An experimental study of dolomite dissolution rates as a function of pH from −0.5 to 5 and temperature from 25 to 80°C
Author:
Publisher
Elsevier BV
Subject
Geochemistry and Petrology,Geology
Reference28 articles.
1. An experimental study of calcite and limestone dissolution rates as a function of pH from −1 to 3 and temperatures from 25 to 80°C;Alkattan;Chem. Geol.,1998
2. Anderson, M.S., 1991. Reactivity of San Andres dolomite. SPE 20115, presented at the 1990 SPE Permian Basin Oil and Gas Recovery Conference, Midland, TX, March 8–9.
3. 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;Berger;Geochim. Cosmochim. Acta,1994
4. The kinetics of dissolution of dolomite in CO2–H2O systems at 1.5 to 65°C and 0 to 1 atm PCO2;Busenberg;Am. J. Sci.,1982
5. On the temperature dependence of mineral dissolution rates;Casey;Geochim. Cosmochim. Acta,1992
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