The dissolution kinetics and apparent solubility of natural apatite in closed reactors at temperatures from 5 to 50 °C and pH from 1 to 6

Author:

Harouiya Najatte,Chaïrat Claire,Köhler Stephan J.,Gout Robert,Oelkers Eric H.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference54 articles.

1. Thermodynamic and kinetic constraints on the dissolution of feldspars;Aagaard;Geol. Soc. Am.,1977

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

3. A comparative study of the dissolution of hydroxyapatite and fluorapatite in the absence and presence of organic ligands;Bengtsson;Geochim. Cosmochim. Acta,2005

4. Dissolution rate of quartz in Pb and Na electrolyte solutions. Effect of the nature of surface complexes and reaction affinity;Berger;Geochim. Cosmochim. Acta,1994

5. The influence of phosphate co-precipitation on rare earth distributions in natural waters;Byrne;Geochim. Cosmochim. Acta,1996

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