The use of a surface complexation model to describe the kinetics of ligand-promoted dissolution of anorthite
- 31 December 1988
- journal article
- Published by Elsevier BV in Geochimica et Cosmochimica Acta
- Vol. 52 (12), 2785-2793
- https://doi.org/10.1016/0016-7037(88)90146-9
Abstract
No abstract availableKeywords
This publication has 26 references indexed in Scilit:
- Some Observations on the Stoichiometry of Feldspar Hydrolysis in Granitic SoilJournal of Environmental Quality, 1988
- The coordination chemistry of weathering: I. Dissolution kinetics of δ-Al2O3 and BeOGeochimica et Cosmochimica Acta, 1986
- Steady-state kinetics and dissolution mechanisms of albiteAmerican Journal of Science, 1985
- Dissolution kinetics of chrysotile at pH 7 to 10Geochimica et Cosmochimica Acta, 1985
- The Role of Organic Acids in the Acid‐Base Status of Surface Waters at Bickford Watershed, MassachusettsWater Resources Research, 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
- Thermodynamic and kinetic constraints on reaction rates among minerals and aqueous solutions; I, Theoretical considerationsAmerican Journal of Science, 1982
- The dissolution kinetics of feldspars at 25°C and 1 atm CO2 partial pressureGeochimica et Cosmochimica Acta, 1976
- The role of humic acids from Tasmanian podzolic soils in mineral degradation and metal mobilizationGeochimica et Cosmochimica Acta, 1973
- A Study in Rock-WeatheringThe Journal of Geology, 1938