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Critical assessment of classical potentials for MgSiO _3 perovskite with application to thermal conductivity calculations

机译:对MgSiO _3钙钛矿经典势能的临界评估及其在热导率计算中的应用

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摘要

Atomistic simulations using classical empirical potentials are an invaluable tool for studying minerals in lower-mantle conditions. Here we systematically survey literature potentials for MgSiO _3 perovskite. The value of the present work is two-fold: (i) a systematic data set for a large number of potentials is determined, reproducing previous results where they exist and filling in gaps where they do not, and (ii) the first predictions using these potentials for the thermal-transport properties critical to geothermal models is provided. We focus particularly on the thermal expansion and the thermal-transport properties, both of which probe the anharmonic structure of the potential. Simple two-body potentials with the partially-ionic charges are found to be the most successful representation of MgSiO _3 perovskite properties. The addition of a shell model or many-body interactions does not lead to any systematic improvement.
机译:使用经典经验势能进行的原子模拟是研究下地幔条件下矿物的宝贵工具。在这里,我们系统地调查了MgSiO _3钙钛矿的文学潜力。当前工作的价值是双重的:(i)确定了大量潜力的系统数据集,在存在这些潜力的情况下重现以前的结果,在没有潜力的情况下填补空白,以及(ii)使用提供了对地热模型至关重要的热传输特性的这些潜力。我们特别关注热膨胀和热传输特性,这两者都探究了电势的非谐结构。发现具有部分离子电荷的简单两体势是MgSiO _3钙钛矿性质的最成功表示。壳模型的添加或多体交互作用不会导致任何系统的改进。

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