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Description
I'm trying to comprehend the following heat transport tutorial based on MODFLOW-2005 and MT3DMS: http://gmstutorials-10.1.aquaveo.com/MT3DMS-HeatTransport.pdf ¹
Which also is available on YouTube.
The tutorial and video are created for GMS but I like to use Flopy (I don't have GMS).
The model is adapted from example 9 of the 1999 MT3DMS report (see jupyter notebook):
Basically the area contains a low K-zone (purple area in right chart). There is an injection well (green point in right chart) and an extraction well (blue point in right chart). And there is a slope in head from 250 meter at top to 240 meter at bottom (see left chart)
After lots of reading and trying with Flopy model code I cannot get the heat transport to produce similar results to the tutorial. I started with using MT3D-USGS, but I get similar behaviour using the MT3DMS model.
I always end up with the same or almost the same result, that looks like the following:

The flowing pattern seems to be in line with the tutorial. First a bit to the north and then over time around the low K-zone towards the extraction well.
But the temperature values are around 0 (and even below 0), where the units are Kelvin! Thats very cold flowing water.. I was hoping to see heat transport values close to the injection temperature of 298 Kelvin.
I would greatly appreciate if someone can have a look what I must be doing wrong. The reproducible notebook is located here:
At the same time this issue also aims to create some documentation for doing heat transport using Flopy, since this information seems to be scarce on the internet (I can't find it).
¹ The GMS MODFLOW model can be found at: http://gmstutorials-10.1.aquaveo.com/heat_transport.zip
