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- W2490095539 abstract "The usual basis of predictions of migratory behavior of ions in geological strata is the treatment of this behavior as an equilibrium chromatographic elution (1,2). This then leads to the following expression for the migratory velocity (v) of a species: where vw = velocity of the water front Kd = concentration ratio of absorbed and dissolved solute ε = porosity of the strata ρ = bulk density of the strata. This expression will predict the movement of a solute whose adsorption is in equilibrium with the surrounding strata. This equilibrium chromatographic motion will result in the migration of a band of activity whose concentration profile is gaussian and whose deviation will be a function of the hydrodynamic dispersion, Th (due to statistical variations in path length) and absorptive dispersion Ta (due to statistical variations in the absorption and desorption process). While these dispersions are interactive and do not sum in" @default.
- W2490095539 created "2016-08-23" @default.
- W2490095539 creator A5017336688 @default.
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- W2490095539 date "1979-04-06" @default.
- W2490095539 modified "2023-09-26" @default.
- W2490095539 title "Kinetic Effects in Migration" @default.
- W2490095539 doi "https://doi.org/10.1021/bk-1979-0100.ch011" @default.
- W2490095539 hasPublicationYear "1979" @default.
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