Common microscopic structural origin for water's thermodynamic and dynamic anomalies

被引:81
作者
Shi, Rui [1 ]
Russo, John [1 ,2 ]
Tanaka, Hajime [1 ]
机构
[1] Univ Tokyo, Inst Ind Sci, Dept Fundamental Engn, Meguro Ku, 4-6-1 Komaba, Tokyo 1538505, Japan
[2] Univ Bristol, Sch Math, Bristol BS8 1TW, Avon, England
基金
日本学术振兴会; 欧洲研究理事会;
关键词
TO-STRONG TRANSITION; LIQUID-LIQUID TRANSITION; SUPERCOOLED WATER; GLASS-TRANSITION; CONFINED WATER; HIGH-DENSITY; FRAGILE; VISCOSITY; MODEL; RELAXATION;
D O I
10.1063/1.5055908
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Water displays a vast array of unique properties, known as water's anomalies, whose origin remains subject to hot debate. Our aim in this article is to provide a unified microscopic physical picture of water's anomalies in terms of locally favored structures, encompassing both thermodynamic and dynamic anomalies, which are often attributed to different origins. We first identify locally favored structures via a microscopic structural descriptor that measures local translational order and provide direct evidence that they have a hierarchical impact on the anomalies. At each state point, the strength of thermodynamic anomalies is directly proportional to the amount of locally favored structures, while the dynamic properties of each molecule depend on the local structure surrounding both itself and its nearest neighbors. To incorporate this, we develop a novel hierarchical two-state model. We show by extensive simulations of two popular water models that both thermodynamic and kinetic anomalies can be almost perfectly explained by the temperature and pressure dependence of these local and non-local versions of the same structural descriptor, respectively. Moreover, our scenario makes three unique predictions in supercooled water, setting it apart from other scenarios: (1) Presence of an " Arrhenius-to-Arrhenius" crossover upon cooling, as the origin of the apparent "fragile-to-strong" transition; (2) maximum of dynamic heterogeneity around 20 K below theWidom line and far above the glass transition; (3) violation of the Stokes-Einstein-Debye relation at similar to 2T(g), rather than 1.2T(g) typical of normal glass-formers. These predictions are verified by recent measurement of water's diffusion at very low temperatures (point 1) and discoveries from our extensive simulations (points 2-3). We suggest that the same scenario may generally apply to water-like anomalies in liquids tending to form locally favored structures, including not only other important tetrahedral liquids such as silicon, germanium, and silica, but also metallic and chalcogenide liquids. Published by AIP Publishing.
引用
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页数:21
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