Abstract

Early deployment of carbon dioxide storage is likely to focus on injection into mature oil reservoirs, most of which occur in carbonate rock units. Observations and modeling have shown how capillary trapping leads to the immobilization of CO2 in saline aquifers, enhancing the security and capacity of storage. There are, however, no observations of trapping in rocks with a mixed-wet-state characteristic of hydrocarbon-bearing carbonate reservoirs. Here, we found that residual trapping of supercritical CO2 in a limestone altered to a mixed-wet state with oil was significantly less than trapping in the unaltered rock. In unaltered samples, the trapping of CO2 and N2 were indistinguishable, with a maximum residual saturation of 24%. After the alteration of the wetting state, the trapping of N2 was reduced, with a maximum residual saturation of 19%. The trapping of CO2 was reduced even further, with a maximum residual saturation of 15%. Best-fit Land-model constants shifted from C = 1.73 in the water-wet rock to C = 2.82 for N2 and C = 4.11 for the CO2 in the mixed-wet rock. The results indicate that plume migration will be less constrained by capillary trapping for CO2 storage projects using oil fields compared with those for saline aquifers.

Highlights

  • The capture of carbon dioxide emitted from industrial processes and subsequent storage in subsurface geologic units has been identified as a key technology in the global reduction of anthropogenic CO2 emissions to the atmosphere.[1]

  • Saline aquifer storage presents the largest potential for global CO2 storage capacity,[12] and the focus of the previous observations has been on the characterization of rocks unaltered by hydrocarbons

  • The displacement followed the pattern of a rapid saturation maps show that CO2 and N2 were uniformly distributed in the core sample in central parts of the core where the residual trapping was characterized and not affected by mass transfer or gravity segregation

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Summary

Introduction

The capture of carbon dioxide emitted from industrial processes and subsequent storage in subsurface geologic units has been identified as a key technology in the global reduction of anthropogenic CO2 emissions to the atmosphere.[1]. Oil fields have a number of characteristics that could lead to their having an outsize importance during the early deployment of carbon storage

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