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水在疏水溶质周围的结构和冰山模型。

Water's structure around hydrophobic solutes and the iceberg model.

机构信息

Grupo de Física-Matemática, Universidade de Lisboa, Avenida Prof. Gama Pinto 2, 1649-003 Lisboa, Portugal.

出版信息

J Phys Chem B. 2013 Feb 21;117(7):2153-9. doi: 10.1021/jp310649n. Epub 2013 Feb 7.

DOI:10.1021/jp310649n
PMID:23360515
Abstract

The structure of water in the hydration shells of small hydrophobic solutes was investigated through molecular dynamics. The results show that a subset of water molecules in the first hydration shell of a nonpolar solute have a significantly enhanced tetrahedrality and a slightly larger number of hydrogen bonds, relative to the molecules in water at room temperature, consistent with the experimentally observed negative excess entropy and increased heat capacity of hydrophobic solutions at room temperature. This ordering results from the rearrangement of a small number of water molecules near the nonpolar solutes that occupy one to two vertices of the enhanced water tetrahedra. Although this structuring is not nearly like that often associated with a literal interpretation of the term "iceberg" in the Frank and Evans iceberg model, it does support a moderate interpretation of this model. Thus, the tetrahedral orientational order of this ensemble of water molecules is comparable to that of liquid water at ~10 °C, although not accompanied by the small contraction of the O-O distance observed in cold water. Further, we show that the structural changes of water in the vicinity of small nonpolar solutes cannot be inferred from the water radial distribution functions, explaining why this increased ordering is not observed through neutron diffraction experiments. The present results restore a molecular view where the slower translational and reorientational dynamics of water near hydrophobic groups has a structural equivalent resembling water at low temperatures.

摘要

通过分子动力学研究了小疏水分子水合壳中水分子的结构。结果表明,与室温下水相比,非极性溶质第一水合壳中部分水分子的四面体化程度显著增强,氢键数量略多,这与实验观察到的疏水性溶液在室温下的负过剩熵和热容增加一致。这种有序性是由少量水分子在非极性溶质附近的重新排列引起的,这些水分子占据增强的水分子四面体的一个到两个顶点。尽管这种结构与弗兰克和埃文斯冰山模型中“冰山”一词的字面解释并不完全相同,但它确实支持对该模型的适度解释。因此,尽管没有观察到冷水中 O-O 距离的小收缩,但该水分子集合的四面体取向有序性与约 10°C 时的液态水相当。此外,我们还表明,无法从水分子径向分布函数推断出小非极性溶质附近水分子的结构变化,这解释了为什么通过中子衍射实验无法观察到这种有序性增加。本研究结果恢复了一种分子观点,即疏水分子附近的水分子较慢的平移和重取向动力学具有类似于低温下水的结构等价物。

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