Experimental studies of halite dissolution kinetics: II. The effect of the presence of aqueous trace anions and K3Fe(CN)6-Reference-Cited by-同舟云学术

Experimental studies of halite dissolution kinetics: II. The effect of the presence of aqueous trace anions and K3Fe(CN)6

Published:1997-11 Issue:1-2 Volume:143 Page:17-26
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Alkattan Marwan,Oelkers Eric H.,Dandurand Jean-Louis,Schott Jacques

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference25 articles.

1. Thermodynamic and kinetics constraints on the dissolution of feldspars;Aagaard;Geol. Soc. Am. Abstracts with Program,1977

2. Thermodynamic and kinetics constraints on reaction among minerals and aqueous solution: Theoretical consideration;Aagaard;Am. J. Sci.,1982

3. Experimental studies of halite dissolution kinetics: I. The effects of saturation state and the presence of trace metals;Alkattan;Chem. Geol.,1997

4. Experimental studies of halite dissolution kinetics: III. The effect of aqueous trace ions on the dissolution rates of single halite crystals;Alkattan,1997

5. Dissolution rate of quartz in lead and sodium electrolyte solutions between 25 and 300°C: Effect of the nature of surface complex and reaction affinity;Berger;Geochim. Cosmochim. Acta,1994

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