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Molecular probe dynamics reveals suppression of ice-like regions in strongly confined supercooled water

机译:分子探针动力学揭示了对强受限过冷水中冰状区域的抑制

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摘要

The structure of the hydrogen bond network is a key element for understanding water's thermodynamic and kinetic anomalies. While ambient water is strongly believed to be a uniform, continuous hydrogen-bonded liquid, there is growing consensus that supercooled water is better described in terms of distinct domains with either a low-density ice-like structure or a high-density disordered one. We evidenced two distinct rotational mobilities of probe molecules in interstitial supercooled water of polycrystalline ice Banerjee D, et al. (2009) ESR evidence for 2 coexisting liquid phases in deeply supercooled bulk water. Proc Natl Acad Sci USA 106: 11448-11453]. Here we show that, by increasing the confinement of interstitial water, the mobility of probe molecules, surprisingly, increases. We argue that loose confinement allows the presence of ice-like regions in supercooled water, whereas a tighter confinement yields the suppression of this ordered fraction and leads to higher fluidity. Compelling evidence of the presence of ice-like regions is provided by the probe orientational entropy barrier which is set, through hydrogen bonding, by the configuration of the surrounding water molecules and yields a direct measure of the configurational entropy of the same. We find that, under loose confinement of supercooled water, the entropy barrier surmounted by the slower probe fraction exceeds that of equilibrium water by the melting entropy of ice, whereas no increase of the barrier is observed under stronger confinement. The lower limit of metastability of supercooled water is discussed.
机译:氢键网络的结构是了解水的热力学和动力学异常的关键要素。尽管人们坚信周围的水是一种均匀的,连续的氢键结合的液体,但越来越多的共识是,过冷的水可以用低密度的类冰结构或高密度的无序结构更好地描述。我们证明了在多晶冰Banerjee D等人的间隙过冷水中,探针分子有两种不同的旋转运动。 (2009年)ESR证据表明,在深度过冷的散装水中有2种液相共存。美国国家科学院院刊106:11448-11453]。在这里,我们表明,通过增加间隙水的限制,探针分子的迁移率出人意料地增加了。我们认为,松散的封闭允许在过冷的水中存在冰状区域,而紧密的封闭则会抑制这种有序的馏分并导致更高的流动性。冰样区域存在的令人信服的证据是由探针取向的熵屏障提供的,该探针的取向熵屏障是通过氢键结合周围的水分子的构型而设置的,并直接测量了其结构熵。我们发现,在过冷水的松散约束下,较慢的探针分数所克服的熵垒由于冰的融化熵而超过了平衡水的熵垒,而在较强的约束条件下未观察到势垒的增加。讨论了过冷水的亚稳态下限。

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