Abstract

We present the equations for wicking in two- and three-dimensional porous media when liquid is evaporating through the wet front using the Green--Ampt saturated capillary flow model in polar and spherical geometries. The time-dependent behavior of two-dimensional wicking influenced by front interface evaporation manifests distinctly from the influence on wicking by normal surface evaporation. This is shown in several ways; notably, the first-order effects of the front evaporation, as considered via an evaporation-capillary number, is of a lower order in the front position than normal evaporation. Furthermore, the front evaporation-induced steady states of the front position and bulk velocity vary significantly with the dimensionality of the flow expansion in the porous domain; with respect to the dimensionality, the front position decreases while the bulk velocity increases.

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