Hi
a few answers.
wrt 1) No, Taylor adn VPSC models are not the same. Taylor assumes iso-strain. Depending on the situations results may be still similar or significantly different.
wrt 2) I'd say any advanges/disadvantages of one over the otehr depend on the assumptions you are making and what exactly you want to model.
wrt 3) Yes, just write the orientations for each step i to a variable e.g. o_out(:,i)=ori. Than you do whatever you like with those later on.
wrt 4) Maybe you need to specify a little more what you mean here. All in one step? Or the average Tayler factor for each orientation averaged over all steps? If the latter, just save all the Taylor factors to a n-by-i variable (similar to the orientations) and calculate the mean afterwards.
wrt 5) Depending on the definition of strain (tension is positive for many engineers, negative for geologists), it looks like you are pulling or pushing in the Z-direction.
Hope that helps.
Cheers,
Rüdiger
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Subject: {MTEX} Texture evolution during plastic deformation?
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