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Pressure dependence of viscosity in supercooled water and a unified approach for thermodynamic and dynamic anomalies of water

机译:过冷水中粘度的压力依赖性以及水的热力学和动态异常的统一方法

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摘要

The anomalous decrease of the viscosity of water with applied pressure has been known for over a century. It occurs concurrently with major structural changes: The second coordination shell around a molecule collapses onto the first shell. Viscosity is thus a macroscopic witness of the progressive breaking of the tetrahedral hydrogen bond network that makes water so peculiar. At low temperature, water at ambient pressure becomes more tetrahedral and the effect of pressure becomes stronger. However, surprisingly, no data are available for the viscosity of supercooled water under pressure, in which dramatic anomalies are expected based on interpolation between ambient pressure data for supercooled water and high pressure data for stable water. Here we report measurements with a time-of-flight viscometer down to 244K and up to 300MPa, revealing a reduction of viscosity by pressure by as much as 42%. Inspired by a previous attempt [Tanaka H (2000) J Chem Phys 112:799–809], we show that a remarkably simple extension of a two-state model [Holten V, Sengers JV, Anisimov MA (2014) J Phys Chem Ref Data 43:043101], initially developed to reproduce thermodynamic properties, is able to accurately describe dynamic properties (viscosity, self-diffusion coefficient, and rotational correlation time) as well. Our results support the idea that water is a mixture of a high density, “fragile” liquid, and a low density, “strong” liquid, the varying proportion of which explains the anomalies and fragile-to-strong crossover in water.
机译:在施加压力的情况下,水的粘度反常下降已有一个多世纪的历史了。它与主要结构变化同时发生:分子周围的第二个配位壳塌陷到第一个壳上。因此,粘度是使水变得如此独特的四面体氢键网络逐渐破坏的宏观见证。在低温下,环境压力下的水变得更四面体,并且压力作用变得更强。然而,令人惊讶的是,没有关于压力下的过冷水的粘度的数据,其中基于过冷水的环境压力数据与稳定水的高压数据之间的插值,预计会出现明显的异常。在这里,我们报告了使用飞行时间粘度计(低至244K和最高300MPa)进行的测量,结果显示压力降低了粘度达42%。受先前尝试的启发[Tanaka H(2000)J Chem Phys 112:799–809],我们显示了两种状态模型的非常简单的扩展[Holten V,Sengers JV,Anisimov MA(2014)J Phys Chem Ref最初开发用于重现热力学性质的数据43:043101]也能够准确地描述动力学性质(粘度,自扩散系数和旋转相关时间)。我们的结果支持以下观点:水是高密度“易碎”液体和低密度“强”液体的混合物,其比例的变化解释了水的异常现象和脆弱到强烈的交叉。

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