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基于增强采样分子动力学模拟的液态水与六方冰的相平衡

Phase equilibrium of liquid water and hexagonal ice from enhanced sampling molecular dynamics simulations.

作者信息

Piaggi Pablo M, Car Roberto

机构信息

Department of Chemistry, Princeton University, Princeton, New Jersey 08544, USA.

Department of Chemistry and Department of Physics, Princeton University, Princeton, New Jersey 08544, USA.

出版信息

J Chem Phys. 2020 May 29;152(20):204116. doi: 10.1063/5.0011140.

Abstract

We study the phase equilibrium between liquid water and ice Ih modeled by the TIP4P/Ice interatomic potential using enhanced sampling molecular dynamics simulations. Our approach is based on the calculation of ice Ih-liquid free energy differences from simulations that visit reversibly both phases. The reversible interconversion is achieved by introducing a static bias potential as a function of an order parameter. The order parameter was tailored to crystallize the hexagonal diamond structure of oxygen in ice Ih. We analyze the effect of the system size on the ice Ih-liquid free energy differences, and we obtain a melting temperature of 270 K in the thermodynamic limit. This result is in agreement with estimates from thermodynamic integration (272 K) and coexistence simulations (270 K). Since the order parameter does not include information about the coordinates of the protons, the spontaneously formed solid configurations contain proton disorder as expected for ice Ih.

摘要

我们使用增强采样分子动力学模拟,研究了由TIP4P/Ice原子间势建模的液态水和冰Ih之间的相平衡。我们的方法基于从可逆访问两个相的模拟中计算冰Ih - 液体的自由能差。通过引入作为序参量函数的静态偏置势来实现可逆相互转化。该序参量经过调整,以使冰Ih中氧的六方金刚石结构结晶。我们分析了系统尺寸对冰Ih - 液体自由能差的影响,并在热力学极限下获得了270 K的熔化温度。该结果与热力学积分(272 K)和共存模拟(270 K)的估计值一致。由于序参量不包含有关质子坐标的信息,自发形成的固体构型包含冰Ih预期的质子无序。

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