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Pablo G. Debenedetti
Department of Chemical Engineering, Princeton University, Princeton, NJ 08544, USA and Department of Chemistry, Princeton University, Princeton, New Jersey 08544, USA Frank H. Stillinger
M.S. Shell
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Received: July 18, 2003, in Final Form: October 10, 2003
Abstract: The multidimensional potential-energy "landscape" formalism offers useful insights into the properties of supercooled liquids and glasses. However, its mathematical fundamentals present formidable subtlety and complexity. In the interests of developing a useful approximation for the statistical mechanics of landscapes, we have developed a simple family of models describing the energy-depth distribution of landscape basins. Our analysis begins with the "Gaussian" model that has been advocated in the recent literature, a physically appealing and thermodynamically rather accurate description that straightforwardly predicts a positive-temperature ideal glass transition. Careful enumeration of low-lying basins reveals however that the Gaussian model requires modification in the form of a logarithmic correction. Consequently, we have carried out algebraic and numerical analyses of a logarithmically modified Gaussian model, including depth dependence of the mean intrabasin vibrational free energy. The logarithmic modification has the effect of eliminating the positive-temperature ideal glass transition of the precursor pure-Gaussian model. Nevertheless, it is sufficiently similar to that unmodified model at and above any kinetic glass transition temperature to be able to represent measurable calorimetric data with reasonable accuracy.