The dissolution rates of naturally altered basalts at pH 3 and 120 °C: Implications for the in-situ mineralization of CO2 injected into the subsurface
Sylvain Delerce, Pascale Bénézeth, Jacques Schott, Éric H. Oelkers
Topics & Concepts
BasaltGeologyMineralogyHydrothermal circulationGeochemistryMineralization (soil science)CalcitePlagioclaseDissolutionCrustQuartzChemistrySoil scienceSeismologySoil waterPhysical chemistryPaleontologyCO2 Sequestration and Geologic InteractionsGeological and Geochemical AnalysisMethane Hydrates and Related Phenomena