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首页> 外文期刊>The American mineralogist >Modeling the plastic deformation of olivine by dislocation dynamics simulations
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Modeling the plastic deformation of olivine by dislocation dynamics simulations

机译:通过位错动力学模拟对橄榄石的塑性变形进行建模

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摘要

This work addresses the modeling of dislocation interactions and dynamics in olivine. A 3D dislocation dynamics (DD) simulation developed for cubic and hexagonal metals is adapted to the orthorhombic symmetry of this mineral. Dislocation core effects and mobilities are introduced through available models or phenomenological laws and fitted based on available experimental results on single crystals. The stress dependencies of the mobilities of [100] and [001] dislocations are emphasized. Dislocations interactions are studied through a simple elastic analysis and further using a more realistic approach based on DID simulations. It is shown that no junction formation results from the interaction between [100] and [001] dislocations. The collinear interaction is thus the only potential mechanism for forest hardening although its efficiency is significantly reduced by lattice friction on screw dislocations, which decreases the probability for dislocation reactions. The Taylor relationship is often used to model the dependence of the flow stress with the dislocation density. In the presence of a strong lattice friction, Taylor strengthening is shown here to be only a minor contribution to the flow stress and should not be responsible for it.
机译:这项工作解决了橄榄石中位错相互作用和动力学的建模。针对立方和六方金属开发的3D位错动力学(DD)模拟适用于该矿物的斜方对称性。通过可用的模型或现象学法则介绍了位错核心效应和迁移率,并根据对单晶的可用实验结果进行了拟合。强调了[100]和[001]位错迁移率的应力依赖性。通过简单的弹性分析,并进一步使用基于DID模拟的更现实的方法,研究位错相互作用。结果表明,[100]和[001]位错之间的相互作用不会导致结形成。因此,共线相互作用是森林硬化的唯一潜在机制,尽管其效率由于螺旋位错上的晶格摩擦而大大降低,这降低了位错反应的可能性。泰勒关系通常用于模拟流应力与位错密度之间的关系。在存在强烈的晶格摩擦的情况下,此处显示的泰勒强度只是对流变应力的很小贡献,不应对此负责。

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