The surface layer susceptibility χ₁ is investigated for critical wetting transitions in three dimensions. Whereas mean-field treatments predict that χ₁ diverges symmetrically at the transition, a renormalization-group (RG) analysis predicts that the critical amplitude ratio R should be a rapidly increasing function of the parameter {ω} that determines the strength of interfacial fluctuations. Existing Monte Carlo data for the simple-cubic Ising model show pronounced asymmetry in χ₁ and yield a value for the ratio R that is significantly greater than the mean-field result (unity). The data are consistent with RG predictions, provided {ω}{~}0.3 for the Ising model at the temperature of the simulation.
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Parry et al. (1991) studied this question.
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