Isosteric heats of adsorption of CH₄ on exfoliated graphite (Grafoil) have been measured calorimetrically at 69.5, 77, 84.5, and 92.5 K up to surface coverages of the equivalent of 3.5 layers. At the lowest two temperatures, qₛₜ varies rather little with the amount adsorbed beyond a monolayer. In the same region of adsorption, qₛₜ at the highest two temperatures changes by as much as 10% in an oscillatory manner. A qualitative analysis of the results suggests that they are consistent with a transition (roughening?) occurring in the methane multilayers in the vicinity of $T=80$ K. From isotherm and heat-capacity measurements on the same system, Hamilton and Goodstein [Phys. Rev. B 28, 3838 (1983)] have deduced that critical points in the multilayers occur at approximately 78 K.
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Piper et al. (1984) studied this question.
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