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Derivation of equations describing solute transport in ground water
[report]
1977
unpublished
A general equation describing the three-dimensional transport and dispersion of a reacting solute in flowing ground water is derived from the principle of conservation of mass. The derivation presented in this report is more detailed but less rigorous than derivations published previously. The general solute-transport equation relates concentration changes to hydrodynamic dispersion, convective transport, fluid sources and sinks, and chemical reactions. Because both dispersion and convective
doi:10.3133/wri7719
fatcat:kzhm2nvia5dyflimhahjvifvgy