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首页> 外文期刊>Langmuir: The ACS Journal of Surfaces and Colloids >Interfacial Water at Hydrophobic and Hydrophilic Surfaces:Slip, Viscosity, and Diffusion
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Interfacial Water at Hydrophobic and Hydrophilic Surfaces:Slip, Viscosity, and Diffusion

机译:疏水和亲水表面的界面水:滑移,粘度和扩散

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摘要

The dynamics and structure of water at hydrophobic and hydrophilic diamond surfaces is examined via nonequilibrium Molecular Dynamics simulations. For hydrophobic surfaces under shearing conditions, the general hydrodynamic boundary condition involves a finite surface slip. The value of the slip length depends sensitively on the surface water interaction strength and the surface roughness; heuristic scaling relations between slip length, contact angle, and depletion layer thickness are proposed. Inert gas in the aqueous phase exhibits pronounced surface activity but only mildly increases the slip length. On polar hydrophilic surfaces, in contrast, slip is absent, but the water viscosity is found to be increased within a thin surface layer. The viscosity and the thickness of this surface layer depend on the density of polar surface groups. The dynamics of single water molecules in the surface layer exhibits a similar distinction: on hydrophobic surfaces the dynamics is purely diffusive, while close to a hydrophilic surface transient binding or trapping of water molecules over times of the order of hundreds of picoseconds occurs. We also discuss in detail the effect of the Lennard-Jones cutoff length on the interfacial properties.
机译:通过非平衡分子动力学模拟检查了疏水性和亲水性金刚石表面上水的动力学和结构。对于在剪切条件下的疏水表面,一般的流体动力边界条件涉及有限的表面滑移。滑移长度的值敏感地取决于表面水的相互作用强度和表面粗糙度。提出了滑移长度,接触角和耗尽层厚度之间的启发式比例关系。水相中的惰性气体表现出明显的表面活性,但仅适度增加了滑移长度。相反,在极性亲水性表面上没有滑动,但是发现在薄表层内水粘度增加。该表面层的粘度和厚度取决于极性表面基团的密度。表面层中单个水分子的动力学表现出相似的区别:在疏水表面上,动力学纯粹是扩散性的,而接近亲水表面时,水分子在数百皮秒量级的时间内发生瞬态结合或捕获。我们还将详细讨论Lennard-Jones截止长度对界面性质的影响。

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