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Beyond Cavity Statistics - A Two-moment Model of the Hydrophobic EffectFor atomic or small molecule-sized cavities, p0 can be calculated directly. Larger cavities, however, are so rare that determining p0 with sufficient statistical precision becomes impractical. A different strategy is clearly needed. To this end, we observe that p0 is just one element in the set of probabilities pn of finding exactly n solvent centers in the volume excluded by the solute. These probabilities are subject to the constraint: In practice, the summation extends only to nmax, the maximum number of solvent centers that can be placed in the excluded volume of the solute, v. An attempt to obtain p0 directly from Eq. 7 by calculating the remaining The parameters where <n> is the average number of water molecules displaced by the solute with the excluded volume v. In this model The proposed model can be readily applied to solutes of arbitrary shapes. No explicit
simulations of the solute in the liquid are necessary. The only thing that needs to be
calculated is <n> and <n2> inside ``imprints'' of the
solute in the neat solvent. In spite of its conceptual and technical simplicity, the model
is remarkably accurate. It reproduces practically exactly The proposed model has been postulated rather than derived from statistical mechanical
principles and, therefore, should be considered as heuristic. Nevertheless, it has strong
connections to both experiment and theory. The first two moments in Eq. 10 can be directly related to two readily available
properties of liquid water -- the density, By relying on the nearly parabolic behavior of As the sizes of solutes increase, it is expected that the two-moment model will require extensions to describe correctly dewetting of large hydrophobic surfaces. One possibility is to increase the number of moments included in Eq. 8. This yields, however, only minor improvements unless almost all moments are considered. A more promising approach is to appeal to information theory, originally used for the derivation of the model. [38] An improved model for the probabilities can be obtained by maximizing information entropy using a ``default model'' that better captures physical effects responsible for dewetting. A default model provides an estimate of probabilities if no further information is supplied. Active work on discovering effective default models is underway.
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