Experimental chemical weathering of various bedrock types at different pH-values: 1. Sandstone and granite
- 10 June 1985
- journal article
- Published by Elsevier in Chemical Geology
- Vol. 49 (1-3) , 87-113
- https://doi.org/10.1016/0009-2541(85)90149-4
Abstract
No abstract availableKeywords
This publication has 27 references indexed in Scilit:
- Thermodynamic and kinetic constraints on reaction rates among minerals and aqueous solutions; I, Theoretical considerationsAmerican Journal of Science, 1982
- Non-equilibrium water/rock interactions—I. Model for interface-controlled reactionsGeochimica et Cosmochimica Acta, 1981
- Dissolution of Pyroxenes and Amphiboles During WeatheringScience, 1980
- Mechanism of feldspar weathering—II. Observations of feldspars from soilsGeochimica et Cosmochimica Acta, 1979
- The products of the interaction of feldspars with aqueous solutions at 25°CGeochimica et Cosmochimica Acta, 1978
- Rate control of mineral dissolution under Earth surface conditionsAmerican Journal of Science, 1978
- Mechanism of feldspar weathering: Some observational evidenceGeology, 1977
- The dissolution kinetics of feldspars at 25°C and 1 atm CO2 partial pressureGeochimica et Cosmochimica Acta, 1976
- The Experimental Chemical Weathering of SilicatesClay Minerals, 1961
- Oxygen in Rocks: A Basis for Petrographic CalculationsThe Journal of Geology, 1948