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氢键和界面水的振动能量弛豫:全 DFT 分子动力学模拟。

Hydrogen bonding and vibrational energy relaxation of interfacial water: A full DFT molecular dynamics simulation.

机构信息

Center for Molecular Spectroscopy and Dynamics, Institute for Basic Science (IBS), Seoul 02841, South Korea.

Department for Molecular Spectroscopy, Max Planck Institute for Polymer Research, Ackermannweg 10, D-55128 Mainz, Germany.

出版信息

J Chem Phys. 2017 Jul 28;147(4):044707. doi: 10.1063/1.4995437.

Abstract

The air-water interface has been a subject of extensive theoretical and experimental studies due to its ubiquity in nature and its importance as a model system for aqueous hydrophobic interfaces. We report on the structure and vibrational energy transfer dynamics of this interfacial water system studied with equilibrium and non-equilibrium molecular dynamics simulations employing a density functional theory -based description of the system and the kinetic energy spectral density analysis. The interfacial water molecules are found to make fewer and weaker hydrogen (H)-bonds on average compared to those in the bulk. We also find that (i) the H-bonded OH groups conjugate to the free OH exhibit rather low vibrational frequencies (3000-3500 cm); (ii) the presence of a significant fraction (>10%) of free and randomly oriented water molecules at the interface ("labile water"), neither of whose OH groups are strong H-bond donors; (iii) the inertial rotation of free OH groups, especially from the labile water, contribute to the population decay of excited free OH groups with comparable rate and magnitude as intramolecular energy transfer between the OH groups. These results suggest that the labile water, which might not be easily detectable by the conventional vibrational sum frequency generation method, plays an important role in the surface water dynamics.

摘要

由于其在自然界中的普遍性以及作为水-疏水性界面模型系统的重要性,气-水界面一直是广泛的理论和实验研究的主题。我们报告了使用平衡和非平衡分子动力学模拟,采用基于密度泛函理论的系统描述和动能谱密度分析,对该界面水分子系统的结构和振动能量转移动力学进行了研究。与体相中的水分子相比,界面处的水分子平均形成的氢键更少且更弱。我们还发现:(i) 与自由 OH 共轭的氢键化 OH 基团表现出相当低的振动频率(3000-3500 cm);(ii) 在界面处存在相当大比例(>10%)的自由且随机取向的水分子(“不稳定水”),其 OH 基团都不是强氢键供体;(iii) 自由 OH 基团的惯性旋转,特别是来自不稳定水的旋转,对激发态自由 OH 基团的种群衰减的贡献与 OH 基团之间的分子内能量转移相当。这些结果表明,不稳定水可能不容易被传统的振动和频产生方法检测到,但在表面水动力学中起着重要作用。

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