The composition of weathering solutions on granitic rocks: Comparison between field observations and water-rock interaction simulations based on thermodynamic and kinetic laws
- 1 July 1990
- journal article
- Published by Elsevier in Chemical Geology
- Vol. 84 (1-4), 100-104
- https://doi.org/10.1016/0009-2541(90)90176-8
Abstract
No abstract availableThis publication has 9 references indexed in Scilit:
- The effect of organic acids on the dissolution of K-feldspar under conditions relevant to burial diagenesisMineralogical Magazine, 1989
- Dependence of albite dissolution kinetics on ph and time at 25°c and 70°cGeochimica et Cosmochimica Acta, 1986
- Geochemical mass balances and weathering rates in forested watersheds of the southern Blue RidgeAmerican Journal of Science, 1985
- Thermodynamic and kinetic constraints on reaction rates among minerals and aqueous solutions. II. Rate constants, effective surface area, and the hydrolysis of feldsparGeochimica et Cosmochimica Acta, 1984
- Chemical kinetics of water‐rock interactionsJournal of Geophysical Research, 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
- Thermodynamic and kinetic constraints on reaction rates among minerals and aqueous solutions; I, Theoretical considerationsAmerican Journal of Science, 1982
- The kinetics of dissolution of muscovites at 25°C and 1 atm CO2 partial pressureGeochimica et Cosmochimica Acta, 1981
- The kinetics of silica-water reactionsGeochimica et Cosmochimica Acta, 1980