John D. Rogers, SPE, Vice President, Operations, Fusion Reservoir Engineering Services
Research-and-development modeling has shown that CO2 can diffuse a small distance into the thick shale caprocks above brine aquifers used for sequestration and cause migration of siderite (iron carbonate), magnesite (magnesium carbonate), calcite, and other precipitates back into the target zone, which is what is wanted for mineral sequestration of CO2.