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疏水溶质附近水的密度耗尽与涨落增强:确定其背后的物理原理

Density Depletion and Enhanced Fluctuations in Water near Hydrophobic Solutes: Identifying the Underlying Physics.

作者信息

Coe Mary K, Evans Robert, Wilding Nigel B

机构信息

H. H. Wills Physics Lab, University of Bristol, Tyndall Avenue, Bristol BS8 1TL, United Kingdom.

出版信息

Phys Rev Lett. 2022 Jan 28;128(4):045501. doi: 10.1103/PhysRevLett.128.045501.

Abstract

We investigate the origin of the density depletion and enhanced density fluctuations that occur in water in the vicinity of an extended hydrophobic solute. We argue that both phenomena are remnants of the critical drying surface phase transition that occurs at liquid-vapor coexistence in the macroscopic planar limit, i.e., as the solute radius R_{s}→∞. Focusing on the density profile ρ(r) and a sensitive spatial measure of fluctuations, the local compressibility profile χ(r), we develop a scaling theory which expresses the extent of the density depletion and enhancement in compressibility in terms of R_{s}, the strength of solute-water attraction ϵ_{s}, and the deviation from liquid-vapor coexistence δμ. Testing the predictions against results of classical density functional theory for a simple solvent and grand canonical Monte Carlo simulations of a popular water model, we find that the theory provides a firm physical basis for understanding how water behaves at a hydrophobe.

摘要

我们研究了在延伸的疏水溶质附近的水中出现的密度耗尽和增强的密度涨落的起源。我们认为这两种现象都是在宏观平面极限下液-气共存时发生的临界干燥表面相变的残余,即当溶质半径(R_{s}→∞)时。聚焦于密度分布(\rho(r))和涨落的灵敏空间度量——局部压缩率分布(\chi(r)),我们发展了一种标度理论,该理论根据(R_{s})、溶质-水吸引力强度(\epsilon_{s})以及与液-气共存的偏差(\delta\mu)来表达密度耗尽的程度和压缩率的增强。将这些预测与简单溶剂的经典密度泛函理论结果以及流行水模型的巨正则蒙特卡罗模拟结果进行对比测试,我们发现该理论为理解水在疏水物处的行为提供了坚实的物理基础。

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