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- W2890210446 abstract "Abstract During geological storage in deep saline aquifers, immobilization of CO 2 in reservoir rock determines both storage safety and capacity. Assessment of the sensitivity of residual trapping to different parameters (interfacial tension and contact angles) and the storage conditions affecting these is therefore of great importance. One aspect of concern is the presence of co‐contaminants such as SO 2 in the injected gas. Using experimentally measured values of interfacial tensions and contact angles, we apply pore‐network modelling (which accounts for pore‐scale mechanisms such as snap‐off, cooperative pore body filling and piston‐type displacement) to a generic sandstone network to quantify the impact of SO 2 co‐injection on residual CO 2 trapping, and its relative importance as compared to the influences of thermodynamic conditions and salinity. We show that the presence of small amounts of SO 2 in the injected CO 2 has a notable positive effect on the amount of CO 2 becoming residually trapped (∼3% increase at 1 wt% SO 2 ). However, this effect is small compared to that of the brine salinity (∼20% decrease in residually trapped CO 2 over the salinity range 0.2 to 5 M NaCl). Still, co‐injection of SO 2 could potentially favour the residual trapping of CO 2 in reservoir rocks, especially at storage sites with inclined aquifers where the CO 2 is set to migrate hydro‐dynamically over long distances. The salinity of the resident brine is of primary importance during storage site selection. Furthermore, sensitivity analysis shows that the advancing contact angle strongly impacts residual CO 2 trapping. © 2018 Society of Chemical Industry and John Wiley & Sons, Ltd." @default.
- W2890210446 created "2018-09-27" @default.
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- W2890210446 date "2018-09-07" @default.
- W2890210446 modified "2023-09-25" @default.
- W2890210446 title "The impact of co-contaminant SO<sub>2</sub> , versus salinity and thermodynamic conditions, on residual CO<sub>2</sub> trapping during geological storage" @default.
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- W2890210446 doi "https://doi.org/10.1002/ghg.1816" @default.
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