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The phase diagram of water at negative pressures: Virtual ices

机译:水在负压下的相图:虚拟冰

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The phase diagram of water at negative pressures as obtained from computer simulations for twomodels of water, TIP4P/2005 and TIP5P is presented. Several solid structures with lower densitiesthan ice Ih, so-called virtual ices, were considered as possible candidates to occupy the negativepressure region of the phase diagram of water. In particular the empty hydrate structures sI, sII, andsH and another, recently proposed, low-density ice structure. The relative stabilities of thesestructures at 0 K was determined using empirical water potentials and density functional theorycalculations. By performing free energy calculations and Gibbs–Duhem integration the phasediagram of TIP4P/2005 was determined at negative pressures. The empty hydrates sII and sH appearto be the stable solid phases of water at negative pressures. The phase boundary between ice Ih andsII clathrate occurs at moderate negative pressures, while at large negative pressures sH becomes themost stable phase. This behavior is in reasonable agreement with what is observed in densityfunctional theory calculations.
机译:给出了从两种水模型TIP4P / 2005和TIP5P的计算机模拟获得的负压水的相图。几种密度比冰Ih低的固体结构(所谓的虚拟冰)被认为是占据水相图负压区域的可能候选者。特别是空的水合物结构sI,sII和sH,以及最近提出的另一种低密度冰结构。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。通过执行自由能计算和Gibbs-Duhem积分,在负压下确定了TIP4P / 2005的相图。空的水合物sII和sH似乎是水在负压下的稳定固相。冰Ih和sII包合物之间的相界出现在中等的负压下,而在大的负压下sH成为最稳定的相。此行为与密度泛函理论计算中观察到的行为合理吻合。

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