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
Keywords: کلسیت; Calcite; Dolomite; Magnesite; Dissolution; Kinetics; Carbon dioxide sequestration