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Metastable liquid-liquid transition in a molecular model of water

机译:水分子模型中的亚稳态液-液转变

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摘要

Liquid water's isothermal compressibility and isobaric heat capacity, and the magnitude of its thermal expansion coefficient, increase sharply on cooling below the equilibrium freezing point. Many experimental theoretical and computational studies have sought to understand the molecular origin and implications of this anomalous behaviour. Of the different theoretical scenarios put forward, one posits the existence of a first-order phase transition that involves two forms of liquid water and terminates at a critical point located at deeply supercooled conditions. Some experimental evidence is consistent with this hypothesis, but no definitive proof of a liquid-liquid transition in water has been obtained to date: rapid ice crystallization has so far prevented decisive measurements on deeply supercooled water, although this challenge has been overcome recently. Computer simulations are therefore crucial for exploring water's structure and behaviour in this regime, and have shown that some water models exhibit liquid-liquid transitions and others do not. However, recent work has argued that the liquid-liquid transition has been mistakenly interpreted, and is in fact a liquid-crystal transition in all atomistic models of water. Here we show, by studying the liquid-liquid transition in the ST2 model of water with the use of six advanced sampling methods to compute the free-energy surface, that two metastable liquid phases and a stable crystal phase exist at the same deeply supercooled ther-modynamic condition, and that the transition between the two liquids satisfies the thermodynamic criteria of a first-order transition. We follow the rearrangement of water's coordination shell and topo-logical ring structure along a thermodynamically reversible path from the low-density liquid to cubic ice. We also show that the system fluctuates freely between the two liquid phases rather than crystallizing. These findings provide unambiguous evidence for a liquid-liquid transition in the ST2 model of water, and point to the separation of time scales between crystallization and relaxation as being crucial for enabling it.
机译:在冷却到平衡凝固点以下时,液态水的等温可压缩性和等压热容量及其热膨胀系数的大小会急剧增加。许多实验理论和计算研究都试图了解这种异常行为的分子起源和含义。在提出的不同理论情景中,一个假设存在一阶相变,该相变涉及两种形式的液态水,并终止于处于过冷状态的临界点。一些实验证据与此假说相符,但是迄今为止,尚无确切的证据证明水中发生液-液转变:尽管最近已经克服了这一难题,但快速的冰结晶至今仍无法对深过冷的水进行决定性的测量。因此,计算机模拟对于探索这种状态下的水的结构和行为至关重要,并且已经表明某些水模型表现出液-液转换,而另一些则没有。但是,最近的工作认为,液-液相转变已被错误地解释,并且实际上在所有水原子模型中都是液晶转变。在这里,我们通过使用六种先进的采样方法计算水的ST2模型中的液-液转变来计算自由能表面,表明两个亚稳态液相和一个稳定的结晶相在同一深度过冷状态下同时存在。 -热力学条件,并且两种液体之间的转变满足一阶转变的热力学标准。我们沿着从低密度液体到立方冰的热力学可逆路径,对水的配位壳和拓扑环结构进行了重新排列。我们还表明,该系统在两个液相之间自由波动,而不是结晶。这些发现为水在ST2模型中进行液-液转变提供了明确的证据,并指出结晶和弛豫之间的时间尺度分离对于实现此过程至关重要。

著录项

  • 来源
    《Nature》 |2014年第7505期|385-388|共4页
  • 作者单位

    Department of Chemical and Biological Engineering, Princeton University, Princeton, New Jersey 08544, USA;

    Department of Chemistry, Princeton University, Princeton, New Jersey 08544, USA;

    Department of Chemical and Biological Engineering, Princeton University, Princeton, New Jersey 08544, USA,Air Products and Chemicals Inc., Allentown, Pennsylvania 18195, USA;

    Department of Chemistry, Princeton University, Princeton, New Jersey 08544, USA;

    Department of Chemical and Biological Engineering, Princeton University, Princeton, New Jersey 08544, USA;

    Department of Chemical and Biological Engineering, Princeton University, Princeton, New Jersey 08544, USA;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
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  • 正文语种 eng
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