A method of estimateng the Gibbs free energies of formation of hydrated and dehydrated clay minerals
- 1 August 1992
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 56 (8) , 3007-3029
- https://doi.org/10.1016/0016-7037(92)90287-s
Abstract
No abstract availableKeywords
This publication has 27 references indexed in Scilit:
- The Polymer Model of Thermochemical Clay Mineral StabilityClays and Clay Minerals, 1986
- Activity/Composition Relations among Silicates and Aqueous Solutions: II. Chemical and Thermodynamic Consequences of Ideal Mixing of Atoms on Homological Sites in Montmorillonites, Illites, and Mixed-Layer ClaysClays and Clay Minerals, 1983
- Free Energies of Formation of Illite Solid Solutions and Their Compositional DependenceClays and Clay Minerals, 1982
- An ideal solid solution model for calculating solubility of clay mineralsClay Minerals, 1981
- Relationships among Gibbs energies of formation of compoundsAmerican Journal of Science, 1979
- A method of estimation of standard free energies of formation of silicate minerals at 298.15 degrees KAmerican Journal of Science, 1975
- A method of estimating the Gibbs energies of formation of layer silicatesGeochimica et Cosmochimica Acta, 1974
- Cation exchange in clays interpreted by regular solution theoryAmerican Journal of Science, 1968
- CATION EXCHANGE IN MICACEOUS MINERALSSoil Science, 1954
- Adsorption of Water Vapor by Montmorillonite. I. Heat of Desorption and Application of BET Theory1Journal of the American Chemical Society, 1952