Coupled alkali-feldspar dissolution and secondary mineral precipitation in batch systems: 1. New experiments at 200 °C and 300 bars

Author:

Fu Qi,Lu Peng,Konishi Hiromi,Dilmore Robert,Xu Huifang,Seyfried W.E.,Zhu Chen

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference84 articles.

1. Thermodynamic and kinetic constraints on reaction rates among minerals and aqueous solutions: I. Theoretical considerations;Aagaard;American Journal of Science,1982

2. Rates of congruent dissolution of feldspars in acid and alkaline hydrothermal solutions;Alekseyev;Geochemistry International,1993

3. Change in the dissolution rates of alkali feldspars as a result of secondary mineral precipitation and approach to equilibrium;Alekseyev;Geochimica et Cosmochimica Acta,1997

4. The use of a surface complexation model to describe the kinetics of ligand-promoted dissolution of anorthite;Amrhein;Geochimica et Cosmochimica Acta,1988

5. Some factors affecting the dissolution kinetics of anorthite at 25 °C;Amrhein;Geochimica et Cosmochimica Acta,1992

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