The quasi-stationary state approximation to coupled mass transport and fluid-rock interaction in a porous medium
- 1 January 1988
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 52 (1) , 143-165
- https://doi.org/10.1016/0016-7037(88)90063-4
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- Calculation of the thermodynamic and transport properties of aqueous species at high pressures and temperatures: Aqueous tracer diffusion coefficients of ions to 1000°C and 5 kbGeochimica et Cosmochimica Acta, 1988
- Geochemical self-organization I; reaction-transport feedbacks and modeling approachAmerican Journal of Science, 1987
- Physico-chemical mechanisms of weathering processes and corresponding models of dynamics of mineral zonality evolutionChemical Geology, 1987
- Interdiffusion with multiple precipitation/dissolution reactions: Transient model and the steady-state limitGeochimica et Cosmochimica Acta, 1986
- Temperature dependence of calcite dissolution kinetics between 1 and 62°C at pH 2.7 to 8.4 in aqueous solutionsGeochimica et Cosmochimica Acta, 1984
- Calculation of mass transfer among minerals and aqueous solutions as a function of time and surface area in geochemical processes. I. computational approachMathematical Geology, 1983
- The kinetics of silica-water reactionsGeochimica et Cosmochimica Acta, 1980
- Bimetasomatism resulting from intergranular diffusion; II, Prediction of multimineralic zone sequencesAmerican Journal of Science, 1979
- Diffusion metasomatism and mineral reaction zones; general principles and application to feldspar alterationAmerican Journal of Science, 1976
- Bimetasomatism resulting from intergranular diffusion; I, A theoretical model for monomineralic reaction zone sequencesAmerican Journal of Science, 1976