Abstract
The Gibbs energy Δcav G of formation of cavities in water was calculated by thermodynamic integration. The cavities corresponded to organic molecules of various volumes and shapes with characteristic radii of 3–7 A and spheres of radii 3–6 A. Statistical integrals were calculated by the Monte Carlo simulation of an ensemble of water molecules with periodic boundary conditions at 25°C and pressure 1 atm. Interaction between water molecules was described by the TIP4P four-point nonpolarizable model. It was found that the proportionality of Δcav G to cavity volume V obtained earlier for spheres with radii not exceeding 5 A remained valid for cavities corresponding to organic molecules of different volumes and shapes, including cavities with the characteristic radii exceeding 5 A. A possible explanation of the retention of the Δcav G ∞ V dependence at large characteristic radii was suggested in terms of the two-peak binomial model of the cavitation effect. The conclusion was drawn that the Δcav G = αV dependence could be used for calculating the nonpolar part of the Gibbs energy of solvation in implicit water models.
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