CRYSTALLOGRAPHIC PREFERRD ORIENTATION
Since during plastic deformation of a crystal the CRRS controls the
movement of dislocations, grains which are well oriented for slip on a
particular slip system will in principal be able to deform more easily
than those whose slip system orientations result in low resolved shear
stresses. Fig after Urai and Jessel shows a numerical simulation of
deformation in a polycrystal with only one slip system, notice how in the
the three coloured grains have undergone virtually no deformation (yellow)
a lot of deformation (orange) and a lot of deformation with internal
kinking as well (green). The short lines within grains show the local slip
system orientation.
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