Determination of phase diagrams via computer simulation: methodology and applications to water, electrolytes and proteins

相图 冰Ih 统计物理学 固溶体 相(物质) 计算 水模型 Crystal(编程语言) 热力学 硬球 材料科学 物理 化学 分子动力学 计算机科学 分子 计算化学 算法 量子力学 冶金 程序设计语言
作者
Carlos Vega,Eduardo Sanz,J. L. F. Abascal,Eva G. Noya
出处
期刊:Journal of Physics: Condensed Matter [IOP Publishing]
卷期号:20 (15): 153101-153101 被引量:199
标识
DOI:10.1088/0953-8984/20/15/153101
摘要

In this review we focus on the determination of phase diagrams by computer simulation, with particular attention to the fluid–solid and solid–solid equilibria. The methodology to compute the free energy of solid phases will be discussed. In particular, the Einstein crystal and Einstein molecule methodologies are described in a comprehensive way. It is shown that both methodologies yield the same free energies and that free energies of solid phases present noticeable finite size effects. In fact, this is the case for hard spheres in the solid phase. Finite size corrections can be introduced, although in an approximate way, to correct for the dependence of the free energy on the size of the system. The computation of free energies of solid phases can be extended to molecular fluids. The procedure to compute free energies of solid phases of water (ices) will be described in detail. The free energies of ices Ih, II, III, IV, V, VI, VII, VIII, IX, XI and XII will be presented for the SPC/E and TIP4P models of water. Initial coexistence points leading to the determination of the phase diagram of water for these two models will be provided. Other methods to estimate the melting point of a solid, such as the direct fluid–solid coexistence or simulations of the free surface of the solid, will be discussed. It will be shown that the melting points of ice Ih for several water models, obtained from free energy calculations, direct coexistence simulations and free surface simulations agree within their statistical uncertainty. Phase diagram calculations can indeed help to improve potential models of molecular fluids. For instance, for water, the potential model TIP4P/2005 can be regarded as an improved version of TIP4P. Here we will review some recent work on the phase diagram of the simplest ionic model, the restricted primitive model. Although originally devised to describe ionic liquids, the model is becoming quite popular to describe the behavior of charged colloids. Moreover, the possibility of obtaining fluid–solid equilibria for simple protein models will be discussed. In these primitive models, the protein is described by a spherical potential with certain anisotropic bonding sites (patchy sites).

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