Calculation of mass transfer among minerals and aqueous solutions as a function of time and surface area in geochemical processes. I. computational approach
- 1 February 1983
- journal article
- Published by Springer Nature in Mathematical Geology
- Vol. 15 (1) , 109-130
- https://doi.org/10.1007/bf01030078
Abstract
No abstract availableKeywords
This publication has 40 references indexed in Scilit:
- Thermodynamic and kinetic constraints on reaction rates among minerals and aqueous solutions; I, Theoretical considerationsAmerican Journal of Science, 1982
- Theoretical prediction of the thermodynamic behavior of aqueous electrolytes by high pressures and temperatures; IV, Calculation of activity coefficients, osmotic coefficients, and apparent molal and standard and relative partial molal properties to 600 degrees C and 5kbAmerican Journal of Science, 1981
- Dissolution of Pyroxenes and Amphiboles During WeatheringScience, 1980
- Mechanism of feldspar weathering—II. Observations of feldspars from soilsGeochimica et Cosmochimica Acta, 1979
- Lithologic determination of mass transfer mechanisms of multiple-stage porphyry copper mineralization at Butte, Montana; vein formation by hypogene leaching and enrichment of potassium-silicate protoreEconomic Geology, 1979
- A Comparison of Computerized Chemical Models for Equilibrium Calculations in Aqueous SystemsPublished by American Chemical Society (ACS) ,1979
- Rate control of mineral dissolution under Earth surface conditionsAmerican Journal of Science, 1978
- Metasomatic zones in metamorphic rocksGeochimica et Cosmochimica Acta, 1977
- Mechanism of feldspar weathering: Some observational evidenceGeology, 1977
- Diffusion metasomatism and mineral reaction zones; general principles and application to feldspar alterationAmerican Journal of Science, 1976