Dissolution rate of quartz in lead and sodium electrolyte solutions between 25 and 300°C: Effect of the nature of surface complexes and reaction affinity-Reference-Cited by-同舟云学术

Dissolution rate of quartz in lead and sodium electrolyte solutions between 25 and 300°C: Effect of the nature of surface complexes and reaction affinity

Published:1994-01 Issue:2 Volume:58 Page:541-551
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Berger Gilles,Cadore Eric,Schott Jacques,Dove Patricia M

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference45 articles.

1. Thermodynamic and kinetic constraints on reaction among minerals and aqueous solutions. I: Theoretical considerations;Aagaard;Amer. J. Sci.,1982

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

3. Quartz dissolution in organic-rich aqueous systems;Bennett;Geochim. Cosmochim. Acta,1991

4. The dissolution of quartz in dilute aqueous solutions of organic acids at 25°C;Bennett;Geochim. Cosmochim. Acta,1988

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

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