Dept. Química-Física I, Facultad de Ciencias Químicas, Universidad Complutense de Madrid, 28040 Madrid, Spain.
J Chem Phys. 2010 Aug 14;133(6):064507. doi: 10.1063/1.3466751.
Molecular dynamics simulations have been performed to estimate the three-phase (solid hydrate-liquid water-gaseous methane) coexistence line for the water-methane binary mixture. The temperature at which the three phases are in equilibrium was determined for three different pressures, namely, 40, 100, and 400 bar by using direct coexistence simulations. In the simulations water was described by using either TIP4P, TIP4P/2005, or TIP4P/Ice models and methane was described as simple Lennard-Jones interaction site. Lorentz-Berthelot combining rules were used to obtain the parameters of the cross interactions. For the TIP4P/2005 model positive deviations from the energetic Lorentz-Berthelot rule were also considered to indirectly account for the polarization of methane when introduced in liquid water. To locate the three-phase coexistence point, two different global compositions were used, which yielded (to within statistical uncertainty) the same predictions for the three-phase coexistence temperatures, although with a somewhat different time evolution. The three-phase coexistence temperatures obtained at different pressures when using the TIP4P/Ice model of water were in agreement with the experimental results. The main reason for this is that the TIP4P/Ice model reproduces the melting point of ice I(h).
已经进行了分子动力学模拟,以估计水-甲烷二元混合物的三相(固体水合物-液态水-气态甲烷)共存线。通过直接共存模拟,确定了在三个不同压力(分别为 40、100 和 400 巴)下三相处于平衡的温度。在模拟中,水分别用 TIP4P、TIP4P/2005 或 TIP4P/Ice 模型描述,甲烷用简单的 Lennard-Jones 相互作用位点描述。使用 Lorentz-Berthelot 组合规则获得交叉相互作用的参数。对于 TIP4P/2005 模型,还考虑了从能量 Lorentz-Berthelot 规则的正偏差,以间接说明甲烷在引入液态水时的极化。为了定位三相共存点,使用了两种不同的全局组成,它们对三相共存温度的预测(在统计不确定性范围内)相同,尽管时间演化略有不同。当使用 TIP4P/Ice 模型的水时,在不同压力下获得的三相共存温度与实验结果一致。主要原因是 TIP4P/Ice 模型再现了冰 I(h)的熔点。