Abstract
As pointed out in Chap. 1, the geochemical migration of substances is described by a system of equations of material balance and the kinetics of interaction processes (adsorption, ion exchange, and chemical reactions) of the substances with rocks under certain initial and boundary conditions. Consequently, the interaction rate of solutions and gases with the rocks determines the laws of geochemical migration (Chaps. 6 and 7). This makes it important to consider the kinetics of adsorption, ion exchange, and chemical reactions of solutions and gases with rocks.
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