A surface complex reaction model for the pH-dependence of corundum and kaolinite dissolution rates

Author:

Carroll-Webb Susan A,Walther John V

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference54 articles.

1. Thermodynamic and kinetic constraints on the dissolution of feldspars (abstr.);Aagaard;Geol. Soc. Amer. Abstr. Prog.,1977

2. Thermodynamic and kinetic constraints on reaction rates among minerals and aqueous solutions. I. Theoretical consideration;Aagaard;Amer. J. Sci.,1982

3. Dissolution kinetics of chrysotile at pH 7 to 10;Bales;Geochim. Cosmochim. Acta,1985

4. Role of surface speciation in the low-temperature dissolution of minerals;Blum;Nature,1988

5. Operation of chemically sensitive field effect sensors as a function of the insulatorelectrolyte interface;Bousse;IEEE Trans. Electron Devices,1983

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