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- W4205244920 abstract "Kinetic modeling was used to estimate the effective surface area of aquifer in contact with a unit volume of ground water for a composite saturated-unsaturated groundwater system in southern Nevada. This aquifer property, not obtainable by other means, is necessary for realistic modeling of solute transport in groundwater systems. The results of the kinetic modeling indicate that only a small part of the total interconnected pore space is available for transport of water to the water table. The aquifer studied is composed of both vitric (glassy) and divitrified (crystalline) volcanic tuff of nearly identical chemical composition. Comparison of laboratory and field data indicated that only the vitric phase has a significant influence on ground-water composition. Laboratory determination of mass-transfer rates from the vitric material to solution as functions of pH allowed a simulation of the natural water's cation composition. Simulated results were improved considerably when the model was modified to take into account precipitation of the clay mineral, montmorillonite. Estimates of surface area per unit volume obtained from the kinetic model are about 3 percent of those obtained independently from surface area measurements using the Braunauer, Emmett, and Teller (B.E.T.) equation." @default.
- W4205244920 created "2022-01-26" @default.
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- W4205244920 date "1979-03-19" @default.
- W4205244920 modified "2023-09-26" @default.
- W4205244920 title "Application of Geochemical Kinetic Data to Ground-water Systems" @default.
- W4205244920 doi "https://doi.org/10.1021/bk-1979-0093.ch034" @default.
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