Reservoir scale reactive-transport modeling of a buoyancy-controlled CO2 plume with impurities (SO2, NO2, O2). (October 2019)

• Record Type: Journal Article
• Authors: Spycher, Nicolas F.; Llanos, Ella María; Vu, Hong P.; Haese, Ralf R.
• Is Part Of: International journal of greenhouse gas control. Volume 89(2019)
• Page Start: 40
• Page End: 51
• Publication Date: 2019-10
• Subjects: Carbon -- Sequestration -- Simulation -- Aquifer -- Geologic storage -- Co-injectants -- Injection -- Carbon dioxide -- Sulfur dioxide -- Nitrogen dioxide -- Oxygen -- NOx -- SOx -- Chemistry -- Water quality; Greenhouse gases -- Environmental aspects -- Periodicals; Air -- Purification -- Technological innovations -- Periodicals; Gaz à effet de serre -- Périodiques; Gaz à effet de serre -- Réduction -- Périodiques; Air -- Purification -- Technological innovations; Greenhouse gases -- Environmental aspects; Periodicals; 363.73874605
• DOI: 10.1016/j.ijggc.2019.06.026
• Languages: English
• ISSNs: 1750-5836

Abstract

Highlights: The predicted CO2 flow pattern is quite sensitive to fine-scale heterogeneities and the resolution of the numerical mesh. Co-injected SO2 and NO2 readily partition into the aqueous phase in close vicinity of their injection point, whereas O2 may persist farther in the supercritical CO2 phase. Acidification takes place near the wellbore due to the preferential stripping of impurities. Mineral dissolution (muscovite, chlorite and calcite) and precipitation (ankerite, kaolinite and chalcedony) occur along a lithostratigraphic boundary above the target formation. Abstract: A demonstration project for the geological storage of CO2 is currently being considered in the deep Precipice Sandstone formation of the Surat Basin, Queensland, Australia. Because of the presence of potential fresh water resources in this formation, a reservoir-scale two-dimensional reactive-transport model was developed to assess temporal and spatial changes in water quality imposed by co-injecting CO2 with SO2, NO2, and O2 at this location. The model shows that because the injection rate is relatively low (60, 000 tons/year), flow is buoyancy-dominated and under these conditions the predicted CO2 flow pattern is quite sensitive to fine-scale heterogeneities and the resolution of the numerical mesh. The model also shows that SO2 and NO2 readily partition into the aqueous phase in close vicinity of their injection point, lowering pH somewhat beyond the acidification from CO2 dissolution. Only O2 under redox disequilibrium conditions is modeled to persist in the CO2 plume away from the injection point, however at sub-ppm levels. This modeling effort demonstrates acidification near the wellbore due to the preferential stripping of gas impurities, and accumulation of CO2 around a lithostratigraphic boundary above the target formation, where relatively rapid mineral dissolution (muscovite, chlorite and calcite) and precipitation (ankerite, kaolinite and chalcedony) occur.