ew describe several methods of evaluating the surface fractal dimension of porous media. These include the thermodynamic method and the fractal version of Frenkel-Halsey-Hill theory. Neither method yields accurate estimates of the fractal dimensions of porous solids under the Whole range of experimental scales. We propose a modified thermodynamic method hat is Relatively simple but is significantly more accurate than Neimark's relation from the adsorption Experiments.
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