Abstract
Analytic calculations of \ensuremath{\Lambda}, a pore-size parameter which characterizes surface effects on transport in porous media, are carried out using two distinct approximations: (1) effective-medium theory and (2) percolation ideas recently applied by Katz and Thompson to the permeability of sedimentary rocks. Our calculations suggest that \ensuremath{\Lambda} may be determined by mercury injection experiments. We also study the phenomenon of electrical surface conduction using both approximations.
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