Behavior of CO₂/water flow in porous media for CO₂ geological storage

A clear understanding of two-phase fluid flow properties in porous media is of importance to CO₂ geological storage. The study visually measured the immiscible and miscible displacement of water by CO₂ using MRI (magnetic resonance imaging), and investigated the factor influencing the displacement process in porous media which were filled with quartz glass beads. For immiscible displacement at slow flow rates, the MR signal intensity of images increased because of CO₂ dissolution; before the dissolution phenomenon became inconspicuous at flow rate of 0.8mLmin^-1. For miscible displacement, the MR signal intensity decreased gradually independent of flow rates, because supercritical CO₂ and water became miscible in the beginning of CO₂ injection. CO₂ channeling or fingering phenomena were more obviously observed with lower permeable porous media. Capillary force decreases with increasing particle size, which would increase permeability and allow CO₂ and water to invade into small pore spaces more easily. The study also showed CO₂ flow patterns were dominated by dimensionless capillary number, changing from capillary finger to stable flow. The relative permeability curve was calculated using Brooks-Corey model, while the results showed the relative permeability of CO₂ slightly decreases with the increase of capillary number.