Department of Chemical Engineering, University of California, Santa Barbara, CA 93106, USA.
Faraday Discuss. 2010;146:299-308; discussion 367-93, 395-401. doi: 10.1039/b926184b.
After nearly 30 years of research on the hydrophobic interaction, the search for the hydrophobic force law is still continuing. Indeed, there are more questions than answers, and the experimental data are often quite different for nominally similar conditions, as well as, apparently, for nano-, micro-, and macroscopic surfaces. This has led to the conclusion that the experimentally observed force-distance relationships are either a combination of different 'fundamental' interactions, or that the hydrophobic force-law, if there is one, is complex--depending on numerous parameters. The only unexpectedly strong attractive force measured in all experiments so far has a range of D approximately 100-200 angstroms, increasing roughly exponentially down to approximately 10-20 angstroms and then more steeply down to adhesive contact at D = 0 or, for power-law potentials, effectively at D approximately 2 angstroms. The measured forces in this regime (100-200 angstroms) and especially the adhesive forces are much stronger, and have a different distance-dependence from the continuum VDW force (Lifshitz theory) for non-conducting dielectric media. We suggest a three-regime force-law for the forces observed between hydrophobic surfaces: In the first, from 100-200 angstroms to thousands of angstroms, the dominating force is created by complementary electrostatic domains or patches on the apposing surfaces and/or bridging vapour cavities; a 'pure' but still not well-understood 'long-range hydrophobic force' dominates the second regime from approximately 150 to approximately 15 angstroms, possibly due to an enhanced Hamaker constant associated with the 'proton-hopping' polarizability of water; while below approximately 10-15 anstroms to contact there is another 'pure short-range hydrophobic force' related to water structuring effects associated with surface-induced changes in the orientation and/or density of water molecules and H-bonds at the water-hydrophobic interface. We present recent SFA and other experimental results, as well as a simplified model for water based on a spherically-symmetric potential that is able to capture some basic features of hydrophobic association. Such a model may be useful for theoretical studies of the HI over the broad range of scales observed in SFA experiments.
经过近 30 年对疏水相互作用的研究,对疏水力定律的探索仍在继续。事实上,问题多于答案,实验数据对于名义上相似的条件往往有很大差异,而且对于纳米、微观和宏观表面也是如此。这导致的结论是,实验观察到的力-距离关系要么是不同“基本”相互作用的组合,要么是如果存在疏水力定律,它是复杂的——取决于众多参数。迄今为止,在所有实验中测量到的唯一一种出乎意料的强吸引力,其范围约为 D 为 100-200 埃,向下约呈指数增长至约 10-20 埃,然后更陡峭地下降至 D = 0 时的粘合接触,或者对于幂律势,实际上在 D 约为 2 埃时。在这个范围内(100-200 埃)测量到的力,特别是粘合力,比非导体电介质的连续体 VDW 力(Lifshitz 理论)要强得多,并且与距离的依赖性不同。我们建议了一个用于观察到的疏水表面之间的力的三区域力定律:在第一个区域,从 100-200 埃到数千埃,主导力是由互补的静电域或相邻表面上的补丁或桥接蒸气腔产生的;从大约 150 到大约 15 埃的第二个区域,主导力是“纯”但仍未被很好理解的“长程疏水力”,可能是由于与水的质子跳跃极化率相关的增强的 Hamaker 常数;而在大约 10-15 埃到接触的范围内,还有另一种与水结构效应相关的“纯短程疏水力”,与表面诱导的水分子取向和/或密度变化以及水-疏水界面处氢键有关。我们介绍了最近的 SFA 和其他实验结果,以及一种基于具有球形对称势的简化水模型,该模型能够捕捉疏水缔合的一些基本特征。这样的模型对于 SFA 实验中观察到的广泛范围内的 HI 的理论研究可能是有用的。