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亲水性水合作用负热容的分子起源

Molecular origin of the negative heat capacity of hydrophilic hydration.

作者信息

Kinoshita Masahiro, Yoshidome Takashi

机构信息

Institute of Advanced Energy, Kyoto University, Uji, Kyoto 611-0011, Japan.

出版信息

J Chem Phys. 2009 Apr 14;130(14):144705. doi: 10.1063/1.3112610.

DOI:10.1063/1.3112610
PMID:19368463
Abstract

The hydrophobic and hydrophilic hydrations are analyzed with the emphasis on the sign of the heat capacity of hydration (HCH). The angle-dependent integral equation theory combined with a multipolar water model is employed in the analysis. The hydration entropy (HE) is decomposed into the translational and orientational parts. It is found that the orientational part governs the temperature dependence of the HE. The orientational part is further decomposed into the solute-water pair correlation component (component 1) and the water reorganization component (component 2). For hydrophilic solutes, components 1 and 2 are negative and positive, respectively. As the temperature becomes higher, component 1 increases while component 2 decreases: They make positive and negative contributions to the HCH, respectively. The strong solute-water electrostatic attractive interactions induce the distortion of water structure near the solute and the break of hydrogen bonds. As the temperature increases, the effect of the attractive interactions becomes smaller and the distortion of water structure is reduced (i.e., more hydrogen bonds are recovered with increasing temperature). The latter effect dominates, leading to negative HCH. During the heat addition the formation of hydrogen bonds, which accompanies heat generation, occurs near the solute. Consequently, the addition of the same amount of heat leads to a larger increase in the thermal energy (or equivalently, in the temperature) than in the case of pure water. The hydrophobic hydration, which is opposite to the hydrophilic hydration in many respects, is also discussed in detail.

摘要

对疏水水合作用和亲水水合作用进行了分析,重点关注水合热容量(HCH)的符号。分析中采用了与多极水模型相结合的角度相关积分方程理论。水合熵(HE)被分解为平动部分和取向部分。发现取向部分决定了HE的温度依赖性。取向部分进一步分解为溶质 - 水对关联成分(成分1)和水重组成分(成分2)。对于亲水性溶质,成分1和成分2分别为负和正。随着温度升高,成分1增加而成分2减少:它们分别对HCH产生正贡献和负贡献。溶质 - 水之间强烈的静电吸引相互作用会导致溶质附近水结构的扭曲和氢键的断裂。随着温度升高,吸引相互作用的影响变小,水结构的扭曲减小(即随着温度升高,更多的氢键得以恢复)。后一种效应占主导,导致HCH为负。在加热过程中,溶质附近会形成伴随着热量产生的氢键。因此,加入相同量的热量会导致热能(或等效地,温度)的增加比纯水情况下更大。在许多方面与亲水水合作用相反的疏水水合作用也进行了详细讨论。

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