Article ID Journal Published Year Pages File Type
8910272 Chemical Geology 2018 52 Pages PDF
Abstract
The steady-state dissolution rate of dolomite was studied at 25 °C and 1 atm CO2 total pressure in deionised water in the absence (control) and presence of twenty seven different organic and inorganic additives at low concentration (1 mM). These additives are most likely present at low concentrations (
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Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
Preview
Dolomite dissolution kinetics in aqueous solutions in the presence of organic and inorganic additives at 25 °C and pCO2 ~ 1 atm
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