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Including latent hardening of multiple slip planes allowed the model to explain the decrease in flow stress when changing from equal-biaxial to uniaxial deformation.
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A model is proposed to analyze the interaction between dislocations gliding in the multiple {1 0 0}〈0 1 1〉 slip planes and the interaction of dislocations with the tetragonal variants, taking into account the peculiar microstructure of the material.
Hereinto, alloying elements occupy preferable Ti sites near slip planes.
This defines the slip planes as (001) and (101).
The (111) slip plane is chosen as a study case because symmetries of the four independent slip planes exist.
Dimon won't let the multiple slip without fighting.
The model is used to predict the shear strength of Cr2O3 along three relevant slip planes and slip directions.
These independent slip planes belong to the {111} crystal planes family.
The results show that, in accordance with experimental observations, there is a clear preference to chain slip over transverse slip for all considered slip planes.
These crystals are subjected to multiple slip deformation.
Additionally, regions in which slip steps resulted primarily from a single slip plane prior to hydrogen charging exhibited slip steps from two different slip planes after hydrogen charging.
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