Injection of supercritical carbon dioxide (CO2) into formations containing carbonate minerals may affect the porosity and permeability of the host rock and overlying caprock, due to dissolution of the primary carbonate minerals and possible precipitation of secondary minerals. Simulations of pilot-scale CO2 injection with co-sequestration of sulfur dioxide (SO2) were conducted to assess the competing effects of dolomite dissolution and anhydrite precipitation on formation hydraulic properties. A geochemical model of two promising host formations in the midwestern United States (Rose Run and Copper Ridge) was developed for the purpose of assessing mineral dissolution and precipitation effects on injectivity and containment.
Revised: July 22, 2010 |
Published: April 1, 2009
Citation
Bacon D.H., B.M. Sass, M. Bhargava, J.R. Sminchak, N. Gupta, and N. Gupta. 2009.Reactive Transport Modeling of CO2 and SO2 Injection into Deep Saline Formations and Their Effect on the Hydraulic Properties of Host Rocks. In Energy Procedia: GHGT-9: 9th International Conference on Greenhouse Gas Technologies, 1, 3283-3290. Amsterdam:Elsevier. PNWD-SA-8379. doi:10.1016/j.egypro.2009.02.114