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理解水中模拟的电冷冻现象。

Understanding electrofreezing in water simulations.

作者信息

Yan J Y, Overduin S D, Patey G N

机构信息

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

出版信息

J Chem Phys. 2014 Aug 21;141(7):074501. doi: 10.1063/1.4892586.

Abstract

Molecular dynamics simulations are used to investigate why external electric fields promote the freezing of liquid water models. It is shown that the melting point of water at a pressure of 1 bar increases significantly when water is polarized by a uniform field. Fields of 1 V/nm and 2 V/nm increase the melting point by 24 K and 44 K, respectively. The increased melting point is mainly due to the favorable interaction of near perfectly polarized cubic ice with the applied field. For a fixed temperature, we demonstrate that the size of the critical ice nucleus decreases with field strength, mostly because the melting point, and hence the true degree of supercooling, is increasing with field. On simulation timescales, ice nucleation is observed at ∼40 K below the field-dependent melting point, independent of the particular value of the field applied. Indeed, we find that even quite highly polarized liquid water retains the characteristic local structures, and the related anomalous properties of water. Our results are obviously relevant to the mechanism of heterogeneous ice nucleation by local surface fields. Local fields will effectively increase the degree of supercooling of locally polarized liquid, decreasing the size of the critical nucleus in the region influenced by the field, hence facilitating ice nucleation.

摘要

分子动力学模拟用于研究外部电场为何会促进液态水模型的冻结。结果表明,当水受到均匀电场极化时,在1巴压力下的水熔点会显著升高。1 V/nm和2 V/nm的电场分别使熔点升高24 K和44 K。熔点升高主要是由于近乎完美极化的立方冰与外加电场之间的有利相互作用。对于固定温度,我们证明临界冰核的尺寸随场强减小,主要是因为熔点以及因此真正的过冷度随场强增加。在模拟时间尺度上,在比场依赖熔点低约40 K处观察到冰核形成,与所施加电场的具体值无关。实际上,我们发现即使是极化程度相当高的液态水仍保留了水的特征局部结构及相关异常性质。我们的结果显然与局部表面场引发的异质冰核形成机制相关。局部场将有效增加局部极化液体的过冷度,减小受场影响区域内临界核的尺寸,从而促进冰核形成。

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