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负压下水的相图:虚拟冰

The phase diagram of water at negative pressures: virtual ices.

作者信息

Conde M M, Vega C, Tribello G A, Slater B

机构信息

Departamento de Quimica Fisica, Facultad de Ciencias Quimicas, Universidad Complutense, 28040 Madrid, Spain.

出版信息

J Chem Phys. 2009 Jul 21;131(3):034510. doi: 10.1063/1.3182727.

Abstract

The phase diagram of water at negative pressures as obtained from computer simulations for two models of water, TIP4P/2005 and TIP5P is presented. Several solid structures with lower densities than ice Ih, so-called virtual ices, were considered as possible candidates to occupy the negative pressure region of the phase diagram of water. In particular the empty hydrate structures sI, sII, and sH and another, recently proposed, low-density ice structure. The relative stabilities of these structures at 0 K was determined using empirical water potentials and density functional theory calculations. By performing free energy calculations and Gibbs-Duhem integration the phase diagram of TIP4P/2005 was determined at negative pressures. The empty hydrates sII and sH appear to be the stable solid phases of water at negative pressures. The phase boundary between ice Ih and sII clathrate occurs at moderate negative pressures, while at large negative pressures sH becomes the most stable phase. This behavior is in reasonable agreement with what is observed in density functional theory calculations.

摘要

给出了通过计算机模拟得到的两种水模型(TIP4P/2005和TIP5P)在负压下的水相图。几种密度低于冰Ih的固体结构,即所谓的虚拟冰,被认为是占据水相图负压区域的可能候选物。特别是空穴水合物结构sI、sII和sH以及另一种最近提出的低密度冰结构。使用经验水势和密度泛函理论计算确定了这些结构在0 K时的相对稳定性。通过进行自由能计算和吉布斯-杜亥姆积分,确定了TIP4P/2005在负压下的相图。空穴水合物sII和sH似乎是水在负压下的稳定固相。冰Ih和sII笼形物之间的相界出现在中等负压下,而在大负压下sH成为最稳定的相。这种行为与密度泛函理论计算中观察到的结果合理一致。

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