期刊
COMPUTATIONAL CONDENSED MATTER
卷 27, 期 -, 页码 -出版社
ELSEVIER
DOI: 10.1016/j.cocom.2021.e00560
关键词
Uniaxial compression; Molecular dynamics; Phase transition; Plasticity; Iron; Lattice defects; Twinning; Mono- and poly-crystal
Using Molecular Dynamics computations, a shear stiffening effect was found in defect-free iron single crystals, shifting the structural phase transition to higher pressure levels. Plasticity in iron samples under compression was studied, revealing an interplay between grain size, point defects, and phase transition behavior influenced by defect density. In polycrystalline iron, the transition to phase transition at lower pressures is attributed to complex interactions between intra-grain twinning and dislocation activities.
Using Molecular Dynamics (MD) computations we have reported recently a shear stiffening (hardening-like) effect in [001]-oriented defect-free iron single crystal. This effect makes shift the structural phase transition to a particularly high pressure level under ramp compression, but not under shock compression, so that the question arises about the essential role of the compression path and wave evolution in the solid state response including phase transition. Here, plasticity and phase transition are studied for iron samples under non-equilibrium uni-axial compression. Our focus is put on the effects of grain size and point defects such as atoms vacancy. Consistently with our previous results, it is found that, after yielding via twinning, both defect-free and defective iron single crystals exhibit a hardening-like effect while the twins progressively recede upon further compression and no dislocations activity is detected. This leads to mounting of the deviatoric stress. Yet, the transition onset pressure shift and temperature behavior are found to be defect-density dependent. Considering polycrystalline lattice, plasticity consists in complex interplay of intra-grain twinning and dislocation activities from grain boundaries. The elastic stiffening is attenuated now as compared to single crystal so that the phase transition is found to occur at much lower pressure in polycrystalline iron.
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