Variant pairing question #26
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Hi Frank, Just a quick question regarding your comment in our last discussion: I saw some authors also did variants pairing outside of a packet (e.g., V1-V16). Would we be able to do that with Thanks Frank and have a nice day. |
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Replies: 4 comments 7 replies
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Hi Linh, have a look at Table 2 in the paper Morito, S., Tanaka, H., Konishi, R., Furuhara, T., & Maki, T. (2003). The morphology and crystallography of lath martensite in Fe-C alloys. Acta Materialia, 51, 1789–1799. https://doi.org/10.1016/j.actamat.2006.07.009
Here you have listed all 24 variants of the Kurdjumov-Sachs (K-S) orientation relationship. You will see that groups of 6 variants are assigned to a packet (1-6, 7-12, 13-18 and 19-24). A packet is the collection of variants that form on a specific habit plane. Within each packet there are 6 different combinations of how the parallel crystal directions can be paired. This is illustrated in Figure 1 of the paper. The misorientations between the variants within one packet are the same for each group of 6 variants. Let me demonstrate this: Considering you have defined the K-S orientation relationship as shown in Example 1, you can check the misorientation of the first 6 variants with the 1st variant:
Doing the same for variants 7 to 12 with respect to variant 7 gives the same misorientations:
This means that the boundaries that the variants form within each packet are equivalent, they "share the same characteristics". Therefore we translate all 24 variants in plotMap_variantPairs to their equivalent variants 1 to 6 and check the fraction of grain boundaries between the different variants. This type of analysis is described here: Morito, S., Pham, A. H., Hayashi, T., & Ohba, T. (2015). Block boundary analyses to identify martensite and bainite. Materials Today: Proceedings, 2, S913–S916. https://doi.If you really want to do this, you could filter your dataset to only get variants of a certain packet and limit the naorg/10.1016/j.matpr.2015.07.430
I cannot see the point in doing a variant pairing analysis for all 24 variants, it does not give you any additional information. Best wishes |
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Because the boundary misorientations are the same, 60 degrees around [011] as stated in the above referenced paper. |
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Hi Frank, I realized that there are some other pairings with characteristics similar to the typical pairing with V1, the same as what Morito et al. described in Table 3. For example, V2/V5 & V3/V6 are similar to V1/V4, or V3/V2 & V5/V4 are similar to V1-V6. In the Morito et al. paper: Morito, S., Tanaka, H., Konishi, R., Furuhara, T., & Maki, T. (2003). The morphology and crystallography of lath martensite in Fe-C alloys. Acta Materialia, 51, 1789–1799. https://doi.org/10.1016/j.actamat.2006.07.009 Thanks Frank. |
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It's a great honor to communicate with you. If possible, can you give the statistics of the boundary length ratio of the remaining variant pairs (16 kinds, Figure 5 in DOI: 10.1016/j.actamat.2011. 12.018)? I would appreciate it if you could make corresponding codes. |
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Hi Linh,
have a look at Table 2 in the paper
Here you have listed all 24 variants of the Kurdjumov-Sachs (K-S) orientation relationship. You will see that groups of 6 variants are assigned to a packet (1-6, 7-12, 13-18 and 19-24). A packet is the collection of variants that form on a specific habit plane. Within each packet there are 6 different combinations of how the parallel crystal directions can be paired. This is illustrated in Figure 1 of the paper. The misorientation…