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Analysis of dynamic shear bands in an FCC single crystal
Institution:1. Department of Science and Technology, Iwaki Meisei University, 5-5-1 Chuodai-Iino, Iwaki 970-8551, Japan;2. Cooperative Research Center, Iwaki Meisei University, 5-5-1 Chuodai-Iino, Iwaki 970-8551, Japan;1. Defence Metallurgical Research Laboratory, Hyderabad, India;2. Department of Materials Engineering, Indian Institute of Science Bangalore, India;1. ArqueoUIB Research Group, Department of Historical Sciences and Theory of Art, University of the Balearic Islands, Carretera de Valldemossa Km 7,5, CP07122 Palma, Mallorca, Spain;2. SERP, Seminary of Prehistoric Studies and Research Department of History and Archaeology, Section Prehistory and Archaeology, University of Barcelona, C/Montalegre 6, 08001 Barcelona, Spain;3. Archéozoologies, Archéobotanique: Sociétés, Pratiques et Environnements, UMR 7209 of the CNRS - Muséum National d''Histoire Naturelle and Sorbonne Universités, 55 Rue Buffon, 75005 Paris, France;4. School of Earth and Ocean Sciences, Cardiff University, United Kingdom;5. Department of Biology, University of the Balearic Islands, Carretera de Valldemossa Km 7,5, CP07122 Palma, Mallorca, Spain;6. Université de Limoges, Géolab, 39E rue Camille Guérin, F-87036 Limoges, France;7. CNRS, Géolab - Laboratoire de Géographie Physique et Environnementale, F-87036 Limoges, France
Abstract:We study plane strain dynamic thermomechanical deformations of an fcc single crystal compressed along the crystallographic direction 010] at an average strain rate of 1000 sec−1. Two cases are studied; one in which the plane of deformation is parallel tothe plane (001) of the single crystal, and another one with deformation occuring in the plane (101̄) of the single crystal. In each case, the 12 slip systems are aligned symmetrically about the two centroidal axes. We assume that the elastic and plastic deformations of the crystal are symmetrical about these two axes. The crystal material is presumed to exhibit strain hardening, strain-rate hardening, and thermal softening. A simple combined isotropic-kinematic hardening expression for the critical resolved shear stress, proposed by Weng, is modified to account for the affine thermal softening of the material. When the deformation is in the plane (001) of the single crystal, four slip systems (111)11̄0], (111̄)11̄0], (11̄;1̄;)110], and (11̄1)110] are active in the sense that significant plastic deformations occur along these slip systems. However, when the plane of deformation is parallel to the plane (101̄;) of the single crystal, slip systems (11̄;1)110], (11̄1)011], (111)11̄0], and (111)01̄1] are more active than the other eight slip systems. At an average strain of 0.0108, the maximum angle of rotation of a slip system within a shear band, about an axis perpendicular to the plane of deformation, is found to be 20.3° in the former case, and 22.9° in the latter.
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