Publication | Closed Access
Experimental dissolution of dolomite by CO2-charged brine at 100°C and 150bar: Evolution of porosity, permeability, and reactive surface area
120
Citations
82
References
2014
Year
Materials ScienceEngineeringBrine MiningMineral-fluid InteractionGeologyExperimental DissolutionGeochemistryCo2-charged BrineChemistryWater-rock InteractionMineral ProcessingPetrologyReactive Surface Area
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