SPE Annual Technical Conference and Exhibition 2006
DOI: 10.2118/102796-ms
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Scaling Analysis of the Migration of CO2 in Saline Aquifers

Abstract: TX 75083-3836, U.S.A., fax 01-972-952-9435.Abstract CO 2 storage in saline aquifers may be used to reduce greenhouse gas emissions. After injection the CO 2 -plume migrates along the top of the aquifer for hundreds to thousands of years. An estimate of the area invaded by the CO 2 -plume is of interest for site selection. During plume migration, CO 2 is trapped as residual gas in the wake of the plume. Reduction of the mobile CO 2 volume by residual trapping would limit potential leakage.Plume evolution can be… Show more

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Cited by 64 publications
(38 citation statements)
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“…The density difference results in gas override, which leads to poor reservoir sweep by injected fluids. This buoyancy effect has been investigated for CO 2 in aquifers (Hesse et al 2006;Silin et al 2006;Møll Nilsen et al 2011). Injected CO 2 rises to the top of the reservoir until it reaches a low-permeability caprock, where it spreads out as a mobile plume of dense gas.…”
Section: Introductionmentioning
confidence: 99%
“…The density difference results in gas override, which leads to poor reservoir sweep by injected fluids. This buoyancy effect has been investigated for CO 2 in aquifers (Hesse et al 2006;Silin et al 2006;Møll Nilsen et al 2011). Injected CO 2 rises to the top of the reservoir until it reaches a low-permeability caprock, where it spreads out as a mobile plume of dense gas.…”
Section: Introductionmentioning
confidence: 99%
“…Integration over the vertical section is used to obtain vertically averaged (lumped) properties and pseudofunctions. Such models are widely used to describe carbon dioxide sequestration in brine aquifers (Gasda et al 2007;Hesse et al 2006;Ligaarden and Nilsen 2010). Lake (1989) presented a detailed discussion of the different cases of vertical equilibrium.…”
Section: Introductionmentioning
confidence: 99%
“…This process occurs at the trailing edge of the plume as the CO 2 migrates upward, when it is displaced by natural groundwater flow or by the injection of chase brine. It is a rapid and effective trapping mechanism that reduces the need to ensure caprock integrity (Kumar et al 2005;Hesse et al 2006;Obi and Blunt 2006;Juanes et al 2006;Ide et al 2007;Qi et al 2009;Saadatpoor et al 2008). In addition, the process can be designed such that capillary trapping is maximized.…”
Section: Introductionmentioning
confidence: 99%