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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:关于范德华包容密度 - 函数理论的准确性   环境和高压冰的交换相关函数

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摘要

Density-functional theory (DFT) has been widely used to study water and icefor at least 20 years. However, the reliability of different DFTexchange-correlation (xc) functionals for water remains a matter ofconsiderable debate. This is particularly true in light of the recentdevelopment 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 protonordered phases of ice. Consistent with our previous study [Phys. Rev. Lett.107, 185701 (2011)] which showed that vdW forces become increasingly importantat high pressures, we find here that all vdW inclusive methods consideredimprove the relative energies and transition pressures of the high-pressure icephases compared to those obtained with semi-local or hybrid xc functionals.However, we also find that significant discrepancies between experiment and thevdW inclusive approaches remain in the cohesive properties of the variousphases, causing certain phases to be absent from the phase diagram. Therefore,room for improvement in the description of water at ambient and high pressuresremains and we suggest that because of the stern test the high pressure icephases pose they should be used in future benchmark studies of simulationmethods 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。然而,水的不同DFT交换相关(xc)功能的可靠性仍然值得商debate。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和冰的六个质子有序相的几种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。 Rev. Lett.107,185701(2011)]指出vdW力在高压下变得越来越重要,我们发现在这里,所有vdW包含在内的方法与半冰相比获得了改善的高压冰相的相对能量和转变压力。但是,我们还发现,实验和vdW包含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,由于进行了船尾试验,高压冰相的姿势使它们应用于未来水模拟方法的基准研究中。

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