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块状相和团簇中模型卤化锂的晶体结构。

Crystal structures of model lithium halides in bulk phase and in clusters.

机构信息

Department of Chemistry, University of British Columbia, Vancouver, British Columbia V6T 1Z1, Canada.

出版信息

J Chem Phys. 2017 Apr 21;146(15):154501. doi: 10.1063/1.4979926.

Abstract

We employ lattice energy calculations and molecular dynamics simulations to compare the stability of wurtzite and rock salt crystal structures of four lithium halides (LiF, LiCl, LiBr, and LiI) modeled using the Tosi-Fumi and Joung-Cheatham potentials, which are models frequently used in simulation studies. Both infinite crystals and finite clusters are considered. For the Tosi-Fumi model, we find that all four salts prefer the wurtzite structure both at 0 K and at finite temperatures, in disagreement with experiments, where rock salt is the stable structure and wurtzite exists as a metastable state. For Joung-Cheatham potentials, rock salt is more stable for LiF and LiCl, but the wurtzite structure is preferred by LiBr and LiI. It is clear that the available lithium halide force fields need improvement to bring them into better accord with the experiment. Finite-size clusters that are more stable as rock salt in the bulk phase tend to solidify as small rock salt crystals. However, small clusters of salts that prefer the wurtzite structure as bulk crystals tend to form structures that have hexagonal motifs, but are not finite-size wurtzite crystals. We show that small wurtzite structures are unstable due to the presence of a dipole and rearrange into more stable, size-dependent structures. We also show that entropic contributions can act in favor of the wurtzite structure at higher temperatures. The possible relevance of our results for simulation studies of crystal nucleation from melts and/or aqueous solutions is discussed.

摘要

我们采用晶格能计算和分子动力学模拟来比较四方相和岩盐相晶体结构在使用 Tosi-Fumi 和 Joung-Cheatham 势的四种锂卤化物(LiF、LiCl、LiBr 和 LiI)中的稳定性,这两种势是模拟研究中常用的模型。我们同时考虑了无限晶体和有限团簇。对于 Tosi-Fumi 模型,我们发现所有四种盐在 0 K 和有限温度下都优先采用纤锌矿结构,这与实验结果不符,实验中岩盐是稳定结构,纤锌矿是亚稳相。对于 Joung-Cheatham 势,LiF 和 LiCl 更倾向于岩盐相,而 LiBr 和 LiI 则倾向于纤锌矿相。显然,现有的锂卤化物力场需要改进,以使其与实验结果更好地吻合。在体相中更稳定的岩盐相的有限团簇往往会凝固成小的岩盐晶体。然而,作为体相晶体更倾向于纤锌矿结构的小盐团簇往往会形成具有六方图案的结构,但不是有限尺寸的纤锌矿晶体。我们表明,由于存在偶极子,小纤锌矿结构是不稳定的,并重新排列成更稳定的、依赖于尺寸的结构。我们还表明,在较高温度下,熵贡献可以有利于纤锌矿结构。我们的结果对于熔体和/或水溶液中晶体成核的模拟研究可能具有相关性。

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