Numerical modeling of coupled variably saturated fluid flow and reactive transport with fast and slow chemical reactions.
The couplings among chemical reaction rates, advective and diffusive transport in fractured media or soils, and changes in hydraulic properties due to precipitation and dissolution within fractures and in rock matrix are important for both nuclear waste disposal and remediation of contaminated sites. This paper describes the development and application of LEHGC2.0, a mechanistically based numerical model for simulation of coupled fluid flow and reactive chemical transport, including both fast and slow reactions in variably saturated media. Theoretical bases and numerical implementations are summarized, and two example problems are demonstrated. The first example deals with the effect of precipitation/dissolution on fluid flow and matrix diffusion in a two-dimensional fractured media. Because of the precipitation and decreased diffusion of solute from the fracture into the matrix, retardation in the fractured medium is not as large as the case wherein interactions between chemical reactions and transport are not considered. The second example focuses on a complicated but realistic advective-dispersive-reactive transport problem. This example exemplifies the need for innovative numerical algorithms to solve problems involving stiff geochemical reactions.
Yeh
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GT
Department of Civil and Environmental Engineering, The Pennsylvania State University, 212 Sackett Building, University Park, PA 16802, USA. gty@darcy.cee.psu.edu
Siegel
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MD
Li
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MH
D004058:Diffusion; D055593:Geological Phenomena; D005844:Geology; D007700:Kinetics; D008962:Models, Theoretical; D014874:Water Pollutants, Chemical; D014875:Water Pollutants, Radioactive
D014874:Water Pollutants, Chemical; D014875:Water Pollutants, Radioactive