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• W2039478839 startingPage "613" @default.
• W2039478839 abstract "Abstract In polycrystalline material, minerals with pronounced plastic anisotropy may experience inhomogeneous deformation and significant mechanical interaction between neighboring crystals. To study the effect of crystal interaction on preferred orientation, pure shear of a polycrystalline material with identical, orthogonal slip systems was modeled two-dimensionally by the finite-element method. Such a material is non-ductile in the formal von Mises sense because it lacks five independent slip systems. As a result, each crystal has highly anisotropic strength. Because a homogeneous, irrotational strain history in a two-dimensional crystal with identical, orthogonal slip systems does not cause lattice rotation, rotation caused by crystal interaction is readily observed. In the finite-element models, slip planes rotate toward a preferred orientation parallel to maximum shear stress (45° to shortening and extension directions). Mechanical interaction between neighboring crystals produces this preferred orientation by rigid-body rotation of crystals or parts of crystals not favorably oriented for slip." @default.
• W2039478839 created "2016-06-24" @default.
• W2039478839 creator A5041584990 @default.
• W2039478839 date "1989-01-01" @default.
• W2039478839 modified "2023-09-24" @default.
• W2039478839 title "Crystal rotation by mechanical interaction between plastically anisotropic crystals" @default.
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• W2039478839 doi "https://doi.org/10.1016/0191-8141(89)90092-8" @default.
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