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On the Accuracy of van der Waals Inclusive Density-Functional Theory Exchange-Correlation Functionals for Ice at Ambient and High Pressures

机译:关于环境和高压下冰的范德华包容密度 - 功能理论交换相关函数的准确性

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摘要

Density-functional theory (DFT) has been widely used to study water and ice for at least 20 years. However, the reliability of different DFT exchange-correlation (xc) functionals for water remains a matter of considerable debate. This is particularly true in light of the recent development of DFT based methods that account for van der Waals (vdW) dispersion forces. Here, we report a detailed study with several xc functionals (semi-local, hybrid, and vdW inclusive approaches) on ice Ih and six proton ordered phases of ice. Consistent with our previous study [Phys. Rev. Lett. 107, 185701 (2011)] which showed that vdW forces become increasingly important at high pressures, we find here that all vdW inclusive methods considered improve the relative energies and transition pressures of the high-pressure ice phases compared to those obtained with semi-local or hybrid xc functionals. However, we also find that significant discrepancies between experiment and the vdW inclusive approaches remain in the cohesive properties of the various phases, causing certain phases to be absent from the phase diagram. Therefore, room for improvement in the description of water at ambient and high pressures remains and we suggest that because of the stern test the high pressure ice phases pose they should be used in future benchmark studies of simulation methods for water.
机译:密度泛函理论(DFT)已被广泛用于研究水和冰至少20年了。但是,对于水而言,不同的DFT交换相关(xc)功能的可靠性仍然存在很多争议。鉴于考虑到范德华(vdW)分散力的基于DFT的方法的最新发展,尤其如此。在这里,我们报告了关于冰Ih和六个质子有序相冰的几种xc功能(半局部,混合和vdW包含方法)的详细研究。与我们之前的研究一致[Phys。牧师107,185701(2011)],这表明vdW力在高压下变得越来越重要,我们在这里发现,与半局部法相比,所有考虑的vdW包容性方法都可以改善高压冰相的相对能量和转变压力。或混合xc功能。但是,我们还发现,实验与包含vdW的方法之间的重大差异仍然存在于各个阶段的内聚性中,从而导致相图中缺少某些阶段。因此,在常压和高压下对水的描述仍有改进的余地,我们建议,由于进行了船尾测试,高压冰相的姿态在将来的水模拟方法基准研究中应使用。

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