论文标题

TIP4P/冰水模型的自扩散和剪切粘度

Self-diffusion and shear viscosity for the TIP4P/Ice water model

论文作者

Baran, Łukasz, Rżysko, Wojciech, MacDowell, Luis G.

论文摘要

由于对水性质的兴趣不断增加,已经提出了许多分子间力场来描述水的行为。不幸的是,液态水的好模型通常无法同时提供冰的准确熔点。因此,TIP4P/ICE模型是在靶向熔点时开发的,并已成为模拟冰的首选选择。不幸的是,其在液态状态下的动态特性的可用数据很少。因此,我们演示了一系列旨在在各种热力学条件下计算TIP4P/ICE模型的传输系数的模拟,从$ T = 245 $ K到温度的$ T = 350 $ K,从$ P = 0 $到$ P = 500 $ P = 500 $ MPA的压力。我们发现,自扩散(剪切粘度)的值比TIP4P/2005和实验表现出更小的(增加)值。但是,像在相应的状态图中相对于三点温度的温度重新缩放温度,我们发现TIP4P/ICE与TIP4P/2005和实验相比非常好。这样的观察结果使我们能够推断出,尽管此处检查的这两个模型的原始目的不同,但人们可以从有关TIP4P/2005模型的传输系数行为的大量报告中受益,并按照本文中描述的例行使用。

With an ever-increasing interest in water properties, many intermolecular force fields have been proposed to describe the behavior of water. Unfortunately, good models for liquid water usually cannot provide simultaneously an accurate melting point for ice. For this reason, the TIP4P/Ice model was developed at targeting the melting point, and has become the preferred choice for simulating ice at coexistence. Unfortunately, available data for its dynamic properties in the liquid state are scarce. Therefore, we demonstrate a series of simulations aimed at the calculation of transport coefficients for the TIP4P/Ice model over a large range of thermodynamic conditions, ranging from $T=245$ K to $T=350$ K for the temperature and from $p=0$ to $p=500$ MPa for the pressure. We have found that the self-diffusion (shear viscosity) exhibits smaller (increased) values than TIP4P/2005 and experiments. However, rescaling the temperature with respect to the triple point temperature as in a corresponding states plot we find TIP4P/Ice compares very well with TIP4P/2005 and to experiment. Such observations allow us to infer that despite the different original purposes of these two models examined here, one can benefit from a vast number of reports regarding the behavior of transport coefficients for the TIP4P/2005 model and utilize them following the routine described in this paper.

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