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Modeling the creep properties of olivine by 2.5-dimensional dislocation dynamics simulations

机译:通过2.5维位错动力学模拟对橄榄石的蠕变特性进行建模

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摘要

In this work we performed 2.5-dimensional (2.5D) dislocation dynamics simulations coupling climb with the glide dislocation motion to model the creep behavior of olivine, one of the main component of the Earth's upper mantle. In particular, we present an application of this method to determine the creep strain rate in a material with high lattice resistance, such as olivine. We show that by including the climb mechanism we reach steady state creep conditions. Moreover, we find that a creep power law with a stress exponent close to 3 can be extracted from our simulations and we provide a model based on Orowan's law to predict the creep strain rates in the high temperature and low stress regime. The model presented is relevant to describe the plastic flow of olivine in the Earth's mantle deformation conditions and can be useful to derive the high temperature creep behavior of other materials.
机译:在这项工作中,我们进行了2.5维(2.5D)的位错动力学模拟,将爬升与滑动位错运动耦合在一起,以模拟橄榄石的蠕变行为,橄榄石是地球上地幔的主要组成部分之一。特别是,我们介绍了此方法的应用,以确定具有高晶格电阻的材料(例如橄榄石)的蠕变应变率。我们表明,通过包括爬升机制,我们可以达到稳态蠕变条件。此外,我们发现可以从我们的仿真中提取应力指数接近3的蠕变幂定律,并提供基于Orowan定律的模型来预测高温和低应力状态下的蠕变应变率。提出的模型与描述在地幔变形条件下橄榄石的塑性流动有关,可用于推导其他材料的高温蠕变行为。

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