl5": 8.0,
+ "sl6": 7.4,
+ "sl7": 7.83
+ },
+ "sand": {
+ "sl1": 55.0,
+ "sl2": 55.0,
+ "sl3": 55.0,
+ "sl4": 54.0,
+ "sl5": 53.71,
+ "sl6": 52.8,
+ "sl7": 52.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 101346,
+ "distance": 0.0,
+ "mapunitID": 103,
+ "minCompDistance": 0.0,
+ "share": 5,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ",
+ "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ",
+ "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ",
+ "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ",
+ "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ",
+ "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.",
+ "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ",
+ "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy loam",
+ "sl5": "Sandy loam",
+ "sl6": "Sandy loam",
+ "sl7": "Sandy loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20
+ },
+ "cec": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0
+ },
+ "clay": {
+ "sl1": 12.0,
+ "sl2": 12.0,
+ "sl3": 12.0
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0
+ },
+ "id": {
+ "component": "Lithic leptosols",
+ "name": "Lithic leptosols",
+ "rank_loc": "6",
+ "score_loc": 0.05
+ },
+ "ph": {
+ "sl1": 7.4,
+ "sl2": 7.4,
+ "sl3": 7.4
+ },
+ "rock_fragments": {
+ "sl1": 18.0,
+ "sl2": 18.0,
+ "sl3": 18.0
+ },
+ "sand": {
+ "sl1": 66.0,
+ "sl2": 66.0,
+ "sl3": 66.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 101347,
+ "distance": 0.0,
+ "mapunitID": 103,
+ "minCompDistance": 0.0,
+ "share": 5,
+ "soilDepth": 20
+ },
+ "siteDescription": {
+ "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ",
+ "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ",
+ "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.",
+ "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ",
+ "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam"
+ }
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "global",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Solonchaks",
+ "componentData": "Data Complete",
+ "componentID": 101343,
+ "name": "Solonchaks",
+ "rank_data": "2",
+ "rank_data_loc": "1",
+ "rank_loc": 4,
+ "score_data": 0.403,
+ "score_data_loc": 1.0,
+ "score_loc": 0.2
+ },
+ {
+ "component": "Calcaric regosols",
+ "componentData": "Data Complete",
+ "componentID": 101346,
+ "name": "Calcaric regosols",
+ "rank_data": "1",
+ "rank_data_loc": "2",
+ "rank_loc": 5,
+ "score_data": 0.499,
+ "score_data_loc": 0.91,
+ "score_loc": 0.05
+ },
+ {
+ "component": "Chromic cambisols",
+ "componentData": "Data Complete",
+ "componentID": 101344,
+ "name": "Chromic cambisols",
+ "rank_data": "3",
+ "rank_data_loc": "3",
+ "rank_loc": 2,
+ "score_data": 0.349,
+ "score_data_loc": 0.909,
+ "score_loc": 0.2
+ },
+ {
+ "component": "Calcaric fluvisols",
+ "componentData": "Data Complete",
+ "componentID": 101342,
+ "name": "Calcaric fluvisols",
+ "rank_data": "6",
+ "rank_data_loc": "4",
+ "rank_loc": 1,
+ "score_data": 0.183,
+ "score_data_loc": 0.8,
+ "score_loc": 0.3
+ },
+ {
+ "component": "Haplic calcisols",
+ "componentData": "Data Complete",
+ "componentID": 101345,
+ "name": "Haplic calcisols",
+ "rank_data": "4",
+ "rank_data_loc": "5",
+ "rank_loc": 3,
+ "score_data": 0.234,
+ "score_data_loc": 0.719,
+ "score_loc": 0.2
+ },
+ {
+ "component": "Lithic leptosols",
+ "componentData": "Missing Data",
+ "componentID": 101347,
+ "name": "Lithic leptosols",
+ "rank_data": "5",
+ "rank_data_loc": "6",
+ "rank_loc": 6,
+ "score_data": 0.233,
+ "score_data_loc": 0.003,
+ "score_loc": 0.05
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[34.5,69.16667].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[34.5,69.16667].json
new file mode 100644
index 0000000..2c5e16a
--- /dev/null
+++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[34.5,69.16667].json
@@ -0,0 +1,443 @@
+{
+ "list": {
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 16.4,
+ "sl5": 16.29,
+ "sl6": 16.0,
+ "sl7": 15.67
+ },
+ "clay": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0,
+ "sl4": 21.2,
+ "sl5": 21.29,
+ "sl6": 21.0,
+ "sl7": 20.83
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 0.86,
+ "sl6": 0.6,
+ "sl7": 0.67
+ },
+ "id": {
+ "component": "Calcaric cambisols",
+ "name": "Calcaric cambisols",
+ "rank_loc": "1",
+ "score_loc": 0.526
+ },
+ "ph": {
+ "sl1": 8.2,
+ "sl2": 8.2,
+ "sl3": 8.2,
+ "sl4": 8.22,
+ "sl5": 8.24,
+ "sl6": 8.26,
+ "sl7": 8.27
+ },
+ "rock_fragments": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 5.0,
+ "sl5": 6.14,
+ "sl6": 7.4,
+ "sl7": 7.17
+ },
+ "sand": {
+ "sl1": 43.0,
+ "sl2": 43.0,
+ "sl3": 43.0,
+ "sl4": 41.2,
+ "sl5": 41.14,
+ "sl6": 41.6,
+ "sl7": 41.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 128962,
+ "distance": 0.0,
+ "mapunitID": 33040,
+ "minCompDistance": 0.0,
+ "share": 51,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.",
+ "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.",
+ "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.",
+ "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.",
+ "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ",
+ "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.",
+ "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ",
+ "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 13.4,
+ "sl5": 13.29,
+ "sl6": 13.0,
+ "sl7": 12.67
+ },
+ "clay": {
+ "sl1": 15.0,
+ "sl2": 15.0,
+ "sl3": 15.0,
+ "sl4": 15.4,
+ "sl5": 15.43,
+ "sl6": 15.8,
+ "sl7": 16.17
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.6,
+ "sl5": 1.71,
+ "sl6": 1.6,
+ "sl7": 1.83
+ },
+ "id": {
+ "component": "Calcaric regosols",
+ "name": "Calcaric regosols",
+ "rank_loc": "2",
+ "score_loc": 0.363
+ },
+ "ph": {
+ "sl1": 8.2,
+ "sl2": 8.2,
+ "sl3": 8.2,
+ "sl4": 8.26,
+ "sl5": 8.27,
+ "sl6": 8.28,
+ "sl7": 8.28
+ },
+ "rock_fragments": {
+ "sl1": 9.0,
+ "sl2": 9.0,
+ "sl3": 9.0,
+ "sl4": 9.4,
+ "sl5": 8.0,
+ "sl6": 7.4,
+ "sl7": 7.83
+ },
+ "sand": {
+ "sl1": 55.0,
+ "sl2": 55.0,
+ "sl3": 55.0,
+ "sl4": 54.0,
+ "sl5": 53.71,
+ "sl6": 52.8,
+ "sl7": 52.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 128963,
+ "distance": 0.0,
+ "mapunitID": 33040,
+ "minCompDistance": 0.0,
+ "share": 49,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ",
+ "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ",
+ "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ",
+ "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ",
+ "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ",
+ "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.",
+ "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ",
+ "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy loam",
+ "sl5": "Sandy loam",
+ "sl6": "Sandy loam",
+ "sl7": "Sandy loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20
+ },
+ "cec": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0
+ },
+ "clay": {
+ "sl1": 12.0,
+ "sl2": 12.0,
+ "sl3": 12.0
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0
+ },
+ "id": {
+ "component": "Lithic leptosols",
+ "name": "Lithic leptosols",
+ "rank_loc": "3",
+ "score_loc": 0.1
+ },
+ "ph": {
+ "sl1": 7.4,
+ "sl2": 7.4,
+ "sl3": 7.4
+ },
+ "rock_fragments": {
+ "sl1": 18.0,
+ "sl2": 18.0,
+ "sl3": 18.0
+ },
+ "sand": {
+ "sl1": 66.0,
+ "sl2": 66.0,
+ "sl3": 66.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 129018,
+ "distance": 1530.36,
+ "mapunitID": 33077,
+ "minCompDistance": 1530.36022174,
+ "share": 72,
+ "soilDepth": 20
+ },
+ "siteDescription": {
+ "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ",
+ "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ",
+ "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.",
+ "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ",
+ "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 89.0,
+ "sl2": 89.0,
+ "sl3": 89.0,
+ "sl4": 87.6,
+ "sl5": 85.14,
+ "sl6": 80.0,
+ "sl7": 75.67
+ },
+ "clay": {
+ "sl1": 30.0,
+ "sl2": 30.0,
+ "sl3": 30.0,
+ "sl4": 27.2,
+ "sl5": 25.86,
+ "sl6": 23.8,
+ "sl7": 22.5
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.0,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Histosols",
+ "name": "Histosols",
+ "rank_loc": "4",
+ "score_loc": 0.012
+ },
+ "ph": {
+ "sl1": 5.0,
+ "sl2": 5.0,
+ "sl3": 5.0,
+ "sl4": 5.06,
+ "sl5": 5.09,
+ "sl6": 5.14,
+ "sl7": 5.18
+ },
+ "rock_fragments": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 12.2,
+ "sl5": 13.86,
+ "sl6": 15.0,
+ "sl7": 15.5
+ },
+ "sand": {
+ "sl1": 30.0,
+ "sl2": 30.0,
+ "sl3": 30.0,
+ "sl4": 32.2,
+ "sl5": 33.86,
+ "sl6": 37.6,
+ "sl7": 40.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 133064,
+ "distance": 9275.857,
+ "mapunitID": 35395,
+ "minCompDistance": 9275.85743626,
+ "share": 100,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Histosols are organic soils that typically form in wet environments.
Their properties are largely dependent on the type and degree of decomposition of the organic soil materials.
The soils can be productive with intensive management including soil drainage, but their fragile nature and habitat suggests preservation of these soils is warranted where possible.
When cultivated, subsidence and sulfide oxidation present management challenges. ",
+ "Description_es": "Los Histosoles son suelos orgánicos que suelen formarse en ambientes húmedos.
Sus propiedades dependen en gran medida del tipo y el grado de descomposición de los materiales orgánicos del suelo.
Los suelos pueden ser productivos con una gestión intensiva que incluya el drenaje del suelo, pero su naturaleza frágil y su hábitat sugieren que se garantice la preservación de estos suelos cuando sea posible.
Cuando se cultivan, el hundimiento y la oxidación de los sulfuros plantean problemas de gestión. ",
+ "Description_fr": "Histosols are organic soils that typically form in wet environments.
Their properties are largely dependent on the type and degree of decomposition of the organic soil materials.
The soils can be productive with intensive management including soil drainage, but their fragile nature and habitat suggests preservation of these soils is warranted where possible.
When cultivated, subsidence and sulfide oxidation present management challenges. ",
+ "Description_ks": "Histosols are organic soils that typically form in wet environments.
Their properties are largely dependent on the type and degree of decomposition of the organic soil materials.
The soils can be productive with intensive management including soil drainage, but their fragile nature and habitat suggests preservation of these soils is warranted where possible.
When cultivated, subsidence and sulfide oxidation present management challenges. ",
+ "Management_en": "These soils can be some of our most productive soils, especially for specialty crops such as vegetables.
However, they must be drained for use, and this will lead to subsidence of the soil, as exposed peat is rapidly mineralized, and organic matter content quickly drops.
This will lead to increasingly acid soils, and thus regular liming will be needed.
These organic soils must be managed differently from mineral soils, and techniques that minimize organic matter degradation are a priority.
Maintenance of native vegetation is the best use. ",
+ "Management_es": "Estos suelos pueden ser algunos de los más productivos, especialmente para cultivos especiales como las hortalizas.
Sin embargo, deben ser drenados para su uso, y esto conducirá al hundimiento del suelo, ya que la turba expuesta se mineraliza rápidamente, y el contenido de materia orgánica disminuye rápidamente.
Esto hará que los suelos sean cada vez más ácidos, por lo que será necesario un encalado regular.
Estos suelos orgánicos deben gestionarse de forma diferente a los suelos minerales, y las técnicas que minimizan la degradación de la materia orgánica son una prioridad.
El mantenimiento de la vegetación autóctona es el mejor uso.",
+ "Management_fr": "These soils can be some of our most productive soils, especially for specialty crops such as vegetables.
However, they must be drained for use, and this will lead to subsidence of the soil, as exposed peat is rapidly mineralized, and organic matter content quickly drops.
This will lead to increasingly acid soils, and thus regular liming will be needed.
These organic soils must be managed differently from mineral soils, and techniques that minimize organic matter degradation are a priority.
Maintenance of native vegetation is the best use. ",
+ "Management_ks": "These soils can be some of our most productive soils, especially for specialty crops such as vegetables.
However, they must be drained for use, and this will lead to subsidence of the soil, as exposed peat is rapidly mineralized, and organic matter content quickly drops.
This will lead to increasingly acid soils, and thus regular liming will be needed.
These organic soils must be managed differently from mineral soils, and techniques that minimize organic matter degradation are a priority.
Maintenance of native vegetation is the best use. "
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "global",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Calcaric cambisols",
+ "componentData": "Data Complete",
+ "componentID": 128962,
+ "name": "Calcaric cambisols",
+ "rank_data": "1",
+ "rank_data_loc": "1",
+ "rank_loc": 1,
+ "score_data": 1.0,
+ "score_data_loc": 1.0,
+ "score_loc": 0.526
+ },
+ {
+ "component": "Calcaric regosols",
+ "componentData": "Data Complete",
+ "componentID": 128963,
+ "name": "Calcaric regosols",
+ "rank_data": "3",
+ "rank_data_loc": "2",
+ "rank_loc": 2,
+ "score_data": 0.437,
+ "score_data_loc": 0.524,
+ "score_loc": 0.363
+ },
+ {
+ "component": "Histosols",
+ "componentData": "Data Complete",
+ "componentID": 133064,
+ "name": "Histosols",
+ "rank_data": "4",
+ "rank_data_loc": "3",
+ "rank_loc": 4,
+ "score_data": 0.437,
+ "score_data_loc": 0.295,
+ "score_loc": 0.012
+ },
+ {
+ "component": "Lithic leptosols",
+ "componentData": "Missing Data",
+ "componentID": 129018,
+ "name": "Lithic leptosols",
+ "rank_data": "2",
+ "rank_data_loc": "4",
+ "rank_loc": 3,
+ "score_data": 0.563,
+ "score_data_loc": 0.001,
+ "score_loc": 0.1
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[37.33333,-5.4].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[37.33333,-5.4].json
new file mode 100644
index 0000000..7d3cf8b
--- /dev/null
+++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[37.33333,-5.4].json
@@ -0,0 +1,1427 @@
+{
+ "list": {
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 41.0,
+ "sl2": 41.0,
+ "sl3": 41.0,
+ "sl4": 41.0,
+ "sl5": 41.0,
+ "sl6": 41.0,
+ "sl7": 40.5
+ },
+ "clay": {
+ "sl1": 55.0,
+ "sl2": 55.0,
+ "sl3": 55.0,
+ "sl4": 56.8,
+ "sl5": 57.14,
+ "sl6": 57.0,
+ "sl7": 56.5
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.2,
+ "sl5": 0.43,
+ "sl6": 0.6,
+ "sl7": 0.67
+ },
+ "id": {
+ "component": "Eutric vertisols",
+ "name": "Eutric vertisols",
+ "rank_loc": "1",
+ "score_loc": 0.278
+ },
+ "ph": {
+ "sl1": 6.8,
+ "sl2": 6.8,
+ "sl3": 6.8,
+ "sl4": 7.02,
+ "sl5": 7.13,
+ "sl6": 7.26,
+ "sl7": 7.33
+ },
+ "rock_fragments": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 4.0,
+ "sl5": 4.14,
+ "sl6": 4.2,
+ "sl7": 4.0
+ },
+ "sand": {
+ "sl1": 13.0,
+ "sl2": 13.0,
+ "sl3": 13.0,
+ "sl4": 12.4,
+ "sl5": 12.29,
+ "sl6": 12.4,
+ "sl7": 12.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 157428,
+ "distance": 0.0,
+ "mapunitID": 9683,
+ "minCompDistance": 0.0,
+ "share": 80,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.",
+ "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ",
+ "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.",
+ "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.",
+ "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ",
+ "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.",
+ "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ",
+ "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. "
+ }
+ },
+ "texture": {
+ "sl1": "Unknown",
+ "sl2": "Unknown",
+ "sl3": "Unknown",
+ "sl4": "Unknown",
+ "sl5": "Unknown",
+ "sl6": "Unknown",
+ "sl7": "Unknown"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 16.4,
+ "sl5": 16.29,
+ "sl6": 16.0,
+ "sl7": 15.67
+ },
+ "clay": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0,
+ "sl4": 21.2,
+ "sl5": 21.29,
+ "sl6": 21.0,
+ "sl7": 20.83
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 0.86,
+ "sl6": 0.6,
+ "sl7": 0.67
+ },
+ "id": {
+ "component": "Calcaric cambisols",
+ "name": "Calcaric cambisols",
+ "rank_loc": "2",
+ "score_loc": 0.268
+ },
+ "ph": {
+ "sl1": 8.2,
+ "sl2": 8.2,
+ "sl3": 8.2,
+ "sl4": 8.22,
+ "sl5": 8.24,
+ "sl6": 8.26,
+ "sl7": 8.27
+ },
+ "rock_fragments": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 5.0,
+ "sl5": 6.14,
+ "sl6": 7.4,
+ "sl7": 7.17
+ },
+ "sand": {
+ "sl1": 43.0,
+ "sl2": 43.0,
+ "sl3": 43.0,
+ "sl4": 41.2,
+ "sl5": 41.14,
+ "sl6": 41.6,
+ "sl7": 41.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 157533,
+ "distance": 0.0,
+ "mapunitID": 9718,
+ "minCompDistance": 0.0,
+ "share": 60,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.",
+ "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.",
+ "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.",
+ "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.",
+ "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ",
+ "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.",
+ "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ",
+ "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 17.0,
+ "sl2": 17.0,
+ "sl3": 17.0,
+ "sl4": 16.4,
+ "sl5": 16.29,
+ "sl6": 16.2,
+ "sl7": 16.33
+ },
+ "clay": {
+ "sl1": 29.0,
+ "sl2": 29.0,
+ "sl3": 29.0,
+ "sl4": 30.2,
+ "sl5": 30.14,
+ "sl6": 29.8,
+ "sl7": 30.0
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 0.6,
+ "sl5": 0.57,
+ "sl6": 0.4,
+ "sl7": 0.5
+ },
+ "id": {
+ "component": "Eutric regosols",
+ "name": "Eutric regosols",
+ "rank_loc": "3",
+ "score_loc": 0.078
+ },
+ "ph": {
+ "sl1": 8.0,
+ "sl2": 8.0,
+ "sl3": 8.0,
+ "sl4": 8.06,
+ "sl5": 8.09,
+ "sl6": 8.1,
+ "sl7": 8.1
+ },
+ "rock_fragments": {
+ "sl1": 5.0,
+ "sl2": 5.0,
+ "sl3": 5.0,
+ "sl4": 5.6,
+ "sl5": 6.57,
+ "sl6": 8.8,
+ "sl7": 10.17
+ },
+ "sand": {
+ "sl1": 31.0,
+ "sl2": 31.0,
+ "sl3": 31.0,
+ "sl4": 29.6,
+ "sl5": 29.29,
+ "sl6": 29.2,
+ "sl7": 28.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 157429,
+ "distance": 0.0,
+ "mapunitID": 9683,
+ "minCompDistance": 0.0,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ",
+ "Description_es": "Regosoles Éutricos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Eutricos tienen una alta saturación de base en el subsuelo. ",
+ "Description_fr": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ",
+ "Description_ks": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ",
+ "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ",
+ "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Estos suelos pueden ser productivos, si se les proporciona riego y fertilización.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.",
+ "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ",
+ "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. "
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 12.0,
+ "sl2": 12.0,
+ "sl3": 12.0,
+ "sl4": 12.0,
+ "sl5": 12.0,
+ "sl6": 12.0,
+ "sl7": 12.0
+ },
+ "clay": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 17.2,
+ "sl5": 17.29,
+ "sl6": 17.2,
+ "sl7": 17.5
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.14,
+ "sl6": 1.2,
+ "sl7": 1.17
+ },
+ "id": {
+ "component": "Gleyic acrisols",
+ "name": "Gleyic acrisols",
+ "rank_loc": "4",
+ "score_loc": 0.065
+ },
+ "ph": {
+ "sl1": 6.6,
+ "sl2": 6.6,
+ "sl3": 6.6,
+ "sl4": 6.7,
+ "sl5": 6.76,
+ "sl6": 6.8,
+ "sl7": 6.83
+ },
+ "rock_fragments": {
+ "sl1": 18.0,
+ "sl2": 18.0,
+ "sl3": 18.0,
+ "sl4": 18.8,
+ "sl5": 21.0,
+ "sl6": 22.8,
+ "sl7": 22.17
+ },
+ "sand": {
+ "sl1": 56.0,
+ "sl2": 56.0,
+ "sl3": 56.0,
+ "sl4": 55.6,
+ "sl5": 55.86,
+ "sl6": 56.2,
+ "sl7": 54.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 157547,
+ "distance": 1849.359,
+ "mapunitID": 9723,
+ "minCompDistance": 1849.35910793,
+ "share": 45,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Gleyic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Gleyic Acrisols have a seasonal high-water table resulting in saturation during some time of the year.",
+ "Description_es": "Los Acrisoles Gleyicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Los acrisoles gleyicos tienen un nivel freático alto estacional que provoca la saturación durante algunas épocas del año. ",
+ "Description_fr": "Gleyic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Gleyic Acrisols have a seasonal high-water table resulting in saturation during some time of the year.",
+ "Description_ks": "Gleyic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Gleyic Acrisols have a seasonal high-water table resulting in saturation during some time of the year.",
+ "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Periods of saturation limit root growth and increase nitrogen loss.
To prevent N loss from leaching anddenitrification consider use of slow-release N fertilizers (sulfur-coated urea (SCU), for example), if those slow-release products are available, or use manures or other organic wastes for their slow-release properties.
Drainage of these soils may be needed, but this can be problematic, as the wetness is due to the high water table. ",
+ "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.
Los períodos de saturación limitan el crecimiento de las raíces y aumentan la pérdida de nitrógeno.
Para evitar la pérdida de N por lixiviación y/o desnitrificación, considere el uso de fertilizantes de liberación lenta de N (urea recubierta de azufre (SCU), por ejemplo), si esos productos de liberación lenta están disponibles, o utilice estiércol u otros residuos orgánicos por sus propiedades de liberación lenta.
Puede ser necesario el drenaje de estos suelos, pero esto puede ser problemático, ya que la humedad se debe al alto nivel freático. ",
+ "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Periods of saturation limit root growth and increase nitrogen loss.
To prevent N loss from leaching anddenitrification consider use of slow-release N fertilizers (sulfur-coated urea (SCU), for example), if those slow-release products are available, or use manures or other organic wastes for their slow-release properties.
Drainage of these soils may be needed, but this can be problematic, as the wetness is due to the high water table. ",
+ "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Periods of saturation limit root growth and increase nitrogen loss.
To prevent N loss from leaching anddenitrification consider use of slow-release N fertilizers (sulfur-coated urea (SCU), for example), if those slow-release products are available, or use manures or other organic wastes for their slow-release properties.
Drainage of these soils may be needed, but this can be problematic, as the wetness is due to the high water table. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy loam",
+ "sl5": "Sandy loam",
+ "sl6": "Sandy loam",
+ "sl7": "Sandy loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 7.0,
+ "sl2": 7.0,
+ "sl3": 7.0,
+ "sl4": 7.0,
+ "sl5": 7.0,
+ "sl6": 7.4,
+ "sl7": 7.83
+ },
+ "clay": {
+ "sl1": 15.0,
+ "sl2": 15.0,
+ "sl3": 15.0,
+ "sl4": 21.4,
+ "sl5": 24.86,
+ "sl6": 28.2,
+ "sl7": 29.17
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Calcaric fluvisols",
+ "name": "Calcaric fluvisols",
+ "rank_loc": "5",
+ "score_loc": 0.057
+ },
+ "ph": {
+ "sl1": 5.2,
+ "sl2": 5.2,
+ "sl3": 5.2,
+ "sl4": 5.1,
+ "sl5": 5.03,
+ "sl6": 4.96,
+ "sl7": 4.93
+ },
+ "rock_fragments": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 2.0,
+ "sl5": 3.0,
+ "sl6": 4.0,
+ "sl7": 4.5
+ },
+ "sand": {
+ "sl1": 57.0,
+ "sl2": 57.0,
+ "sl3": 57.0,
+ "sl4": 51.8,
+ "sl5": 49.57,
+ "sl6": 48.0,
+ "sl7": 47.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 157400,
+ "distance": 21368.302,
+ "mapunitID": 9673,
+ "minCompDistance": 21368.30187518,
+ "share": 80,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.",
+ "Description_es": "Los Fluvisoles Calcáricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles calcáricos tienen carbonatos y un pH elevado en la parte superior del suelo.",
+ "Description_fr": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.",
+ "Description_ks": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.",
+ "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o el manejo de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Una vez en cultivo continuo se debe tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una vía para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).",
+ "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 13.0,
+ "sl2": 13.0,
+ "sl3": 13.0,
+ "sl4": 14.0,
+ "sl5": 14.0,
+ "sl6": 14.0,
+ "sl7": 14.0
+ },
+ "clay": {
+ "sl1": 17.0,
+ "sl2": 17.0,
+ "sl3": 17.0,
+ "sl4": 20.2,
+ "sl5": 20.86,
+ "sl6": 21.2,
+ "sl7": 21.33
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.0,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Calcic luvisols",
+ "name": "Calcic luvisols",
+ "rank_loc": "6",
+ "score_loc": 0.057
+ },
+ "ph": {
+ "sl1": 7.5,
+ "sl2": 7.5,
+ "sl3": 7.5,
+ "sl4": 7.72,
+ "sl5": 7.81,
+ "sl6": 7.92,
+ "sl7": 8.0
+ },
+ "rock_fragments": {
+ "sl1": 18.0,
+ "sl2": 18.0,
+ "sl3": 18.0,
+ "sl4": 24.8,
+ "sl5": 27.86,
+ "sl6": 29.8,
+ "sl7": 30.17
+ },
+ "sand": {
+ "sl1": 65.0,
+ "sl2": 65.0,
+ "sl3": 65.0,
+ "sl4": 62.4,
+ "sl5": 62.0,
+ "sl6": 62.0,
+ "sl7": 61.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 157534,
+ "distance": 0.0,
+ "mapunitID": 9718,
+ "minCompDistance": 0.0,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.",
+ "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.",
+ "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.",
+ "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.",
+ "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ",
+ "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.",
+ "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ",
+ "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20
+ },
+ "cec": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0
+ },
+ "clay": {
+ "sl1": 12.0,
+ "sl2": 12.0,
+ "sl3": 12.0
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0
+ },
+ "id": {
+ "component": "Lithic leptosols",
+ "name": "Lithic leptosols",
+ "rank_loc": "7",
+ "score_loc": 0.057
+ },
+ "ph": {
+ "sl1": 7.4,
+ "sl2": 7.4,
+ "sl3": 7.4
+ },
+ "rock_fragments": {
+ "sl1": 18.0,
+ "sl2": 18.0,
+ "sl3": 18.0
+ },
+ "sand": {
+ "sl1": 66.0,
+ "sl2": 66.0,
+ "sl3": 66.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 157535,
+ "distance": 0.0,
+ "mapunitID": 9718,
+ "minCompDistance": 0.0,
+ "share": 20,
+ "soilDepth": 20
+ },
+ "siteDescription": {
+ "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ",
+ "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ",
+ "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.",
+ "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ",
+ "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 13.0,
+ "sl2": 13.0,
+ "sl3": 13.0,
+ "sl4": 13.6,
+ "sl5": 13.57,
+ "sl6": 13.6,
+ "sl7": 14.0
+ },
+ "clay": {
+ "sl1": 21.0,
+ "sl2": 21.0,
+ "sl3": 21.0,
+ "sl4": 21.2,
+ "sl5": 21.43,
+ "sl6": 21.8,
+ "sl7": 22.0
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 2.0,
+ "sl5": 2.29,
+ "sl6": 2.4,
+ "sl7": 2.33
+ },
+ "id": {
+ "component": "Gleyic luvisols",
+ "name": "Gleyic luvisols",
+ "rank_loc": "8",
+ "score_loc": 0.05
+ },
+ "ph": {
+ "sl1": 7.9,
+ "sl2": 7.9,
+ "sl3": 7.9,
+ "sl4": 8.02,
+ "sl5": 8.04,
+ "sl6": 8.06,
+ "sl7": 8.05
+ },
+ "rock_fragments": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 3.4,
+ "sl5": 3.86,
+ "sl6": 5.0,
+ "sl7": 5.83
+ },
+ "sand": {
+ "sl1": 39.0,
+ "sl2": 39.0,
+ "sl3": 39.0,
+ "sl4": 39.6,
+ "sl5": 39.71,
+ "sl6": 39.4,
+ "sl7": 38.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 157548,
+ "distance": 1849.359,
+ "mapunitID": 9723,
+ "minCompDistance": 1849.35910793,
+ "share": 35,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.",
+ "Description_es": "Los Luvisoles Gleyicos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles Gleyicos están saturados con agua subterránea poco profunda en el metro superior del perfil del suelo.",
+ "Description_fr": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.",
+ "Description_ks": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.",
+ "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ",
+ "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación a través de las aguas subterráneas, esto puede no ser posible, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).",
+ "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ",
+ "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 15.6,
+ "sl5": 16.43,
+ "sl6": 17.0,
+ "sl7": 17.0
+ },
+ "clay": {
+ "sl1": 18.0,
+ "sl2": 18.0,
+ "sl3": 18.0,
+ "sl4": 24.0,
+ "sl5": 26.43,
+ "sl6": 27.8,
+ "sl7": 27.67
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.2,
+ "sl5": 0.57,
+ "sl6": 1.0,
+ "sl7": 1.33
+ },
+ "id": {
+ "component": "Calcaric regosols",
+ "name": "Calcaric regosols",
+ "rank_loc": "9",
+ "score_loc": 0.043
+ },
+ "ph": {
+ "sl1": 5.7,
+ "sl2": 5.7,
+ "sl3": 5.7,
+ "sl4": 5.76,
+ "sl5": 5.8,
+ "sl6": 5.9,
+ "sl7": 5.98
+ },
+ "rock_fragments": {
+ "sl1": 3.0,
+ "sl2": 3.0,
+ "sl3": 3.0,
+ "sl4": 2.4,
+ "sl5": 2.43,
+ "sl6": 2.6,
+ "sl7": 2.5
+ },
+ "sand": {
+ "sl1": 31.0,
+ "sl2": 31.0,
+ "sl3": 31.0,
+ "sl4": 28.2,
+ "sl5": 27.14,
+ "sl6": 26.8,
+ "sl7": 27.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 157495,
+ "distance": 13892.147,
+ "mapunitID": 9703,
+ "minCompDistance": 13892.14700639,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ",
+ "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ",
+ "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ",
+ "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ",
+ "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ",
+ "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.",
+ "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ",
+ "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. "
+ }
+ },
+ "texture": {
+ "sl1": "Silt loam",
+ "sl2": "Silt loam",
+ "sl3": "Silt loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 16.4,
+ "sl5": 16.43,
+ "sl6": 16.6,
+ "sl7": 16.17
+ },
+ "clay": {
+ "sl1": 24.0,
+ "sl2": 24.0,
+ "sl3": 24.0,
+ "sl4": 24.6,
+ "sl5": 25.0,
+ "sl6": 25.4,
+ "sl7": 25.17
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.14,
+ "sl6": 1.2,
+ "sl7": 1.5
+ },
+ "id": {
+ "component": "Dystric planosols",
+ "name": "Dystric planosols",
+ "rank_loc": "10",
+ "score_loc": 0.029
+ },
+ "ph": {
+ "sl1": 7.9,
+ "sl2": 7.9,
+ "sl3": 7.9,
+ "sl4": 7.98,
+ "sl5": 8.01,
+ "sl6": 8.06,
+ "sl7": 8.03
+ },
+ "rock_fragments": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 13.4,
+ "sl5": 12.86,
+ "sl6": 12.4,
+ "sl7": 12.5
+ },
+ "sand": {
+ "sl1": 44.0,
+ "sl2": 44.0,
+ "sl3": 44.0,
+ "sl4": 42.8,
+ "sl5": 42.14,
+ "sl6": 41.2,
+ "sl7": 41.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 157549,
+ "distance": 1849.359,
+ "mapunitID": 9723,
+ "minCompDistance": 1849.35910793,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.",
+ "Description_es": "Los Planosoles Dístricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren de drenaje para la producción de cultivos.
Los Planosoles Dístricos son suelos menos productivos con baja saturación de base en el subsuelo.",
+ "Description_fr": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.",
+ "Description_ks": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.",
+ "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed.",
+ "Management_es": "Situados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requerirán una fertilización adicional.
Los niveles de calcio son muy bajos en el perfil inferior de este suelo.
Se necesitará una fertilización suplementaria.",
+ "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed.",
+ "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed."
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 13.4,
+ "sl5": 13.29,
+ "sl6": 13.0,
+ "sl7": 12.67
+ },
+ "clay": {
+ "sl1": 15.0,
+ "sl2": 15.0,
+ "sl3": 15.0,
+ "sl4": 15.4,
+ "sl5": 15.43,
+ "sl6": 15.8,
+ "sl7": 16.17
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.6,
+ "sl5": 1.71,
+ "sl6": 1.6,
+ "sl7": 1.83
+ },
+ "id": {
+ "component": "Rendzic leptosols",
+ "name": "Rendzic leptosols",
+ "rank_loc": "11",
+ "score_loc": 0.018
+ },
+ "ph": {
+ "sl1": 8.2,
+ "sl2": 8.2,
+ "sl3": 8.2,
+ "sl4": 8.26,
+ "sl5": 8.27,
+ "sl6": 8.28,
+ "sl7": 8.28
+ },
+ "rock_fragments": {
+ "sl1": 9.0,
+ "sl2": 9.0,
+ "sl3": 9.0,
+ "sl4": 9.4,
+ "sl5": 8.0,
+ "sl6": 7.4,
+ "sl7": 7.83
+ },
+ "sand": {
+ "sl1": 55.0,
+ "sl2": 55.0,
+ "sl3": 55.0,
+ "sl4": 54.0,
+ "sl5": 53.71,
+ "sl6": 52.8,
+ "sl7": 52.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 157494,
+ "distance": 13892.147,
+ "mapunitID": 9703,
+ "minCompDistance": 13892.14700639,
+ "share": 25,
+ "soilDepth": 40
+ },
+ "siteDescription": {
+ "Description_en": "Rendzic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Rendzic Leptosols are highly calcareous at the soil surface. ",
+ "Description_es": "Los Leptosoles Rendzicos tienen un volumen de enraizamiento muy limitado debido a la roca continua, material altamente calcáreo, horizontes cementados, o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles Rendzic son altamente calcáreos en la superficie del suelo. ",
+ "Description_fr": "Rendzic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Rendzic Leptosols are highly calcareous at the soil surface. ",
+ "Description_ks": "Rendzic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Rendzic Leptosols are highly calcareous at the soil surface. ",
+ "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Soil pH will be high (> 7.0) in these soils, and no liming will be needed.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ",
+ "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
El pH del suelo será alto (> 7,0) en estos suelos, y no será necesario el encalado.
Cualquier uso agrícola debe ser para el pastoreo o la agrosilvicultura, con el mantenimiento continuo de la cubierta.",
+ "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Soil pH will be high (> 7.0) in these soils, and no liming will be needed.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ",
+ "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Soil pH will be high (> 7.0) in these soils, and no liming will be needed.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy loam",
+ "sl5": "Sandy loam",
+ "sl6": "Sandy loam",
+ "sl7": "Sandy loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 12.0,
+ "sl2": 12.0,
+ "sl3": 12.0,
+ "sl4": 13.2,
+ "sl5": 14.71,
+ "sl6": 15.8,
+ "sl7": 15.67
+ },
+ "clay": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 25.6,
+ "sl5": 31.86,
+ "sl6": 36.2,
+ "sl7": 36.33
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Calcaric cambisols",
+ "name": "Calcaric cambisols2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.268
+ },
+ "ph": {
+ "sl1": 4.7,
+ "sl2": 4.7,
+ "sl3": 4.7,
+ "sl4": 4.78,
+ "sl5": 4.76,
+ "sl6": 4.74,
+ "sl7": 4.87
+ },
+ "rock_fragments": {
+ "sl1": 15.0,
+ "sl2": 15.0,
+ "sl3": 15.0,
+ "sl4": 13.2,
+ "sl5": 11.14,
+ "sl6": 10.2,
+ "sl7": 12.67
+ },
+ "sand": {
+ "sl1": 51.0,
+ "sl2": 51.0,
+ "sl3": 51.0,
+ "sl4": 43.0,
+ "sl5": 38.14,
+ "sl6": 35.2,
+ "sl7": 36.33
+ },
+ "site": {
+ "siteData": {
+ "componentID": 157493,
+ "distance": 13892.147,
+ "mapunitID": 9703,
+ "minCompDistance": 0.0,
+ "share": 55,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.",
+ "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.",
+ "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.",
+ "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.",
+ "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ",
+ "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.",
+ "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ",
+ "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 40
+ },
+ "cec": {
+ "sl1": 24.0,
+ "sl2": 24.0,
+ "sl3": 24.0,
+ "sl4": 20.5
+ },
+ "clay": {
+ "sl1": 27.0,
+ "sl2": 27.0,
+ "sl3": 27.0,
+ "sl4": 27.5
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 2.0
+ },
+ "id": {
+ "component": "Calcaric regosols",
+ "name": "Calcaric regosols2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.043
+ },
+ "ph": {
+ "sl1": 7.7,
+ "sl2": 7.7,
+ "sl3": 7.7,
+ "sl4": 7.8
+ },
+ "rock_fragments": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 27.0
+ },
+ "sand": {
+ "sl1": 36.0,
+ "sl2": 36.0,
+ "sl3": 36.0,
+ "sl4": 36.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 157511,
+ "distance": 20400.034,
+ "mapunitID": 9708,
+ "minCompDistance": 13892.14700639,
+ "share": 40,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ",
+ "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ",
+ "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ",
+ "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ",
+ "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ",
+ "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.",
+ "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ",
+ "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Clay loam"
+ }
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "global",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Calcaric cambisols",
+ "componentData": "Data Complete",
+ "componentID": 157493,
+ "name": "Calcaric cambisols2",
+ "rank_data": "2",
+ "rank_data_loc": "1",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.836,
+ "score_data_loc": 1.0,
+ "score_loc": 0.268
+ },
+ {
+ "component": "Eutric vertisols",
+ "componentData": "No Data",
+ "componentID": 157428,
+ "name": "Eutric vertisols",
+ "rank_data": "5",
+ "rank_data_loc": "2",
+ "rank_loc": "1",
+ "score_data": 0.699,
+ "score_data_loc": 0.885,
+ "score_loc": 0.278
+ },
+ {
+ "component": "Calcaric regosols",
+ "componentData": "Data Complete",
+ "componentID": 157511,
+ "name": "Calcaric regosols2",
+ "rank_data": "1",
+ "rank_data_loc": "3",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.894,
+ "score_data_loc": 0.848,
+ "score_loc": 0.043
+ },
+ {
+ "component": "Eutric regosols",
+ "componentData": "Data Complete",
+ "componentID": 157429,
+ "name": "Eutric regosols",
+ "rank_data": "4",
+ "rank_data_loc": "4",
+ "rank_loc": "3",
+ "score_data": 0.699,
+ "score_data_loc": 0.704,
+ "score_loc": 0.078
+ },
+ {
+ "component": "Gleyic acrisols",
+ "componentData": "Data Complete",
+ "componentID": 157547,
+ "name": "Gleyic acrisols",
+ "rank_data": "6",
+ "rank_data_loc": "5",
+ "rank_loc": "4",
+ "score_data": 0.699,
+ "score_data_loc": 0.692,
+ "score_loc": 0.065
+ },
+ {
+ "component": "Calcaric fluvisols",
+ "componentData": "Data Complete",
+ "componentID": 157400,
+ "name": "Calcaric fluvisols",
+ "rank_data": "7",
+ "rank_data_loc": "6",
+ "rank_loc": "5",
+ "score_data": 0.625,
+ "score_data_loc": 0.618,
+ "score_loc": 0.057
+ },
+ {
+ "component": "Gleyic luvisols",
+ "componentData": "Data Complete",
+ "componentID": 157548,
+ "name": "Gleyic luvisols",
+ "rank_data": "8",
+ "rank_data_loc": "7",
+ "rank_loc": "8",
+ "score_data": 0.625,
+ "score_data_loc": 0.612,
+ "score_loc": 0.05
+ },
+ {
+ "component": "Calcic luvisols",
+ "componentData": "Data Complete",
+ "componentID": 157534,
+ "name": "Calcic luvisols",
+ "rank_data": "11",
+ "rank_data_loc": "8",
+ "rank_loc": "6",
+ "score_data": 0.412,
+ "score_data_loc": 0.425,
+ "score_loc": 0.057
+ },
+ {
+ "component": "Dystric planosols",
+ "componentData": "Missing Data",
+ "componentID": 157549,
+ "name": "Dystric planosols",
+ "rank_data": "10",
+ "rank_data_loc": "9",
+ "rank_loc": "10",
+ "score_data": 0.421,
+ "score_data_loc": 0.407,
+ "score_loc": 0.029
+ },
+ {
+ "component": "Lithic leptosols",
+ "componentData": "Missing Data",
+ "componentID": 157535,
+ "name": "Lithic leptosols",
+ "rank_data": "9",
+ "rank_data_loc": "10",
+ "rank_loc": "7",
+ "score_data": 0.49,
+ "score_data_loc": 0.002,
+ "score_loc": 0.057
+ },
+ {
+ "component": "Rendzic leptosols",
+ "componentData": "Missing Data",
+ "componentID": 157494,
+ "name": "Rendzic leptosols",
+ "rank_data": "3",
+ "rank_data_loc": "11",
+ "rank_loc": "11",
+ "score_data": 0.711,
+ "score_data_loc": 0.002,
+ "score_loc": 0.018
+ },
+ {
+ "component": "Calcaric regosols",
+ "componentData": "Data Complete",
+ "componentID": 157495,
+ "name": "Calcaric regosols",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "9",
+ "score_data": 0.864,
+ "score_data_loc": 0.821,
+ "score_loc": 0.043
+ },
+ {
+ "component": "Calcaric cambisols",
+ "componentData": "Data Complete",
+ "componentID": 157533,
+ "name": "Calcaric cambisols",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "2",
+ "score_data": 0.525,
+ "score_data_loc": 0.718,
+ "score_loc": 0.268
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[48.71667,126.13333].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[48.71667,126.13333].json
new file mode 100644
index 0000000..13ff35c
--- /dev/null
+++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[48.71667,126.13333].json
@@ -0,0 +1,811 @@
+{
+ "list": {
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 34.0,
+ "sl2": 34.0,
+ "sl3": 34.0,
+ "sl4": 30.2,
+ "sl5": 28.86,
+ "sl6": 26.8,
+ "sl7": 25.67
+ },
+ "clay": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 19.8,
+ "sl5": 19.71,
+ "sl6": 18.8,
+ "sl7": 18.5
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.6,
+ "sl5": 0.71,
+ "sl6": 0.8,
+ "sl7": 0.83
+ },
+ "id": {
+ "component": "Haplic andosols",
+ "name": "Haplic andosols",
+ "rank_loc": "1",
+ "score_loc": 0.366
+ },
+ "ph": {
+ "sl1": 5.9,
+ "sl2": 5.9,
+ "sl3": 5.9,
+ "sl4": 6.08,
+ "sl5": 6.13,
+ "sl6": 6.18,
+ "sl7": 6.18
+ },
+ "rock_fragments": {
+ "sl1": 13.0,
+ "sl2": 13.0,
+ "sl3": 13.0,
+ "sl4": 13.6,
+ "sl5": 14.43,
+ "sl6": 16.8,
+ "sl7": 18.5
+ },
+ "sand": {
+ "sl1": 40.0,
+ "sl2": 40.0,
+ "sl3": 40.0,
+ "sl4": 39.4,
+ "sl5": 40.14,
+ "sl6": 42.4,
+ "sl7": 43.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 103929,
+ "distance": 0.0,
+ "mapunitID": 11372,
+ "minCompDistance": 0.0,
+ "share": 100,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility. ",
+ "Description_es": "Los Andosoles Háplicos se forman en materiales volcánicos.
Estos suelos son muy erosionables y tienen una alta fijación de P, pero la mayoría tienen una capacidad de retención de agua y una fertilidad del suelo relativamente buenas. ",
+ "Description_fr": "Haplic Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility. ",
+ "Description_ks": "Haplic Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility. ",
+ "Management_en": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion. ",
+ "Management_es": "La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Debido a que estos suelos se forman a partir de materiales volcánicos, una parte de su carga es positiva, lo que significa que pueden \"fijar\" el fósforo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y rendimiento adecuados de los cultivos.
Los cultivos de cobertura y las rotaciones que incluyan leguminosas y la inclusión de cultivos con alta biomasa serán beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Los sistemas agroforestales pueden ayudar a minimizar la erosión.",
+ "Management_fr": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion. ",
+ "Management_ks": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 22.0,
+ "sl2": 22.0,
+ "sl3": 22.0,
+ "sl4": 21.2,
+ "sl5": 20.57,
+ "sl6": 19.6,
+ "sl7": 19.0
+ },
+ "clay": {
+ "sl1": 26.0,
+ "sl2": 26.0,
+ "sl3": 26.0,
+ "sl4": 26.4,
+ "sl5": 26.14,
+ "sl6": 25.6,
+ "sl7": 25.0
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Haplic phaeozems",
+ "name": "Haplic phaeozems",
+ "rank_loc": "2",
+ "score_loc": 0.194
+ },
+ "ph": {
+ "sl1": 6.2,
+ "sl2": 6.2,
+ "sl3": 6.2,
+ "sl4": 6.36,
+ "sl5": 6.46,
+ "sl6": 6.58,
+ "sl7": 6.68
+ },
+ "rock_fragments": {
+ "sl1": 5.0,
+ "sl2": 5.0,
+ "sl3": 5.0,
+ "sl4": 4.8,
+ "sl5": 4.57,
+ "sl6": 4.6,
+ "sl7": 4.67
+ },
+ "sand": {
+ "sl1": 28.0,
+ "sl2": 28.0,
+ "sl3": 28.0,
+ "sl4": 28.4,
+ "sl5": 29.14,
+ "sl6": 30.2,
+ "sl7": 31.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 103604,
+ "distance": 2611.703,
+ "mapunitID": 11112,
+ "minCompDistance": 2611.70290883,
+ "share": 100,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.",
+ "Description_es": "Los Phaeozems Háplicos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que se necesite el riego para la producción.",
+ "Description_fr": "Haplic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.",
+ "Description_ks": "Haplic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.",
+ "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.",
+ "Management_es": "Estos suelos son altamente productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).",
+ "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.",
+ "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed."
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 15.0,
+ "sl2": 15.0,
+ "sl3": 15.0,
+ "sl4": 15.0,
+ "sl5": 15.0,
+ "sl6": 14.8,
+ "sl7": 14.5
+ },
+ "clay": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 23.0,
+ "sl5": 24.14,
+ "sl6": 24.6,
+ "sl7": 24.5
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.0,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Haplic luvisols",
+ "name": "Haplic luvisols",
+ "rank_loc": "3",
+ "score_loc": 0.165
+ },
+ "ph": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 6.02,
+ "sl5": 6.06,
+ "sl6": 6.12,
+ "sl7": 6.2
+ },
+ "rock_fragments": {
+ "sl1": 7.0,
+ "sl2": 7.0,
+ "sl3": 7.0,
+ "sl4": 11.0,
+ "sl5": 12.29,
+ "sl6": 13.6,
+ "sl7": 14.17
+ },
+ "sand": {
+ "sl1": 31.0,
+ "sl2": 31.0,
+ "sl3": 31.0,
+ "sl4": 31.2,
+ "sl5": 31.71,
+ "sl6": 33.0,
+ "sl7": 33.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 104599,
+ "distance": 9855.721,
+ "mapunitID": 11910,
+ "minCompDistance": 9855.72065557,
+ "share": 100,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.",
+ "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.",
+ "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.",
+ "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.",
+ "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.",
+ "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops."
+ }
+ },
+ "texture": {
+ "sl1": "Silt loam",
+ "sl2": "Silt loam",
+ "sl3": "Silt loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 27.0,
+ "sl2": 27.0,
+ "sl3": 27.0,
+ "sl4": 26.4,
+ "sl5": 25.57,
+ "sl6": 24.6,
+ "sl7": 24.0
+ },
+ "clay": {
+ "sl1": 28.0,
+ "sl2": 28.0,
+ "sl3": 28.0,
+ "sl4": 28.8,
+ "sl5": 29.29,
+ "sl6": 29.4,
+ "sl7": 29.17
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Gleyic phaeozems",
+ "name": "Gleyic phaeozems",
+ "rank_loc": "4",
+ "score_loc": 0.11
+ },
+ "ph": {
+ "sl1": 7.1,
+ "sl2": 7.1,
+ "sl3": 7.1,
+ "sl4": 7.16,
+ "sl5": 7.19,
+ "sl6": 7.24,
+ "sl7": 7.28
+ },
+ "rock_fragments": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 7.4,
+ "sl5": 9.43,
+ "sl6": 11.2,
+ "sl7": 10.5
+ },
+ "sand": {
+ "sl1": 34.0,
+ "sl2": 34.0,
+ "sl3": 34.0,
+ "sl4": 33.8,
+ "sl5": 33.71,
+ "sl6": 34.4,
+ "sl7": 34.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 103605,
+ "distance": 12988.596,
+ "mapunitID": 11113,
+ "minCompDistance": 12988.59595592,
+ "share": 100,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Gleyic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Gleyic Phaeozems are saturated with shallow groundwater within one meter of the soil surface.",
+ "Description_es": "Los Phaeozems Gléyicos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los feozems gleyicos están saturados de agua subterránea poco profunda a menos de un metro de la superficie del suelo.",
+ "Description_fr": "Gleyic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Gleyic Phaeozems are saturated with shallow groundwater within one meter of the soil surface.",
+ "Description_ks": "Gleyic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Gleyic Phaeozems are saturated with shallow groundwater within one meter of the soil surface.",
+ "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ",
+ "Management_es": "Estos suelos son muy productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación a través de las aguas subterráneas, esto puede no ser posible, por lo que hay que considerar los cultivos de raíz superficial.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).",
+ "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ",
+ "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). "
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 35.0,
+ "sl2": 35.0,
+ "sl3": 35.0,
+ "sl4": 28.4,
+ "sl5": 25.71,
+ "sl6": 22.6,
+ "sl7": 21.17
+ },
+ "clay": {
+ "sl1": 28.0,
+ "sl2": 28.0,
+ "sl3": 28.0,
+ "sl4": 26.8,
+ "sl5": 26.57,
+ "sl6": 26.0,
+ "sl7": 25.67
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 0.8,
+ "sl5": 0.57,
+ "sl6": 1.0,
+ "sl7": 1.33
+ },
+ "id": {
+ "component": "Eutric gleysols",
+ "name": "Eutric gleysols",
+ "rank_loc": "5",
+ "score_loc": 0.055
+ },
+ "ph": {
+ "sl1": 6.7,
+ "sl2": 6.7,
+ "sl3": 6.7,
+ "sl4": 6.98,
+ "sl5": 7.09,
+ "sl6": 7.2,
+ "sl7": 7.25
+ },
+ "rock_fragments": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 2.2,
+ "sl5": 2.43,
+ "sl6": 2.8,
+ "sl7": 3.0
+ },
+ "sand": {
+ "sl1": 31.0,
+ "sl2": 31.0,
+ "sl3": 31.0,
+ "sl4": 34.0,
+ "sl5": 34.57,
+ "sl6": 35.8,
+ "sl7": 36.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 104276,
+ "distance": 14827.397,
+ "mapunitID": 11663,
+ "minCompDistance": 14827.39744996,
+ "share": 100,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.",
+ "Description_es": "Los gleysoles Eútricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles Eutricos son suelos productivos con una alta saturación de la base en la parte superior del suelo.",
+ "Description_fr": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.",
+ "Description_ks": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.",
+ "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ",
+ "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.",
+ "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ",
+ "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. "
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 28.0,
+ "sl2": 28.0,
+ "sl3": 28.0,
+ "sl4": 23.4,
+ "sl5": 21.0,
+ "sl6": 18.2,
+ "sl7": 16.83
+ },
+ "clay": {
+ "sl1": 10.0,
+ "sl2": 10.0,
+ "sl3": 10.0,
+ "sl4": 10.0,
+ "sl5": 10.14,
+ "sl6": 10.2,
+ "sl7": 9.83
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Mollic gleysols",
+ "name": "Mollic gleysols",
+ "rank_loc": "6",
+ "score_loc": 0.055
+ },
+ "ph": {
+ "sl1": 5.7,
+ "sl2": 5.7,
+ "sl3": 5.7,
+ "sl4": 5.82,
+ "sl5": 5.84,
+ "sl6": 5.84,
+ "sl7": 5.85
+ },
+ "rock_fragments": {
+ "sl1": 12.0,
+ "sl2": 12.0,
+ "sl3": 12.0,
+ "sl4": 15.0,
+ "sl5": 17.43,
+ "sl6": 20.0,
+ "sl7": 21.0
+ },
+ "sand": {
+ "sl1": 37.0,
+ "sl2": 37.0,
+ "sl3": 37.0,
+ "sl4": 39.6,
+ "sl5": 41.29,
+ "sl6": 43.6,
+ "sl7": 46.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 104133,
+ "distance": 6486.577,
+ "mapunitID": 11540,
+ "minCompDistance": 6486.5766191,
+ "share": 100,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Mollic Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Mollic Gleysols have relatively higher organic matter and nutrients in surface horizons.",
+ "Description_es": "Los Mollic Gleysols tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles móllicos tienen relativamente más materia orgánica y nutrientes en los horizontes superficiales.",
+ "Description_fr": "Mollic Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Mollic Gleysols have relatively higher organic matter and nutrients in surface horizons.",
+ "Description_ks": "Mollic Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Mollic Gleysols have relatively higher organic matter and nutrients in surface horizons.",
+ "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ",
+ "Management_es": "Estos suelos están saturados y, si se cultivan, se requiere un drenaje importante.
Una vez drenados, estos suelos pueden ser muy productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.",
+ "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ",
+ "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. "
+ }
+ },
+ "texture": {
+ "sl1": "Silt loam",
+ "sl2": "Silt loam",
+ "sl3": "Silt loam",
+ "sl4": "Silt loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 18.0,
+ "sl2": 18.0,
+ "sl3": 18.0,
+ "sl4": 17.4,
+ "sl5": 17.43,
+ "sl6": 17.4,
+ "sl7": 17.0
+ },
+ "clay": {
+ "sl1": 30.0,
+ "sl2": 30.0,
+ "sl3": 30.0,
+ "sl4": 31.8,
+ "sl5": 32.0,
+ "sl6": 31.8,
+ "sl7": 31.17
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 0.8,
+ "sl5": 0.57,
+ "sl6": 0.6,
+ "sl7": 0.83
+ },
+ "id": {
+ "component": "Umbric andosols",
+ "name": "Umbric andosols",
+ "rank_loc": "7",
+ "score_loc": 0.055
+ },
+ "ph": {
+ "sl1": 6.3,
+ "sl2": 6.3,
+ "sl3": 6.3,
+ "sl4": 6.5,
+ "sl5": 6.57,
+ "sl6": 6.66,
+ "sl7": 6.75
+ },
+ "rock_fragments": {
+ "sl1": 8.0,
+ "sl2": 8.0,
+ "sl3": 8.0,
+ "sl4": 8.0,
+ "sl5": 8.86,
+ "sl6": 9.0,
+ "sl7": 9.33
+ },
+ "sand": {
+ "sl1": 24.0,
+ "sl2": 24.0,
+ "sl3": 24.0,
+ "sl4": 23.0,
+ "sl5": 23.14,
+ "sl6": 23.2,
+ "sl7": 23.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 103928,
+ "distance": 7836.2,
+ "mapunitID": 11371,
+ "minCompDistance": 7836.200108,
+ "share": 100,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Umbric Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility.
Umbric Andosols have a thick surface horizon but soils are wetter and have fewer nutrients than Mollic Andosols. ",
+ "Description_es": "Los Andosoles Úmbricos se forman en materiales volcánicos.
Estos suelos son muy erosionables y tienen una alta fijación de P, pero la mayoría tienen una capacidad de retención de agua y una fertilidad del suelo relativamente buenas.
Los Andosoles úmbricos tienen un horizonte superficial grueso, pero los suelos son más húmedos y tienen menos nutrientes que los Andosoles móllicos. ",
+ "Description_fr": "Umbric Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility.
Umbric Andosols have a thick surface horizon but soils are wetter and have fewer nutrients than Mollic Andosols. ",
+ "Description_ks": "Umbric Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility.
Umbric Andosols have a thick surface horizon but soils are wetter and have fewer nutrients than Mollic Andosols. ",
+ "Management_en": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion.
Additional drainage may make these soils more productive.
Fertilization will be essential for effective crop production. ",
+ "Management_es": "La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Dado que estos suelos se forman a partir de materiales volcánicos, una parte de su carga es positiva, lo que significa que pueden \"fijar\" el fósforo, haciéndolo inaccesible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y rendimiento adecuados de los cultivos.
Los cultivos de cobertura y las rotaciones que incluyan leguminosas y la inclusión de cultivos con alta biomasa serán beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Los sistemas agroforestales pueden ayudar a minimizar la erosión.
El drenaje adicional puede hacer que estos suelos sean más productivos.
La fertilización será esencial para la producción efectiva de los cultivos.",
+ "Management_fr": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion.
Additional drainage may make these soils more productive.
Fertilization will be essential for effective crop production. ",
+ "Management_ks": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion.
Additional drainage may make these soils more productive.
Fertilization will be essential for effective crop production. "
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "global",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Haplic luvisols",
+ "componentData": "Data Complete",
+ "componentID": 104599,
+ "name": "Haplic luvisols",
+ "rank_data": "2",
+ "rank_data_loc": "1",
+ "rank_loc": 3,
+ "score_data": 0.431,
+ "score_data_loc": 1.0,
+ "score_loc": 0.165
+ },
+ {
+ "component": "Gleyic phaeozems",
+ "componentData": "Missing Data",
+ "componentID": 103605,
+ "name": "Gleyic phaeozems",
+ "rank_data": "3",
+ "rank_data_loc": "2",
+ "rank_loc": 4,
+ "score_data": 0.385,
+ "score_data_loc": 0.83,
+ "score_loc": 0.11
+ },
+ {
+ "component": "Eutric gleysols",
+ "componentData": "Data Complete",
+ "componentID": 104276,
+ "name": "Eutric gleysols",
+ "rank_data": "1",
+ "rank_data_loc": "3",
+ "rank_loc": 5,
+ "score_data": 0.431,
+ "score_data_loc": 0.815,
+ "score_loc": 0.055
+ },
+ {
+ "component": "Umbric andosols",
+ "componentData": "Data Complete",
+ "componentID": 103928,
+ "name": "Umbric andosols",
+ "rank_data": "4",
+ "rank_data_loc": "4",
+ "rank_loc": 7,
+ "score_data": 0.385,
+ "score_data_loc": 0.738,
+ "score_loc": 0.055
+ },
+ {
+ "component": "Haplic andosols",
+ "componentData": "Data Complete",
+ "componentID": 103929,
+ "name": "Haplic andosols",
+ "rank_data": "5",
+ "rank_data_loc": "5",
+ "rank_loc": 1,
+ "score_data": 0.068,
+ "score_data_loc": 0.729,
+ "score_loc": 0.366
+ },
+ {
+ "component": "Haplic phaeozems",
+ "componentData": "Data Complete",
+ "componentID": 103604,
+ "name": "Haplic phaeozems",
+ "rank_data": "6",
+ "rank_data_loc": "6",
+ "rank_loc": 2,
+ "score_data": 0.068,
+ "score_data_loc": 0.44,
+ "score_loc": 0.194
+ },
+ {
+ "component": "Mollic gleysols",
+ "componentData": "Data Complete",
+ "componentID": 104133,
+ "name": "Mollic gleysols",
+ "rank_data": "7",
+ "rank_data_loc": "7",
+ "rank_loc": 6,
+ "score_data": 0.068,
+ "score_data_loc": 0.207,
+ "score_loc": 0.055
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[7.3318,-1.4631].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[7.3318,-1.4631].json
new file mode 100644
index 0000000..679fe1a
--- /dev/null
+++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[7.3318,-1.4631].json
@@ -0,0 +1,1347 @@
+{
+ "list": {
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 8.0,
+ "sl2": 8.0,
+ "sl3": 8.0,
+ "sl4": 6.8,
+ "sl5": 6.57,
+ "sl6": 6.4,
+ "sl7": 6.33
+ },
+ "clay": {
+ "sl1": 24.0,
+ "sl2": 24.0,
+ "sl3": 24.0,
+ "sl4": 31.2,
+ "sl5": 34.0,
+ "sl6": 36.6,
+ "sl7": 37.67
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Ferric acrisols",
+ "name": "Ferric acrisols",
+ "rank_loc": "1",
+ "score_loc": 0.124
+ },
+ "ph": {
+ "sl1": 5.3,
+ "sl2": 5.3,
+ "sl3": 5.3,
+ "sl4": 5.18,
+ "sl5": 5.16,
+ "sl6": 5.14,
+ "sl7": 5.13
+ },
+ "rock_fragments": {
+ "sl1": 21.0,
+ "sl2": 21.0,
+ "sl3": 21.0,
+ "sl4": 27.8,
+ "sl5": 28.29,
+ "sl6": 27.2,
+ "sl7": 26.33
+ },
+ "sand": {
+ "sl1": 56.0,
+ "sl2": 56.0,
+ "sl3": 56.0,
+ "sl4": 50.2,
+ "sl5": 47.71,
+ "sl6": 45.2,
+ "sl7": 43.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 133233,
+ "distance": 0.0,
+ "mapunitID": 36001,
+ "minCompDistance": 0.0,
+ "share": 15,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.",
+ "Description_es": "Los Acrisoles Férricos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Estos suelos tienen un alto contenido de hierro y es común la presencia de nódulos de hierro.",
+ "Description_fr": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.",
+ "Description_ks": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.",
+ "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ",
+ "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.",
+ "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ",
+ "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy clay loam",
+ "sl2": "Sandy clay loam",
+ "sl3": "Sandy clay loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 9.4,
+ "sl5": 8.57,
+ "sl6": 7.8,
+ "sl7": 8.17
+ },
+ "clay": {
+ "sl1": 23.0,
+ "sl2": 23.0,
+ "sl3": 23.0,
+ "sl4": 24.2,
+ "sl5": 24.29,
+ "sl6": 24.2,
+ "sl7": 24.5
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 1.4,
+ "sl5": 1.43,
+ "sl6": 1.6,
+ "sl7": 1.67
+ },
+ "id": {
+ "component": "Dystric fluvisols",
+ "name": "Dystric fluvisols",
+ "rank_loc": "2",
+ "score_loc": 0.116
+ },
+ "ph": {
+ "sl1": 4.9,
+ "sl2": 4.9,
+ "sl3": 4.9,
+ "sl4": 4.96,
+ "sl5": 4.99,
+ "sl6": 5.04,
+ "sl7": 5.08
+ },
+ "rock_fragments": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 4.8,
+ "sl5": 7.0,
+ "sl6": 9.4,
+ "sl7": 9.67
+ },
+ "sand": {
+ "sl1": 49.0,
+ "sl2": 49.0,
+ "sl3": 49.0,
+ "sl4": 49.2,
+ "sl5": 49.71,
+ "sl6": 50.8,
+ "sl7": 50.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 133237,
+ "distance": 0.0,
+ "mapunitID": 36001,
+ "minCompDistance": 0.0,
+ "share": 5,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_es": "Los Fluvisoles Dístricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los Fluvisoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.",
+ "Description_fr": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_ks": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.",
+ "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ",
+ "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (acolchados, cultivos de cobertura), que mejoren la infiltración del agua o que proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).
Una baja saturación de bases (presencia de Ca, Mg, K) indica que el pH del suelo puede ser bajo, y puede estar justificado el encalado.",
+ "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ",
+ "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 18.0,
+ "sl2": 18.0,
+ "sl3": 18.0,
+ "sl4": 17.6,
+ "sl5": 17.86,
+ "sl6": 18.4,
+ "sl7": 18.83
+ },
+ "clay": {
+ "sl1": 33.0,
+ "sl2": 33.0,
+ "sl3": 33.0,
+ "sl4": 35.8,
+ "sl5": 36.71,
+ "sl6": 37.8,
+ "sl7": 38.5
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 0.8,
+ "sl5": 0.57,
+ "sl6": 0.6,
+ "sl7": 0.67
+ },
+ "id": {
+ "component": "Eutric gleysols",
+ "name": "Eutric gleysols",
+ "rank_loc": "3",
+ "score_loc": 0.083
+ },
+ "ph": {
+ "sl1": 5.9,
+ "sl2": 5.9,
+ "sl3": 5.9,
+ "sl4": 5.96,
+ "sl5": 5.97,
+ "sl6": 6.02,
+ "sl7": 6.05
+ },
+ "rock_fragments": {
+ "sl1": 13.0,
+ "sl2": 13.0,
+ "sl3": 13.0,
+ "sl4": 17.6,
+ "sl5": 17.14,
+ "sl6": 14.8,
+ "sl7": 15.83
+ },
+ "sand": {
+ "sl1": 35.0,
+ "sl2": 35.0,
+ "sl3": 35.0,
+ "sl4": 33.6,
+ "sl5": 33.29,
+ "sl6": 32.8,
+ "sl7": 31.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 134228,
+ "distance": 2478.588,
+ "mapunitID": 36231,
+ "minCompDistance": 2478.58765257,
+ "share": 100,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.",
+ "Description_es": "Los gleysoles Eútricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles Eutricos son suelos productivos con una alta saturación de la base en la parte superior del suelo.",
+ "Description_fr": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.",
+ "Description_ks": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.",
+ "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ",
+ "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.",
+ "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ",
+ "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. "
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 13.0,
+ "sl2": 13.0,
+ "sl3": 13.0,
+ "sl4": 11.2,
+ "sl5": 10.57,
+ "sl6": 10.2,
+ "sl7": 10.5
+ },
+ "clay": {
+ "sl1": 27.0,
+ "sl2": 27.0,
+ "sl3": 27.0,
+ "sl4": 30.0,
+ "sl5": 31.57,
+ "sl6": 33.0,
+ "sl7": 33.67
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 0.8,
+ "sl5": 0.57,
+ "sl6": 0.4,
+ "sl7": 0.33
+ },
+ "id": {
+ "component": "Dystric gleysols",
+ "name": "Dystric gleysols",
+ "rank_loc": "4",
+ "score_loc": 0.08
+ },
+ "ph": {
+ "sl1": 4.8,
+ "sl2": 4.8,
+ "sl3": 4.8,
+ "sl4": 4.94,
+ "sl5": 5.0,
+ "sl6": 5.06,
+ "sl7": 5.08
+ },
+ "rock_fragments": {
+ "sl1": 7.0,
+ "sl2": 7.0,
+ "sl3": 7.0,
+ "sl4": 4.8,
+ "sl5": 4.86,
+ "sl6": 5.4,
+ "sl7": 5.33
+ },
+ "sand": {
+ "sl1": 43.0,
+ "sl2": 43.0,
+ "sl3": 43.0,
+ "sl4": 41.2,
+ "sl5": 40.71,
+ "sl6": 40.6,
+ "sl7": 40.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 133232,
+ "distance": 0.0,
+ "mapunitID": 36001,
+ "minCompDistance": 0.0,
+ "share": 5,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_es": "Los Gleysoles Dístricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
Es necesario un drenaje profundo para su cultivo.
Los Gleysoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.",
+ "Description_fr": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_ks": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.",
+ "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. ",
+ "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.
Estos suelos tienen poco calcio, magnesio u otras bases disponibles en el suelo, y pueden requerir fertilización suplementaria.
Si es necesario, el encalado aportará el calcio, y posiblemente el magnesio (cal dolomítica)..",
+ "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. ",
+ "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 8.0,
+ "sl2": 8.0,
+ "sl3": 8.0,
+ "sl4": 7.0,
+ "sl5": 7.0,
+ "sl6": 7.0,
+ "sl7": 7.0
+ },
+ "clay": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 21.6,
+ "sl5": 24.71,
+ "sl6": 28.0,
+ "sl7": 29.33
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Ferric lixisols",
+ "name": "Ferric lixisols",
+ "rank_loc": "5",
+ "score_loc": 0.072
+ },
+ "ph": {
+ "sl1": 6.2,
+ "sl2": 6.2,
+ "sl3": 6.2,
+ "sl4": 6.1,
+ "sl5": 6.03,
+ "sl6": 5.96,
+ "sl7": 5.93
+ },
+ "rock_fragments": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 18.6,
+ "sl5": 19.43,
+ "sl6": 20.2,
+ "sl7": 19.83
+ },
+ "sand": {
+ "sl1": 68.0,
+ "sl2": 68.0,
+ "sl3": 68.0,
+ "sl4": 63.2,
+ "sl5": 60.43,
+ "sl6": 57.0,
+ "sl7": 55.33
+ },
+ "site": {
+ "siteData": {
+ "componentID": 133617,
+ "distance": 3154.198,
+ "mapunitID": 36084,
+ "minCompDistance": 3154.19808851,
+ "share": 50,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Ferric Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation.
Ferric Lixisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ",
+ "Description_es": "Los Lixisoles Férricos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta.
Los Lixisoles férricos tienen concentraciones de hierro blandas y cementadas en los subsuelos, y una estructura poco desarrollada entre las concentraciones de hierro que puede ser susceptible de compactación. ",
+ "Description_fr": "Ferric Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation.
Ferric Lixisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ",
+ "Description_ks": "Ferric Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation.
Ferric Lixisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ",
+ "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
These soils are particularly sensitive to erosion, and so practices that work to maintain surface cover and strong soil structure (such as perennial crops) are needed. ",
+ "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.
Estos suelos son especialmente sensibles a la erosión, por lo que se necesitan prácticas que trabajen para mantener una estructura fuerte del suelo (como los cultivos perennes).",
+ "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
These soils are particularly sensitive to erosion, and so practices that work to maintain surface cover and strong soil structure (such as perennial crops) are needed. ",
+ "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
These soils are particularly sensitive to erosion, and so practices that work to maintain surface cover and strong soil structure (such as perennial crops) are needed. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 6.8,
+ "sl5": 7.29,
+ "sl6": 7.8,
+ "sl7": 7.83
+ },
+ "clay": {
+ "sl1": 17.0,
+ "sl2": 17.0,
+ "sl3": 17.0,
+ "sl4": 23.4,
+ "sl5": 26.57,
+ "sl6": 29.6,
+ "sl7": 30.83
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Eutric plinthosols",
+ "name": "Eutric plinthosols",
+ "rank_loc": "6",
+ "score_loc": 0.062
+ },
+ "ph": {
+ "sl1": 5.9,
+ "sl2": 5.9,
+ "sl3": 5.9,
+ "sl4": 5.82,
+ "sl5": 5.8,
+ "sl6": 5.8,
+ "sl7": 5.8
+ },
+ "rock_fragments": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 16.4,
+ "sl5": 19.71,
+ "sl6": 23.4,
+ "sl7": 25.33
+ },
+ "sand": {
+ "sl1": 63.0,
+ "sl2": 63.0,
+ "sl3": 63.0,
+ "sl4": 57.8,
+ "sl5": 54.86,
+ "sl6": 51.8,
+ "sl7": 50.33
+ },
+ "site": {
+ "siteData": {
+ "componentID": 133231,
+ "distance": 0.0,
+ "mapunitID": 36001,
+ "minCompDistance": 0.0,
+ "share": 35,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Eutric Plinthosols are have high base saturation in subsoils.",
+ "Description_es": "Los Plinthosoles Éutricos son suelos relativamente improductivos que se encuentran en regiones subtropicales o tropicales con altas cantidades de concentraciones ricas en hierro y pobres en humus de dureza y cementación variables.
Las concentraciones de hierro más blandas se endurecen irreversiblemente cuando se exponen en la superficie.
Estos suelos tienen un bajo volumen de enraizamiento y son relativamente ácidos, infértiles, muy erosionables y a menudo húmedos.
Los Plinthosoles eútricos tienen una alta saturación de bases en los subsuelos.",
+ "Description_fr": "Eutric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Eutric Plinthosols are have high base saturation in subsoils.",
+ "Description_ks": "Eutric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Eutric Plinthosols are have high base saturation in subsoils.",
+ "Management_en": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.",
+ "Management_es": "Este suelo no es muy adecuado para la agricultura.
La combinación de hierro duro y cementación hacen que este suelo sea el más adecuado para la construcción.
Tiene una escasa fertilidad del suelo, que combinada con un suelo poco profundo y rocoso hace que no sea posible la agricultura.
Estos suelos deberían utilizarse para cosas como materiales de superficie para carreteras.",
+ "Management_fr": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.",
+ "Management_ks": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 40
+ },
+ "cec": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 7.0
+ },
+ "clay": {
+ "sl1": 23.0,
+ "sl2": 23.0,
+ "sl3": 23.0,
+ "sl4": 22.0
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 0.5
+ },
+ "id": {
+ "component": "Dystric leptosols",
+ "name": "Dystric leptosols",
+ "rank_loc": "7",
+ "score_loc": 0.05
+ },
+ "ph": {
+ "sl1": 5.0,
+ "sl2": 5.0,
+ "sl3": 5.0,
+ "sl4": 5.0
+ },
+ "rock_fragments": {
+ "sl1": 22.0,
+ "sl2": 22.0,
+ "sl3": 22.0,
+ "sl4": 25.5
+ },
+ "sand": {
+ "sl1": 51.0,
+ "sl2": 51.0,
+ "sl3": 51.0,
+ "sl4": 51.5
+ },
+ "site": {
+ "siteData": {
+ "componentID": 133621,
+ "distance": 3154.198,
+ "mapunitID": 36084,
+ "minCompDistance": 3154.19808851,
+ "share": 10,
+ "soilDepth": 40
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Dystic Leptosols have low base saturation over the shallow root limiting layer. ",
+ "Description_es": "Los Leptosoles Dístricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles dísticos tienen una baja saturación de la base sobre la capa limitante de las raíces poco profundas. ",
+ "Description_fr": "Dystric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Dystic Leptosols have low base saturation over the shallow root limiting layer. ",
+ "Description_ks": "Dystric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Dystic Leptosols have low base saturation over the shallow root limiting layer. ",
+ "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
This soil has virtually no calcium available for plant use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ",
+ "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Este suelo prácticamente no tiene calcio disponible para el uso de las plantas.
Cualquier uso agrícola debe ser para el pastoreo o la agroforestería, con el mantenimiento continuo de la cobertura.",
+ "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
This soil has virtually no calcium available for plant use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ",
+ "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
This soil has virtually no calcium available for plant use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy clay loam",
+ "sl2": "Sandy clay loam",
+ "sl3": "Sandy clay loam",
+ "sl4": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 5.0,
+ "sl2": 5.0,
+ "sl3": 5.0,
+ "sl4": 5.2,
+ "sl5": 5.71,
+ "sl6": 6.2,
+ "sl7": 6.33
+ },
+ "clay": {
+ "sl1": 13.0,
+ "sl2": 13.0,
+ "sl3": 13.0,
+ "sl4": 19.6,
+ "sl5": 24.43,
+ "sl6": 29.4,
+ "sl7": 31.5
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Dystric planosols",
+ "name": "Dystric planosols",
+ "rank_loc": "8",
+ "score_loc": 0.045
+ },
+ "ph": {
+ "sl1": 5.0,
+ "sl2": 5.0,
+ "sl3": 5.0,
+ "sl4": 5.06,
+ "sl5": 5.07,
+ "sl6": 5.08,
+ "sl7": 5.08
+ },
+ "rock_fragments": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 5.2,
+ "sl5": 5.71,
+ "sl6": 7.6,
+ "sl7": 8.67
+ },
+ "sand": {
+ "sl1": 63.0,
+ "sl2": 63.0,
+ "sl3": 63.0,
+ "sl4": 56.0,
+ "sl5": 52.57,
+ "sl6": 49.4,
+ "sl7": 47.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 133240,
+ "distance": 0.0,
+ "mapunitID": 36001,
+ "minCompDistance": 0.0,
+ "share": 5,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.",
+ "Description_es": "Los Planosoles Dístricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren de drenaje para la producción de cultivos.
Los Planosoles Dístricos son suelos menos productivos con baja saturación de base en el subsuelo.",
+ "Description_fr": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.",
+ "Description_ks": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.",
+ "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed.",
+ "Management_es": "Situados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requerirán una fertilización adicional.
Los niveles de calcio son muy bajos en el perfil inferior de este suelo.
Se necesitará una fertilización suplementaria.",
+ "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed.",
+ "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 14.6,
+ "sl5": 14.71,
+ "sl6": 15.0,
+ "sl7": 15.17
+ },
+ "clay": {
+ "sl1": 24.0,
+ "sl2": 24.0,
+ "sl3": 24.0,
+ "sl4": 28.6,
+ "sl5": 29.86,
+ "sl6": 30.6,
+ "sl7": 30.5
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.0,
+ "sl6": 1.0,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Chromic luvisols",
+ "name": "Chromic luvisols",
+ "rank_loc": "9",
+ "score_loc": 0.042
+ },
+ "ph": {
+ "sl1": 6.4,
+ "sl2": 6.4,
+ "sl3": 6.4,
+ "sl4": 6.42,
+ "sl5": 6.44,
+ "sl6": 6.44,
+ "sl7": 6.43
+ },
+ "rock_fragments": {
+ "sl1": 6.0,
+ "sl2": 6.0,
+ "sl3": 6.0,
+ "sl4": 6.8,
+ "sl5": 9.29,
+ "sl6": 13.4,
+ "sl7": 12.5
+ },
+ "sand": {
+ "sl1": 53.0,
+ "sl2": 53.0,
+ "sl3": 53.0,
+ "sl4": 49.0,
+ "sl5": 47.71,
+ "sl6": 46.6,
+ "sl7": 46.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 133685,
+ "distance": 11933.891,
+ "mapunitID": 36102,
+ "minCompDistance": 11933.89145014,
+ "share": 50,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.",
+ "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.",
+ "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.",
+ "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.",
+ "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy clay loam",
+ "sl2": "Sandy clay loam",
+ "sl3": "Sandy clay loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 17.0,
+ "sl5": 16.29,
+ "sl6": 15.6,
+ "sl7": 15.33
+ },
+ "clay": {
+ "sl1": 29.0,
+ "sl2": 29.0,
+ "sl3": 29.0,
+ "sl4": 29.8,
+ "sl5": 30.14,
+ "sl6": 30.0,
+ "sl7": 29.67
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 0.86,
+ "sl6": 0.6,
+ "sl7": 0.5
+ },
+ "id": {
+ "component": "Dystric cambisols",
+ "name": "Dystric cambisols",
+ "rank_loc": "10",
+ "score_loc": 0.018
+ },
+ "ph": {
+ "sl1": 5.0,
+ "sl2": 5.0,
+ "sl3": 5.0,
+ "sl4": 5.02,
+ "sl5": 5.06,
+ "sl6": 5.12,
+ "sl7": 5.13
+ },
+ "rock_fragments": {
+ "sl1": 14.0,
+ "sl2": 14.0,
+ "sl3": 14.0,
+ "sl4": 14.4,
+ "sl5": 14.43,
+ "sl6": 15.2,
+ "sl7": 16.67
+ },
+ "sand": {
+ "sl1": 42.0,
+ "sl2": 42.0,
+ "sl3": 42.0,
+ "sl4": 42.6,
+ "sl5": 42.57,
+ "sl6": 42.6,
+ "sl7": 43.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 133494,
+ "distance": 15267.702,
+ "mapunitID": 36051,
+ "minCompDistance": 15267.70170318,
+ "share": 5,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_es": "Los Cambisoles Dístricos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos menos productivos con baja saturación de bases en la parte superior del suelo.",
+ "Description_fr": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_ks": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.",
+ "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ",
+ "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Debido a que este suelo tiene una baja saturación de bases, puede ser necesaria la aplicación de bases (a través de la fertlización) para un rendimiento más productivo del cultivo.
Si el pH del suelo es bajo, el calcio (y posiblemente el magnesio, si se utiliza cal dolomítica) puede ser suministrado a través de la adición de cal.
Si el pH del suelo es adecuado para la producción de cultivos, entonces el yeso (CaSO4) puede ser utilizado como fuente de Ca, si es necesario, u otras fuentes como MgSO4 podrían ser aplicadas (si la prueba del suelo indica una necesidad).
Una fertilización adecuada también aportará potasio, si el análisis del suelo indica que es necesario.",
+ "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ",
+ "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. "
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 5.0,
+ "sl2": 5.0,
+ "sl3": 5.0,
+ "sl4": 5.6,
+ "sl5": 6.0,
+ "sl6": 6.4,
+ "sl7": 6.67
+ },
+ "clay": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0,
+ "sl4": 26.4,
+ "sl5": 29.0,
+ "sl6": 31.6,
+ "sl7": 33.17
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Dystric plinthosols",
+ "name": "Dystric plinthosols",
+ "rank_loc": "11",
+ "score_loc": 0.018
+ },
+ "ph": {
+ "sl1": 5.2,
+ "sl2": 5.2,
+ "sl3": 5.2,
+ "sl4": 5.16,
+ "sl5": 5.17,
+ "sl6": 5.18,
+ "sl7": 5.18
+ },
+ "rock_fragments": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0,
+ "sl4": 20.2,
+ "sl5": 20.71,
+ "sl6": 21.4,
+ "sl7": 20.33
+ },
+ "sand": {
+ "sl1": 53.0,
+ "sl2": 53.0,
+ "sl3": 53.0,
+ "sl4": 47.2,
+ "sl5": 44.86,
+ "sl6": 42.4,
+ "sl7": 40.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 133239,
+ "distance": 0.0,
+ "mapunitID": 36001,
+ "minCompDistance": 0.0,
+ "share": 5,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.",
+ "Description_es": "Los Plinthosoles Dístricos son suelos relativamente improductivos que se encuentran en regiones subtropicales o tropicales con altas cantidades de concentraciones ricas en hierro y pobres en humus de dureza y cementación variables.
Las concentraciones de hierro más blandas se endurecen irreversiblemente cuando se exponen en la superficie.
Estos suelos tienen un bajo volumen de enraizamiento y son relativamente ácidos, infértiles, muy erosionables y a menudo húmedos.
Los Plinthosoles Dístricos son suelos improductivos con baja saturación de bases en los subsuelos.",
+ "Description_fr": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.",
+ "Description_ks": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.",
+ "Management_en": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil.",
+ "Management_es": "Este suelo no es muy adecuado para la agricultura.
La combinación de hierro duro y cementación hacen que este suelo sea el más adecuado para la construcción.
Tiene una pobre fertilidad del suelo, que cuando se combina con un suelo poco profundo y rocoso hace que la agricultura no sea posible.
Estos suelos deben utilizarse para cosas como materiales de superficie para carreteras.
Este suelo prácticamente no tiene calcio disponible en el subsuelo.",
+ "Management_fr": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil.",
+ "Management_ks": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 18.4,
+ "sl5": 18.14,
+ "sl6": 17.6,
+ "sl7": 17.5
+ },
+ "clay": {
+ "sl1": 31.0,
+ "sl2": 31.0,
+ "sl3": 31.0,
+ "sl4": 32.2,
+ "sl5": 32.14,
+ "sl6": 31.6,
+ "sl7": 31.33
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 1.4,
+ "sl5": 1.43,
+ "sl6": 1.6,
+ "sl7": 1.67
+ },
+ "id": {
+ "component": "Eutric fluvisols",
+ "name": "Eutric fluvisols",
+ "rank_loc": "12",
+ "score_loc": 0.002
+ },
+ "ph": {
+ "sl1": 6.1,
+ "sl2": 6.1,
+ "sl3": 6.1,
+ "sl4": 6.24,
+ "sl5": 6.3,
+ "sl6": 6.38,
+ "sl7": 6.43
+ },
+ "rock_fragments": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 11.6,
+ "sl5": 9.86,
+ "sl6": 10.2,
+ "sl7": 10.33
+ },
+ "sand": {
+ "sl1": 37.0,
+ "sl2": 37.0,
+ "sl3": 37.0,
+ "sl4": 36.2,
+ "sl5": 36.86,
+ "sl6": 38.4,
+ "sl7": 38.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 133913,
+ "distance": 26374.257,
+ "mapunitID": 36150,
+ "minCompDistance": 26374.25651323,
+ "share": 5,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ",
+ "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).",
+ "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered."
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "global",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Eutric gleysols",
+ "componentData": "Missing Data",
+ "componentID": 134228,
+ "name": "Eutric gleysols",
+ "rank_data": "2",
+ "rank_data_loc": "1",
+ "rank_loc": 3,
+ "score_data": 1.0,
+ "score_data_loc": 1.0,
+ "score_loc": 0.083
+ },
+ {
+ "component": "Dystric gleysols",
+ "componentData": "Missing Data",
+ "componentID": 133232,
+ "name": "Dystric gleysols",
+ "rank_data": "1",
+ "rank_data_loc": "2",
+ "rank_loc": 4,
+ "score_data": 1.0,
+ "score_data_loc": 0.998,
+ "score_loc": 0.08
+ },
+ {
+ "component": "Dystric fluvisols",
+ "componentData": "Data Complete",
+ "componentID": 133237,
+ "name": "Dystric fluvisols",
+ "rank_data": "4",
+ "rank_data_loc": "3",
+ "rank_loc": 2,
+ "score_data": 0.566,
+ "score_data_loc": 0.629,
+ "score_loc": 0.116
+ },
+ {
+ "component": "Dystric planosols",
+ "componentData": "Missing Data",
+ "componentID": 133240,
+ "name": "Dystric planosols",
+ "rank_data": "5",
+ "rank_data_loc": "4",
+ "rank_loc": 8,
+ "score_data": 0.566,
+ "score_data_loc": 0.564,
+ "score_loc": 0.045
+ },
+ {
+ "component": "Chromic luvisols",
+ "componentData": "Data Complete",
+ "componentID": 133685,
+ "name": "Chromic luvisols",
+ "rank_data": "3",
+ "rank_data_loc": "5",
+ "rank_loc": 9,
+ "score_data": 0.566,
+ "score_data_loc": 0.562,
+ "score_loc": 0.042
+ },
+ {
+ "component": "Eutric plinthosols",
+ "componentData": "Data Complete",
+ "componentID": 133231,
+ "name": "Eutric plinthosols",
+ "rank_data": "9",
+ "rank_data_loc": "6",
+ "rank_loc": 6,
+ "score_data": 0.451,
+ "score_data_loc": 0.474,
+ "score_loc": 0.062
+ },
+ {
+ "component": "Ferric acrisols",
+ "componentData": "Missing Data",
+ "componentID": 133233,
+ "name": "Ferric acrisols",
+ "rank_data": "11",
+ "rank_data_loc": "7",
+ "rank_loc": 1,
+ "score_data": 0.36,
+ "score_data_loc": 0.447,
+ "score_loc": 0.124
+ },
+ {
+ "component": "Dystric cambisols",
+ "componentData": "Data Complete",
+ "componentID": 133494,
+ "name": "Dystric cambisols",
+ "rank_data": "6",
+ "rank_data_loc": "8",
+ "rank_loc": 10,
+ "score_data": 0.451,
+ "score_data_loc": 0.433,
+ "score_loc": 0.018
+ },
+ {
+ "component": "Eutric fluvisols",
+ "componentData": "Data Complete",
+ "componentID": 133913,
+ "name": "Eutric fluvisols",
+ "rank_data": "8",
+ "rank_data_loc": "9",
+ "rank_loc": 12,
+ "score_data": 0.451,
+ "score_data_loc": 0.419,
+ "score_loc": 0.002
+ },
+ {
+ "component": "Ferric lixisols",
+ "componentData": "Data Complete",
+ "componentID": 133617,
+ "name": "Ferric lixisols",
+ "rank_data": "12",
+ "rank_data_loc": "10",
+ "rank_loc": 5,
+ "score_data": 0.36,
+ "score_data_loc": 0.399,
+ "score_loc": 0.072
+ },
+ {
+ "component": "Dystric plinthosols",
+ "componentData": "Missing Data",
+ "componentID": 133239,
+ "name": "Dystric plinthosols",
+ "rank_data": "10",
+ "rank_data_loc": "11",
+ "rank_loc": 11,
+ "score_data": 0.36,
+ "score_data_loc": 0.349,
+ "score_loc": 0.018
+ },
+ {
+ "component": "Dystric leptosols",
+ "componentData": "Missing Data",
+ "componentID": 133621,
+ "name": "Dystric leptosols",
+ "rank_data": "7",
+ "rank_data_loc": "12",
+ "rank_loc": 7,
+ "score_data": 0.451,
+ "score_data_loc": 0.002,
+ "score_loc": 0.05
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[8.48333,76.95].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[8.48333,76.95].json
new file mode 100644
index 0000000..1e03934
--- /dev/null
+++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[8.48333,76.95].json
@@ -0,0 +1,1227 @@
+{
+ "list": {
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 9.0,
+ "sl2": 9.0,
+ "sl3": 9.0,
+ "sl4": 7.6,
+ "sl5": 7.0,
+ "sl6": 6.4,
+ "sl7": 6.0
+ },
+ "clay": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0,
+ "sl4": 18.0,
+ "sl5": 17.14,
+ "sl6": 16.0,
+ "sl7": 15.67
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.14,
+ "sl6": 1.2,
+ "sl7": 1.0
+ },
+ "id": {
+ "component": "Dystric regosols",
+ "name": "Dystric regosols",
+ "rank_loc": "1",
+ "score_loc": 0.166
+ },
+ "ph": {
+ "sl1": 5.1,
+ "sl2": 5.1,
+ "sl3": 5.1,
+ "sl4": 5.08,
+ "sl5": 5.13,
+ "sl6": 5.16,
+ "sl7": 5.18
+ },
+ "rock_fragments": {
+ "sl1": 24.0,
+ "sl2": 24.0,
+ "sl3": 24.0,
+ "sl4": 30.6,
+ "sl5": 31.14,
+ "sl6": 35.2,
+ "sl7": 36.67
+ },
+ "sand": {
+ "sl1": 55.0,
+ "sl2": 55.0,
+ "sl3": 55.0,
+ "sl4": 57.6,
+ "sl5": 58.71,
+ "sl6": 60.2,
+ "sl7": 60.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 136281,
+ "distance": 1300.283,
+ "mapunitID": 3844,
+ "minCompDistance": 1300.28309411,
+ "share": 30,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ",
+ "Description_es": "Los Regosoles Dístricos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.
Los Regosoles Dístricos tienen una baja saturación de base en el subsuelo. ",
+ "Description_fr": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ",
+ "Description_ks": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ",
+ "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ",
+ "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo. *Incluso cuando se utilizan para el pastoreo, el riego será necesario debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos. *Con una baja saturación de bases, estos suelos pueden responder a la adición de bases como el potasio, el calcio o el magnesio. ",
+ "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ",
+ "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy loam",
+ "sl5": "Sandy loam",
+ "sl6": "Sandy loam",
+ "sl7": "Sandy loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 18.4,
+ "sl5": 18.29,
+ "sl6": 18.4,
+ "sl7": 18.5
+ },
+ "clay": {
+ "sl1": 34.0,
+ "sl2": 34.0,
+ "sl3": 34.0,
+ "sl4": 36.6,
+ "sl5": 37.29,
+ "sl6": 38.0,
+ "sl7": 38.33
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 0.8,
+ "sl5": 0.57,
+ "sl6": 0.4,
+ "sl7": 0.33
+ },
+ "id": {
+ "component": "Gleysols",
+ "name": "Gleysols",
+ "rank_loc": "2",
+ "score_loc": 0.155
+ },
+ "ph": {
+ "sl1": 5.6,
+ "sl2": 5.6,
+ "sl3": 5.6,
+ "sl4": 5.66,
+ "sl5": 5.69,
+ "sl6": 5.74,
+ "sl7": 5.77
+ },
+ "rock_fragments": {
+ "sl1": 10.0,
+ "sl2": 10.0,
+ "sl3": 10.0,
+ "sl4": 9.6,
+ "sl5": 10.43,
+ "sl6": 10.8,
+ "sl7": 11.83
+ },
+ "sand": {
+ "sl1": 35.0,
+ "sl2": 35.0,
+ "sl3": 35.0,
+ "sl4": 33.8,
+ "sl5": 33.71,
+ "sl6": 33.6,
+ "sl7": 33.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 136282,
+ "distance": 1300.283,
+ "mapunitID": 3844,
+ "minCompDistance": 1300.28309411,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Gleysols are productive soils with high base saturation in the upper portion of soil.",
+ "Description_es": "Los Gleysoles tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los gleysoles son suelos productivos con una alta saturación de la base en la parte superior del suelo.",
+ "Description_fr": "Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Gleysols are productive soils with high base saturation in the upper portion of soil.",
+ "Description_ks": "Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Gleysols are productive soils with high base saturation in the upper portion of soil.",
+ "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ",
+ "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.",
+ "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ",
+ "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. "
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 5.0,
+ "sl2": 5.0,
+ "sl3": 5.0,
+ "sl4": 5.6,
+ "sl5": 6.0,
+ "sl6": 6.4,
+ "sl7": 6.67
+ },
+ "clay": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0,
+ "sl4": 26.4,
+ "sl5": 29.0,
+ "sl6": 31.6,
+ "sl7": 33.17
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Dystric plinthosols",
+ "name": "Dystric plinthosols",
+ "rank_loc": "3",
+ "score_loc": 0.134
+ },
+ "ph": {
+ "sl1": 5.2,
+ "sl2": 5.2,
+ "sl3": 5.2,
+ "sl4": 5.16,
+ "sl5": 5.17,
+ "sl6": 5.18,
+ "sl7": 5.18
+ },
+ "rock_fragments": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0,
+ "sl4": 20.2,
+ "sl5": 20.71,
+ "sl6": 21.4,
+ "sl7": 20.33
+ },
+ "sand": {
+ "sl1": 53.0,
+ "sl2": 53.0,
+ "sl3": 53.0,
+ "sl4": 47.2,
+ "sl5": 44.86,
+ "sl6": 42.4,
+ "sl7": 40.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 134462,
+ "distance": 22688.376,
+ "mapunitID": 3656,
+ "minCompDistance": 22688.37560234,
+ "share": 60,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.",
+ "Description_es": "Los Plinthosoles Dístricos son suelos relativamente improductivos que se encuentran en regiones subtropicales o tropicales con altas cantidades de concentraciones ricas en hierro y pobres en humus de dureza y cementación variables.
Las concentraciones de hierro más blandas se endurecen irreversiblemente cuando se exponen en la superficie.
Estos suelos tienen un bajo volumen de enraizamiento y son relativamente ácidos, infértiles, muy erosionables y a menudo húmedos.
Los Plinthosoles Dístricos son suelos improductivos con baja saturación de bases en los subsuelos.",
+ "Description_fr": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.",
+ "Description_ks": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.",
+ "Management_en": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil.",
+ "Management_es": "Este suelo no es muy adecuado para la agricultura.
La combinación de hierro duro y cementación hacen que este suelo sea el más adecuado para la construcción.
Tiene una pobre fertilidad del suelo, que cuando se combina con un suelo poco profundo y rocoso hace que la agricultura no sea posible.
Estos suelos deben utilizarse para cosas como materiales de superficie para carreteras.
Este suelo prácticamente no tiene calcio disponible en el subsuelo.",
+ "Management_fr": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil.",
+ "Management_ks": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy loam",
+ "sl2": "Sandy loam",
+ "sl3": "Sandy loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 11.0,
+ "sl5": 11.0,
+ "sl6": 11.0,
+ "sl7": 10.83
+ },
+ "clay": {
+ "sl1": 30.0,
+ "sl2": 30.0,
+ "sl3": 30.0,
+ "sl4": 37.6,
+ "sl5": 41.0,
+ "sl6": 44.2,
+ "sl7": 45.17
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Haplic nitisols",
+ "name": "Haplic nitisols",
+ "rank_loc": "4",
+ "score_loc": 0.112
+ },
+ "ph": {
+ "sl1": 5.5,
+ "sl2": 5.5,
+ "sl3": 5.5,
+ "sl4": 5.36,
+ "sl5": 5.31,
+ "sl6": 5.28,
+ "sl7": 5.27
+ },
+ "rock_fragments": {
+ "sl1": 10.0,
+ "sl2": 10.0,
+ "sl3": 10.0,
+ "sl4": 13.2,
+ "sl5": 14.14,
+ "sl6": 13.0,
+ "sl7": 11.5
+ },
+ "sand": {
+ "sl1": 46.0,
+ "sl2": 46.0,
+ "sl3": 46.0,
+ "sl4": 40.6,
+ "sl5": 38.0,
+ "sl6": 35.4,
+ "sl7": 34.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 136007,
+ "distance": 5885.649,
+ "mapunitID": 3817,
+ "minCompDistance": 5885.64855813,
+ "share": 50,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.",
+ "Description_es": "Los Nitisoles Háplicos son los suelos subtropicales y tropicales húmedos más productivos.
Tienen una estructura bien desarrollada con subsuelos relativamente arcillosos y enriquecidos en hierro que retienen agua y nutrientes.",
+ "Description_fr": "Haplic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.",
+ "Description_ks": "Haplic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.",
+ "Management_en": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.",
+ "Management_es": "Son suelos productivos y pueden utilizarse para la producción de cultivos.
Tienen un excelente drenaje interno y una buena capacidad de retención de agua.
Estos suelos tienen un alto grado de absorción de fósforo y fijan el fósforo, por lo que no está disponible para la planta durante la temporada de cultivo.
La fertilización con fósforo será necesaria para obtener la mejor productividad.
Las prácticas bien documentadas, como la aplicación de fertilizantes fosfatados en banda (directamente sobre la semilla o a un lado y abajo de la semilla), ayudarán a reducir la fijación de P.",
+ "Management_fr": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.",
+ "Management_ks": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation."
+ }
+ },
+ "texture": {
+ "sl1": "Sandy clay loam",
+ "sl2": "Sandy clay loam",
+ "sl3": "Sandy clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Unknown",
+ "sl6": "Unknown",
+ "sl7": "Unknown"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 18.4,
+ "sl5": 18.14,
+ "sl6": 17.6,
+ "sl7": 17.5
+ },
+ "clay": {
+ "sl1": 31.0,
+ "sl2": 31.0,
+ "sl3": 31.0,
+ "sl4": 32.2,
+ "sl5": 32.14,
+ "sl6": 31.6,
+ "sl7": 31.33
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 1.4,
+ "sl5": 1.43,
+ "sl6": 1.6,
+ "sl7": 1.67
+ },
+ "id": {
+ "component": "Eutric fluvisols",
+ "name": "Eutric fluvisols",
+ "rank_loc": "5",
+ "score_loc": 0.111
+ },
+ "ph": {
+ "sl1": 6.1,
+ "sl2": 6.1,
+ "sl3": 6.1,
+ "sl4": 6.24,
+ "sl5": 6.3,
+ "sl6": 6.38,
+ "sl7": 6.43
+ },
+ "rock_fragments": {
+ "sl1": 19.0,
+ "sl2": 19.0,
+ "sl3": 19.0,
+ "sl4": 11.6,
+ "sl5": 9.86,
+ "sl6": 10.2,
+ "sl7": 10.33
+ },
+ "sand": {
+ "sl1": 37.0,
+ "sl2": 37.0,
+ "sl3": 37.0,
+ "sl4": 36.2,
+ "sl5": 36.86,
+ "sl6": 38.4,
+ "sl7": 38.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 136283,
+ "distance": 1300.283,
+ "mapunitID": 3844,
+ "minCompDistance": 1300.28309411,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ",
+ "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ",
+ "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).",
+ "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.",
+ "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered."
+ }
+ },
+ "texture": {
+ "sl1": "Clay loam",
+ "sl2": "Clay loam",
+ "sl3": "Clay loam",
+ "sl4": "Clay loam",
+ "sl5": "Clay loam",
+ "sl6": "Clay loam",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 8.0,
+ "sl2": 8.0,
+ "sl3": 8.0,
+ "sl4": 6.8,
+ "sl5": 6.57,
+ "sl6": 6.4,
+ "sl7": 6.33
+ },
+ "clay": {
+ "sl1": 24.0,
+ "sl2": 24.0,
+ "sl3": 24.0,
+ "sl4": 31.2,
+ "sl5": 34.0,
+ "sl6": 36.6,
+ "sl7": 37.67
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Ferric acrisols",
+ "name": "Ferric acrisols",
+ "rank_loc": "6",
+ "score_loc": 0.089
+ },
+ "ph": {
+ "sl1": 5.3,
+ "sl2": 5.3,
+ "sl3": 5.3,
+ "sl4": 5.18,
+ "sl5": 5.16,
+ "sl6": 5.14,
+ "sl7": 5.13
+ },
+ "rock_fragments": {
+ "sl1": 21.0,
+ "sl2": 21.0,
+ "sl3": 21.0,
+ "sl4": 27.8,
+ "sl5": 28.29,
+ "sl6": 27.2,
+ "sl7": 26.33
+ },
+ "sand": {
+ "sl1": 56.0,
+ "sl2": 56.0,
+ "sl3": 56.0,
+ "sl4": 50.2,
+ "sl5": 47.71,
+ "sl6": 45.2,
+ "sl7": 43.83
+ },
+ "site": {
+ "siteData": {
+ "componentID": 136010,
+ "distance": 5885.649,
+ "mapunitID": 3817,
+ "minCompDistance": 5885.64855813,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.",
+ "Description_es": "Los Acrisoles Férricos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Estos suelos tienen un alto contenido de hierro y es común la presencia de nódulos de hierro.",
+ "Description_fr": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.",
+ "Description_ks": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.",
+ "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ",
+ "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.",
+ "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ",
+ "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy clay loam",
+ "sl2": "Sandy clay loam",
+ "sl3": "Sandy clay loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay",
+ "sl7": "Clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 3.0,
+ "sl2": 3.0,
+ "sl3": 3.0,
+ "sl4": 1.8,
+ "sl5": 1.57,
+ "sl6": 1.4,
+ "sl7": 1.33
+ },
+ "clay": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 4.0,
+ "sl5": 4.0,
+ "sl6": 4.0,
+ "sl7": 4.17
+ },
+ "ec": {
+ "sl1": 0.0,
+ "sl2": 0.0,
+ "sl3": 0.0,
+ "sl4": 0.0,
+ "sl5": 0.0,
+ "sl6": 0.0,
+ "sl7": 0.0
+ },
+ "id": {
+ "component": "Albic arenosols",
+ "name": "Albic arenosols",
+ "rank_loc": "7",
+ "score_loc": 0.055
+ },
+ "ph": {
+ "sl1": 5.3,
+ "sl2": 5.3,
+ "sl3": 5.3,
+ "sl4": 5.32,
+ "sl5": 5.36,
+ "sl6": 5.42,
+ "sl7": 5.43
+ },
+ "rock_fragments": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 3.2,
+ "sl5": 3.43,
+ "sl6": 3.6,
+ "sl7": 4.5
+ },
+ "sand": {
+ "sl1": 86.0,
+ "sl2": 86.0,
+ "sl3": 86.0,
+ "sl4": 86.8,
+ "sl5": 86.86,
+ "sl6": 86.6,
+ "sl7": 86.33
+ },
+ "site": {
+ "siteData": {
+ "componentID": 136286,
+ "distance": 1300.283,
+ "mapunitID": 3844,
+ "minCompDistance": 1300.28309411,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.",
+ "Description_es": "Los Arenosoles Álbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos están muy lixiviados con pocos nutrientes y agua disponible.",
+ "Description_fr": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.",
+ "Description_ks": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.",
+ "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. ",
+ "Management_es": "Dado que estos suelos tienen poca retención de agua y nutrientes, deben ser fertilizados y regados para lograr una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
En estos suelos se debe prestar especial atención a minimizar la pérdida de nutrientes durante la fertilización.
Si se dispone de ellas, deben considerarse fuentes de N de liberación lenta, o una aplicación más frecuente de N a tasas más bajas.",
+ "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. ",
+ "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. "
+ }
+ },
+ "texture": {
+ "sl1": "Loamy sand",
+ "sl2": "Loamy sand",
+ "sl3": "Loamy sand",
+ "sl4": "Loamy sand",
+ "sl5": "Loamy sand",
+ "sl6": "Loamy sand",
+ "sl7": "Loamy sand"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 21.0,
+ "sl2": 21.0,
+ "sl3": 21.0,
+ "sl4": 17.8,
+ "sl5": 16.57,
+ "sl6": 15.8,
+ "sl7": 15.5
+ },
+ "clay": {
+ "sl1": 26.0,
+ "sl2": 26.0,
+ "sl3": 26.0,
+ "sl4": 21.6,
+ "sl5": 20.0,
+ "sl6": 19.6,
+ "sl7": 19.67
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0,
+ "sl4": 1.0,
+ "sl5": 1.14,
+ "sl6": 1.2,
+ "sl7": 1.5
+ },
+ "id": {
+ "component": "Calcaric regosols",
+ "name": "Calcaric regosols",
+ "rank_loc": "8",
+ "score_loc": 0.055
+ },
+ "ph": {
+ "sl1": 7.9,
+ "sl2": 7.9,
+ "sl3": 7.9,
+ "sl4": 7.94,
+ "sl5": 8.0,
+ "sl6": 8.06,
+ "sl7": 8.08
+ },
+ "rock_fragments": {
+ "sl1": 10.0,
+ "sl2": 10.0,
+ "sl3": 10.0,
+ "sl4": 13.0,
+ "sl5": 12.71,
+ "sl6": 11.6,
+ "sl7": 11.67
+ },
+ "sand": {
+ "sl1": 51.0,
+ "sl2": 51.0,
+ "sl3": 51.0,
+ "sl4": 53.8,
+ "sl5": 54.14,
+ "sl6": 52.4,
+ "sl7": 51.17
+ },
+ "site": {
+ "siteData": {
+ "componentID": 136285,
+ "distance": 1300.283,
+ "mapunitID": 3844,
+ "minCompDistance": 1300.28309411,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ",
+ "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ",
+ "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ",
+ "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ",
+ "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ",
+ "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.",
+ "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ",
+ "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. "
+ }
+ },
+ "texture": {
+ "sl1": "Sandy clay loam",
+ "sl2": "Sandy clay loam",
+ "sl3": "Sandy clay loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy loam",
+ "sl6": "Sandy loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 17.0,
+ "sl2": 17.0,
+ "sl3": 17.0,
+ "sl4": 16.2,
+ "sl5": 15.29,
+ "sl6": 14.6,
+ "sl7": 14.67
+ },
+ "clay": {
+ "sl1": 25.0,
+ "sl2": 25.0,
+ "sl3": 25.0,
+ "sl4": 24.8,
+ "sl5": 24.43,
+ "sl6": 23.8,
+ "sl7": 23.0
+ },
+ "ec": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0,
+ "sl4": 16.2,
+ "sl5": 16.86,
+ "sl6": 17.4,
+ "sl7": 17.5
+ },
+ "id": {
+ "component": "Haplic solonchaks",
+ "name": "Haplic solonchaks",
+ "rank_loc": "9",
+ "score_loc": 0.055
+ },
+ "ph": {
+ "sl1": 8.1,
+ "sl2": 8.1,
+ "sl3": 8.1,
+ "sl4": 8.22,
+ "sl5": 8.24,
+ "sl6": 8.28,
+ "sl7": 8.32
+ },
+ "rock_fragments": {
+ "sl1": 10.0,
+ "sl2": 10.0,
+ "sl3": 10.0,
+ "sl4": 12.0,
+ "sl5": 11.43,
+ "sl6": 9.4,
+ "sl7": 9.67
+ },
+ "sand": {
+ "sl1": 43.0,
+ "sl2": 43.0,
+ "sl3": 43.0,
+ "sl4": 44.0,
+ "sl5": 44.57,
+ "sl6": 45.4,
+ "sl7": 46.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 136284,
+ "distance": 1300.283,
+ "mapunitID": 3844,
+ "minCompDistance": 1300.28309411,
+ "share": 10,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Haplic Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.",
+ "Description_es": "Los Solonchaks Háplicos son suelos que contienen sales en la superficie del suelo o cerca de ella. Estos suelos se forman en los desiertos o cerca de las costas.",
+ "Description_fr": "Haplic Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.",
+ "Description_ks": "Haplic Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.",
+ "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ",
+ "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy pobre, y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.",
+ "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ",
+ "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Loam",
+ "sl5": "Loam",
+ "sl6": "Loam",
+ "sl7": "Loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20,
+ "sl4": 50,
+ "sl5": 70,
+ "sl6": 100,
+ "sl7": 120
+ },
+ "cec": {
+ "sl1": 11.0,
+ "sl2": 11.0,
+ "sl3": 11.0,
+ "sl4": 9.4,
+ "sl5": 8.57,
+ "sl6": 7.8,
+ "sl7": 8.17
+ },
+ "clay": {
+ "sl1": 23.0,
+ "sl2": 23.0,
+ "sl3": 23.0,
+ "sl4": 24.2,
+ "sl5": 24.29,
+ "sl6": 24.2,
+ "sl7": 24.5
+ },
+ "ec": {
+ "sl1": 2.0,
+ "sl2": 2.0,
+ "sl3": 2.0,
+ "sl4": 1.4,
+ "sl5": 1.43,
+ "sl6": 1.6,
+ "sl7": 1.67
+ },
+ "id": {
+ "component": "Dystric fluvisols",
+ "name": "Dystric fluvisols",
+ "rank_loc": "10",
+ "score_loc": 0.045
+ },
+ "ph": {
+ "sl1": 4.9,
+ "sl2": 4.9,
+ "sl3": 4.9,
+ "sl4": 4.96,
+ "sl5": 4.99,
+ "sl6": 5.04,
+ "sl7": 5.08
+ },
+ "rock_fragments": {
+ "sl1": 4.0,
+ "sl2": 4.0,
+ "sl3": 4.0,
+ "sl4": 4.8,
+ "sl5": 7.0,
+ "sl6": 9.4,
+ "sl7": 9.67
+ },
+ "sand": {
+ "sl1": 49.0,
+ "sl2": 49.0,
+ "sl3": 49.0,
+ "sl4": 49.2,
+ "sl5": 49.71,
+ "sl6": 50.8,
+ "sl7": 50.67
+ },
+ "site": {
+ "siteData": {
+ "componentID": 136009,
+ "distance": 5885.649,
+ "mapunitID": 3817,
+ "minCompDistance": 5885.64855813,
+ "share": 20,
+ "soilDepth": 200
+ },
+ "siteDescription": {
+ "Description_en": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_es": "Los Fluvisoles Dístricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los Fluvisoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.",
+ "Description_fr": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.",
+ "Description_ks": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.",
+ "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ",
+ "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (acolchados, cultivos de cobertura), que mejoren la infiltración del agua o que proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).
Una baja saturación de bases (presencia de Ca, Mg, K) indica que el pH del suelo puede ser bajo, y puede estar justificado el encalado.",
+ "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ",
+ "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam",
+ "sl4": "Sandy clay loam",
+ "sl5": "Sandy clay loam",
+ "sl6": "Sandy clay loam",
+ "sl7": "Sandy clay loam"
+ }
+ },
+ {
+ "bottom_depth": {
+ "sl1": 1,
+ "sl2": 10,
+ "sl3": 20
+ },
+ "cec": {
+ "sl1": 16.0,
+ "sl2": 16.0,
+ "sl3": 16.0
+ },
+ "clay": {
+ "sl1": 20.0,
+ "sl2": 20.0,
+ "sl3": 20.0
+ },
+ "ec": {
+ "sl1": 1.0,
+ "sl2": 1.0,
+ "sl3": 1.0
+ },
+ "id": {
+ "component": "Lithic leptosols",
+ "name": "Lithic leptosols",
+ "rank_loc": "11",
+ "score_loc": 0.022
+ },
+ "ph": {
+ "sl1": 6.7,
+ "sl2": 6.7,
+ "sl3": 6.7
+ },
+ "rock_fragments": {
+ "sl1": 36.0,
+ "sl2": 36.0,
+ "sl3": 36.0
+ },
+ "sand": {
+ "sl1": 51.0,
+ "sl2": 51.0,
+ "sl3": 51.0
+ },
+ "site": {
+ "siteData": {
+ "componentID": 134464,
+ "distance": 22688.376,
+ "mapunitID": 3656,
+ "minCompDistance": 22688.37560234,
+ "share": 10,
+ "soilDepth": 20
+ },
+ "siteDescription": {
+ "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ",
+ "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ",
+ "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ",
+ "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.",
+ "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ",
+ "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. "
+ }
+ },
+ "texture": {
+ "sl1": "Loam",
+ "sl2": "Loam",
+ "sl3": "Loam"
+ }
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "global",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Haplic nitisols",
+ "componentData": "Missing Data",
+ "componentID": 136007,
+ "name": "Haplic nitisols",
+ "rank_data": "2",
+ "rank_data_loc": "1",
+ "rank_loc": 4,
+ "score_data": 0.524,
+ "score_data_loc": 1.0,
+ "score_loc": 0.112
+ },
+ {
+ "component": "Calcaric regosols",
+ "componentData": "Data Complete",
+ "componentID": 136285,
+ "name": "Calcaric regosols",
+ "rank_data": "1",
+ "rank_data_loc": "2",
+ "rank_loc": 8,
+ "score_data": 0.568,
+ "score_data_loc": 0.98,
+ "score_loc": 0.055
+ },
+ {
+ "component": "Ferric acrisols",
+ "componentData": "Missing Data",
+ "componentID": 136010,
+ "name": "Ferric acrisols",
+ "rank_data": "3",
+ "rank_data_loc": "3",
+ "rank_loc": 6,
+ "score_data": 0.484,
+ "score_data_loc": 0.903,
+ "score_loc": 0.089
+ },
+ {
+ "component": "Gleysols",
+ "componentData": "Missing Data",
+ "componentID": 136282,
+ "name": "Gleysols",
+ "rank_data": "8",
+ "rank_data_loc": "4",
+ "rank_loc": 2,
+ "score_data": 0.401,
+ "score_data_loc": 0.875,
+ "score_loc": 0.155
+ },
+ {
+ "component": "Albic arenosols",
+ "componentData": "Data Complete",
+ "componentID": 136286,
+ "name": "Albic arenosols",
+ "rank_data": "4",
+ "rank_data_loc": "5",
+ "rank_loc": 7,
+ "score_data": 0.444,
+ "score_data_loc": 0.786,
+ "score_loc": 0.055
+ },
+ {
+ "component": "Dystric plinthosols",
+ "componentData": "Missing Data",
+ "componentID": 134462,
+ "name": "Dystric plinthosols",
+ "rank_data": "9",
+ "rank_data_loc": "6",
+ "rank_loc": 3,
+ "score_data": 0.349,
+ "score_data_loc": 0.76,
+ "score_loc": 0.134
+ },
+ {
+ "component": "Haplic solonchaks",
+ "componentData": "Data Complete",
+ "componentID": 136284,
+ "name": "Haplic solonchaks",
+ "rank_data": "7",
+ "rank_data_loc": "7",
+ "rank_loc": 9,
+ "score_data": 0.427,
+ "score_data_loc": 0.759,
+ "score_loc": 0.055
+ },
+ {
+ "component": "Dystric fluvisols",
+ "componentData": "Data Complete",
+ "componentID": 136009,
+ "name": "Dystric fluvisols",
+ "rank_data": "5",
+ "rank_data_loc": "8",
+ "rank_loc": 10,
+ "score_data": 0.432,
+ "score_data_loc": 0.75,
+ "score_loc": 0.045
+ },
+ {
+ "component": "Eutric fluvisols",
+ "componentData": "Data Complete",
+ "componentID": 136283,
+ "name": "Eutric fluvisols",
+ "rank_data": "10",
+ "rank_data_loc": "9",
+ "rank_loc": 5,
+ "score_data": 0.238,
+ "score_data_loc": 0.549,
+ "score_loc": 0.111
+ },
+ {
+ "component": "Dystric regosols",
+ "componentData": "Data Complete",
+ "componentID": 136281,
+ "name": "Dystric regosols",
+ "rank_data": "11",
+ "rank_data_loc": "10",
+ "rank_loc": 1,
+ "score_data": 0.083,
+ "score_data_loc": 0.392,
+ "score_loc": 0.166
+ },
+ {
+ "component": "Lithic leptosols",
+ "componentData": "Missing Data",
+ "componentID": 134464,
+ "name": "Lithic leptosols",
+ "rank_data": "6",
+ "rank_data_loc": "11",
+ "rank_loc": 11,
+ "score_data": 0.432,
+ "score_data_loc": 0.003,
+ "score_loc": 0.022
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/global/test_global.py b/soil_id/tests/global/test_global.py
index c60dba2..ef99f2c 100644
--- a/soil_id/tests/global/test_global.py
+++ b/soil_id/tests/global/test_global.py
@@ -17,6 +17,7 @@
import time
import pytest
+from syrupy.extensions.json import JSONSnapshotExtension
from soil_id.db import get_datastore_connection
from soil_id.global_soil import list_soils_global, rank_soils_global
@@ -26,26 +27,180 @@
{"lat": -10.950086, "lon": 17.573093},
{"lat": 34.5, "lon": 69.16667},
{"lat": -10.07856, "lon": 15.107436},
+ {
+ "lat": -19.13333,
+ "lon": 145.5125,
+ "data": {
+ "bottomDepth": [10, 24],
+ "lab_Color": [
+ [81.36696398, 2.011595682, 13.47178439],
+ [81.36696398, 2.011595682, 13.47178439],
+ ],
+ "rfvDepth": [None, None],
+ "soilHorizon": ["Sandy loam", "Loam"],
+ "topDepth": [0, 10],
+ },
+ },
+ {
+ "lat": 48.71667,
+ "lon": 126.13333,
+ "data": {
+ "bottomDepth": [20],
+ "lab_Color": [[51.58348661, 4.985592123, 11.10506759]],
+ "rfvDepth": [None],
+ "soilHorizon": ["Loamy sand"],
+ "topDepth": [0],
+ },
+ },
+ {
+ "lat": 37.33333,
+ "lon": -5.4,
+ "data": {
+ "bottomDepth": [25, 160],
+ "lab_Color": [
+ [41.22423435, 1.447890286, 6.167240052],
+ [51.59649652, 4.791128549, 18.92743224],
+ ],
+ "rfvDepth": [None, None],
+ "soilHorizon": ["Clay", "Clay"],
+ "topDepth": [0, 125],
+ },
+ },
+ {
+ "lat": -1.75,
+ "lon": 13.6,
+ "data": {
+ "bottomDepth": [10, 30],
+ "lab_Color": [
+ [30.77416274, 5.568356326, 18.03952892],
+ [41.23714543, 7.282579218, 25.96353458],
+ ],
+ "rfvDepth": [None, None],
+ "soilHorizon": ["Clay", "Clay"],
+ "topDepth": [0, 10],
+ },
+ },
+ {
+ "lat": 8.48333,
+ "lon": 76.95,
+ "data": {
+ "bottomDepth": [9, 25, 52],
+ "lab_Color": [
+ [61.6838179, 11.454856, 19.93103357],
+ [61.68224615, 17.08123986, 30.77963923],
+ [51.60588072, 9.821763719, 38.77054648],
+ ],
+ "rfvDepth": [42.0, 41.0, 56.0],
+ "soilHorizon": ["Clay", "Clay", "Clay"],
+ "topDepth": [0, 9, 25],
+ },
+ },
+ {
+ "lat": 30.38333,
+ "lon": 35.53333,
+ "data": {
+ "bottomDepth": [5],
+ "lab_Color": [[71.62679033, 5.183026621, 25.83506164]],
+ "rfvDepth": [50.0],
+ "soilHorizon": ["Loam"],
+ "topDepth": [0],
+ },
+ },
+ {
+ "lat": -2.06972,
+ "lon": 37.29,
+ "data": {
+ "bottomDepth": [80, 125, 140],
+ "lab_Color": [
+ [30.73434089, 19.87611528, 21.31856213],
+ [30.73434089, 19.87611528, 21.31856213],
+ [30.73434089, 19.87611528, 21.31856213],
+ ],
+ "rfvDepth": [None, None, None],
+ "soilHorizon": ["Clay", "Clay", "Silty clay loam"],
+ "topDepth": [37, 80, 125],
+ },
+ },
+ {
+ "lat": 32.11667,
+ "lon": 20.08333,
+ "data": {
+ "bottomDepth": [20, 47, 120],
+ "lab_Color": [
+ [81.35859545, 3.799237833, 11.54430451],
+ [81.35859545, 3.799237833, 11.54430451],
+ [81.35859545, 3.799237833, 11.54430451],
+ ],
+ "rfvDepth": [None, None, None],
+ "soilHorizon": ["Sand", "Sand", "Sand"],
+ "topDepth": [0, 20, 47],
+ },
+ },
+ {
+ "lat": -24.53333,
+ "lon": 33.36667,
+ "data": {
+ "bottomDepth": [5, 10],
+ "lab_Color": [
+ [51.59117331, 3.180150056, 12.67936276],
+ [71.60636516, 1.125498577, 6.932398776],
+ ],
+ "rfvDepth": [None, None],
+ "soilHorizon": ["Sandy loam", "Loamy sand"],
+ "topDepth": [0, 5],
+ },
+ },
+ {
+ "lat": 15.73333,
+ "lon": 120.31667,
+ "data": {
+ "bottomDepth": [10, 23, 38],
+ "lab_Color": [
+ [41.22423435, 1.447890286, 6.167240052],
+ [41.22423435, 1.447890286, 6.167240052],
+ [51.5981893, 1.26834264, 13.74773572],
+ ],
+ "rfvDepth": [None, None, None],
+ "soilHorizon": ["Silty clay loam", "Silty clay loam", "Silt loam"],
+ "topDepth": [0, 10, 23],
+ },
+ },
]
+test_params = []
+for idx, coords in enumerate(test_locations):
+ test_params.append(pytest.param(coords, id=f"{coords['lat']},{coords['lon']}"))
+
+
+@pytest.mark.parametrize("location", test_params)
+def test_soil_location(location, snapshot):
+ if "data" in location:
+ data = location["data"]
+ else:
+ data = {
+ "soilHorizon": ["Loam"],
+ "topDepth": [0],
+ "bottomDepth": [15],
+ "rfvDepth": [20],
+ "lab_Color": [[41.23035939, 3.623018224, 13.27654356]],
+ }
-@pytest.mark.parametrize("location", test_locations)
-def test_soil_location(location):
with get_datastore_connection() as connection:
logging.info(f"Testing {location['lon']}, {location['lat']}")
start_time = time.perf_counter()
list_soils_result = list_soils_global(connection, location["lon"], location["lat"])
logging.info(f"...time: {(time.perf_counter() - start_time):.2f}s")
- rank_soils_global(
+ rank_result = rank_soils_global(
connection,
location["lon"],
location["lat"],
list_output_data=list_soils_result,
- soilHorizon=["Loam"],
- topDepth=[0],
- bottomDepth=[15],
- rfvDepth=[20],
- lab_Color=[[41.23035939, 3.623018224, 13.27654356]],
+ **data,
bedrock=None,
cracks=None,
)
+
+ assert snapshot.with_defaults(extension_class=JSONSnapshotExtension) == {
+ "list": list_soils_result.soil_list_json,
+ "rank": rank_result,
+ }
diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[33.81246789,-101.9733687].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[33.81246789,-101.9733687].json
new file mode 100644
index 0000000..042f837
--- /dev/null
+++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[33.81246789,-101.9733687].json
@@ -0,0 +1,794 @@
+{
+ "list": {
+ "AWS_PIW90": 5.09,
+ "Soil Data Value": [
+ [
+ "rfv_class_30",
+ 0.12794865070214412
+ ],
+ [
+ "texture_0",
+ 0.0
+ ],
+ [
+ "texture_30",
+ 0.0
+ ],
+ [
+ "rfv_class_0",
+ 0.0
+ ]
+ ],
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R077CY022TX"
+ ],
+ "ecoclassname": [
+ "Deep Hardland 16-21 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY022TX"
+ ]
+ }
+ },
+ "id": {
+ "component": "Randall",
+ "name": "Randall",
+ "rank_loc": "1",
+ "score_loc": 0.474
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25623332",
+ "componentKind": "Series",
+ "componentPct": 80,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "369864",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "w",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=randall",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#randall",
+ "slope": 0.5,
+ "taxsubgrp": "Ustic Epiaquerts",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Randall series consists of very deep, poorly drained, very slowly permeable soils that formed in clayey lacustrine sediments derived from the Blackwater Draw Formation of Pleistocene age. These nearly level soils are on the floor of playa basins 3 to 15 m (10 to 50 ft) below the surrounding plain and range in size from 10 to more than 150 acres. Slope ranges from 0 to 1 percent. Mean annual precipitation is 483 mm (19 in), and mean annual temperature is 15 degrees C (59 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R077CY036TX"
+ ],
+ "ecoclassname": [
+ "Sandy Loam 16-21 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY036TX"
+ ]
+ }
+ },
+ "id": {
+ "component": "Acuff",
+ "name": "Acuff",
+ "rank_loc": "2",
+ "score_loc": 0.253
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25623211",
+ "componentKind": "Series",
+ "componentPct": 85,
+ "dataSource": "SSURGO",
+ "distance": 90.0,
+ "irrcapcl": "3",
+ "irrcapscl": "e",
+ "irrcapunit": "None",
+ "mapunitID": "369839",
+ "minCompDistance": 90.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=acuff",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#acuff",
+ "slope": 2.0,
+ "taxsubgrp": "Aridic Paleustolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Acuff series consists of very deep, well drained, moderately permeable soils. These soils formed in loamy eolian sediments in the Blackwater Draw Formation of Pleistocene age. Acuff soils are on nearly level to gently sloping plains and playa slopes. Slope ranges from 0 to 5 percent. Mean annual precipitation is about 483 mm (19 in) and the mean annual air temperature is about 16 degrees C (60 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R077CY022TX"
+ ],
+ "ecoclassname": [
+ "Deep Hardland 16-21 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY022TX"
+ ]
+ }
+ },
+ "id": {
+ "component": "Olton",
+ "name": "Olton",
+ "rank_loc": "3",
+ "score_loc": 0.126
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25623299",
+ "componentKind": "Series",
+ "componentPct": 85,
+ "dataSource": "SSURGO",
+ "distance": 204.0,
+ "irrcapcl": "1",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "369851",
+ "minCompDistance": 204.0,
+ "nirrcapcl": "2",
+ "nirrcapscl": "c",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=olton",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#olton",
+ "slope": 0.4,
+ "taxsubgrp": "Aridic Paleustolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Olton series consists of very deep, well drained, moderately slowly permeable soils that formed in clayey, calcareous eolian sediments in the\nBlackwater Draw Formation of Pleistocene age. These soils are on nearly level to gently sloping plains and upper side slopes of playas and draws. Slope ranges from 0 to 5 percent. Mean annual precipitation is 483 mm (19 in), and mean annual temperature is 15 degrees C (59 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R077CY022TX"
+ ],
+ "ecoclassname": [
+ "Deep Hardland 16-21 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY022TX"
+ ]
+ }
+ },
+ "id": {
+ "component": "Mclean",
+ "name": "Mclean",
+ "rank_loc": "4",
+ "score_loc": 0.059
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25623333",
+ "componentKind": "Series",
+ "componentPct": 10,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "4",
+ "irrcapscl": "w",
+ "irrcapunit": "None",
+ "mapunitID": "369864",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "4",
+ "nirrcapscl": "w",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=mclean",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#mclean",
+ "slope": 0.5,
+ "taxsubgrp": "Udic Haplusterts",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The McLean series consists of very deep, somewhat poorly drained, very slowly permeable soils that formed in clayey lacustrine deposits of Quaternary age. These nearly level soils are on the floor of playas 1.5 to 23 m (5 to 75 ft) below the surrounding plain and range in size from a few acres to more than 200 acres. Slope ranges from 0 to 1 percent. Mean annual precipitation is 483 mm (19 in), and mean annual temperature is 16 degrees C (61 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R077CY022TX"
+ ],
+ "ecoclassname": [
+ "Deep Hardland 16-21 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY022TX"
+ ]
+ }
+ },
+ "id": {
+ "component": "Lockney",
+ "name": "Lockney",
+ "rank_loc": "5",
+ "score_loc": 0.03
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25623334",
+ "componentKind": "Series",
+ "componentPct": 5,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "2",
+ "irrcapscl": "s",
+ "irrcapunit": "None",
+ "mapunitID": "369864",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=lockney",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#lockney",
+ "slope": 0.5,
+ "taxsubgrp": "Typic Haplusterts",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Lockney series consists of very deep, moderately well drained, very slowly permeable soils that formed in clayey lacustrine deposits of Quaternary age. These nearly level soils are on a playa step in large playa basins. Slope ranges from 0 to 1 percent. Mean annual precipitation is 483 mm (19 inches) and mean annual temperature is 16 degrees C (61 F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R077CY022TX"
+ ],
+ "ecoclassname": [
+ "Deep Hardland 16-21 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY022TX"
+ ]
+ }
+ },
+ "id": {
+ "component": "Estacado",
+ "name": "Estacado",
+ "rank_loc": "6",
+ "score_loc": 0.021
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25623213",
+ "componentKind": "Series",
+ "componentPct": 6,
+ "dataSource": "SSURGO",
+ "distance": 90.0,
+ "irrcapcl": "3",
+ "irrcapscl": "e",
+ "irrcapunit": "None",
+ "mapunitID": "369839",
+ "minCompDistance": 90.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=estacado",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#estacado",
+ "slope": 2.0,
+ "taxsubgrp": "Aridic Paleustolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Estacado series consists of very deep, well drained, moderately slowly permeable soils that formed in calcareous, loamy eolian deposits of the Blackwater Draw Formation of Pleistocene age. These soils are on nearly level to gently sloping plains and playa slopes. Slope ranges from 0 to 5 percent. Mean annual precipitation is 483 mm (19 in) and mean annual air temperature is 16 degrees C (61 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R077CY027TX"
+ ],
+ "ecoclassname": [
+ "Playa 16-21 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY027TX"
+ ]
+ }
+ },
+ "id": {
+ "component": "Friona",
+ "name": "Friona",
+ "rank_loc": "7",
+ "score_loc": 0.014
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25623214",
+ "componentKind": "Series",
+ "componentPct": 5,
+ "dataSource": "SSURGO",
+ "distance": 90.0,
+ "irrcapcl": "3",
+ "irrcapscl": "e",
+ "irrcapunit": "None",
+ "mapunitID": "369839",
+ "minCompDistance": 90.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=friona",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#friona",
+ "slope": 2.0,
+ "taxsubgrp": "Petrocalcic Paleustolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Friona series consists of soils that are moderately deep to a petrocalcic horizon. They are well drained, moderately permeable soils that formed in loamy eolian sediments from the Blackwater Draw Formation of Pleistocene age. These soils are on nearly level to gently sloping plains. Slope ranges from 0 to 3 percent. Mean annual precipitation is about 483 mm (19 in), and mean annual air temperature is about 16 degrees C (61 degrees F)"
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R077CY027TX"
+ ],
+ "ecoclassname": [
+ "Playa 16-21 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY027TX"
+ ]
+ }
+ },
+ "id": {
+ "component": "Amarillo",
+ "name": "Amarillo",
+ "rank_loc": "8",
+ "score_loc": 0.011
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25623212",
+ "componentKind": "Series",
+ "componentPct": 4,
+ "dataSource": "SSURGO",
+ "distance": 90.0,
+ "irrcapcl": "3",
+ "irrcapscl": "e",
+ "irrcapunit": "None",
+ "mapunitID": "369839",
+ "minCompDistance": 90.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=amarillo",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#amarillo",
+ "slope": 2.0,
+ "taxsubgrp": "Aridic Paleustalfs",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Amarillo series consists of very deep, well drained, moderately permeable soils. These soils formed in loamy eolian deposits from the Blackwater Draw Formation of Pleistocene age. Amarillo soils are on nearly level to gently sloping plains and playa slopes. Slope ranges from 0 to 5 percent. Mean annual precipitation is 483 mm (19 in) and the mean annual air temperature is 16 degrees C (61 degrees F)"
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R077CY022TX"
+ ],
+ "ecoclassname": [
+ "Deep Hardland 16-21 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY022TX"
+ ]
+ }
+ },
+ "id": {
+ "component": "Pullman",
+ "name": "Pullman",
+ "rank_loc": "9",
+ "score_loc": 0.011
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25623298",
+ "componentKind": "Series",
+ "componentPct": 7,
+ "dataSource": "SSURGO",
+ "distance": 204.0,
+ "irrcapcl": "3",
+ "irrcapscl": "s",
+ "irrcapunit": "None",
+ "mapunitID": "369851",
+ "minCompDistance": 204.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=pullman",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#pullman",
+ "slope": 0.4,
+ "taxsubgrp": "Torrertic Paleustolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Pullman series consists of very deep, well drained, slowly permeable soils that formed in clayey eolian deposits from the Blackwater Draw Formation of Pleistocene age. These soils occur on nearly level to very gently sloping plains or playa slopes. Slope ranges from 0 to 3 percent. The mean annual precipitation is about 483 mm (19 in) and the mean annual temperature is about 16 degrees C (60 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R077CY022TX"
+ ],
+ "ecoclassname": [
+ "Deep Hardland 16-21 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY022TX"
+ ]
+ }
+ },
+ "id": {
+ "component": "Acuff",
+ "name": "Acuff2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.253
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25623297",
+ "componentKind": "Series",
+ "componentPct": 5,
+ "dataSource": "SSURGO",
+ "distance": 204.0,
+ "irrcapcl": "2",
+ "irrcapscl": "s",
+ "irrcapunit": "None",
+ "mapunitID": "369851",
+ "minCompDistance": 90.0,
+ "nirrcapcl": "2",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=acuff",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#acuff",
+ "slope": 0.5,
+ "taxsubgrp": "Aridic Paleustolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Acuff series consists of very deep, well drained, moderately permeable soils. These soils formed in loamy eolian sediments in the Blackwater Draw Formation of Pleistocene age. Acuff soils are on nearly level to gently sloping plains and playa slopes. Slope ranges from 0 to 5 percent. Mean annual precipitation is about 483 mm (19 in) and the mean annual air temperature is about 16 degrees C (60 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R077CY022TX"
+ ],
+ "ecoclassname": [
+ "Deep Hardland 16-21 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY022TX"
+ ]
+ }
+ },
+ "id": {
+ "component": "Estacado",
+ "name": "Estacado2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.021
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25623296",
+ "componentKind": "Series",
+ "componentPct": 3,
+ "dataSource": "SSURGO",
+ "distance": 204.0,
+ "irrcapcl": "1",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "369851",
+ "minCompDistance": 90.0,
+ "nirrcapcl": "2",
+ "nirrcapscl": "c",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=estacado",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#estacado",
+ "slope": 0.5,
+ "taxsubgrp": "Aridic Paleustolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Estacado series consists of very deep, well drained, moderately slowly permeable soils that formed in calcareous, loamy eolian deposits of the Blackwater Draw Formation of Pleistocene age. These soils are on nearly level to gently sloping plains and playa slopes. Slope ranges from 0 to 5 percent. Mean annual precipitation is 483 mm (19 in) and mean annual air temperature is 16 degrees C (61 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "us",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Randall",
+ "componentData": "Missing Data",
+ "componentID": 25623332,
+ "name": "Randall",
+ "rank_data": "8",
+ "rank_data_loc": "1",
+ "rank_loc": "1",
+ "score_data": 0.429,
+ "score_data_loc": 0.452,
+ "score_loc": 0.474
+ },
+ {
+ "component": "Acuff",
+ "componentData": "Data Complete",
+ "componentID": 25623297,
+ "name": "Acuff2",
+ "rank_data": "1",
+ "rank_data_loc": "2",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.591,
+ "score_data_loc": 0.422,
+ "score_loc": 0.253
+ },
+ {
+ "component": "Friona",
+ "componentData": "Data Complete",
+ "componentID": 25623214,
+ "name": "Friona",
+ "rank_data": "2",
+ "rank_data_loc": "3",
+ "rank_loc": "7",
+ "score_data": 0.571,
+ "score_data_loc": 0.293,
+ "score_loc": 0.014
+ },
+ {
+ "component": "Olton",
+ "componentData": "Data Complete",
+ "componentID": 25623299,
+ "name": "Olton",
+ "rank_data": "7",
+ "rank_data_loc": "4",
+ "rank_loc": "3",
+ "score_data": 0.457,
+ "score_data_loc": 0.292,
+ "score_loc": 0.126
+ },
+ {
+ "component": "Amarillo",
+ "componentData": "Data Complete",
+ "componentID": 25623212,
+ "name": "Amarillo",
+ "rank_data": "3",
+ "rank_data_loc": "5",
+ "rank_loc": "8",
+ "score_data": 0.554,
+ "score_data_loc": 0.283,
+ "score_loc": 0.011
+ },
+ {
+ "component": "Lockney",
+ "componentData": "Missing Data",
+ "componentID": 25623334,
+ "name": "Lockney",
+ "rank_data": "5",
+ "rank_data_loc": "6",
+ "rank_loc": "5",
+ "score_data": 0.531,
+ "score_data_loc": 0.28,
+ "score_loc": 0.03
+ },
+ {
+ "component": "Pullman",
+ "componentData": "Data Complete",
+ "componentID": 25623298,
+ "name": "Pullman",
+ "rank_data": "4",
+ "rank_data_loc": "7",
+ "rank_loc": "9",
+ "score_data": 0.536,
+ "score_data_loc": 0.274,
+ "score_loc": 0.011
+ },
+ {
+ "component": "Estacado",
+ "componentData": "Data Complete",
+ "componentID": 25623213,
+ "name": "Estacado",
+ "rank_data": "6",
+ "rank_data_loc": "8",
+ "rank_loc": "6",
+ "score_data": 0.493,
+ "score_data_loc": 0.257,
+ "score_loc": 0.021
+ },
+ {
+ "component": "Mclean",
+ "componentData": "Missing Data",
+ "componentID": 25623333,
+ "name": "Mclean",
+ "rank_data": "9",
+ "rank_data_loc": "9",
+ "rank_loc": "4",
+ "score_data": 0.412,
+ "score_data_loc": 0.236,
+ "score_loc": 0.059
+ },
+ {
+ "component": "Acuff",
+ "componentData": "Data Complete",
+ "componentID": 25623211,
+ "name": "Acuff",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "2",
+ "score_data": 0.578,
+ "score_data_loc": 0.416,
+ "score_loc": 0.253
+ },
+ {
+ "component": "Estacado",
+ "componentData": "Data Complete",
+ "componentID": 25623296,
+ "name": "Estacado2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.443,
+ "score_data_loc": 0.232,
+ "score_loc": 0.021
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[34.92816,-114.80764].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[34.92816,-114.80764].json
new file mode 100644
index 0000000..5cd3860
--- /dev/null
+++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[34.92816,-114.80764].json
@@ -0,0 +1,976 @@
+{
+ "list": {
+ "AWS_PIW90": 12.64,
+ "Soil Data Value": [
+ [
+ "rfv_class_30",
+ 0.5074815208577954
+ ],
+ [
+ "texture_30",
+ 0.38007948871089425
+ ],
+ [
+ "rfv_class_0",
+ 0.3160432490369194
+ ],
+ [
+ "texture_0",
+ 0.0
+ ]
+ ],
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "Carrizo",
+ "name": "Carrizo",
+ "rank_loc": "1",
+ "score_loc": 0.269
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "14185637",
+ "componentKind": "Series",
+ "componentPct": 6,
+ "dataSource": "STATSGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "660587",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 1.0,
+ "taxsubgrp": "Typic Torriorthents",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "Gunsight",
+ "name": "Gunsight",
+ "rank_loc": "2",
+ "score_loc": 0.18
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+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
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+ "componentPct": 27,
+ "dataSource": "STATSGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "660587",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 21.0,
+ "taxsubgrp": "Typic Haplocalcids",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "Chuckawalla",
+ "name": "Chuckawalla",
+ "rank_loc": "3",
+ "score_loc": 0.051
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "14185642",
+ "componentKind": "Series",
+ "componentPct": 8,
+ "dataSource": "STATSGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "660587",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 15.0,
+ "taxsubgrp": "Typic Calciargids",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "Beeline",
+ "name": "Beeline",
+ "rank_loc": "4",
+ "score_loc": 0.026
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "14185640",
+ "componentKind": "Series",
+ "componentPct": 5,
+ "dataSource": "STATSGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "660587",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 24.0,
+ "taxsubgrp": "Typic Torriorthents",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "Cipriano",
+ "name": "Cipriano",
+ "rank_loc": "5",
+ "score_loc": 0.026
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "14185643",
+ "componentKind": "Series",
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diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[35.59918,-120.491439].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[35.59918,-120.491439].json
new file mode 100644
index 0000000..7e31ea0
--- /dev/null
+++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[35.59918,-120.491439].json
@@ -0,0 +1,318 @@
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+ "distance": 0.0,
+ "irrcapcl": "6",
+ "irrcapscl": "e",
+ "irrcapunit": "nan",
+ "mapunitID": "457283",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "nan",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=balcom",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#balcom",
+ "slope": 40.0,
+ "taxsubgrp": "Typic Argixerolls",
+ "textureInfill": "Yes"
+ },
+ "siteDescription": "The Los Osos series consists of moderately deep, well drained soils that formed in material weathered from sandstone and shale. Los Osos soils are on uplands and have slopes of 5 to 75 percent. The mean annual precipitation is about 25 inches and the mean annual air temperature is about 60 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R015XE082CA"
+ ],
+ "ecoclassname": [
+ "Loamy South"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/015X/R015XE082CA"
+ ]
+ }
+ },
+ "id": {
+ "component": "Balcom",
+ "name": "Balcom3",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.252
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "26027125",
+ "componentKind": "Series",
+ "componentPct": 45,
+ "dataSource": "SSURGO",
+ "distance": 670.0,
+ "irrcapcl": "4",
+ "irrcapscl": "e",
+ "irrcapunit": "1.0",
+ "mapunitID": "457217",
+ "minCompDistance": 44.0,
+ "nirrcapcl": "4",
+ "nirrcapscl": "e",
+ "nirrcapunit": "1.0",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=balcom",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#balcom",
+ "slope": 20.0,
+ "taxsubgrp": "Calcixerollic Xerochrepts",
+ "textureInfill": "Yes"
+ },
+ "siteDescription": "The Balcom series consists of moderately deep, well drained soils that formed in material that weathered from soft, calcareous shale and sandstone. Balcom soils are on hills and have slopes of 5 to 75 percent. The mean annual precipitation is about 18 inches and the mean annual air temperature is about 61 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R015XE020CA"
+ ],
+ "ecoclassname": [
+ "Fine Loamy 9-13"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/015X/R015XE020CA"
+ ]
+ }
+ },
+ "id": {
+ "component": "Los osos",
+ "name": "Los osos2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.125
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "26027715",
+ "componentKind": "Series",
+ "componentPct": 20,
+ "dataSource": "SSURGO",
+ "distance": 385.0,
+ "irrcapcl": "4",
+ "irrcapscl": "e",
+ "irrcapunit": "3.0",
+ "mapunitID": "457282",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "4",
+ "nirrcapscl": "e",
+ "nirrcapunit": "3.0",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=los_osos",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#los_osos",
+ "slope": 20.0,
+ "taxsubgrp": "Typic Argixerolls",
+ "textureInfill": "Yes"
+ },
+ "siteDescription": "The Los Osos series consists of moderately deep, well drained soils that formed in material weathered from sandstone and shale. Los Osos soils are on uplands and have slopes of 5 to 75 percent. The mean annual precipitation is about 25 inches and the mean annual air temperature is about 60 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "us",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Balcom",
+ "componentData": "Data Complete",
+ "componentID": 26027125,
+ "name": "Balcom3",
+ "rank_data": "1",
+ "rank_data_loc": "1",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.552,
+ "score_data_loc": 0.402,
+ "score_loc": 0.252
+ },
+ {
+ "component": "Los osos",
+ "componentData": NaN,
+ "componentID": 26027715,
+ "name": "Los osos2",
+ "rank_data": "2",
+ "rank_data_loc": "2",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.535,
+ "score_data_loc": 0.33,
+ "score_loc": 0.125
+ },
+ {
+ "component": "Balcom",
+ "componentData": "Data Complete",
+ "componentID": 26027166,
+ "name": "Balcom2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "1",
+ "score_data": 0.345,
+ "score_data_loc": 0.299,
+ "score_loc": 0.252
+ },
+ {
+ "component": "Los osos",
+ "componentData": NaN,
+ "componentID": 26027683,
+ "name": "Los osos",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "2",
+ "score_data": 0.37,
+ "score_data_loc": 0.248,
+ "score_loc": 0.125
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.422,-122.084].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.422,-122.084].json
new file mode 100644
index 0000000..c1822a3
--- /dev/null
+++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.422,-122.084].json
@@ -0,0 +1,522 @@
+{
+ "list": {
+ "AWS_PIW90": 5.98,
+ "Soil Data Value": [
+ [
+ "rfv_class_0",
+ 1.2450871546455828
+ ],
+ [
+ "rfv_class_30",
+ 0.7766173768825435
+ ],
+ [
+ "texture_0",
+ 0.0
+ ],
+ [
+ "texture_30",
+ 0.0
+ ]
+ ],
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R014XG903CA"
+ ],
+ "ecoclassname": [
+ "Salt Marsh"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/014X/R014XG903CA"
+ ]
+ }
+ },
+ "id": {
+ "component": "Hangerone",
+ "name": "Hangerone",
+ "rank_loc": "1",
+ "score_loc": 0.39
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "26038467",
+ "componentKind": "Series",
+ "componentPct": 25,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "2",
+ "irrcapscl": "s",
+ "irrcapunit": "5.0",
+ "mapunitID": "1543362",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "s",
+ "nirrcapunit": "5.0",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hangerone",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hangerone",
+ "slope": 1.0,
+ "taxsubgrp": "Cumulic Vertic Endoaquolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Hangerone series consists of very deep, poorly drained soils that formed in alluvium from mixed rock sources. Hangerone soils are in basins. Slopes range from 0 to 2 percent. The mean annual precipitation is about 14 inches and the mean annual temperature is about 60 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R014XG903CA"
+ ],
+ "ecoclassname": [
+ "Salt Marsh"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/014X/R014XG903CA"
+ ]
+ }
+ },
+ "id": {
+ "component": "Xerorthents",
+ "name": "Xerorthents",
+ "rank_loc": "2",
+ "score_loc": 0.386
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "26038503",
+ "componentKind": "Taxon above family",
+ "componentPct": 100,
+ "dataSource": "SSURGO",
+ "distance": 149.0,
+ "irrcapcl": "4",
+ "irrcapscl": "e",
+ "irrcapunit": "9.0",
+ "mapunitID": "1602803",
+ "minCompDistance": 149.0,
+ "nirrcapcl": "4",
+ "nirrcapscl": "e",
+ "nirrcapunit": "9.0",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 22.0,
+ "taxsubgrp": "None",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ ""
+ ],
+ "ecoclassname": [
+ ""
+ ],
+ "edit_url": [
+ ""
+ ]
+ }
+ },
+ "id": {
+ "component": "Aquic xerorthents",
+ "name": "Aquic xerorthents",
+ "rank_loc": "3",
+ "score_loc": 0.165
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "26038456",
+ "componentKind": "Family",
+ "componentPct": 95,
+ "dataSource": "SSURGO",
+ "distance": 717.0,
+ "irrcapcl": "3",
+ "irrcapscl": "w",
+ "irrcapunit": "2.0",
+ "mapunitID": "1602806",
+ "minCompDistance": 717.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "w",
+ "nirrcapunit": "2.0",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=aquic_xerorthents",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#aquic_xerorthents",
+ "slope": 4.0,
+ "taxsubgrp": "Aquic Xerorthents",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R014XG904CA"
+ ],
+ "ecoclassname": [
+ "Dry Clayey Bottom"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/014X/R014XG904CA"
+ ]
+ }
+ },
+ "id": {
+ "component": "Clear lake",
+ "name": "Clear lake",
+ "rank_loc": "4",
+ "score_loc": 0.029
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "26038466",
+ "componentKind": "Series",
+ "componentPct": 2,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "2",
+ "irrcapscl": "s",
+ "irrcapunit": "5.0",
+ "mapunitID": "1543362",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "s",
+ "nirrcapunit": "5.0",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=clear_lake",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#clear_lake",
+ "slope": 1.0,
+ "taxsubgrp": "Xeric Endoaquerts",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Clear Lake series consists of very deep, poorly drained soils that formed in fine textured alluvium derived from mixed rock sources. Clear Lake soils are in flood basins, flood plains and in swales of drainageways. Slopes are 0 to 5 percent. The mean annual precipitation is about 20 inches and the mean annual air temperature is about 60 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ ""
+ ],
+ "ecoclassname": [
+ ""
+ ],
+ "edit_url": [
+ ""
+ ]
+ }
+ },
+ "id": {
+ "component": "Bayshore",
+ "name": "Bayshore",
+ "rank_loc": "5",
+ "score_loc": 0.019
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "26038468",
+ "componentKind": "Taxadjunct",
+ "componentPct": 2,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "1",
+ "irrcapscl": "None",
+ "irrcapunit": "nan",
+ "mapunitID": "1543362",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "s",
+ "nirrcapunit": "nan",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=bayshore",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#bayshore",
+ "slope": 1.0,
+ "taxsubgrp": "Typic Argiaquolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Bayshore series consists of very deep, somewhat poorly and poorly drained soils formed in nearly level basins from alluvium. Slopes are 0 to 1 percent. The mean annual precipitation is about 13 to 15 inches and the mean annual temperature is about 59 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R014XG903CA"
+ ],
+ "ecoclassname": [
+ "Salt Marsh"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/014X/R014XG903CA"
+ ]
+ }
+ },
+ "id": {
+ "component": "Embarcadero",
+ "name": "Embarcadero",
+ "rank_loc": "6",
+ "score_loc": 0.012
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "26038464",
+ "componentKind": "Series",
+ "componentPct": 1,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "4",
+ "irrcapscl": "s",
+ "irrcapunit": "6.0",
+ "mapunitID": "1543362",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "4",
+ "nirrcapscl": "s",
+ "nirrcapunit": "6.0",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=embarcadero",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#embarcadero",
+ "slope": 1.0,
+ "taxsubgrp": "Fluvaquentic Endoaquolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Embarcadero series consists of very deep, naturally poorly drained soils, now artificially drained that formed in alluvium from mixed rock sources. Embarcadero soils are in basins near the edge of marshes. Slopes range from 0 to 2 percent. The mean annual precipitation is about 13 inches and the mean annual temperature is about 60 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ ""
+ ],
+ "ecoclassname": [
+ ""
+ ],
+ "edit_url": [
+ ""
+ ]
+ }
+ },
+ "id": {
+ "component": "Xerorthents",
+ "name": "Xerorthents2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.386
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "26038454",
+ "componentKind": "Taxon above family",
+ "componentPct": 100,
+ "dataSource": "SSURGO",
+ "distance": 776.0,
+ "irrcapcl": "6",
+ "irrcapscl": "e",
+ "irrcapunit": "9.0",
+ "mapunitID": "1602804",
+ "minCompDistance": 149.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "9.0",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 40.0,
+ "taxsubgrp": "None",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "us",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Xerorthents",
+ "componentData": "Data Complete",
+ "componentID": 26038503,
+ "name": "Xerorthents",
+ "rank_data": "1",
+ "rank_data_loc": "1",
+ "rank_loc": "2",
+ "score_data": 0.76,
+ "score_data_loc": 0.573,
+ "score_loc": 0.386
+ },
+ {
+ "component": "Hangerone",
+ "componentData": "Data Complete",
+ "componentID": 26038467,
+ "name": "Hangerone",
+ "rank_data": "6",
+ "rank_data_loc": "2",
+ "rank_loc": "1",
+ "score_data": 0.554,
+ "score_data_loc": 0.472,
+ "score_loc": 0.39
+ },
+ {
+ "component": "Aquic xerorthents",
+ "componentData": "Missing Data",
+ "componentID": 26038456,
+ "name": "Aquic xerorthents",
+ "rank_data": "3",
+ "rank_data_loc": "3",
+ "rank_loc": "3",
+ "score_data": 0.626,
+ "score_data_loc": 0.395,
+ "score_loc": 0.165
+ },
+ {
+ "component": "Embarcadero",
+ "componentData": "Missing Data",
+ "componentID": 26038464,
+ "name": "Embarcadero",
+ "rank_data": "2",
+ "rank_data_loc": "4",
+ "rank_loc": "6",
+ "score_data": 0.712,
+ "score_data_loc": 0.362,
+ "score_loc": 0.012
+ },
+ {
+ "component": "Clear lake",
+ "componentData": "Missing Data",
+ "componentID": 26038466,
+ "name": "Clear lake",
+ "rank_data": "4",
+ "rank_data_loc": "5",
+ "rank_loc": "4",
+ "score_data": 0.617,
+ "score_data_loc": 0.323,
+ "score_loc": 0.029
+ },
+ {
+ "component": "Bayshore",
+ "componentData": "Data Complete",
+ "componentID": 26038468,
+ "name": "Bayshore",
+ "rank_data": "5",
+ "rank_data_loc": "6",
+ "rank_loc": "5",
+ "score_data": 0.607,
+ "score_data_loc": 0.313,
+ "score_loc": 0.019
+ },
+ {
+ "component": "Xerorthents",
+ "componentData": "Data Complete",
+ "componentID": 26038454,
+ "name": "Xerorthents2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.652,
+ "score_data_loc": 0.519,
+ "score_loc": 0.386
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.48216451,-99.55016693].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.48216451,-99.55016693].json
new file mode 100644
index 0000000..3267a5d
--- /dev/null
+++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.48216451,-99.55016693].json
@@ -0,0 +1,1066 @@
+{
+ "list": {
+ "AWS_PIW90": 5.13,
+ "Soil Data Value": [
+ [
+ "rfv_class_30",
+ 0.33402123132077044
+ ],
+ [
+ "rfv_class_0",
+ 0.27699134340154963
+ ],
+ [
+ "texture_0",
+ 0.0
+ ],
+ [
+ "texture_30",
+ 0.0
+ ]
+ ],
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R073XY101KS"
+ ],
+ "ecoclassname": [
+ "Limy Slopes"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY101KS"
+ ]
+ }
+ },
+ "id": {
+ "component": "Uly",
+ "name": "Uly",
+ "rank_loc": "1",
+ "score_loc": 0.295
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
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+ "componentPct": 90,
+ "dataSource": "SSURGO",
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+ "irrcapcl": "3",
+ "irrcapscl": "e",
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+ "nirrcapcl": "3",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=uly",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#uly",
+ "slope": 5.0,
+ "taxsubgrp": "Typic Haplustolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Uly series includes very deep, well drained formed in loess on uplands. Slopes range from 0 to 30 percent. Mean annual temperature is 10 degrees C. (50 degrees F), and mean annual precipitation is 53 centimeters (21 inches) at the type location."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
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+ ],
+ "ecoclassname": [
+ "Loamy Plains"
+ ],
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+ "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY100KS"
+ ]
+ }
+ },
+ "id": {
+ "component": "Harney",
+ "name": "Harney",
+ "rank_loc": "2",
+ "score_loc": 0.263
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25865346",
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+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "3",
+ "irrcapscl": "e",
+ "irrcapunit": "None",
+ "mapunitID": "2669027",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=harney",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#harney",
+ "slope": 5.0,
+ "taxsubgrp": "Typic Argiustolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Harney series consists of deep, well drained, moderately slowly permeable soils that formed in loess. These soils are on uplands on slopes that range from 0 to 8 percent."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R073XY108KS"
+ ],
+ "ecoclassname": [
+ "Loamy Floodplain"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY108KS"
+ ]
+ }
+ },
+ "id": {
+ "component": "Coly",
+ "name": "Coly",
+ "rank_loc": "3",
+ "score_loc": 0.215
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25865492",
+ "componentKind": "Series",
+ "componentPct": 40,
+ "dataSource": "SSURGO",
+ "distance": 42.0,
+ "irrcapcl": "4",
+ "irrcapscl": "e",
+ "irrcapunit": "None",
+ "mapunitID": "1380503",
+ "minCompDistance": 42.0,
+ "nirrcapcl": "4",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=coly",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#coly",
+ "slope": 6.0,
+ "taxsubgrp": "Typic Ustorthents",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Coly series consists of very deep, well drained, moderately permeable soils formed in loess. Coly soils are on sideslopes of uplands in MLRA 73-Rolling Plains and Breaks. Slopes range from 1 to 60 percent. Mean annual temperature is 10 degrees C ( 50 degrees F), and mean annual precipitation is 53 centimeters ( 21 inches) at the type location."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R073XY108KS"
+ ],
+ "ecoclassname": [
+ "Loamy Floodplain"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY108KS"
+ ]
+ }
+ },
+ "id": {
+ "component": "Holdrege",
+ "name": "Holdrege",
+ "rank_loc": "4",
+ "score_loc": 0.104
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25865493",
+ "componentKind": "Taxadjunct",
+ "componentPct": 45,
+ "dataSource": "SSURGO",
+ "distance": 42.0,
+ "irrcapcl": "4",
+ "irrcapscl": "e",
+ "irrcapunit": "None",
+ "mapunitID": "1380503",
+ "minCompDistance": 42.0,
+ "nirrcapcl": "4",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=holdrege",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#holdrege",
+ "slope": 6.0,
+ "taxsubgrp": "Typic Haplustalfs",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Holdrege series consists of very deep, well drained, moderately permeable soils formed in calcareous loess. These upland soils have slopes ranging from 0 to 15 percent. Mean annual temperature is about 54 degrees F, and mean annual precipitation is about 23 inches at the type location."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R073XY112KS"
+ ],
+ "ecoclassname": [
+ "Shallow Limy"
+ ],
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+ "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY112KS"
+ ]
+ }
+ },
+ "id": {
+ "component": "Tobin",
+ "name": "Tobin",
+ "rank_loc": "5",
+ "score_loc": 0.057
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25865519",
+ "componentKind": "Series",
+ "componentPct": 30,
+ "dataSource": "SSURGO",
+ "distance": 67.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "1380504",
+ "minCompDistance": 67.0,
+ "nirrcapcl": "5",
+ "nirrcapscl": "w",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=tobin",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#tobin",
+ "slope": 1.0,
+ "taxsubgrp": "Cumulic Haplustolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Tobin series consists of very deep, well drained soils that formed in silty alluvium. Tobin soils are on flood plains on river valleys in MLRA 73, Rolling Plains and Breaks. Slopes range from 0 to 2 percent. Mean annual precipitation is about 740 millimeters (29 inches) and the mean annual temperature is about 12 degrees C (54 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R073XY100KS"
+ ],
+ "ecoclassname": [
+ "Loamy Plains"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY100KS"
+ ]
+ }
+ },
+ "id": {
+ "component": "Case",
+ "name": "Case",
+ "rank_loc": "6",
+ "score_loc": 0.023
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25865495",
+ "componentKind": "Series",
+ "componentPct": 10,
+ "dataSource": "SSURGO",
+ "distance": 42.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "1380503",
+ "minCompDistance": 42.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=case",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#case",
+ "slope": 6.0,
+ "taxsubgrp": "Typic Calciustepts",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Case series consists of very deep, well drained, moderately permeable soils formed in calcareous old alluvium of Tertiary age on uplands of the Southern High Plains Breaks (MLRA-77E). Slopes range from 1 to 15 percent. Mean annual temperature is about 58 degrees F, and mean annual precipitation is about 24 inches."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
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+ ],
+ "ecoclassname": [
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+ ],
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+ "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY100KS"
+ ]
+ }
+ },
+ "id": {
+ "component": "Penden",
+ "name": "Penden",
+ "rank_loc": "7",
+ "score_loc": 0.016
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25865344",
+ "componentKind": "Series",
+ "componentPct": 5,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "3",
+ "irrcapscl": "e",
+ "irrcapunit": "None",
+ "mapunitID": "2669027",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=penden",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#penden",
+ "slope": 5.0,
+ "taxsubgrp": "Typic Calciustolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Penden series consists of deep, well drained soils formed in calcareous loamy sediments on uplands. Slope ranges from 0 to 15 percent. Mean annual temperature is 13 degrees C. (56 degrees F.), and mean annual precipitation is 48 centimeters (19 inches)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
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+ ],
+ "ecoclassname": [
+ "Limy Slopes"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY101KS"
+ ]
+ }
+ },
+ "id": {
+ "component": "Bridgeport",
+ "name": "Bridgeport",
+ "rank_loc": "8",
+ "score_loc": 0.012
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25865494",
+ "componentKind": "Series",
+ "componentPct": 5,
+ "dataSource": "SSURGO",
+ "distance": 42.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "1380503",
+ "minCompDistance": 42.0,
+ "nirrcapcl": "5",
+ "nirrcapscl": "w",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=bridgeport",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#bridgeport",
+ "slope": 3.0,
+ "taxsubgrp": "Fluventic Haplustolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Bridgeport series consists of deep, well drained, moderately permeable soils that formed in calcareous alluvial sediments. These soils are on flood plains or low stream terraces."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
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+ ],
+ "ecoclassname": [
+ "Loamy Plains"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY100KS"
+ ]
+ }
+ },
+ "id": {
+ "component": "Wakeen",
+ "name": "Wakeen",
+ "rank_loc": "9",
+ "score_loc": 0.01
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25865551",
+ "componentKind": "Series",
+ "componentPct": 4,
+ "dataSource": "SSURGO",
+ "distance": 29.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "2605949",
+ "minCompDistance": 29.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=wakeen",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#wakeen",
+ "slope": 2.0,
+ "taxsubgrp": "Entic Haplustolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Wakeen series consists of well drained soils that are moderately deep over chalky limestone. These soils are on plains, knolls and ridgetops in the Rolling Plains and Breaks (MLRA 73). Slopes range from 1 to 20 percent. Mean annual temperature is about 12 degrees C. (54 degrees F.), and mean annual precipitation is about 58 centimeters (23 inches)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R073XY101KS"
+ ],
+ "ecoclassname": [
+ "Limy Slopes"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY101KS"
+ ]
+ }
+ },
+ "id": {
+ "component": "Aquolls",
+ "name": "Aquolls",
+ "rank_loc": "10",
+ "score_loc": 0.003
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25865552",
+ "componentKind": "Taxon above family",
+ "componentPct": 1,
+ "dataSource": "SSURGO",
+ "distance": 29.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "2605949",
+ "minCompDistance": 29.0,
+ "nirrcapcl": "nan",
+ "nirrcapscl": "None",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 1.0,
+ "taxsubgrp": "None",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R073XY103KS"
+ ],
+ "ecoclassname": [
+ "Subirrigated"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY103KS"
+ ]
+ }
+ },
+ "id": {
+ "component": "Canlon",
+ "name": "Canlon",
+ "rank_loc": "11",
+ "score_loc": 0.002
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25865520",
+ "componentKind": "Series",
+ "componentPct": 1,
+ "dataSource": "SSURGO",
+ "distance": 67.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "1380504",
+ "minCompDistance": 67.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=canlon",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#canlon",
+ "slope": 12.0,
+ "taxsubgrp": "Lithic Ustorthents",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Canlon series consist of shallow, well drained and somewhat excessively drained, moderately permeable soils on uplands. They formed in residuum weathered from lime-cemented sandstone or caliche and have slopes ranging from 2 to 50 percent. The average annual precipitation is about 24 inches, and the mean annual temperature is about 54 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
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+ ],
+ "ecoclassname": [
+ "Loamy Plains"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY100KS"
+ ]
+ }
+ },
+ "id": {
+ "component": "Uly",
+ "name": "Uly2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.295
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25865522",
+ "componentKind": "Series",
+ "componentPct": 2,
+ "dataSource": "SSURGO",
+ "distance": 67.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "1380504",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=uly",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#uly",
+ "slope": 5.0,
+ "taxsubgrp": "Typic Haplustolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Uly series includes very deep, well drained formed in loess on uplands. Slopes range from 0 to 30 percent. Mean annual temperature is 10 degrees C. (50 degrees F), and mean annual precipitation is 53 centimeters (21 inches) at the type location."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
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+ "ecoclassname": [
+ "Limy Slopes"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY101KS"
+ ]
+ }
+ },
+ "id": {
+ "component": "Harney",
+ "name": "Harney2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.263
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25865550",
+ "componentKind": "Series",
+ "componentPct": 95,
+ "dataSource": "SSURGO",
+ "distance": 29.0,
+ "irrcapcl": "2",
+ "irrcapscl": "e",
+ "irrcapunit": "None",
+ "mapunitID": "2605949",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "2",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=harney",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#harney",
+ "slope": 2.0,
+ "taxsubgrp": "Typic Argiustolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Harney series consists of deep, well drained, moderately slowly permeable soils that formed in loess. These soils are on uplands on slopes that range from 0 to 8 percent."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R073XY100KS"
+ ],
+ "ecoclassname": [
+ "Loamy Plains"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY100KS"
+ ]
+ }
+ },
+ "id": {
+ "component": "Harney",
+ "name": "Harney3",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.263
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25865521",
+ "componentKind": "Series",
+ "componentPct": 2,
+ "dataSource": "SSURGO",
+ "distance": 67.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "1380504",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=harney",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#harney",
+ "slope": 4.0,
+ "taxsubgrp": "Typic Argiustolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Harney series consists of deep, well drained, moderately slowly permeable soils that formed in loess. These soils are on uplands on slopes that range from 0 to 8 percent."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R079XY112KS"
+ ],
+ "ecoclassname": [
+ "Limy Plains"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/079X/R079XY112KS"
+ ]
+ }
+ },
+ "id": {
+ "component": "Coly",
+ "name": "Coly2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.215
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25865523",
+ "componentKind": "Series",
+ "componentPct": 65,
+ "dataSource": "SSURGO",
+ "distance": 67.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "1380504",
+ "minCompDistance": 42.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=coly",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#coly",
+ "slope": 12.0,
+ "taxsubgrp": "Typic Ustorthents",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Coly series consists of very deep, well drained, moderately permeable soils formed in loess. Coly soils are on sideslopes of uplands in MLRA 73-Rolling Plains and Breaks. Slopes range from 1 to 60 percent. Mean annual temperature is 10 degrees C ( 50 degrees F), and mean annual precipitation is 53 centimeters ( 21 inches) at the type location."
+ },
+ "texture": {},
+ "top_depth": {}
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "us",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Harney",
+ "componentData": "Data Complete",
+ "componentID": 25865346,
+ "name": "Harney",
+ "rank_data": "4",
+ "rank_data_loc": "1",
+ "rank_loc": "2",
+ "score_data": 0.649,
+ "score_data_loc": 0.456,
+ "score_loc": 0.263
+ },
+ {
+ "component": "Coly",
+ "componentData": "Data Complete",
+ "componentID": 25865523,
+ "name": "Coly2",
+ "rank_data": "1",
+ "rank_data_loc": "2",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.677,
+ "score_data_loc": 0.446,
+ "score_loc": 0.215
+ },
+ {
+ "component": "Uly",
+ "componentData": "Data Complete",
+ "componentID": 25865522,
+ "name": "Uly2",
+ "rank_data": "8",
+ "rank_data_loc": "3",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.571,
+ "score_data_loc": 0.433,
+ "score_loc": 0.295
+ },
+ {
+ "component": "Penden",
+ "componentData": "Data Complete",
+ "componentID": 25865344,
+ "name": "Penden",
+ "rank_data": "2",
+ "rank_data_loc": "4",
+ "rank_loc": "7",
+ "score_data": 0.667,
+ "score_data_loc": 0.341,
+ "score_loc": 0.016
+ },
+ {
+ "component": "Canlon",
+ "componentData": "Data Complete",
+ "componentID": 25865520,
+ "name": "Canlon",
+ "rank_data": "3",
+ "rank_data_loc": "5",
+ "rank_loc": "11",
+ "score_data": 0.659,
+ "score_data_loc": 0.331,
+ "score_loc": 0.002
+ },
+ {
+ "component": "Case",
+ "componentData": "Data Complete",
+ "componentID": 25865495,
+ "name": "Case",
+ "rank_data": "7",
+ "rank_data_loc": "6",
+ "rank_loc": "6",
+ "score_data": 0.58,
+ "score_data_loc": 0.302,
+ "score_loc": 0.023
+ },
+ {
+ "component": "Aquolls",
+ "componentData": "Data Complete",
+ "componentID": 25865552,
+ "name": "Aquolls",
+ "rank_data": "5",
+ "rank_data_loc": "7",
+ "rank_loc": "10",
+ "score_data": 0.594,
+ "score_data_loc": 0.298,
+ "score_loc": 0.003
+ },
+ {
+ "component": "Wakeen",
+ "componentData": "Missing Data",
+ "componentID": 25865551,
+ "name": "Wakeen",
+ "rank_data": "6",
+ "rank_data_loc": "8",
+ "rank_loc": "9",
+ "score_data": 0.585,
+ "score_data_loc": 0.298,
+ "score_loc": 0.01
+ },
+ {
+ "component": "Tobin",
+ "componentData": "Data Complete",
+ "componentID": 25865519,
+ "name": "Tobin",
+ "rank_data": "10",
+ "rank_data_loc": "9",
+ "rank_loc": "5",
+ "score_data": 0.538,
+ "score_data_loc": 0.298,
+ "score_loc": 0.057
+ },
+ {
+ "component": "Bridgeport",
+ "componentData": "Data Complete",
+ "componentID": 25865494,
+ "name": "Bridgeport",
+ "rank_data": "9",
+ "rank_data_loc": "10",
+ "rank_loc": "8",
+ "score_data": 0.551,
+ "score_data_loc": 0.282,
+ "score_loc": 0.012
+ },
+ {
+ "component": "Holdrege",
+ "componentData": "Data Complete",
+ "componentID": 25865493,
+ "name": "Holdrege",
+ "rank_data": "11",
+ "rank_data_loc": "11",
+ "rank_loc": "4",
+ "score_data": 0.44,
+ "score_data_loc": 0.272,
+ "score_loc": 0.104
+ },
+ {
+ "component": "Harney",
+ "componentData": "Data Complete",
+ "componentID": 25865521,
+ "name": "Harney3",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.585,
+ "score_data_loc": 0.424,
+ "score_loc": 0.263
+ },
+ {
+ "component": "Uly",
+ "componentData": "Data Complete",
+ "componentID": 25865345,
+ "name": "Uly",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "1",
+ "score_data": 0.535,
+ "score_data_loc": 0.415,
+ "score_loc": 0.295
+ },
+ {
+ "component": "Harney",
+ "componentData": "Data Complete",
+ "componentID": 25865550,
+ "name": "Harney2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.55,
+ "score_data_loc": 0.407,
+ "score_loc": 0.263
+ },
+ {
+ "component": "Coly",
+ "componentData": "Data Complete",
+ "componentID": 25865492,
+ "name": "Coly",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "3",
+ "score_data": 0.597,
+ "score_data_loc": 0.406,
+ "score_loc": 0.215
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[39.26009312,-85.50621214].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[39.26009312,-85.50621214].json
new file mode 100644
index 0000000..23f7f2a
--- /dev/null
+++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[39.26009312,-85.50621214].json
@@ -0,0 +1,1202 @@
+{
+ "list": {
+ "AWS_PIW90": 5.19,
+ "Soil Data Value": [
+ [
+ "rfv_class_30",
+ 1.0417872772025576
+ ],
+ [
+ "rfv_class_0",
+ 1.0174644063857206
+ ],
+ [
+ "texture_0",
+ 0.0
+ ],
+ [
+ "texture_30",
+ 0.0
+ ]
+ ],
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F111XA008IN"
+ ],
+ "ecoclassname": [
+ "Wet Till Ridge"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA008IN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Hennepin",
+ "name": "Hennepin",
+ "rank_loc": "1",
+ "score_loc": 0.061
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25325347",
+ "componentKind": "Series",
+ "componentPct": 5,
+ "dataSource": "SSURGO",
+ "distance": 59.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "162396",
+ "minCompDistance": 59.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hennepin",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hennepin",
+ "slope": 38.0,
+ "taxsubgrp": "Typic Eutrudepts",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Hennepin series consists of very deep, well drained soils formed in calcareous glacial till. These soils are on upland side slopes that border stream valleys and on moraines. Permeability is moderate or moderately slow. Slopes range from 10 to 70 percent. Mean annual temperature is about 52 degrees F, and mean annual precipitation is about 35 inches."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ ""
+ ],
+ "ecoclassname": [
+ ""
+ ],
+ "edit_url": [
+ ""
+ ]
+ }
+ },
+ "id": {
+ "component": "Fincastle",
+ "name": "Fincastle",
+ "rank_loc": "2",
+ "score_loc": 0.054
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25325308",
+ "componentKind": "Series",
+ "componentPct": 85,
+ "dataSource": "SSURGO",
+ "distance": 170.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "162380",
+ "minCompDistance": 170.0,
+ "nirrcapcl": "2",
+ "nirrcapscl": "w",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=fincastle",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#fincastle",
+ "slope": 1.0,
+ "taxsubgrp": "Aeric Epiaqualfs",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Fincastle series consists of very deep, somewhat poorly drained soils that are deep to dense till. Fincastle soils formed in loess or other silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 6 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ ""
+ ],
+ "ecoclassname": [
+ ""
+ ],
+ "edit_url": [
+ ""
+ ]
+ }
+ },
+ "id": {
+ "component": "Hickory",
+ "name": "Hickory",
+ "rank_loc": "3",
+ "score_loc": 0.051
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25325331",
+ "componentKind": "Series",
+ "componentPct": 87,
+ "dataSource": "SSURGO",
+ "distance": 936.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "162389",
+ "minCompDistance": 936.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hickory",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hickory",
+ "slope": 40.0,
+ "taxsubgrp": "Typic Hapludalfs",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Hickory series consists of very deep, well drained, soils on dissected till plains. They formed in till that can be capped with up to 20 inches of loess. Slope ranges from 5 to 70 percent. Mean annual air temperature is about 54 degrees F., and mean annual precipitation is about 40 inches."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F114XB503IN"
+ ],
+ "ecoclassname": [
+ "Till Upland Forest"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/114X/F114XB503IN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Crosby",
+ "name": "Crosby",
+ "rank_loc": "4",
+ "score_loc": 0.048
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25325341",
+ "componentKind": "Series",
+ "componentPct": 9,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "162394",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "2",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=crosby",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#crosby",
+ "slope": 2.0,
+ "taxsubgrp": "Aeric Epiaqualfs",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Crosby series consists of very deep, somewhat poorly drained soils that are moderately deep to dense till. Crosby soils formed in as much as 56 cm (22 inches) of loess or other silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 6 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ ""
+ ],
+ "ecoclassname": [
+ ""
+ ],
+ "edit_url": [
+ ""
+ ]
+ }
+ },
+ "id": {
+ "component": "Cyclone",
+ "name": "Cyclone",
+ "rank_loc": "5",
+ "score_loc": 0.011
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25325348",
+ "componentKind": "Series",
+ "componentPct": 3,
+ "dataSource": "SSURGO",
+ "distance": 59.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "162396",
+ "minCompDistance": 59.0,
+ "nirrcapcl": "2",
+ "nirrcapscl": "w",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=cyclone",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#cyclone",
+ "slope": 0.5,
+ "taxsubgrp": "Typic Argiaquolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Cyclone series consists of very deep, poorly drained soils that formed in loess or silty material and in the underlying drift. Cyclone soils are on till plains. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 991 mm (39 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F111XA007IN"
+ ],
+ "ecoclassname": [
+ "Till Depression Flatwood"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA007IN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Brookston",
+ "name": "Brookston",
+ "rank_loc": "6",
+ "score_loc": 0.009
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25325342",
+ "componentKind": "Series",
+ "componentPct": 4,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "162394",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "2",
+ "nirrcapscl": "w",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=brookston",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#brookston",
+ "slope": 0.5,
+ "taxsubgrp": "Typic Argiaquolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Brookston series consists of very deep, poorly drained soils formed in as much as 51 cm (20 inches) of silty material and the underlying loamy till in depressions on till plains and moraines. Slope ranges from 0 to 3 percent. Mean annual precipitation is about 889 mm (35 inches), and mean annual temperature is about 10.0 degrees C (50 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F111XA009IN"
+ ],
+ "ecoclassname": [
+ "Till Ridge"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Celina",
+ "name": "Celina",
+ "rank_loc": "7",
+ "score_loc": 0.003
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25325406",
+ "componentKind": "Series",
+ "componentPct": 5,
+ "dataSource": "SSURGO",
+ "distance": 193.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "162416",
+ "minCompDistance": 193.0,
+ "nirrcapcl": "2",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=celina",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#celina",
+ "slope": 4.0,
+ "taxsubgrp": "Aquic Hapludalfs",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Celina series consists of very deep, moderately well drained soils that are moderately deep to dense till. They formed in as much as 46 cm (18 inches) of loess and the underlying loamy till of high-lime content. They are on till plains and moraines. Slope ranges from 0 to 12 percent. Mean annual precipitation is about 965 mm (38 inches), and mean annual air temperature is about 12 degrees C (53 degree F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F111XA007IN"
+ ],
+ "ecoclassname": [
+ "Till Depression Flatwood"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA007IN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Holton",
+ "name": "Holton",
+ "rank_loc": "8",
+ "score_loc": 0.002
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25325333",
+ "componentKind": "Series",
+ "componentPct": 4,
+ "dataSource": "SSURGO",
+ "distance": 936.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "162389",
+ "minCompDistance": 936.0,
+ "nirrcapcl": "2",
+ "nirrcapscl": "w",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=holton",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#holton",
+ "slope": 0.5,
+ "taxsubgrp": "Aeric Endoaquepts",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Holton Series consists of very deep, somewhat poorly drained soils formed in loamy alluvium on flood plains. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 1067 mm (42 inches), and mean annual temperature is about 11 degrees C (52 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
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+ ],
+ "ecoclassname": [
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+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA008IN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Bonnell",
+ "name": "Bonnell",
+ "rank_loc": "9",
+ "score_loc": 0.002
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25325330",
+ "componentKind": "Series",
+ "componentPct": 3,
+ "dataSource": "SSURGO",
+ "distance": 936.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "162389",
+ "minCompDistance": 936.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=bonnell",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#bonnell",
+ "slope": 21.0,
+ "taxsubgrp": "Typic Hapludalfs",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Bonnell series consists of very deep, well drained soils that formed in less than 46 cm (18 inches) of loess or loamy materials and the underlying till. These soils are on dissected till plains. Slope ranges from 6 to 60 percent. Mean annual precipitation is about 1067 mm (42 inches), and mean annual temperature is about 12 degrees C (54 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F111XA008IN"
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+ "ecoclassname": [
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+ ],
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+ "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA008IN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Cincinnati",
+ "name": "Cincinnati",
+ "rank_loc": "10",
+ "score_loc": 0.001
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25325332",
+ "componentKind": "Series",
+ "componentPct": 2,
+ "dataSource": "SSURGO",
+ "distance": 936.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "162389",
+ "minCompDistance": 936.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=cincinnati",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#cincinnati",
+ "slope": 9.0,
+ "taxsubgrp": "Oxyaquic Fragiudalfs",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Cincinnati series consists of very deep, well drained soils that are moderately deep to a fragipan. These soils formed in a mantle of loess, a thin layer of pedisediment, and a paleosol formed in the underlying till. They are on till plains. Slope ranges from 1 to 18 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual air temperature is about 12 degrees C (54 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F111XA009IN"
+ ],
+ "ecoclassname": [
+ "Till Ridge"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Grayford",
+ "name": "Grayford",
+ "rank_loc": "11",
+ "score_loc": 0.001
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25325329",
+ "componentKind": "Series",
+ "componentPct": 2,
+ "dataSource": "SSURGO",
+ "distance": 936.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "162389",
+ "minCompDistance": 936.0,
+ "nirrcapcl": "4",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=grayford",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#grayford",
+ "slope": 17.0,
+ "taxsubgrp": "Ultic Hapludalfs",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Grayford series consists of deep, well drained soils formed in less than 56 cm (22 inches) of loess and in the underlying till of Illinoian age and residuum from limestone. They are on dissected till plains and sinkholes. Slope ranges from 2 to 35 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual temperature is about 13 degrees C (55 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F111XD010IN"
+ ],
+ "ecoclassname": [
+ "Till Ridge"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XD010IN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Jessietown",
+ "name": "Jessietown",
+ "rank_loc": "12",
+ "score_loc": 0.001
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25325334",
+ "componentKind": "Series",
+ "componentPct": 2,
+ "dataSource": "SSURGO",
+ "distance": 936.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "162389",
+ "minCompDistance": 936.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=jessietown",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#jessietown",
+ "slope": 38.0,
+ "taxsubgrp": "Typic Hapludults",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Jessietown series consists of moderately deep, well drained soils formed in a thin mantle of silty material and residuum weathered from black fissile shale. Permeability is moderate. These gently sloping to steep soils are on upland ridges, side slopes, and toe slopes. Slopes range from 2 to 30 percent. The mean annual temperature is about 57 degrees F, and the mean annual precipitation is about 46 inches."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F111XA006IN"
+ ],
+ "ecoclassname": [
+ "Till Depression"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA006IN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Hennepin",
+ "name": "Hennepin2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.061
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25325325",
+ "componentKind": "Series",
+ "componentPct": 90,
+ "dataSource": "SSURGO",
+ "distance": 175.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "162386",
+ "minCompDistance": 59.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hennepin",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hennepin",
+ "slope": 35.0,
+ "taxsubgrp": "Typic Eutrudepts",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Hennepin series consists of very deep, well drained soils formed in calcareous glacial till. These soils are on upland side slopes that border stream valleys and on moraines. Permeability is moderate or moderately slow. Slopes range from 10 to 70 percent. Mean annual temperature is about 52 degrees F, and mean annual precipitation is about 35 inches."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F111XD010IN"
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+ "ecoclassname": [
+ "Till Ridge"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XD010IN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Hennepin",
+ "name": "Hennepin3",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.061
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25325355",
+ "componentKind": "Series",
+ "componentPct": 2,
+ "dataSource": "SSURGO",
+ "distance": 502.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "162398",
+ "minCompDistance": 59.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hennepin",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hennepin",
+ "slope": 22.0,
+ "taxsubgrp": "Typic Eutrudepts",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Hennepin series consists of very deep, well drained soils formed in calcareous glacial till. These soils are on upland side slopes that border stream valleys and on moraines. Permeability is moderate or moderately slow. Slopes range from 10 to 70 percent. Mean annual temperature is about 52 degrees F, and mean annual precipitation is about 35 inches."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ ""
+ ],
+ "ecoclassname": [
+ ""
+ ],
+ "edit_url": [
+ ""
+ ]
+ }
+ },
+ "id": {
+ "component": "Crosby",
+ "name": "Crosby2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.048
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25325351",
+ "componentKind": "Series",
+ "componentPct": 4,
+ "dataSource": "SSURGO",
+ "distance": 85.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "162397",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "2",
+ "nirrcapscl": "w",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=crosby",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#crosby",
+ "slope": 1.0,
+ "taxsubgrp": "Aeric Epiaqualfs",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Crosby series consists of very deep, somewhat poorly drained soils that are moderately deep to dense till. Crosby soils formed in as much as 56 cm (22 inches) of loess or other silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 6 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ ""
+ ],
+ "ecoclassname": [
+ ""
+ ],
+ "edit_url": [
+ ""
+ ]
+ }
+ },
+ "id": {
+ "component": "Crosby",
+ "name": "Crosby3",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.048
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25325353",
+ "componentKind": "Series",
+ "componentPct": 7,
+ "dataSource": "SSURGO",
+ "distance": 502.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "162398",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "2",
+ "nirrcapscl": "w",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=crosby",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#crosby",
+ "slope": 1.0,
+ "taxsubgrp": "Aeric Epiaqualfs",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Crosby series consists of very deep, somewhat poorly drained soils that are moderately deep to dense till. Crosby soils formed in as much as 56 cm (22 inches) of loess or other silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 6 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F111XA008IN"
+ ],
+ "ecoclassname": [
+ "Wet Till Ridge"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA008IN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Cyclone",
+ "name": "Cyclone2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.011
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25325310",
+ "componentKind": "Series",
+ "componentPct": 10,
+ "dataSource": "SSURGO",
+ "distance": 170.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "162380",
+ "minCompDistance": 59.0,
+ "nirrcapcl": "2",
+ "nirrcapscl": "w",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=cyclone",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#cyclone",
+ "slope": 0.5,
+ "taxsubgrp": "Typic Argiaquolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Cyclone series consists of very deep, poorly drained soils that formed in loess or silty material and in the underlying drift. Cyclone soils are on till plains. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 991 mm (39 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "us",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Fincastle",
+ "componentData": "Data Complete",
+ "componentID": 25325308,
+ "name": "Fincastle",
+ "rank_data": "1",
+ "rank_data_loc": "1",
+ "rank_loc": "2",
+ "score_data": 0.671,
+ "score_data_loc": 0.363,
+ "score_loc": 0.054
+ },
+ {
+ "component": "Crosby",
+ "componentData": "Data Complete",
+ "componentID": 25325341,
+ "name": "Crosby",
+ "rank_data": "3",
+ "rank_data_loc": "2",
+ "rank_loc": "4",
+ "score_data": 0.662,
+ "score_data_loc": 0.355,
+ "score_loc": 0.048
+ },
+ {
+ "component": "Bonnell",
+ "componentData": "Data Complete",
+ "componentID": 25325330,
+ "name": "Bonnell",
+ "rank_data": "2",
+ "rank_data_loc": "3",
+ "rank_loc": "9",
+ "score_data": 0.671,
+ "score_data_loc": 0.336,
+ "score_loc": 0.002
+ },
+ {
+ "component": "Holton",
+ "componentData": "Data Complete",
+ "componentID": 25325333,
+ "name": "Holton",
+ "rank_data": "4",
+ "rank_data_loc": "4",
+ "rank_loc": "8",
+ "score_data": 0.643,
+ "score_data_loc": 0.323,
+ "score_loc": 0.002
+ },
+ {
+ "component": "Grayford",
+ "componentData": "Data Complete",
+ "componentID": 25325329,
+ "name": "Grayford",
+ "rank_data": "5",
+ "rank_data_loc": "5",
+ "rank_loc": "11",
+ "score_data": 0.637,
+ "score_data_loc": 0.319,
+ "score_loc": 0.001
+ },
+ {
+ "component": "Brookston",
+ "componentData": "Data Complete",
+ "componentID": 25325342,
+ "name": "Brookston",
+ "rank_data": "6",
+ "rank_data_loc": "6",
+ "rank_loc": "6",
+ "score_data": 0.61,
+ "score_data_loc": 0.31,
+ "score_loc": 0.009
+ },
+ {
+ "component": "Cyclone",
+ "componentData": "Data Complete",
+ "componentID": 25325348,
+ "name": "Cyclone",
+ "rank_data": "7",
+ "rank_data_loc": "7",
+ "rank_loc": "5",
+ "score_data": 0.596,
+ "score_data_loc": 0.303,
+ "score_loc": 0.011
+ },
+ {
+ "component": "Hennepin",
+ "componentData": "Data Complete",
+ "componentID": 25325355,
+ "name": "Hennepin3",
+ "rank_data": "10",
+ "rank_data_loc": "8",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.54,
+ "score_data_loc": 0.301,
+ "score_loc": 0.061
+ },
+ {
+ "component": "Cincinnati",
+ "componentData": "Data Complete",
+ "componentID": 25325332,
+ "name": "Cincinnati",
+ "rank_data": "8",
+ "rank_data_loc": "9",
+ "rank_loc": "10",
+ "score_data": 0.591,
+ "score_data_loc": 0.296,
+ "score_loc": 0.001
+ },
+ {
+ "component": "Celina",
+ "componentData": "Data Complete",
+ "componentID": 25325406,
+ "name": "Celina",
+ "rank_data": "9",
+ "rank_data_loc": "10",
+ "rank_loc": "7",
+ "score_data": 0.555,
+ "score_data_loc": 0.279,
+ "score_loc": 0.003
+ },
+ {
+ "component": "Hickory",
+ "componentData": "Data Complete",
+ "componentID": 25325331,
+ "name": "Hickory",
+ "rank_data": "12",
+ "rank_data_loc": "11",
+ "rank_loc": "3",
+ "score_data": 0.499,
+ "score_data_loc": 0.275,
+ "score_loc": 0.051
+ },
+ {
+ "component": "Jessietown",
+ "componentData": "Data Complete",
+ "componentID": 25325334,
+ "name": "Jessietown",
+ "rank_data": "11",
+ "rank_data_loc": "12",
+ "rank_loc": "12",
+ "score_data": 0.522,
+ "score_data_loc": 0.262,
+ "score_loc": 0.001
+ },
+ {
+ "component": "Crosby",
+ "componentData": "Data Complete",
+ "componentID": 25325353,
+ "name": "Crosby3",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.654,
+ "score_data_loc": 0.351,
+ "score_loc": 0.048
+ },
+ {
+ "component": "Crosby",
+ "componentData": "Data Complete",
+ "componentID": 25325351,
+ "name": "Crosby2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.609,
+ "score_data_loc": 0.328,
+ "score_loc": 0.048
+ },
+ {
+ "component": "Hennepin",
+ "componentData": "Data Complete",
+ "componentID": 25325325,
+ "name": "Hennepin2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.536,
+ "score_data_loc": 0.299,
+ "score_loc": 0.061
+ },
+ {
+ "component": "Hennepin",
+ "componentData": "Data Complete",
+ "componentID": 25325347,
+ "name": "Hennepin",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "1",
+ "score_data": 0.525,
+ "score_data_loc": 0.293,
+ "score_loc": 0.061
+ },
+ {
+ "component": "Cyclone",
+ "componentData": "Data Complete",
+ "componentID": 25325310,
+ "name": "Cyclone2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.555,
+ "score_data_loc": 0.283,
+ "score_loc": 0.011
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.494912,-123.064531].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.494912,-123.064531].json
new file mode 100644
index 0000000..fe10d2c
--- /dev/null
+++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.494912,-123.064531].json
@@ -0,0 +1,726 @@
+{
+ "list": {
+ "AWS_PIW90": 10.16,
+ "Soil Data Value": [
+ [
+ "rfv_class_30",
+ 1.490207948287594
+ ],
+ [
+ "rfv_class_0",
+ 0.8817108392902311
+ ],
+ [
+ "texture_0",
+ 0.0
+ ],
+ [
+ "texture_30",
+ 0.0
+ ]
+ ],
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F005XZ018CA"
+ ],
+ "ecoclassname": [
+ "Moderately Deep Gravelly Mesic Mountains 40-60Ppt"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ018CA"
+ ]
+ }
+ },
+ "id": {
+ "component": "Ruch",
+ "name": "Ruch",
+ "rank_loc": "1",
+ "score_loc": 0.267
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25443415",
+ "componentKind": "Series",
+ "componentPct": 80,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "4",
+ "irrcapscl": "e",
+ "irrcapunit": "None",
+ "mapunitID": "469633",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "4",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=ruch",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#ruch",
+ "slope": 14.0,
+ "taxsubgrp": "Mollic Palexeralfs",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Ruch series consists of very deep, well drained soils that formed in mixed alluvium. Ruch soils are on high stream terraces, alluvial fans and footslopes and have slopes of 2 to 60 percent. The mean annual precipitation is about 30 inches and the mean annual temperature is about 52 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F005XZ018CA"
+ ],
+ "ecoclassname": [
+ "Moderately Deep Gravelly Mesic Mountains 40-60Ppt"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ018CA"
+ ]
+ }
+ },
+ "id": {
+ "component": "Josephine",
+ "name": "Josephine",
+ "rank_loc": "2",
+ "score_loc": 0.125
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25443480",
+ "componentKind": "Series",
+ "componentPct": 40,
+ "dataSource": "SSURGO",
+ "distance": 712.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "469660",
+ "minCompDistance": 712.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=josephine",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#josephine",
+ "slope": 45.0,
+ "taxsubgrp": "Typic Haploxerults",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Josephine series consists of deep, well drained soils that formed in colluvium and residuum weathered from altered sedimentary and extrusive igneous rocks. Josephine soils are on broad ridgetops, toeslopes, footslopes, and side slopes of mountains. Slopes are 2 to 75 percent. The mean annual precipitation is about 45 inches and the mean annual temperature is about 50 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F005XZ003CA"
+ ],
+ "ecoclassname": [
+ "Terraces"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ003CA"
+ ]
+ }
+ },
+ "id": {
+ "component": "Abegg",
+ "name": "Abegg",
+ "rank_loc": "3",
+ "score_loc": 0.069
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25443548",
+ "componentKind": "Series",
+ "componentPct": 83,
+ "dataSource": "SSURGO",
+ "distance": 310.0,
+ "irrcapcl": "4",
+ "irrcapscl": "e",
+ "irrcapunit": "None",
+ "mapunitID": "469691",
+ "minCompDistance": 310.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=abegg",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#abegg",
+ "slope": 10.0,
+ "taxsubgrp": "Ultic Haploxeralfs",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Abegg series consists of very deep, well drained soils that formed in alluvium and colluvium weathered from metamorphosed sedimentary and volcanic bedrock. Abegg soils are on stream terraces and alluvial fans and have slopes of 2 to 30 percent. The mean annual precipitation is about 45 inches and the mean annual temperature is about 52 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F005XZ024CA"
+ ],
+ "ecoclassname": [
+ "Ridges"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ024CA"
+ ]
+ }
+ },
+ "id": {
+ "component": "Caris",
+ "name": "Caris",
+ "rank_loc": "4",
+ "score_loc": 0.05
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25443598",
+ "componentKind": "Series",
+ "componentPct": 60,
+ "dataSource": "SSURGO",
+ "distance": 347.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "469709",
+ "minCompDistance": 347.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=caris",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#caris",
+ "slope": 63.0,
+ "taxsubgrp": "Typic Xerochrepts",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Caris series consists of moderately deep, well drained soils that formed in colluvium weathered from altered sedimentary and extrusive igneous rocks. Caris soils are on mountains and have slopes of 50 to 90 percent. The mean annual temperature is about 50 degrees F and the mean annual precipitation is about 32 inches."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F005XZ003CA"
+ ],
+ "ecoclassname": [
+ "Terraces"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ003CA"
+ ]
+ }
+ },
+ "id": {
+ "component": "Beekman",
+ "name": "Beekman",
+ "rank_loc": "5",
+ "score_loc": 0.046
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25443287",
+ "componentKind": "Series",
+ "componentPct": 55,
+ "dataSource": "SSURGO",
+ "distance": 497.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "469583",
+ "minCompDistance": 497.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=beekman",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#beekman",
+ "slope": 65.0,
+ "taxsubgrp": "Dystric Xerochrepts",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Beekman series consists of moderately deep, well drained soils that formed in colluvium weathered from altered sedimentary and extrusive igneous rocks. Beekman soils are on steep mountainous slopes ranging from 30 to 100 percent. The mean annual precipitation is about 50 inches and the mean annual temperature is about 50 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F005XZ014CA"
+ ],
+ "ecoclassname": [
+ "Mesic Mountains <40Ppt"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ014CA"
+ ]
+ }
+ },
+ "id": {
+ "component": "Colestine",
+ "name": "Colestine",
+ "rank_loc": "6",
+ "score_loc": 0.025
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25443286",
+ "componentKind": "Series",
+ "componentPct": 30,
+ "dataSource": "SSURGO",
+ "distance": 497.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "469583",
+ "minCompDistance": 497.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=colestine",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#colestine",
+ "slope": 65.0,
+ "taxsubgrp": "Dystric Xerochrepts",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Colestine series consists of moderately deep, well drained soils that formed in colluvium and residuum from altered sedimentary and extrusive igneous rocks. Colestine soils are on mountain slopes of 20 to 90 percent. The mean annual precipitation is about 50 inches and the mean annual temperature is about 50 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F005XZ014CA"
+ ],
+ "ecoclassname": [
+ "Mesic Mountains <40Ppt"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ014CA"
+ ]
+ }
+ },
+ "id": {
+ "component": "Pollard",
+ "name": "Pollard",
+ "rank_loc": "7",
+ "score_loc": 0.025
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25443850",
+ "componentKind": "Series",
+ "componentPct": 30,
+ "dataSource": "SSURGO",
+ "distance": 829.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "469806",
+ "minCompDistance": 829.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=pollard",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#pollard",
+ "slope": 24.0,
+ "taxsubgrp": "Typic Haploxerults",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Pollard series consists of very deep, well drained soils that formed in colluvium and residuum weathered from altered sedimentary and extrusive igneous rocks. Pollard soils are on hill slopes and toeslopes, foot slopes, saddles, ridges, and side slopes of mountains. Slopes are 2 to 60 percent. The mean annual precipitation is about 45 inches and the mean annual temperature is about 50 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F005XZ024CA"
+ ],
+ "ecoclassname": [
+ "Ridges"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ024CA"
+ ]
+ }
+ },
+ "id": {
+ "component": "Offenbacher",
+ "name": "Offenbacher",
+ "rank_loc": "8",
+ "score_loc": 0.017
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25443597",
+ "componentKind": "Series",
+ "componentPct": 20,
+ "dataSource": "SSURGO",
+ "distance": 347.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "469709",
+ "minCompDistance": 347.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=offenbacher",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#offenbacher",
+ "slope": 63.0,
+ "taxsubgrp": "Typic Xerochrepts",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Offenbacher series consists of moderately deep, well drained soils that formed in colluvium weathered from altered sedimentary and extrusive igneous rocks. Offenbacher soils are on mountains and have slopes of 50 to 80 percent. The mean annual temperature is about 47 degrees F, and the mean annual precipitation is about 32 inches."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F005XZ009CA"
+ ],
+ "ecoclassname": [
+ "Very Deep Mesic Hills 40-60Ppt"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ009CA"
+ ]
+ }
+ },
+ "id": {
+ "component": "Gregory",
+ "name": "Gregory",
+ "rank_loc": "9",
+ "score_loc": 0.007
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25443414",
+ "componentKind": "Series",
+ "componentPct": 2,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "2",
+ "irrcapscl": "w",
+ "irrcapunit": "None",
+ "mapunitID": "469633",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "4",
+ "nirrcapscl": "w",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=gregory",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#gregory",
+ "slope": 2.0,
+ "taxsubgrp": "Pachic Argixerolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Gregory series consists of deep, poorly drained soils on terraces. They formed in recent alluvium dominantly from sedimentary and metamorphic rocks. Slopes are 0 to 3 percent. The mean annual precipitation is about 24 inches and the mean annual temperature is about 52 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R005XY016OR"
+ ],
+ "ecoclassname": [
+ "Poorly Drained Bottom"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/005X/R005XY016OR"
+ ]
+ }
+ },
+ "id": {
+ "component": "Josephine",
+ "name": "Josephine2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.125
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25443848",
+ "componentKind": "Series",
+ "componentPct": 55,
+ "dataSource": "SSURGO",
+ "distance": 829.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "469806",
+ "minCompDistance": 712.0,
+ "nirrcapcl": "4",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=josephine",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#josephine",
+ "slope": 24.0,
+ "taxsubgrp": "Typic Haploxerults",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Josephine series consists of deep, well drained soils that formed in colluvium and residuum weathered from altered sedimentary and extrusive igneous rocks. Josephine soils are on broad ridgetops, toeslopes, footslopes, and side slopes of mountains. Slopes are 2 to 75 percent. The mean annual precipitation is about 45 inches and the mean annual temperature is about 50 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "us",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Ruch",
+ "componentData": "Data Complete",
+ "componentID": 25443415,
+ "name": "Ruch",
+ "rank_data": "4",
+ "rank_data_loc": "1",
+ "rank_loc": "1",
+ "score_data": 0.677,
+ "score_data_loc": 0.472,
+ "score_loc": 0.267
+ },
+ {
+ "component": "Josephine",
+ "componentData": NaN,
+ "componentID": 25443848,
+ "name": "Josephine2",
+ "rank_data": "3",
+ "rank_data_loc": "2",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.68,
+ "score_data_loc": 0.403,
+ "score_loc": 0.125
+ },
+ {
+ "component": "Abegg",
+ "componentData": "Data Complete",
+ "componentID": 25443548,
+ "name": "Abegg",
+ "rank_data": "2",
+ "rank_data_loc": "3",
+ "rank_loc": "3",
+ "score_data": 0.72,
+ "score_data_loc": 0.395,
+ "score_loc": 0.069
+ },
+ {
+ "component": "Gregory",
+ "componentData": "Data Complete",
+ "componentID": 25443414,
+ "name": "Gregory",
+ "rank_data": "1",
+ "rank_data_loc": "4",
+ "rank_loc": "9",
+ "score_data": 0.749,
+ "score_data_loc": 0.378,
+ "score_loc": 0.007
+ },
+ {
+ "component": "Pollard",
+ "componentData": NaN,
+ "componentID": 25443850,
+ "name": "Pollard",
+ "rank_data": "5",
+ "rank_data_loc": "5",
+ "rank_loc": "7",
+ "score_data": 0.623,
+ "score_data_loc": 0.324,
+ "score_loc": 0.025
+ },
+ {
+ "component": "Offenbacher",
+ "componentData": "Data Complete",
+ "componentID": 25443597,
+ "name": "Offenbacher",
+ "rank_data": "6",
+ "rank_data_loc": "6",
+ "rank_loc": "8",
+ "score_data": 0.472,
+ "score_data_loc": 0.244,
+ "score_loc": 0.017
+ },
+ {
+ "component": "Caris",
+ "componentData": NaN,
+ "componentID": 25443598,
+ "name": "Caris",
+ "rank_data": "7",
+ "rank_data_loc": "7",
+ "rank_loc": "4",
+ "score_data": 0.402,
+ "score_data_loc": 0.226,
+ "score_loc": 0.05
+ },
+ {
+ "component": "Beekman",
+ "componentData": "Data Complete",
+ "componentID": 25443287,
+ "name": "Beekman",
+ "rank_data": "9",
+ "rank_data_loc": "8",
+ "rank_loc": "5",
+ "score_data": 0.385,
+ "score_data_loc": 0.215,
+ "score_loc": 0.046
+ },
+ {
+ "component": "Colestine",
+ "componentData": "Data Complete",
+ "componentID": 25443286,
+ "name": "Colestine",
+ "rank_data": "8",
+ "rank_data_loc": "9",
+ "rank_loc": "6",
+ "score_data": 0.387,
+ "score_data_loc": 0.206,
+ "score_loc": 0.025
+ },
+ {
+ "component": "Josephine",
+ "componentData": "Data Complete",
+ "componentID": 25443480,
+ "name": "Josephine",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "2",
+ "score_data": 0.531,
+ "score_data_loc": 0.328,
+ "score_loc": 0.125
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.63413723,-94.31005777].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.63413723,-94.31005777].json
new file mode 100644
index 0000000..b700429
--- /dev/null
+++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.63413723,-94.31005777].json
@@ -0,0 +1,522 @@
+{
+ "list": {
+ "AWS_PIW90": 2.57,
+ "Soil Data Value": [
+ [
+ "rfv_class_0",
+ 0.2488625668211104
+ ],
+ [
+ "rfv_class_30",
+ 0.24530228329929127
+ ],
+ [
+ "texture_0",
+ 0.0
+ ],
+ [
+ "texture_30",
+ 0.0
+ ]
+ ],
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R103XY002MN"
+ ],
+ "ecoclassname": [
+ "Calcareous Upland Prairies"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/103X/R103XY002MN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Nicollet",
+ "name": "Nicollet",
+ "rank_loc": "1",
+ "score_loc": 0.402
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25584956",
+ "componentKind": "Series",
+ "componentPct": 85,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "797917",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "1",
+ "nirrcapscl": "None",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=nicollet",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#nicollet",
+ "slope": 2.0,
+ "taxsubgrp": "Aquic Hapludolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Nicollet series consists of very deep, somewhat poorly drained soils that formed in calcareous loamy glacial till on till plains and moraines. Slopes range from 0 to 5 percent. Mean annual air temperature is about 9 degrees C (48 degrees F). Mean annual precipitation is about 660 mm (28 inches)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R103XY004MN"
+ ],
+ "ecoclassname": [
+ "Loamy Upland Prairies"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/103X/R103XY004MN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Webster",
+ "name": "Webster",
+ "rank_loc": "2",
+ "score_loc": 0.331
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25584954",
+ "componentKind": "Series",
+ "componentPct": 5,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "797917",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "2",
+ "nirrcapscl": "w",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=webster",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#webster",
+ "slope": 1.0,
+ "taxsubgrp": "Typic Endoaquolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Webster series consists of very deep, poorly drained, moderately permeable soils formed in glacial till or local alluvium derived from till on uplands. Slope ranges from 0 to 3 percent. Mean annual air temperature is about 48 degrees F, and mean annual precipitation is about 30 inches."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R103XY015MN"
+ ],
+ "ecoclassname": [
+ "Depressional Marsh"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/103X/R103XY015MN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Clarion",
+ "name": "Clarion",
+ "rank_loc": "3",
+ "score_loc": 0.2
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25584950",
+ "componentKind": "Taxadjunct",
+ "componentPct": 5,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "797917",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "2",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=clarion",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#clarion",
+ "slope": 3.0,
+ "taxsubgrp": "Oxyaquic Hapludolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Clarion series consists of very deep, moderately well drained soils on uplands. These soils formed in glacial till. Slopes range from 1 to 9 percent. Mean annual air temperature is about 8 degrees C (47 degrees F). Mean annual precipitation is about 74 centimeters (29 inches)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R103XY001MN"
+ ],
+ "ecoclassname": [
+ "Loamy Wet Prairies"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/103X/R103XY001MN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Okoboji",
+ "name": "Okoboji",
+ "rank_loc": "4",
+ "score_loc": 0.04
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25584952",
+ "componentKind": "Series",
+ "componentPct": 5,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "797917",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "w",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=okoboji",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#okoboji",
+ "slope": 0.0,
+ "taxsubgrp": "Cumulic Vertic Endoaquolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Okoboji series consists of very deep, very poorly drained soils formed in alluvium or lacustrine sediments. These soils are in closed depressions on till plains and moraines. Slope ranges from 0 to 1 percent. Mean annual air temperature is about 8 degrees C. Mean annual precipitation is about 740 millimeters."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R103XY004MN"
+ ],
+ "ecoclassname": [
+ "Loamy Upland Prairies"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/103X/R103XY004MN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Glencoe",
+ "name": "Glencoe",
+ "rank_loc": "5",
+ "score_loc": 0.011
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25584960",
+ "componentKind": "Series",
+ "componentPct": 3,
+ "dataSource": "SSURGO",
+ "distance": 28.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "797921",
+ "minCompDistance": 28.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "w",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=glencoe",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#glencoe",
+ "slope": 0.0,
+ "taxsubgrp": "Cumulic Endoaquolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Glencoe series consists of very deep, very poorly drained soils that formed in loamy sediments from till. These soils are in closed depressions on moraines. Slope ranges from 0 to 1 percent. Mean annual air temperature is about 8 degrees C. Mean annual precipitation is about 735 millimeters."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R103XY015MN"
+ ],
+ "ecoclassname": [
+ "Depressional Marsh"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/103X/R103XY015MN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Storden",
+ "name": "Storden",
+ "rank_loc": "6",
+ "score_loc": 0.011
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25584602",
+ "componentKind": "Series",
+ "componentPct": 5,
+ "dataSource": "SSURGO",
+ "distance": 93.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "797923",
+ "minCompDistance": 93.0,
+ "nirrcapcl": "3",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=storden",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#storden",
+ "slope": 8.0,
+ "taxsubgrp": "Typic Eutrudepts",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Storden series consists of very deep, well drained soils that formed in calcareous loamy glacial till on glacial moraines. Slope ranges from 4 to 70 percent. Mean annual precipitation is about 660 mm (26 inches). Mean annual air temperature is about 9 degrees C (48 degrees F)."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R103XY001MN"
+ ],
+ "ecoclassname": [
+ "Loamy Wet Prairies"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/103X/R103XY001MN"
+ ]
+ }
+ },
+ "id": {
+ "component": "Canisteo",
+ "name": "Canisteo",
+ "rank_loc": "7",
+ "score_loc": 0.007
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25584962",
+ "componentKind": "Series",
+ "componentPct": 2,
+ "dataSource": "SSURGO",
+ "distance": 28.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "797921",
+ "minCompDistance": 28.0,
+ "nirrcapcl": "2",
+ "nirrcapscl": "w",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=canisteo",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#canisteo",
+ "slope": 1.0,
+ "taxsubgrp": "Typic Endoaquolls",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Canisteo series consists of very deep, poorly and very poorly drained soils that formed in calcareous, loamy till or in a thin mantle of loamy or silty sediments and the underlying calcareous, loamy till. These soils are on rims of depressions, depressions and flats on moraines or till plains. Slope ranges from 0 to 2 percent. Mean air annual temperature is about 9 degrees C. Mean annual precipitation is about 785 millimeters."
+ },
+ "texture": {},
+ "top_depth": {}
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "us",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Clarion",
+ "componentData": "Data Complete",
+ "componentID": 25584950,
+ "name": "Clarion",
+ "rank_data": "1",
+ "rank_data_loc": "1",
+ "rank_loc": 3,
+ "score_data": 0.517,
+ "score_data_loc": 0.358,
+ "score_loc": 0.2
+ },
+ {
+ "component": "Nicollet",
+ "componentData": "Data Complete",
+ "componentID": 25584956,
+ "name": "Nicollet",
+ "rank_data": "7",
+ "rank_data_loc": "2",
+ "rank_loc": 1,
+ "score_data": 0.22,
+ "score_data_loc": 0.311,
+ "score_loc": 0.402
+ },
+ {
+ "component": "Webster",
+ "componentData": "Data Complete",
+ "componentID": 25584954,
+ "name": "Webster",
+ "rank_data": "6",
+ "rank_data_loc": "3",
+ "rank_loc": 2,
+ "score_data": 0.268,
+ "score_data_loc": 0.299,
+ "score_loc": 0.331
+ },
+ {
+ "component": "Glencoe",
+ "componentData": "Data Complete",
+ "componentID": 25584960,
+ "name": "Glencoe",
+ "rank_data": "2",
+ "rank_data_loc": "4",
+ "rank_loc": 5,
+ "score_data": 0.451,
+ "score_data_loc": 0.231,
+ "score_loc": 0.011
+ },
+ {
+ "component": "Storden",
+ "componentData": "Data Complete",
+ "componentID": 25584602,
+ "name": "Storden",
+ "rank_data": "3",
+ "rank_data_loc": "5",
+ "rank_loc": 6,
+ "score_data": 0.433,
+ "score_data_loc": 0.222,
+ "score_loc": 0.011
+ },
+ {
+ "component": "Okoboji",
+ "componentData": "Missing Data",
+ "componentID": 25584952,
+ "name": "Okoboji",
+ "rank_data": "4",
+ "rank_data_loc": "6",
+ "rank_loc": 4,
+ "score_data": 0.303,
+ "score_data_loc": 0.171,
+ "score_loc": 0.04
+ },
+ {
+ "component": "Canisteo",
+ "componentData": "Data Complete",
+ "componentID": 25584962,
+ "name": "Canisteo",
+ "rank_data": "5",
+ "rank_data_loc": "7",
+ "rank_loc": 7,
+ "score_data": 0.287,
+ "score_data_loc": 0.147,
+ "score_loc": 0.007
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[43.06450312,-119.4596489].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[43.06450312,-119.4596489].json
new file mode 100644
index 0000000..dba3aaa
--- /dev/null
+++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[43.06450312,-119.4596489].json
@@ -0,0 +1,658 @@
+{
+ "list": {
+ "AWS_PIW90": 11.56,
+ "Soil Data Value": [
+ [
+ "rfv_class_30",
+ 1.6875961328426623
+ ],
+ [
+ "rfv_class_0",
+ 1.304781220223484
+ ],
+ [
+ "texture_30",
+ 0.35284738420075
+ ],
+ [
+ "texture_0",
+ 0.0
+ ]
+ ],
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R023XY212OR"
+ ],
+ "ecoclassname": [
+ "Loamy 10-12 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/023X/R023XY212OR"
+ ]
+ }
+ },
+ "id": {
+ "component": "Lonely",
+ "name": "Lonely",
+ "rank_loc": "1",
+ "score_loc": 0.267
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25442849",
+ "componentKind": "Series",
+ "componentPct": 50,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "490552",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=lonely",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#lonely",
+ "slope": 19.0,
+ "taxsubgrp": "Xeric Haplocambids",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Lonely series consists of moderately deep, well drained soils that formed in colluvium overlying igneous bedrock. Lonely soils are on dissected rock pediments and mountain sideslopes and have slopes of 2 to 30 percent. The mean annual precipitation is about 10 inches and the mean annual temperature is about 43 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R024XY003OR"
+ ],
+ "ecoclassname": [
+ "Sodic Bottom "
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/024X/R024XY003OR"
+ ]
+ }
+ },
+ "id": {
+ "component": "Robson",
+ "name": "Robson",
+ "rank_loc": "2",
+ "score_loc": 0.187
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25442848",
+ "componentKind": "Series",
+ "componentPct": 35,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "490552",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=robson",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#robson",
+ "slope": 10.0,
+ "taxsubgrp": "Lithic Xeric Haplargids",
+ "textureInfill": "Yes"
+ },
+ "siteDescription": "The Robson series consists of shallow, well drained soils that formed in residuum derived from igneous rock. Robson soils are on hill and mountain crests and side slopes. Slopes are 2 to 75 percent. The mean annual precipitation is about 380 mm and the mean annual temperature is about 6 degrees C."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R023XY212OR"
+ ],
+ "ecoclassname": [
+ "Loamy 10-12 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/023X/R023XY212OR"
+ ]
+ }
+ },
+ "id": {
+ "component": "Actem",
+ "name": "Actem",
+ "rank_loc": "5",
+ "score_loc": 0.113
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25443068",
+ "componentKind": "Series",
+ "componentPct": 85,
+ "dataSource": "SSURGO",
+ "distance": 858.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "490458",
+ "minCompDistance": 858.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=actem",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#actem",
+ "slope": 11.0,
+ "taxsubgrp": "Xeric Argidurids",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Actem series consists of shallow to a duripan, well drained soils that formed in alluvium and colluvium derived from volcanic rocks. Actem soils are on hills and lava plateaus. Slopes are 2 to 20 percent. The mean annual precipitation is about 250 mm and the mean annual temperature is about 7 degrees C."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R023XY212OR"
+ ],
+ "ecoclassname": [
+ "Loamy 10-12 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/023X/R023XY212OR"
+ ]
+ }
+ },
+ "id": {
+ "component": "Reallis",
+ "name": "Reallis",
+ "rank_loc": "3",
+ "score_loc": 0.113
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25442630",
+ "componentKind": "Series",
+ "componentPct": 85,
+ "dataSource": "SSURGO",
+ "distance": 227.0,
+ "irrcapcl": "4",
+ "irrcapscl": "s",
+ "irrcapunit": "None",
+ "mapunitID": "490685",
+ "minCompDistance": 227.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=reallis",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#reallis",
+ "slope": 2.0,
+ "taxsubgrp": "Durinodic Xeric Haplocambids",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Reallis series consists of very deep, well drained soils that formed in alluvium derived from volcanic rocks and minor amounts of eolian material. Reallis soils are on alluvial fans and lake terraces. Slopes are 0 to 8 percent. The mean annual precipitation is about 250 mm and the mean annual temperature is about 6 degrees C."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R023XY212OR"
+ ],
+ "ecoclassname": [
+ "Loamy 10-12 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/023X/R023XY212OR"
+ ]
+ }
+ },
+ "id": {
+ "component": "Rinconflat",
+ "name": "Rinconflat",
+ "rank_loc": "4",
+ "score_loc": 0.113
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25442616",
+ "componentKind": "Series",
+ "componentPct": 85,
+ "dataSource": "SSURGO",
+ "distance": 717.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "490696",
+ "minCompDistance": 717.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=rinconflat",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#rinconflat",
+ "slope": 7.0,
+ "taxsubgrp": "Xeric Haplocambids",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Rinconflat series consists of very deep, well drained soils that formed in alluvium derived from mixed volcanic rocks. Rinconflat soils are on alluvial fans and fan remnants. Slopes are 3 to 10 percent. The mean annual precipitation is about 280 mm and the mean annual temperature is about 7 degrees C."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R023XY220OR"
+ ],
+ "ecoclassname": [
+ "Clayey 10-12 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/023X/R023XY220OR"
+ ]
+ }
+ },
+ "id": {
+ "component": "Lonegrave",
+ "name": "Lonegrave",
+ "rank_loc": "6",
+ "score_loc": 0.087
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25443055",
+ "componentKind": "Series",
+ "componentPct": 65,
+ "dataSource": "SSURGO",
+ "distance": 546.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "490463",
+ "minCompDistance": 546.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=lonegrave",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#lonegrave",
+ "slope": 55.0,
+ "taxsubgrp": "Xeric Haplocambids",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Lonegrave series consists of moderately deep, well drained soils that formed in colluvium derived from volcanic rocks. Lonegrave soils are on plateaus, hills, canyonlands, and mountains. Slopes are 5 to 70 percent. The mean annual precipitation is about 280 mm and the mean annual temperature is about 7 degrees C."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R023XY212OR"
+ ],
+ "ecoclassname": [
+ "Loamy 10-12 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/023X/R023XY212OR"
+ ]
+ }
+ },
+ "id": {
+ "component": "Raz",
+ "name": "Raz",
+ "rank_loc": "7",
+ "score_loc": 0.067
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25442636",
+ "componentKind": "Series",
+ "componentPct": 50,
+ "dataSource": "SSURGO",
+ "distance": 878.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "490682",
+ "minCompDistance": 878.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=raz",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#raz",
+ "slope": 11.0,
+ "taxsubgrp": "Xeric Haplodurids",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Raz series consists of shallow to a duripan, well drained soils that formed in slope alluvium, colluvium and residuum derived from basalt and tuff. Raz soils are on lava plateaus. Slopes are 1 to 20 percent. The mean annual precipitation is about 230 mm and the mean annual temperature is about 7 degrees C."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R023XY300OR"
+ ],
+ "ecoclassname": [
+ "South Slopes 10-12 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/023X/R023XY300OR"
+ ]
+ }
+ },
+ "id": {
+ "component": "Brace",
+ "name": "Brace",
+ "rank_loc": "8",
+ "score_loc": 0.046
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25442637",
+ "componentKind": "Series",
+ "componentPct": 35,
+ "dataSource": "SSURGO",
+ "distance": 878.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "490682",
+ "minCompDistance": 878.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=brace",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#brace",
+ "slope": 11.0,
+ "taxsubgrp": "Xeric Argidurids",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Brace series consists of moderately deep to a duripan, well drained soils that formed in slope alluvium, colluvium, and residuum derived from welded rhyolitic tuff and basalt. Brace soils are on structural benches, hills, and lava plateaus. Slopes are 1 to 20 percent. The mean annual precipitation is about 300 mm and the mean annual temperature is about 6 degrees C."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "R023XY220OR"
+ ],
+ "ecoclassname": [
+ "Clayey 10-12 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/023X/R023XY220OR"
+ ]
+ }
+ },
+ "id": {
+ "component": "Ausmus",
+ "name": "Ausmus",
+ "rank_loc": "9",
+ "score_loc": 0.005
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25442629",
+ "componentKind": "Series",
+ "componentPct": 4,
+ "dataSource": "SSURGO",
+ "distance": 227.0,
+ "irrcapcl": "4",
+ "irrcapscl": "s",
+ "irrcapunit": "None",
+ "mapunitID": "490685",
+ "minCompDistance": 227.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=ausmus",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#ausmus",
+ "slope": 1.0,
+ "taxsubgrp": "Aquic Natrargids",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Ausmus series consists of very deep, somewhat poorly drained or moderately well drained soils that formed in alluvium and lacustrine deposits derived from volcanic rocks and volcanic ash. Ausmus soils are on low lake terraces. Slopes are 0 to 2 percent. The mean annual precipitation is about 230 mm and the mean annual temperature is about 6.5 degrees C."
+ },
+ "texture": {},
+ "top_depth": {}
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "us",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Lonely",
+ "componentData": "Data Complete",
+ "componentID": 25442849,
+ "name": "Lonely",
+ "rank_data": "6",
+ "rank_data_loc": "1",
+ "rank_loc": 1,
+ "score_data": 0.616,
+ "score_data_loc": 0.442,
+ "score_loc": 0.267
+ },
+ {
+ "component": "Robson",
+ "componentData": "Data Complete",
+ "componentID": 25442848,
+ "name": "Robson",
+ "rank_data": "2",
+ "rank_data_loc": "2",
+ "rank_loc": 2,
+ "score_data": 0.691,
+ "score_data_loc": 0.439,
+ "score_loc": 0.187
+ },
+ {
+ "component": "Actem",
+ "componentData": "Data Complete",
+ "componentID": 25443068,
+ "name": "Actem",
+ "rank_data": "1",
+ "rank_data_loc": "3",
+ "rank_loc": 5,
+ "score_data": 0.697,
+ "score_data_loc": 0.405,
+ "score_loc": 0.113
+ },
+ {
+ "component": "Rinconflat",
+ "componentData": "Data Complete",
+ "componentID": 25442616,
+ "name": "Rinconflat",
+ "rank_data": "5",
+ "rank_data_loc": "4",
+ "rank_loc": 4,
+ "score_data": 0.623,
+ "score_data_loc": 0.368,
+ "score_loc": 0.113
+ },
+ {
+ "component": "Brace",
+ "componentData": "Data Complete",
+ "componentID": 25442637,
+ "name": "Brace",
+ "rank_data": "3",
+ "rank_data_loc": "5",
+ "rank_loc": 8,
+ "score_data": 0.661,
+ "score_data_loc": 0.354,
+ "score_loc": 0.046
+ },
+ {
+ "component": "Raz",
+ "componentData": "Data Complete",
+ "componentID": 25442636,
+ "name": "Raz",
+ "rank_data": "4",
+ "rank_data_loc": "6",
+ "rank_loc": 7,
+ "score_data": 0.63,
+ "score_data_loc": 0.348,
+ "score_loc": 0.067
+ },
+ {
+ "component": "Reallis",
+ "componentData": "Data Complete",
+ "componentID": 25442630,
+ "name": "Reallis",
+ "rank_data": "8",
+ "rank_data_loc": "7",
+ "rank_loc": 3,
+ "score_data": 0.581,
+ "score_data_loc": 0.347,
+ "score_loc": 0.113
+ },
+ {
+ "component": "Ausmus",
+ "componentData": "Data Complete",
+ "componentID": 25442629,
+ "name": "Ausmus",
+ "rank_data": "7",
+ "rank_data_loc": "8",
+ "rank_loc": 9,
+ "score_data": 0.607,
+ "score_data_loc": 0.306,
+ "score_loc": 0.005
+ },
+ {
+ "component": "Lonegrave",
+ "componentData": "Data Complete",
+ "componentID": 25443055,
+ "name": "Lonegrave",
+ "rank_data": "9",
+ "rank_data_loc": "9",
+ "rank_loc": 6,
+ "score_data": 0.437,
+ "score_data_loc": 0.262,
+ "score_loc": 0.087
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[45.6508331,-121.5111084].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[45.6508331,-121.5111084].json
new file mode 100644
index 0000000..3719634
--- /dev/null
+++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[45.6508331,-121.5111084].json
@@ -0,0 +1,233 @@
+{
+ "list": {
+ "AWS_PIW90": "Data not available",
+ "Soil Data Value": "Data not available",
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F006XA804OR"
+ ],
+ "ecoclassname": [
+ "Mesic Xeric Maritime Foothills 30-50 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/006X/F006XA804OR"
+ ]
+ }
+ },
+ "id": {
+ "component": "Hood",
+ "name": "Hood",
+ "rank_loc": "1",
+ "score_loc": 1.0
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25279329",
+ "componentKind": "Series",
+ "componentPct": 85,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "1",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "61998",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "1",
+ "nirrcapscl": "None",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hood",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hood",
+ "slope": 2.0,
+ "taxsubgrp": "Ultic Haploxeralfs",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Hood series consists of very deep, well drained soils formed in silty or loamy lacustrine deposits. Hood soils are on dissected terraces and terrace escarpments. Slopes are 0 to 65 percent. The mean annual precipitation is 38 inches and mean annual temperature is 50 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F006XA804OR"
+ ],
+ "ecoclassname": [
+ "Mesic Xeric Maritime Foothills 30-50 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/006X/F006XA804OR"
+ ]
+ }
+ },
+ "id": {
+ "component": "Hood",
+ "name": "Hood2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 1.0
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25279333",
+ "componentKind": "Series",
+ "componentPct": 85,
+ "dataSource": "SSURGO",
+ "distance": 52.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "62002",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hood",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hood",
+ "slope": 30.0,
+ "taxsubgrp": "Ultic Haploxeralfs",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Hood series consists of very deep, well drained soils formed in silty or loamy lacustrine deposits. Hood soils are on dissected terraces and terrace escarpments. Slopes are 0 to 65 percent. The mean annual precipitation is 38 inches and mean annual temperature is 50 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F006XA804OR"
+ ],
+ "ecoclassname": [
+ "Mesic Xeric Maritime Foothills 30-50 Pz"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/006X/F006XA804OR"
+ ]
+ }
+ },
+ "id": {
+ "component": "Hood",
+ "name": "Hood3",
+ "rank_loc": "Not Displayed",
+ "score_loc": 1.0
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25279330",
+ "componentKind": "Series",
+ "componentPct": 85,
+ "dataSource": "SSURGO",
+ "distance": 82.0,
+ "irrcapcl": "2",
+ "irrcapscl": "e",
+ "irrcapunit": "None",
+ "mapunitID": "61999",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "2",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hood",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hood",
+ "slope": 6.0,
+ "taxsubgrp": "Ultic Haploxeralfs",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Hood series consists of very deep, well drained soils formed in silty or loamy lacustrine deposits. Hood soils are on dissected terraces and terrace escarpments. Slopes are 0 to 65 percent. The mean annual precipitation is 38 inches and mean annual temperature is 50 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "us",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Hood",
+ "componentData": "Data Complete",
+ "componentID": 25279330,
+ "name": "Hood3",
+ "rank_data": "1",
+ "rank_data_loc": "1",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.588,
+ "score_data_loc": 0.794,
+ "score_loc": 1.0
+ },
+ {
+ "component": "Hood",
+ "componentData": "Data Complete",
+ "componentID": 25279329,
+ "name": "Hood",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "1",
+ "score_data": 0.556,
+ "score_data_loc": 0.778,
+ "score_loc": 1.0
+ },
+ {
+ "component": "Hood",
+ "componentData": "Data Complete",
+ "componentID": 25279333,
+ "name": "Hood2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.54,
+ "score_data_loc": 0.77,
+ "score_loc": 1.0
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[45.88932423,-121.0347381].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[45.88932423,-121.0347381].json
new file mode 100644
index 0000000..849b4ce
--- /dev/null
+++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[45.88932423,-121.0347381].json
@@ -0,0 +1,165 @@
+{
+ "list": {
+ "AWS_PIW90": "Data not available",
+ "Soil Data Value": "Data not available",
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F006XD004WA"
+ ],
+ "ecoclassname": [
+ "Mesic Xeric Slopes And Plateaus (Oregon White Oak-Ponderosa Pine Hot Dry Herb/Shrub)"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/006X/F006XD004WA"
+ ]
+ }
+ },
+ "id": {
+ "component": "Gunn",
+ "name": "Gunn",
+ "rank_loc": "1",
+ "score_loc": 0.929
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25483307",
+ "componentKind": "Series",
+ "componentPct": 95,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "3",
+ "irrcapscl": "e",
+ "irrcapunit": "None",
+ "mapunitID": "76223",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "2",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=gunn",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#gunn",
+ "slope": 5.0,
+ "taxsubgrp": "Ultic Haploxeralfs",
+ "textureInfill": "No"
+ },
+ "siteDescription": "Landscape--plateaus, hills\nLandform--structural benches, hillslopes, ridgetops\nSlope--0 to 65 percent\nParent material--loess mixed with colluvium and residuum derived from basalt\nMean annual precipitation--about 530 mm\nMean annual air temperature--about 9 degrees C\nDepth class--deep, very deep\nDrainage class--well drained\nSoil moisture regime--xeric\nSoil temperature regime--mesic\nSoil moisture subclass--typic"
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F006XD004WA"
+ ],
+ "ecoclassname": [
+ "Mesic Xeric Slopes And Plateaus (Oregon White Oak-Ponderosa Pine Hot Dry Herb/Shrub)"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/006X/F006XD004WA"
+ ]
+ }
+ },
+ "id": {
+ "component": "Gunn",
+ "name": "Gunn2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.929
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25483316",
+ "componentKind": "Series",
+ "componentPct": 90,
+ "dataSource": "SSURGO",
+ "distance": 42.0,
+ "irrcapcl": "nan",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "76225",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "4",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=gunn",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#gunn",
+ "slope": 19.0,
+ "taxsubgrp": "Ultic Haploxeralfs",
+ "textureInfill": "Yes"
+ },
+ "siteDescription": "Landscape--plateaus, hills\nLandform--structural benches, hillslopes, ridgetops\nSlope--0 to 65 percent\nParent material--loess mixed with colluvium and residuum derived from basalt\nMean annual precipitation--about 530 mm\nMean annual air temperature--about 9 degrees C\nDepth class--deep, very deep\nDrainage class--well drained\nSoil moisture regime--xeric\nSoil temperature regime--mesic\nSoil moisture subclass--typic"
+ },
+ "texture": {},
+ "top_depth": {}
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "us",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Gunn",
+ "componentData": NaN,
+ "componentID": 25483316,
+ "name": "Gunn2",
+ "rank_data": "1",
+ "rank_data_loc": "1",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.37,
+ "score_data_loc": 0.649,
+ "score_loc": 0.929
+ },
+ {
+ "component": "Gunn",
+ "componentData": "Data Complete",
+ "componentID": 25483307,
+ "name": "Gunn",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "1",
+ "score_data": 0.312,
+ "score_data_loc": 0.62,
+ "score_loc": 0.929
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[47.213922,-69.28246582].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[47.213922,-69.28246582].json
new file mode 100644
index 0000000..a6b3b34
--- /dev/null
+++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[47.213922,-69.28246582].json
@@ -0,0 +1,930 @@
+{
+ "list": {
+ "AWS_PIW90": 10.3,
+ "Soil Data Value": [
+ [
+ "rfv_class_30",
+ 1.3229420838347168
+ ],
+ [
+ "rfv_class_0",
+ 1.1105001941281816
+ ],
+ [
+ "texture_30",
+ 0.9931611211632956
+ ],
+ [
+ "texture_0",
+ 0.0
+ ]
+ ],
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ ""
+ ],
+ "ecoclassname": [
+ ""
+ ],
+ "edit_url": [
+ ""
+ ]
+ }
+ },
+ "id": {
+ "component": "Knob lock",
+ "name": "Knob lock",
+ "rank_loc": "1",
+ "score_loc": 0.325
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25208412",
+ "componentKind": "Series",
+ "componentPct": 46,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "2549870",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=knob_lock",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#knob_lock",
+ "slope": 40.0,
+ "taxsubgrp": "Lithic Udifolists",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Knob Lock series consists of very shallow and shallow, well drained through excessively drained organic soils on mountains and hills. They formed in thin organic deposits underlain in most places by a very thin mineral horizon over bedrock. Saturated hydraulic conductivity is moderately high through very high throughout the soil. Slope ranges from 3 through 80 percent. Mean annual precipitation is about 1092 mm and mean annual temperature is about 5 degrees C."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ ""
+ ],
+ "ecoclassname": [
+ ""
+ ],
+ "edit_url": [
+ ""
+ ]
+ }
+ },
+ "id": {
+ "component": "Chesuncook",
+ "name": "Chesuncook",
+ "rank_loc": "2",
+ "score_loc": 0.277
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25209552",
+ "componentKind": "Series",
+ "componentPct": 3,
+ "dataSource": "SSURGO",
+ "distance": 19.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "2549860",
+ "minCompDistance": 19.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=chesuncook",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#chesuncook",
+ "slope": 12.0,
+ "taxsubgrp": "Aquic Haplorthods",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Chesuncook series consists of very deep, moderately well drained soils on till plains, hills, ridges, and mountains. These soils formed in dense glacial till. Saturated hydraulic conductivity is moderately high or high in the solum, and low to moderately high in the dense substratum. Slope ranges from 3 to 45 percent. Mean annual temperature is about 4 degrees C, and mean annual precipitation is about 1092 mm at the type location."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ ""
+ ],
+ "ecoclassname": [
+ ""
+ ],
+ "edit_url": [
+ ""
+ ]
+ }
+ },
+ "id": {
+ "component": "Elliottsville",
+ "name": "Elliottsville",
+ "rank_loc": "3",
+ "score_loc": 0.211
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25209557",
+ "componentKind": "Series",
+ "componentPct": 35,
+ "dataSource": "SSURGO",
+ "distance": 19.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "2549860",
+ "minCompDistance": 19.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=elliottsville",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#elliottsville",
+ "slope": 25.0,
+ "taxsubgrp": "Typic Haplorthods",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Elliottsville series consists of moderately deep, well drained soils formed in glacial till on till plains, hills, ridges and mountains. Permeability is moderate. Slope ranges from 3 to 65 percent. Mean annual temperature is about 3 degrees C, and mean annual precipitation is about 970 mm at the type location."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ ""
+ ],
+ "ecoclassname": [
+ ""
+ ],
+ "edit_url": [
+ ""
+ ]
+ }
+ },
+ "id": {
+ "component": "Monson",
+ "name": "Monson",
+ "rank_loc": "4",
+ "score_loc": 0.092
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25209554",
+ "componentKind": "Series",
+ "componentPct": 6,
+ "dataSource": "SSURGO",
+ "distance": 19.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "2549860",
+ "minCompDistance": 19.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=monson",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#monson",
+ "slope": 25.0,
+ "taxsubgrp": "Lithic Haplorthods",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Monson series consists of shallow, somewhat excessively drained soils formed in glacial till on knolls of till plains, and on hills, ridges and mountains. Estimated saturated hydraulic conductivity is moderate or high. Slope ranges from 3 to 60 percent. Mean annual temperature is about 3 degrees C, and mean annual precipitation is about 965 mm at the type location."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ ""
+ ],
+ "ecoclassname": [
+ ""
+ ],
+ "edit_url": [
+ ""
+ ]
+ }
+ },
+ "id": {
+ "component": "Abram",
+ "name": "Abram",
+ "rank_loc": "5",
+ "score_loc": 0.036
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25209553",
+ "componentKind": "Series",
+ "componentPct": 4,
+ "dataSource": "SSURGO",
+ "distance": 19.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "2549860",
+ "minCompDistance": 19.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=abram",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#abram",
+ "slope": 30.0,
+ "taxsubgrp": "Lithic Haplorthods",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Abram series consists of very shallow, excessively drained soils formed in a thin mantle of glacial till on ridges and mountains. Permeability is moderately rapid. Slope ranges from 0 to 80 percent. Mean annual temperature is about 7 degrees C, and mean annual precipitation is about 1118 mm at the type location."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F143XY702ME"
+ ],
+ "ecoclassname": [
+ "Shallow And Moderately Deep Till"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/143X/F143XY702ME"
+ ]
+ }
+ },
+ "id": {
+ "component": "Hogback",
+ "name": "Hogback",
+ "rank_loc": "6",
+ "score_loc": 0.03
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25208410",
+ "componentKind": "Series",
+ "componentPct": 5,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "2549870",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hogback",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hogback",
+ "slope": 50.0,
+ "taxsubgrp": "Lithic Haplohumods",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Hogback series consists of shallow, well drained soils on glaciated uplands. They formed in loamy till. Estimated saturated hydraulic conductivity is moderately high to high throughout the mineral soil. Slope ranges from 3 to 70 percent. Mean annual precipitation is about 50 inches, and mean annual temperature is about 43 degrees F."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F143XY702ME"
+ ],
+ "ecoclassname": [
+ "Shallow And Moderately Deep Till"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/143X/F143XY702ME"
+ ]
+ }
+ },
+ "id": {
+ "component": "Rawsonville",
+ "name": "Rawsonville",
+ "rank_loc": "7",
+ "score_loc": 0.03
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25208409",
+ "componentKind": "Series",
+ "componentPct": 5,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "2549870",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "4",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=rawsonville",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#rawsonville",
+ "slope": 20.0,
+ "taxsubgrp": "Typic Haplohumods",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Rawsonville series consists of moderately deep, well drained soils on glaciated uplands. They formed in loamy till. Estimated saturated hydraulic conductivity is moderately high or high in the mineral soil. Slope ranges from 3 to 70 percent. Mean annual precipitation is about 1,270 mm, and mean annual temperature is about 6 degrees C."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ ""
+ ],
+ "ecoclassname": [
+ ""
+ ],
+ "edit_url": [
+ ""
+ ]
+ }
+ },
+ "id": {
+ "component": "Knob lock",
+ "name": "Knob lock2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.325
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25209556",
+ "componentKind": "Series",
+ "componentPct": 2,
+ "dataSource": "SSURGO",
+ "distance": 19.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "2549860",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=knob_lock",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#knob_lock",
+ "slope": 30.0,
+ "taxsubgrp": "Lithic Udifolists",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Knob Lock series consists of very shallow and shallow, well drained through excessively drained organic soils on mountains and hills. They formed in thin organic deposits underlain in most places by a very thin mineral horizon over bedrock. Saturated hydraulic conductivity is moderately high through very high throughout the soil. Slope ranges from 3 through 80 percent. Mean annual precipitation is about 1092 mm and mean annual temperature is about 5 degrees C."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F143XY704ME"
+ ],
+ "ecoclassname": [
+ "Shallow Organic Rock Pocket"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/143X/F143XY704ME"
+ ]
+ }
+ },
+ "id": {
+ "component": "Knob lock",
+ "name": "Knob lock3",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.325
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25209692",
+ "componentKind": "Series",
+ "componentPct": 25,
+ "dataSource": "SSURGO",
+ "distance": 192.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "2549867",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=knob_lock",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#knob_lock",
+ "slope": 50.0,
+ "taxsubgrp": "Lithic Udifolists",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Knob Lock series consists of very shallow and shallow, well drained through excessively drained organic soils on mountains and hills. They formed in thin organic deposits underlain in most places by a very thin mineral horizon over bedrock. Saturated hydraulic conductivity is moderately high through very high throughout the soil. Slope ranges from 3 through 80 percent. Mean annual precipitation is about 1092 mm and mean annual temperature is about 5 degrees C."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ ""
+ ],
+ "ecoclassname": [
+ ""
+ ],
+ "edit_url": [
+ ""
+ ]
+ }
+ },
+ "id": {
+ "component": "Chesuncook",
+ "name": "Chesuncook2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.277
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25209555",
+ "componentKind": "Series",
+ "componentPct": 50,
+ "dataSource": "SSURGO",
+ "distance": 19.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "2549860",
+ "minCompDistance": 19.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=chesuncook",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#chesuncook",
+ "slope": 20.0,
+ "taxsubgrp": "Aquic Haplorthods",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Chesuncook series consists of very deep, moderately well drained soils on till plains, hills, ridges, and mountains. These soils formed in dense glacial till. Saturated hydraulic conductivity is moderately high or high in the solum, and low to moderately high in the dense substratum. Slope ranges from 3 to 45 percent. Mean annual temperature is about 4 degrees C, and mean annual precipitation is about 1092 mm at the type location."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F143XY501ME"
+ ],
+ "ecoclassname": [
+ "Loamy Slope"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/143X/F143XY501ME"
+ ]
+ }
+ },
+ "id": {
+ "component": "Elliottsville",
+ "name": "Elliottsville2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.211
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25209694",
+ "componentKind": "Series",
+ "componentPct": 20,
+ "dataSource": "SSURGO",
+ "distance": 192.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "2549867",
+ "minCompDistance": 19.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=elliottsville",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#elliottsville",
+ "slope": 40.0,
+ "taxsubgrp": "Typic Haplorthods",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Elliottsville series consists of moderately deep, well drained soils formed in glacial till on till plains, hills, ridges and mountains. Permeability is moderate. Slope ranges from 3 to 65 percent. Mean annual temperature is about 3 degrees C, and mean annual precipitation is about 970 mm at the type location."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F143XY501ME"
+ ],
+ "ecoclassname": [
+ "Loamy Slope"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/143X/F143XY501ME"
+ ]
+ }
+ },
+ "id": {
+ "component": "Monson",
+ "name": "Monson2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.092
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25209693",
+ "componentKind": "Series",
+ "componentPct": 40,
+ "dataSource": "SSURGO",
+ "distance": 192.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "2549867",
+ "minCompDistance": 19.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=monson",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#monson",
+ "slope": 40.0,
+ "taxsubgrp": "Lithic Haplorthods",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Monson series consists of shallow, somewhat excessively drained soils formed in glacial till on knolls of till plains, and on hills, ridges and mountains. Estimated saturated hydraulic conductivity is moderate or high. Slope ranges from 3 to 60 percent. Mean annual temperature is about 3 degrees C, and mean annual precipitation is about 965 mm at the type location."
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": [
+ "F143XY704ME"
+ ],
+ "ecoclassname": [
+ "Shallow Organic Rock Pocket"
+ ],
+ "edit_url": [
+ "https://edit.jornada.nmsu.edu/catalogs/esd/143X/F143XY704ME"
+ ]
+ }
+ },
+ "id": {
+ "component": "Abram",
+ "name": "Abram2",
+ "rank_loc": "Not Displayed",
+ "score_loc": 0.036
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "25209690",
+ "componentKind": "Series",
+ "componentPct": 10,
+ "dataSource": "SSURGO",
+ "distance": 192.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "2549867",
+ "minCompDistance": 19.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=abram",
+ "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#abram",
+ "slope": 45.0,
+ "taxsubgrp": "Lithic Haplorthods",
+ "textureInfill": "No"
+ },
+ "siteDescription": "The Abram series consists of very shallow, excessively drained soils formed in a thin mantle of glacial till on ridges and mountains. Permeability is moderately rapid. Slope ranges from 0 to 80 percent. Mean annual temperature is about 7 degrees C, and mean annual precipitation is about 1118 mm at the type location."
+ },
+ "texture": {},
+ "top_depth": {}
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "us",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "Chesuncook",
+ "componentData": "Data Complete",
+ "componentID": 25209552,
+ "name": "Chesuncook",
+ "rank_data": "1",
+ "rank_data_loc": "1",
+ "rank_loc": "2",
+ "score_data": 0.729,
+ "score_data_loc": 0.503,
+ "score_loc": 0.277
+ },
+ {
+ "component": "Knob lock",
+ "componentData": "Data Complete",
+ "componentID": 25209556,
+ "name": "Knob lock2",
+ "rank_data": "3",
+ "rank_data_loc": "2",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.667,
+ "score_data_loc": 0.496,
+ "score_loc": 0.325
+ },
+ {
+ "component": "Elliottsville",
+ "componentData": "Data Complete",
+ "componentID": 25209557,
+ "name": "Elliottsville",
+ "rank_data": "4",
+ "rank_data_loc": "3",
+ "rank_loc": "3",
+ "score_data": 0.648,
+ "score_data_loc": 0.43,
+ "score_loc": 0.211
+ },
+ {
+ "component": "Monson",
+ "componentData": "Data Complete",
+ "componentID": 25209554,
+ "name": "Monson",
+ "rank_data": "5",
+ "rank_data_loc": "4",
+ "rank_loc": "4",
+ "score_data": 0.616,
+ "score_data_loc": 0.354,
+ "score_loc": 0.092
+ },
+ {
+ "component": "Abram",
+ "componentData": "Data Complete",
+ "componentID": 25209553,
+ "name": "Abram",
+ "rank_data": "2",
+ "rank_data_loc": "5",
+ "rank_loc": "5",
+ "score_data": 0.671,
+ "score_data_loc": 0.353,
+ "score_loc": 0.036
+ },
+ {
+ "component": "Rawsonville",
+ "componentData": "Data Complete",
+ "componentID": 25208409,
+ "name": "Rawsonville",
+ "rank_data": "6",
+ "rank_data_loc": "6",
+ "rank_loc": "7",
+ "score_data": 0.615,
+ "score_data_loc": 0.322,
+ "score_loc": 0.03
+ },
+ {
+ "component": "Hogback",
+ "componentData": "Data Complete",
+ "componentID": 25208410,
+ "name": "Hogback",
+ "rank_data": "7",
+ "rank_data_loc": "7",
+ "rank_loc": "6",
+ "score_data": 0.484,
+ "score_data_loc": 0.257,
+ "score_loc": 0.03
+ },
+ {
+ "component": "Chesuncook",
+ "componentData": "Data Complete",
+ "componentID": 25209555,
+ "name": "Chesuncook2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.715,
+ "score_data_loc": 0.496,
+ "score_loc": 0.277
+ },
+ {
+ "component": "Knob lock",
+ "componentData": "Data Complete",
+ "componentID": 25208412,
+ "name": "Knob lock",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "1",
+ "score_data": 0.558,
+ "score_data_loc": 0.441,
+ "score_loc": 0.325
+ },
+ {
+ "component": "Knob lock",
+ "componentData": "Data Complete",
+ "componentID": 25209692,
+ "name": "Knob lock3",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.539,
+ "score_data_loc": 0.432,
+ "score_loc": 0.325
+ },
+ {
+ "component": "Elliottsville",
+ "componentData": "Data Complete",
+ "componentID": 25209694,
+ "name": "Elliottsville2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.546,
+ "score_data_loc": 0.379,
+ "score_loc": 0.211
+ },
+ {
+ "component": "Monson",
+ "componentData": "Data Complete",
+ "componentID": 25209693,
+ "name": "Monson2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.598,
+ "score_data_loc": 0.345,
+ "score_loc": 0.092
+ },
+ {
+ "component": "Abram",
+ "componentData": "Data Complete",
+ "componentID": 25209690,
+ "name": "Abram2",
+ "rank_data": "Not Displayed",
+ "rank_data_loc": "Not Displayed",
+ "rank_loc": "Not Displayed",
+ "score_data": 0.469,
+ "score_data_loc": 0.252,
+ "score_loc": 0.036
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[48.6956,-121.8166].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[48.6956,-121.8166].json
new file mode 100644
index 0000000..374ef98
--- /dev/null
+++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[48.6956,-121.8166].json
@@ -0,0 +1,976 @@
+{
+ "list": {
+ "AWS_PIW90": 14.67,
+ "Soil Data Value": [
+ [
+ "rfv_class_30",
+ 1.1951984103352893
+ ],
+ [
+ "rfv_class_0",
+ 0.9036969260198578
+ ],
+ [
+ "texture_30",
+ 0.7502956564979291
+ ],
+ [
+ "texture_0",
+ 0.0
+ ]
+ ],
+ "metadata": {
+ "location": "us",
+ "model": "v3",
+ "unit_measure": {
+ "cec": "cmol(c)/kg",
+ "clay": "%",
+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "Nimue",
+ "name": "Nimue",
+ "rank_loc": "1",
+ "score_loc": 0.131
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
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+ "dataSource": "STATSGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "675975",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 45.0,
+ "taxsubgrp": "Andic Haplocryods",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "Andic cryumbrepts",
+ "name": "Andic cryumbrepts",
+ "rank_loc": "2",
+ "score_loc": 0.086
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+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
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+ "distance": 994.2109898924772,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "676031",
+ "minCompDistance": 994.2109898924772,
+ "nirrcapcl": "7",
+ "nirrcapscl": "s",
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+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 53.0,
+ "taxsubgrp": "None",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
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+ "name": "Cryorthods",
+ "rank_loc": "3",
+ "score_loc": 0.065
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
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+ "componentPct": 15,
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+ "distance": 994.2109898924772,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "676031",
+ "minCompDistance": 994.2109898924772,
+ "nirrcapcl": "7",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 60.0,
+ "taxsubgrp": "None",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "Getchell",
+ "name": "Getchell",
+ "rank_loc": "4",
+ "score_loc": 0.062
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
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+ "dataSource": "STATSGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "675975",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 17.0,
+ "taxsubgrp": "Aquic Haplocryands",
+ "textureInfill": "Yes"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "Cryumbrepts",
+ "name": "Cryumbrepts",
+ "rank_loc": "5",
+ "score_loc": 0.043
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "14269506",
+ "componentKind": "Taxon above family",
+ "componentPct": 10,
+ "dataSource": "STATSGO",
+ "distance": 994.2109898924772,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "676031",
+ "minCompDistance": 994.2109898924772,
+ "nirrcapcl": "7",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 60.0,
+ "taxsubgrp": "None",
+ "textureInfill": "Yes"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "Diobsud",
+ "name": "Diobsud",
+ "rank_loc": "6",
+ "score_loc": 0.023
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
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+ "componentPct": 4,
+ "dataSource": "STATSGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "675975",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 48.0,
+ "taxsubgrp": "Andic Humicryods",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "Cryaquepts",
+ "name": "Cryaquepts",
+ "rank_loc": "7",
+ "score_loc": 0.022
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
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+ "componentKind": "Taxon above family",
+ "componentPct": 5,
+ "dataSource": "STATSGO",
+ "distance": 994.2109898924772,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "676031",
+ "minCompDistance": 994.2109898924772,
+ "nirrcapcl": "7",
+ "nirrcapscl": "w",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 2.0,
+ "taxsubgrp": "None",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "Cryohumods",
+ "name": "Cryohumods",
+ "rank_loc": "8",
+ "score_loc": 0.022
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "14269509",
+ "componentKind": "Taxon above family",
+ "componentPct": 5,
+ "dataSource": "STATSGO",
+ "distance": 994.2109898924772,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "676031",
+ "minCompDistance": 994.2109898924772,
+ "nirrcapcl": "7",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 60.0,
+ "taxsubgrp": "None",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
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diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[60.42282639,-158.4018264].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[60.42282639,-158.4018264].json
new file mode 100644
index 0000000..f702e18
--- /dev/null
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new file mode 100644
index 0000000..728cf8c
--- /dev/null
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diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[63.52666854,-156.4422738].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[63.52666854,-156.4422738].json
new file mode 100644
index 0000000..c9cce50
--- /dev/null
+++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[63.52666854,-156.4422738].json
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+ "depth": "cm",
+ "distance": "m",
+ "ec": "ds/m",
+ "rock_fragments": "cm3/100cm3",
+ "sand": "%"
+ }
+ },
+ "soilList": [
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "E30-boreal taiga-loamy frozen colluvial slopes",
+ "name": "E30-boreal taiga-loamy frozen colluvial slopes",
+ "rank_loc": "1",
+ "score_loc": 0.272
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "24914406",
+ "componentKind": "Taxon above family",
+ "componentPct": 34,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "3375385",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 4.0,
+ "taxsubgrp": "Typic Historthels",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "E30-boreal scrub-gravelly low flood plains",
+ "name": "E30-boreal scrub-gravelly low flood plains",
+ "rank_loc": "2",
+ "score_loc": 0.152
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "24914408",
+ "componentKind": "Taxon above family",
+ "componentPct": 19,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "3375385",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 1.0,
+ "taxsubgrp": "Oxyaquic Cryorthents",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "E30-boreal taiga-organic frozen peat plateaus",
+ "name": "E30-boreal taiga-organic frozen peat plateaus",
+ "rank_loc": "3",
+ "score_loc": 0.114
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "24914411",
+ "componentKind": "Taxon above family",
+ "componentPct": 12,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "3375385",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 0.0,
+ "taxsubgrp": "Glacic Folistels",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "E30-boreal taiga-silty frozen loess slopes",
+ "name": "E30-boreal taiga-silty frozen loess slopes",
+ "rank_loc": "4",
+ "score_loc": 0.086
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "24914462",
+ "componentKind": "Taxon above family",
+ "componentPct": 43,
+ "dataSource": "SSURGO",
+ "distance": 350.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "3375378",
+ "minCompDistance": 350.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 8.0,
+ "taxsubgrp": "Typic Historthels",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "E30-boreal forest-loamy flood plains",
+ "name": "E30-boreal forest-loamy flood plains",
+ "rank_loc": "5",
+ "score_loc": 0.072
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "24914409",
+ "componentKind": "Taxon above family",
+ "componentPct": 9,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "3375385",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "4",
+ "nirrcapscl": "w",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 1.0,
+ "taxsubgrp": "Typic Cryofluvents",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "E30-boreal forest-silty slopes",
+ "name": "E30-boreal forest-silty slopes",
+ "rank_loc": "6",
+ "score_loc": 0.056
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "24914405",
+ "componentKind": "Taxon above family",
+ "componentPct": 7,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "3375385",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 12.0,
+ "taxsubgrp": "Typic Haplocryods",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "E30-boreal forest-silty loess slopes",
+ "name": "E30-boreal forest-silty loess slopes",
+ "rank_loc": "7",
+ "score_loc": 0.046
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "24914386",
+ "componentKind": "Taxon above family",
+ "componentPct": 23,
+ "dataSource": "SSURGO",
+ "distance": 350.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "3375378",
+ "minCompDistance": 350.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 14.0,
+ "taxsubgrp": "Typic Haplocryepts",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "E30-boreal scrub/sphagnum-organic depressions",
+ "name": "E30-boreal scrub/sphagnum-organic depressions",
+ "rank_loc": "8",
+ "score_loc": 0.024
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "24914410",
+ "componentKind": "Taxon above family",
+ "componentPct": 3,
+ "dataSource": "SSURGO",
+ "distance": 0.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "3375385",
+ "minCompDistance": 0.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 0.0,
+ "taxsubgrp": "Hydric Cryofibrists",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "E30-boreal taiga/tussock-silty frozen slopes",
+ "name": "E30-boreal taiga/tussock-silty frozen slopes",
+ "rank_loc": "9",
+ "score_loc": 0.024
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "24914464",
+ "componentKind": "Taxon above family",
+ "componentPct": 12,
+ "dataSource": "SSURGO",
+ "distance": 350.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "3375378",
+ "minCompDistance": 350.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 2.0,
+ "taxsubgrp": "Typic Histoturbels",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "E30-boreal scrub-silty frozen drainageways",
+ "name": "E30-boreal scrub-silty frozen drainageways",
+ "rank_loc": "10",
+ "score_loc": 0.022
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "24914387",
+ "componentKind": "Taxon above family",
+ "componentPct": 11,
+ "dataSource": "SSURGO",
+ "distance": 350.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "3375378",
+ "minCompDistance": 350.0,
+ "nirrcapcl": "6",
+ "nirrcapscl": "s",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 1.0,
+ "taxsubgrp": "Fluvaquentic Historthels",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "E30-boreal subalpine scrub-loamy colluvial slopes",
+ "name": "E30-boreal subalpine scrub-loamy colluvial slopes",
+ "rank_loc": "11",
+ "score_loc": 0.002
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "24914388",
+ "componentKind": "Taxon above family",
+ "componentPct": 1,
+ "dataSource": "SSURGO",
+ "distance": 350.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "3375378",
+ "minCompDistance": 350.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 25.0,
+ "taxsubgrp": "Typic Dystrocryepts",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ },
+ {
+ "bottom_depth": {},
+ "cec": {},
+ "clay": {},
+ "ec": {},
+ "esd": {
+ "ESD": {
+ "ecoclassid": "",
+ "ecoclassname": "",
+ "edit_url": ""
+ }
+ },
+ "id": {
+ "component": "E30-boreal subalpine woodland-gravelly colluvial slopes",
+ "name": "E30-boreal subalpine woodland-gravelly colluvial slopes",
+ "rank_loc": "12",
+ "score_loc": 0.002
+ },
+ "lab": {},
+ "munsell": {},
+ "ph": {},
+ "rock_fragments": {},
+ "sand": {},
+ "site": {
+ "siteData": {
+ "componentID": "24914463",
+ "componentKind": "Taxon above family",
+ "componentPct": 1,
+ "dataSource": "SSURGO",
+ "distance": 350.0,
+ "irrcapcl": "None",
+ "irrcapscl": "None",
+ "irrcapunit": "None",
+ "mapunitID": "3375378",
+ "minCompDistance": 350.0,
+ "nirrcapcl": "7",
+ "nirrcapscl": "e",
+ "nirrcapunit": "None",
+ "rfvInfill": "No",
+ "sdeURL": "",
+ "seeURL": "",
+ "slope": 18.0,
+ "taxsubgrp": "Typic Dystrocryepts",
+ "textureInfill": "No"
+ },
+ "siteDescription": ""
+ },
+ "texture": {},
+ "top_depth": {}
+ }
+ ]
+ },
+ "rank": {
+ "metadata": {
+ "location": "us",
+ "model": "v2"
+ },
+ "soilRank": [
+ {
+ "component": "E30-boreal taiga-organic frozen peat plateaus",
+ "componentData": "Missing Data",
+ "componentID": 24914411,
+ "name": "E30-boreal taiga-organic frozen peat plateaus",
+ "rank_data": "4",
+ "rank_data_loc": "1",
+ "rank_loc": 3,
+ "score_data": 0.657,
+ "score_data_loc": 0.385,
+ "score_loc": 0.114
+ },
+ {
+ "component": "E30-boreal taiga-loamy frozen colluvial slopes",
+ "componentData": "Missing Data",
+ "componentID": 24914406,
+ "name": "E30-boreal taiga-loamy frozen colluvial slopes",
+ "rank_data": "8",
+ "rank_data_loc": "2",
+ "rank_loc": 1,
+ "score_data": 0.481,
+ "score_data_loc": 0.377,
+ "score_loc": 0.272
+ },
+ {
+ "component": "E30-boreal forest-silty loess slopes",
+ "componentData": "Missing Data",
+ "componentID": 24914386,
+ "name": "E30-boreal forest-silty loess slopes",
+ "rank_data": "1",
+ "rank_data_loc": "3",
+ "rank_loc": 7,
+ "score_data": 0.706,
+ "score_data_loc": 0.376,
+ "score_loc": 0.046
+ },
+ {
+ "component": "E30-boreal forest-loamy flood plains",
+ "componentData": "Missing Data",
+ "componentID": 24914409,
+ "name": "E30-boreal forest-loamy flood plains",
+ "rank_data": "5",
+ "rank_data_loc": "4",
+ "rank_loc": 5,
+ "score_data": 0.649,
+ "score_data_loc": 0.36,
+ "score_loc": 0.072
+ },
+ {
+ "component": "E30-boreal scrub-gravelly low flood plains",
+ "componentData": "Missing Data",
+ "componentID": 24914408,
+ "name": "E30-boreal scrub-gravelly low flood plains",
+ "rank_data": "7",
+ "rank_data_loc": "5",
+ "rank_loc": 2,
+ "score_data": 0.567,
+ "score_data_loc": 0.359,
+ "score_loc": 0.152
+ },
+ {
+ "component": "E30-boreal subalpine woodland-gravelly colluvial slopes",
+ "componentData": "Missing Data",
+ "componentID": 24914463,
+ "name": "E30-boreal subalpine woodland-gravelly colluvial slopes",
+ "rank_data": "2",
+ "rank_data_loc": "6",
+ "rank_loc": 12,
+ "score_data": 0.687,
+ "score_data_loc": 0.345,
+ "score_loc": 0.002
+ },
+ {
+ "component": "E30-boreal subalpine scrub-loamy colluvial slopes",
+ "componentData": "Missing Data",
+ "componentID": 24914388,
+ "name": "E30-boreal subalpine scrub-loamy colluvial slopes",
+ "rank_data": "3",
+ "rank_data_loc": "7",
+ "rank_loc": 11,
+ "score_data": 0.673,
+ "score_data_loc": 0.338,
+ "score_loc": 0.002
+ },
+ {
+ "component": "E30-boreal taiga/tussock-silty frozen slopes",
+ "componentData": "Missing Data",
+ "componentID": 24914464,
+ "name": "E30-boreal taiga/tussock-silty frozen slopes",
+ "rank_data": "6",
+ "rank_data_loc": "8",
+ "rank_loc": 9,
+ "score_data": 0.647,
+ "score_data_loc": 0.335,
+ "score_loc": 0.024
+ },
+ {
+ "component": "E30-boreal forest-silty slopes",
+ "componentData": "Missing Data",
+ "componentID": 24914405,
+ "name": "E30-boreal forest-silty slopes",
+ "rank_data": "10",
+ "rank_data_loc": "9",
+ "rank_loc": 6,
+ "score_data": 0.473,
+ "score_data_loc": 0.264,
+ "score_loc": 0.056
+ },
+ {
+ "component": "E30-boreal scrub/sphagnum-organic depressions",
+ "componentData": "Missing Data",
+ "componentID": 24914410,
+ "name": "E30-boreal scrub/sphagnum-organic depressions",
+ "rank_data": "9",
+ "rank_data_loc": "10",
+ "rank_loc": 8,
+ "score_data": 0.473,
+ "score_data_loc": 0.248,
+ "score_loc": 0.024
+ },
+ {
+ "component": "E30-boreal scrub-silty frozen drainageways",
+ "componentData": "Missing Data",
+ "componentID": 24914387,
+ "name": "E30-boreal scrub-silty frozen drainageways",
+ "rank_data": "11",
+ "rank_data_loc": "11",
+ "rank_loc": 10,
+ "score_data": 0.361,
+ "score_data_loc": 0.192,
+ "score_loc": 0.022
+ },
+ {
+ "component": "E30-boreal taiga-silty frozen loess slopes",
+ "componentData": "Missing Data",
+ "componentID": 24914462,
+ "name": "E30-boreal taiga-silty frozen loess slopes",
+ "rank_data": "12",
+ "rank_data_loc": "12",
+ "rank_loc": 4,
+ "score_data": 0.211,
+ "score_data_loc": 0.148,
+ "score_loc": 0.086
+ }
+ ]
+ }
+}
diff --git a/soil_id/tests/us/generate_bulk_test_results.py b/soil_id/tests/us/generate_bulk_test_results.py
index 22a005e..fb670cf 100644
--- a/soil_id/tests/us/generate_bulk_test_results.py
+++ b/soil_id/tests/us/generate_bulk_test_results.py
@@ -15,26 +15,15 @@
import datetime
import json
-import math
import os
import time
import traceback
import pandas
+from soil_id.tests.utils import clean_soil_list_json
from soil_id.us_soil import list_soils, rank_soils
-
-def clean_soil_list_json(obj):
- if isinstance(obj, float) and math.isnan(obj):
- return None
- elif isinstance(obj, dict):
- return dict((k, clean_soil_list_json(v)) for k, v in obj.items())
- elif isinstance(obj, (list, set, tuple)):
- return list(map(clean_soil_list_json, obj))
- return obj
-
-
test_data_df = pandas.read_csv(
os.path.join(os.path.dirname(__file__), "US_SoilID_KSSL_LPKS_Testing.csv")
)
diff --git a/soil_id/tests/us/test_us.py b/soil_id/tests/us/test_us.py
index 1a104d3..f84c97a 100644
--- a/soil_id/tests/us/test_us.py
+++ b/soil_id/tests/us/test_us.py
@@ -17,7 +17,9 @@
import time
import pytest
+from syrupy.extensions.json import JSONSnapshotExtension
+from soil_id.tests.utils import clean_soil_list_json
from soil_id.us_soil import list_soils, rank_soils
test_locations = [
@@ -40,9 +42,13 @@
# {"lat": 40.79861, "lon": -112.35477}, # crash: str object has no attribute rank_data_csv
]
+test_params = []
+for idx, coords in enumerate(test_locations):
+ test_params.append(pytest.param(coords, id=f"{coords['lat']},{coords['lon']}"))
-@pytest.mark.parametrize("location", test_locations)
-def test_soil_location(location):
+
+@pytest.mark.parametrize("location", test_params)
+def test_soil_location(location, snapshot):
# Dummy Soil Profile Data (replicating the structure provided)
soilHorizon = ["LOAM"] * 7
topDepth = [0, 1, 10, 20, 50, 70, 100]
@@ -57,7 +63,7 @@ def test_soil_location(location):
start_time = time.perf_counter()
list_soils_result = list_soils(location["lon"], location["lat"])
logging.info(f"...time: {(time.perf_counter() - start_time):.2f}s")
- rank_soils(
+ rank_result = rank_soils(
location["lon"],
location["lat"],
list_soils_result,
@@ -72,6 +78,11 @@ def test_soil_location(location):
cracks,
)
+ assert snapshot.with_defaults(extension_class=JSONSnapshotExtension) == {
+ "list": clean_soil_list_json(list_soils_result.soil_list_json),
+ "rank": rank_result,
+ }
+
def test_empty_rank():
SoilListOutputData = list_soils(test_locations[0]["lon"], test_locations[0]["lat"])
diff --git a/soil_id/tests/utils.py b/soil_id/tests/utils.py
new file mode 100644
index 0000000..6ec66e7
--- /dev/null
+++ b/soil_id/tests/utils.py
@@ -0,0 +1,26 @@
+# Copyright © 2025 Technology Matters
+#
+# This program is free software: you can redistribute it and/or modify
+# it under the terms of the GNU Affero General Public License as published
+# by the Free Software Foundation, either version 3 of the License, or
+# (at your option) any later version.
+#
+# This program is distributed in the hope that it will be useful,
+# but WITHOUT ANY WARRANTY; without even the implied warranty of
+# MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE. See the
+# GNU Affero General Public License for more details.
+#
+# You should have received a copy of the GNU Affero General Public License
+# along with this program. If not, see https://www.gnu.org/licenses/.
+
+import math
+
+
+def clean_soil_list_json(obj):
+ if isinstance(obj, float) and math.isnan(obj):
+ return None
+ elif isinstance(obj, dict):
+ return dict((k, clean_soil_list_json(v)) for k, v in obj.items())
+ elif isinstance(obj, (list, set, tuple)):
+ return list(map(clean_soil_list_json, obj))
+ return obj
diff --git a/soil_id/us_soil.py b/soil_id/us_soil.py
index 00b6c5d..cdca332 100644
--- a/soil_id/us_soil.py
+++ b/soil_id/us_soil.py
@@ -133,7 +133,7 @@ def list_soils(lon, lat):
# Location based calculation
# --------------------------------------------------------------------
# Process distance scores and perform group-wise aggregations.
- mucompdata_pd = process_distance_scores(mucompdata_pd, ExpCoeff)
+ mucompdata_pd = process_distance_scores(mucompdata_pd, ExpCoeff, compkind_filter=True)
# Add the data source column
mucompdata_pd["data_source"] = data_source
@@ -202,7 +202,7 @@ def list_soils(lon, lat):
# Merge muhorzdata_pd with selected columns from mucompdata_pd
muhorzdata_pd = pd.merge(
muhorzdata_pd,
- mucompdata_pd[["cokey", "comppct_r", "compname", "distance_score", "slope_r"]],
+ mucompdata_pd[["cokey", "comppct_r", "compname", "cond_prob", "slope_r"]],
on="cokey",
how="left",
)
@@ -214,6 +214,14 @@ def list_soils(lon, lat):
)
muhorzdata_pd = muhorzdata_pd[filter_condition].drop_duplicates().reset_index(drop=True)
+ # Add distance column from mucompdata_pd using cokey link
+ muhorzdata_pd = pd.merge(
+ muhorzdata_pd,
+ mucompdata_pd[["cokey", "distance", "distance_score"]],
+ on="cokey",
+ how="left",
+ )
+
# Check for duplicate component instances
hz_drop = drop_cokey_horz(muhorzdata_pd)
if hz_drop is not None:
@@ -225,8 +233,10 @@ def list_soils(lon, lat):
comp_key = muhorzdata_pd["cokey"].unique().tolist()
mucompdata_pd = mucompdata_pd[mucompdata_pd["cokey"].isin(comp_key)]
- # Sort mucompdata_pd based on 'distance_score' and 'distance'
- mucompdata_pd.sort_values(["distance_score", "distance"], ascending=[False, True], inplace=True)
+ # Sort mucompdata_pd based on 'cond_prob' and 'distance'
+ mucompdata_pd.sort_values(
+ ["cond_prob", "distance", "compname"], ascending=[False, True, True], inplace=True
+ )
mucompdata_pd.reset_index(drop=True, inplace=True)
# Duplicate the 'compname' column for grouping purposes
@@ -250,14 +260,17 @@ def list_soils(lon, lat):
component_names = mucompdata_pd["compname"].tolist()
name_counts = collections.Counter(component_names)
- for name, count in name_counts.items():
+ for name, count in sorted(name_counts.items()): # Sort for deterministic order
if count > 1: # If a component name is duplicated
- suffixes = range(1, count + 1) # Generate suffixes for the duplicate names
- for suffix in suffixes:
- index = component_names.index(
- name
- ) # Find the index of the first occurrence of the duplicate name
- component_names[index] = name + str(suffix) # Append the suffix
+ # Find all indices for this name
+ indices = [i for i, comp_name in enumerate(component_names) if comp_name == name]
+ # Sort indices for deterministic order
+ indices.sort()
+
+ # Add suffixes to all occurrences except the first
+ for i, idx in enumerate(indices):
+ if i > 0: # Skip the first occurrence (keep original name)
+ component_names[idx] = name + str(i + 1) # Append suffix starting from 2
mucompdata_pd["compname"] = component_names
muhorzdata_pd.rename(columns={"compname": "compname_grp"}, inplace=True)
@@ -270,7 +283,7 @@ def list_soils(lon, lat):
muhorzdata_pd = muhorzdata_pd[~muhorzdata_pd["hzname"].str.contains("R", case=False, na=False)]
# Group data by cokey (component key)
- muhorzdata_group_cokey = [group for _, group in muhorzdata_pd.groupby("cokey", sort=False)]
+ muhorzdata_group_cokey = [group for _, group in muhorzdata_pd.groupby("cokey", sort=True)]
getProfile_cokey = []
comp_max_depths = []
@@ -1122,7 +1135,7 @@ def list_soils(lon, lat):
# Create a new column 'soilID_rank' which will be True for the first row in each group sorted
# by 'distance' and False for other rows
- mucompdata_pd = mucompdata_pd.sort_values(["compname_grp", "distance"])
+ mucompdata_pd = mucompdata_pd.sort_values(["compname_grp", "distance", "compname"])
mucompdata_pd["soilID_rank"] = ~mucompdata_pd.duplicated("compname_grp", keep="first")
# Assign the minimum distance for each group to a new column 'min_dist'
@@ -1156,7 +1169,7 @@ def list_soils(lon, lat):
ESDcompdataQry = (
"SELECT cokey, ecoclassid, ecoclassname FROM coecoclass WHERE cokey IN ("
+ ",".join(map(str, comp_key))
- + ")"
+ + ") ORDER BY cokey"
)
ESDcompdata_out = sda_return(propQry=ESDcompdataQry)
@@ -1208,7 +1221,7 @@ def list_soils(lon, lat):
ESDcompdata_pd = update_esd_data(ESDcompdata_pd)
# Aggregate the ESD components for output
- for _, group in ESDcompdata_pd.groupby("cokey"):
+ for _, group in ESDcompdata_pd.groupby("cokey", sort=True):
esd_data = {
"ESD": {
"ecoclassid": group["ecoclassid"].tolist(),
@@ -1252,7 +1265,7 @@ def list_soils(lon, lat):
r"[0-9]+", "", regex=True
)
ESDcompdata_pd_comp_grps = [
- g for _, g in ESDcompdata_pd.groupby(["compname_grp"], sort=False)
+ g for _, g in ESDcompdata_pd.groupby(["compname_grp"], sort=True)
]
ecoList_out = []
for i in range(len(ESDcompdata_pd_comp_grps)):
@@ -1299,7 +1312,7 @@ def list_soils(lon, lat):
ESDcompdata_pd = pd.concat(ecoList_out)
ESDcompdata_group_cokey = [
- g for _, g in ESDcompdata_pd.groupby(["cokey"], sort=False)
+ g for _, g in ESDcompdata_pd.groupby(["cokey"], sort=True)
]
for i in range(len(ESDcompdata_group_cokey)):
if ESDcompdata_group_cokey[i]["ecoclassname"].isnull().values.any():
@@ -1384,9 +1397,9 @@ def list_soils(lon, lat):
# ------------------------------------------------------------
- # Sort mucompdata_cond_prob by soilID_rank and distance_score
+ # Sort mucompdata_cond_prob by soilID_rank, cond_prob, and compname for deterministic tie-breaking
mucompdata_cond_prob = mucompdata_cond_prob.sort_values(
- ["soilID_rank", "distance_score"], ascending=[False, False]
+ ["soilID_rank", "cond_prob", "compname"], ascending=[False, False, True]
)
mucomp_index = mucompdata_cond_prob.index
@@ -1401,7 +1414,7 @@ def list_soils(lon, lat):
for site, comp, sc, rank in zip(
mucompdata_cond_prob["compname"],
mucompdata_cond_prob["compname_grp"],
- mucompdata_cond_prob["distance_score"].round(3),
+ mucompdata_cond_prob["cond_prob"].round(3),
mucompdata_cond_prob["Rank_Loc"],
)
]
@@ -1560,6 +1573,10 @@ def rank_soils(
into site data use 'getColor_deltaE2000_OSD_pedon' and helper functions
located in utils.py
"""
+ # Check if list_output_data is a string (error message) instead of expected object
+ if isinstance(list_output_data, str):
+ return {"error": f"Cannot rank soils: {list_output_data}"}
+
# ---------------------------------------------------------------------------------------
# ------ Load in user data --------#
# Initialize the DataFrame from the input data
@@ -1776,7 +1793,7 @@ def rank_soils(
# Horizon Data Similarity
if soilIDRank_output_pd is not None:
- groups = [group for _, group in soilIDRank_output_pd.groupby(["compname"], sort=False)]
+ groups = [group for _, group in soilIDRank_output_pd.groupby(["compname"], sort=True)]
Comp_Rank_Status = []
Comp_Missing_Status = []
@@ -1797,7 +1814,7 @@ def rank_soils(
Comp_Rank_Status.append("Ranked")
Comp_Missing_Status.append("Data Complete")
- Comp_name.append(group["compname"].unique()[0])
+ Comp_name.append(sorted(group["compname"].unique())[0])
# Consolidate the results into a DataFrame
Rank_Filter = pd.DataFrame(
@@ -2035,7 +2052,7 @@ def rank_soils(
# Sort and rank the components within each group
soilIDList_data = []
- for _, group in D_final.groupby(["compname_grp"], sort=False):
+ for _, group in D_final.groupby(["compname_grp"], sort=True):
# Sort by score, and then by compname
group = group.sort_values(by=["Score_Data", "compname"], ascending=[False, True])
@@ -2051,7 +2068,9 @@ def rank_soils(
D_final = pd.merge(D_final, Rank_Filter, on="compname", how="left")
# Sort dataframe to correctly assign Rank_Data
- D_final = D_final.sort_values(by=["soilID_rank_data", "Score_Data"], ascending=[False, False])
+ D_final = D_final.sort_values(
+ by=["soilID_rank_data", "Score_Data", "compname"], ascending=[False, False, True]
+ )
# Assigning rank based on the soilID rank and rank status
rank_id = 1
@@ -2072,7 +2091,7 @@ def rank_soils(
# ----------------------------------------------------------------
#Data output for testing
D_final_loc = pd.merge(D_final, mucompdata_pd[['compname', 'cokey', 'mukey',
- 'distance_score', 'clay', 'taxorder', 'taxsubgrp', 'OSD_text_int',
+ 'cond_prob', 'clay', 'taxorder', 'taxsubgrp', 'OSD_text_int',
'OSD_rfv_int', 'data_source', 'Rank_Loc', 'majcompflag', 'comppct_r', 'distance',
'nirrcapcl', 'nirrcapscl', 'nirrcapunit', 'irrcapcl', 'irrcapscl', 'irrcapunit',
'ecoclassid_update', 'ecoclassname']], on='compname', how='left')
@@ -2086,7 +2105,7 @@ def rank_soils(
[
"compname",
"cokey",
- "distance_score",
+ "cond_prob",
"clay",
"taxorder",
"taxsubgrp",
@@ -2111,7 +2130,7 @@ def rank_soils(
Score_Data_Loc = [0.0 for _ in range(len(D_final_loc))]
else:
# Calculate the combined score
- Score_Data_Loc = (D_final_loc["Score_Data"] + D_final_loc["distance_score"]) / (
+ Score_Data_Loc = (D_final_loc["Score_Data"] + D_final_loc["cond_prob"]) / (
D_final_loc["data_weight"] + location_weight
)
@@ -2144,8 +2163,10 @@ def rank_soils(
# Sorting and reindexing of final dataframe based on component groups
soilIDList_out = []
- for _, group in D_final_loc.groupby("compname_grp", sort=False):
- group = group.sort_values("Score_Data_Loc", ascending=False).reset_index(drop=True)
+ for _, group in D_final_loc.groupby("compname_grp", sort=True):
+ group = group.sort_values(
+ ["Score_Data_Loc", "compname"], ascending=[False, True]
+ ).reset_index(drop=True)
group["soilID_rank_final"] = [True if idx == 0 else False for idx in range(len(group))]
soilIDList_out.append(group)
@@ -2172,9 +2193,9 @@ def rank_soils(
D_final_loc["Rank_Data_Loc"] = Rank_DataLoc
- # Sort dataframe based on soilID_rank_final and Score_Data_Loc
+ # Sort dataframe based on soilID_rank_final, Score_Data_Loc, and compname for deterministic tie-breaking
D_final_loc = D_final_loc.sort_values(
- ["soilID_rank_final", "Score_Data_Loc"], ascending=[False, False]
+ ["soilID_rank_final", "Score_Data_Loc", "compname"], ascending=[False, False, True]
).reset_index(drop=True)
# Replace NaN values in the specified columns with 0.0
@@ -2184,7 +2205,7 @@ def rank_soils(
"D_horz",
"D_site",
"Score_Data_Loc",
- "distance_score",
+ "cond_prob",
]
] = D_final_loc[
[
@@ -2192,7 +2213,7 @@ def rank_soils(
"D_horz",
"D_site",
"Score_Data_Loc",
- "distance_score",
+ "cond_prob",
]
].fillna(0.0)
@@ -2212,7 +2233,7 @@ def rank_soils(
"" if row.missing_status == "Location data only" else round(row.Score_Data, 3)
),
"rank_data": "" if row.missing_status == "Location data only" else row.Rank_Data,
- "score_loc": round(row.distance_score, 3),
+ "score_loc": round(row.cond_prob, 3),
"rank_loc": row.Rank_Loc,
"componentData": row.missing_status,
}
diff --git a/soil_id/utils.py b/soil_id/utils.py
index 1909758..54a95a1 100644
--- a/soil_id/utils.py
+++ b/soil_id/utils.py
@@ -679,11 +679,12 @@ def getProfile_SG(data, variable, c_bot=False):
def drop_cokey_horz(df):
"""
Function to drop duplicate rows of component horizon data when more than one instance of a
- component are duplicates.
+ component are duplicates. Keeps the duplicate with the smallest distance.
Function assumes that the dataframe contains:
(1) unique cokey identifier ('cokey')
(2) generic compname identifier ('compname')
+ (3) distance column ('distance')
Can handle dataframes that include a 'slope_r' column as well as those that do not.
"""
columns_to_compare = [
@@ -707,13 +708,32 @@ def drop_cokey_horz(df):
# Group by compname
for _, comp_group in df.groupby("compname", sort=False):
# Get unique cokeys and their data signature within this compname group
- cokey_map = comp_group.groupby("cokey")["_cokey_grouped"].first()
+ cokey_map = comp_group.groupby("cokey").agg(
+ {
+ "_cokey_grouped": "first",
+ "distance": "first", # Get the distance for each cokey
+ }
+ )
+
+ # Find duplicates based on the grouped horizon data
+ duplicated_mask = cokey_map["_cokey_grouped"].duplicated(keep=False)
+
+ if duplicated_mask.any():
+ # Get only the duplicated entries
+ duplicated_entries = cokey_map[duplicated_mask]
- # Find duplicates
- duplicated = cokey_map.duplicated(keep="first")
- drop_instances.extend(cokey_map[duplicated].index.tolist())
+ # Group by the duplicated signature to find which cokeys are duplicates of each other
+ for signature, dup_group in duplicated_entries.groupby("_cokey_grouped"):
+ # Sort by distance and keep the one with smallest distance (first after sorting)
+ sorted_by_distance = dup_group.sort_values("distance")
+ # Drop all except the first (smallest distance)
+ cokeys_to_drop = sorted_by_distance.index.tolist()[1:]
+ drop_instances.extend(cokeys_to_drop)
- return pd.Series(drop_instances, name="cokey_to_drop")
+ # Clean up temporary columns
+ df.drop(columns=["_group_key", "_cokey_grouped"], inplace=True)
+
+ return pd.Series(drop_instances, name="cokey_to_drop") if drop_instances else None
def calculate_location_score(group, ExpCoeff):
@@ -1122,21 +1142,31 @@ def trim_fraction(text):
return text.rstrip(".0") if text.endswith(".0") else text
-def calculate_distance_score(row, ExpCoeff):
+def calculate_distance_score(row, ExpCoeff, comp_pct_col="comppct_r"):
"""
- Calculate distance score based on the conditions provided (US).
+ Calculate distance score based on distance and component percentage.
+ This function is generalized to work with different data sources by
+ accepting the component percentage column name as a parameter.
+
+ Parameters:
+ - row (pd.Series): A row of a DataFrame.
+ - ExpCoeff (float): Exponential coefficient for distance decay.
+ - comp_pct_col (str): The name of the component percentage column.
"""
- if row["distance"] == 0:
- if row["comppct_r"] > 100:
+ comp_pct = row[comp_pct_col]
+ distance = row["distance"]
+
+ if distance == 0:
+ if comp_pct > 100:
return 1
else:
- return round(row["comppct_r"] / 100, 3)
+ return round(comp_pct / 100, 3)
else:
- if row["comppct_r"] > 100:
- return round(max(0.25, math.exp(ExpCoeff * row["distance"])), 3)
+ factor = max(0.25, math.exp(ExpCoeff * distance))
+ if comp_pct > 100:
+ return round(factor, 3)
else:
- factor = max(0.25, math.exp(ExpCoeff * row["distance"]))
- return round(row["comppct_r"] / 100 * factor, 3)
+ return round(comp_pct / 100 * factor, 3)
def extract_muhorzdata_STATSGO(mucompdata_pd):
@@ -1168,7 +1198,8 @@ def extract_muhorzdata_STATSGO(mucompdata_pd):
ec_r, lep_r, chfrags.fragvol_r
FROM chorizon
LEFT OUTER JOIN chfrags ON chfrags.chkey = chorizon.chkey
- WHERE cokey IN ({",".join(cokey_list)})"""
+ WHERE cokey IN ({",".join(cokey_list)})
+ ORDER BY cokey, chorizon.chkey, hzdept_r"""
# Execute the query
muhorzdata_out = sda_return(propQry=muhorzdataQry)
@@ -1396,7 +1427,8 @@ def extract_mucompdata_STATSGO(lon, lat):
component.irrcapscl, component.irrcapunit, component.taxorder,
component.taxsubgrp
FROM component
- WHERE mukey IN ({",".join(map(str, mukey_list))})"""
+ WHERE mukey IN ({",".join(map(str, mukey_list))})
+ ORDER BY component.mukey, component.cokey"""
mucompdata_out = sda_return(propQry=mucompdataQry)
if not mucompdata_out.empty:
@@ -1653,12 +1685,30 @@ def fill_missing_comppct_r(mucompdata_pd):
return mucompdata_pd
-def process_distance_scores(mucompdata_pd, ExpCoeff):
+def process_distance_scores(
+ mucompdata_pd,
+ ExpCoeff,
+ comp_pct_col="comppct_r",
+ comp_key_col="cokey",
+ comp_name_col="compname",
+ map_unit_col="mukey",
+ distance_col="distance",
+ comp_kind_col="compkind",
+ compkind_filter=False,
+):
"""
Process distance scores and perform group-wise aggregations.
Parameters:
- mucompdata_pd (pd.DataFrame): DataFrame containing soil data.
+ - ExpCoeff (float): Exponential coefficient for distance decay.
+ - comp_pct_col (str): The name of the component percentage column (e.g., 'comppct_r', 'share').
+ - comp_key_col (str): The name of the unique component key column (e.g., 'cokey').
+ - comp_name_col (str): The name of the component name column (e.g., 'compname').
+ - map_unit_col (str): The name of the map unit key column (e.g., 'mukey').
+ - distance_col (str): The name of the distance column.
+ - comp_kind_col (str): The name of the component kind column for filtering.
+ - compkind_filter (bool): If True, filter out "Miscellaneous area" based on comp_kind_col.
External Functions:
- calculate_distance_score (function): A function to calculate distance scores.
@@ -1673,55 +1723,91 @@ def process_distance_scores(mucompdata_pd, ExpCoeff):
home and adjacent mapunits and dividing this by the sum of all map units
and components. We have modified this approach so that each instance of a
component occurance is evaluated separately and assinged a weight and the
- max distance score for each component group is assigned to all component instances.
+ sum of distance scores for each component group is assigned to all component instances.
# --------------------------------------------------------------------
"""
-
- # Calculate distance score for each group
- mucompdata_pd["distance_score"] = mucompdata_pd.apply(
- lambda row: calculate_distance_score(row, ExpCoeff), axis=1
- )
-
- # Group by cokey and mukey and aggregate required values
+ # Group by component name and map unit to aggregate percentages
grouped_data = (
- mucompdata_pd.groupby(["cokey", "mukey"])
+ mucompdata_pd.groupby([comp_name_col, map_unit_col])
.agg(
- distance_score=("distance_score", "sum"),
- comppct=("comppct_r", "sum"),
- minDistance=("distance", "min"),
+ # Aggregate the specified component percentage column
+ aggregated_pct=(comp_pct_col, "sum"),
+ distance=(distance_col, "min"),
+ cokey_list=(comp_key_col, list),
)
.reset_index()
)
+ # Rename aggregated column to be consistent for the calculation function
+ grouped_data.rename(columns={"aggregated_pct": comp_pct_col}, inplace=True)
+
+ # Calculate a single distance score for each aggregated group
+ # Pass the correct component percentage column name to the calculation function
+ grouped_data["distance_score"] = grouped_data.apply(
+ lambda row: calculate_distance_score(row, ExpCoeff, comp_pct_col=comp_pct_col),
+ axis=1,
+ )
+
+ # Sum distance scores per component group (instead of taking max)
+ sum_scores_per_comp = grouped_data.groupby(comp_name_col)["distance_score"].sum().reset_index()
+ sum_scores_per_comp.rename(columns={"distance_score": "sum_distance_score"}, inplace=True)
+
+ # Merge sum scores back to grouped data
+ grouped_data = grouped_data.merge(sum_scores_per_comp, on=comp_name_col, how="left")
+
+ # Calculate conditional probabilities based on sum scores per component group
+ total_sum_score = sum_scores_per_comp["sum_distance_score"].sum()
+ if total_sum_score > 0:
+ sum_scores_per_comp["cond_prob"] = (
+ sum_scores_per_comp["sum_distance_score"] / total_sum_score
+ )
+ else:
+ sum_scores_per_comp["cond_prob"] = 0
+
+ # Merge conditional probabilities back to grouped data
+ grouped_data = grouped_data.merge(
+ sum_scores_per_comp[[comp_name_col, "cond_prob"]], on=comp_name_col, how="left"
+ )
- # Calculate conditional probabilities
- total_distance_score = grouped_data["distance_score"].sum()
- grouped_data["cond_prob"] = grouped_data["distance_score"] / total_distance_score
+ # Explode the dataframe back to the component key level
+ grouped_data = grouped_data.explode("cokey_list").rename(columns={"cokey_list": comp_key_col})
- # Merge dataframes on 'cokey'
+ # Merge the conditional probability back into the original dataframe
mucompdata_pd = mucompdata_pd.merge(
- grouped_data[["cokey", "cond_prob"]], on="cokey", how="left"
+ grouped_data[[comp_key_col, "cond_prob", "sum_distance_score", "distance_score"]],
+ on=comp_key_col,
+ how="left",
)
+ # Rename sum_distance_score to comp_distance_score for clarity
+ mucompdata_pd.rename(columns={"sum_distance_score": "comp_distance_score"}, inplace=True)
+
# Additional processing
- mucompdata_pd = mucompdata_pd.sort_values("distance_score", ascending=False)
+ mucompdata_pd = mucompdata_pd.sort_values(["cond_prob", comp_name_col], ascending=[False, True])
- mucompdata_pd = mucompdata_pd[~mucompdata_pd["compkind"].str.contains("Miscellaneous area")]
+ # Filter out miscellaneous areas if the flag is set and the column exists
+ if compkind_filter and comp_kind_col in mucompdata_pd.columns:
+ mucompdata_pd = mucompdata_pd[
+ ~mucompdata_pd[comp_kind_col].str.contains("Miscellaneous area", na=False)
+ ]
mucompdata_pd = mucompdata_pd.reset_index(drop=True)
# Create a list of component groups
- mucompdata_comp_grps = [g for _, g in mucompdata_pd.groupby(["compname"], sort=False)]
+ mucompdata_comp_grps = [g for _, g in mucompdata_pd.groupby([comp_name_col], sort=True)]
mucompdata_comp_grps = mucompdata_comp_grps[: min(12, len(mucompdata_comp_grps))]
- # Assign max within-group location-based score to all members of the group
+ # Assign group-level values to all members of the group
for group in mucompdata_comp_grps:
- group["distance_score"] = group["distance_score"].max()
- group = group.sort_values("distance").reset_index(drop=True)
- group["min_dist"] = group["distance"].iloc[0]
+ # distance_score is already set to sum value for the group
+ group = group.sort_values(distance_col).reset_index(drop=True)
+ group["min_dist"] = group[distance_col].iloc[0]
# Concatenate the list of dataframes
- mucompdata_pd = pd.concat(mucompdata_comp_grps).reset_index(drop=True)
+ if mucompdata_comp_grps:
+ mucompdata_pd = pd.concat(mucompdata_comp_grps).reset_index(drop=True)
+ else:
+ mucompdata_pd = pd.DataFrame(columns=mucompdata_pd.columns)
return mucompdata_pd
@@ -2068,7 +2154,7 @@ def slice_and_aggregate_soil_data(df):
missing_row = {col: np.nan for col in result_df.columns}
missing_row["hzdept_r"] = 30
missing_row["hzdepb_r"] = 100
- result_df = result_df.append(missing_row, ignore_index=True)
+ result_df = pd.concat([result_df, pd.DataFrame([missing_row])], ignore_index=True)
return result_df