Abstract

Recently published analytical solutions for nonreactive solute movement in unsaturated porous materials are reviewed with the aim of developing simple algebraic equations that can be used with confidence for predicting solute disposition during absorption. Quasi‐analytical solutions for constant concentration and constant flux boundary conditions using a velocity independent hydrodynamic dispersion coefficient are reduced to a simple yet accurate form. The solutions for systems where the mechanical dispersion forms the dominant component during dispersion are also presented. Systems that lie between the extreme cases where both the molecular diffusion and mechanical dispersion have comparable significance are then analyzed and values of an empirical parameter, which is a necessary term in the resulting equation, determined from computer‐based numerical studies. Finally, equations developed from the alternative governing differential equation for solute movement based on a Fickian model are also detailed.

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