Dept. of Civil and Environmental Engineering, Universitat Politècnica de Catalunya, Jordi Girona 1–3, 08034 Barcelona, Spain
Associated Unit: Hydrogeology Group (UPC-CSIC), Barcelona, Spain
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Total article views: 748 (including HTML, PDF, and XML)
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Total article views: 525 (including HTML, PDF, and XML)
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525
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Cumulative views and downloads
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Viewed (geographical distribution)
Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 748 (including HTML, PDF, and XML)
Thereof 748 with geography defined
and 0 with unknown origin.
Total article views: 525 (including HTML, PDF, and XML)
Thereof 525 with geography defined
and 0 with unknown origin.
Total article views: 223 (including HTML, PDF, and XML)
Thereof 222 with geography defined
and 1 with unknown origin.
During geological carbon sequestration, the injected supercritical CO2, being less dense, floats above the brine. The dissolution of CO2 into brine helps mitigate the risk of CO2 leakage. As CO2 dissolves into the brine, it increases the density of brine in the upper layer, initiating gravity-driven convection (GDC), which significantly enhances the rate of CO2 dissolution. We derived two empirical formulas to predict the asymptotic dissolution rate driven by GDC in heterogeneous fields.
During geological carbon sequestration, the injected supercritical CO2, being less dense, floats...