Answers are grounded in this paper and cite their sources.
In this paper we describe a Monte Carlo calculation of the surface tension of water at 25 °C. The procedure used involves computing the free energy required to create a surface in a system of 256 water molecules with periodic boundary conditions imposed. In order to optimize computing time we have used a modified version of an umbrella sampling algorithm suggested by Torrie and Valleau. The excess surface free energy is computed in a series of steps, the most important of which consist of incremental calculations in which the interface is gradually created. Our final result is γ=97±6 dynes/cm, larger than the experimental value of 72 dyn/cm. Reasons for the rather large difference are discussed. Our result can be used as a basis for comparison of the surface tension of water/air interfaces with the surface tension of other aqueous interfaces calculated using the same technique.
No takes yet. Share an insight, caveat, or question.
Lee et al. (1980) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: