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Calcite, dolomite and magnesite dissolution kinetics in aqueous solutions at acid to circumneutral pH, 25 to 150 °C and 1 to 55 atm pCO2: New constraints on CO2 sequestration in sedimentary basins

Sedimentary BasinsCarbon SequestrationBiogeochemistryEngineeringEnvironmental EngineeringMineral-fluid InteractionAtm Pco2GeologyGeochemistryMagnesite Dissolution KineticsWater-rock InteractionSedimentologyEarth ScienceMineral Geochemistry