The kinetics of the reaction CO2 + H2O → H+ + HCO3− as one of the rate limiting steps for the dissolution of calcite in the system H2OCO2CaCO3
Author:
Publisher
Elsevier BV
Subject
Geochemistry and Petrology
Reference28 articles.
1. Calcite dissolution kinetics in porous media;Baumann;Chem. Geol.,1985
2. The kinetics of calcite dissolution and precipitation in geologically relevant situations of karst areas: 1. Open system;Buhmann;Chem. Geol.,1985
3. The kinetics of calcite dissolution and precipitation in geologically relevant situations of karst areas: 2. Closed system;Buhmann;Chem. Geol.,1985
4. Calcite dissolution kinetics in the system H2OCO2CaCO3 with participation of foreign ions;Buhmann;Chem. Geol.,1987
5. The kinetics of calcite dissolution and its consequences to karst evolution from the initial to the mature state;Dreybrodt;The NSS Bulletin,1987
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