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dc.contributor.authorAmarasinghe, Widuramina
dc.contributor.authorFjelde, Ingebret
dc.contributor.authorGiske, Nils Harald
dc.contributor.authorGuo, Ying
dc.date.accessioned2021-08-25T07:31:22Z
dc.date.available2021-08-25T07:31:22Z
dc.date.created2021-08-09T16:12:13Z
dc.date.issued2021
dc.identifier.issn1996-1073
dc.identifier.urihttps://hdl.handle.net/11250/2771076
dc.description.abstractDuring CO2 storage, CO2 plume mixes with the water and oil present at the reservoir, initiated by diffusion followed by a density gradient that leads to a convective flow. Studies are available where CO2 convective mixing have been studied in water phase but limited in oil phase. This study was conducted to reach this gap, and experiments were conducted in a vertically packed 3-dimensional column with oil-saturated unconsolidated porous media at 100 bar and 50 °C (representative of reservoir pressure and temperature conditions). N-Decane and crude oil were used as oils, and glass beads as porous media. A bromothymol blue water solution-filled sapphire cell connected at the bottom of the column was used to monitor the CO2 breakthrough. With the increase of the Rayleigh number, the CO2 transport rate in n-decane was found to increase as a function of a second order polynomial. Ra number vs. dimensionless time τ had a power relationship in the form of Ra = c×τ−n. The overall pressure decay was faster in n-decane compared to crude oil for similar permeability (4 D), and the crude oil had a breakthrough time three times slower than in n-decane. The results were compared with similar experiments that have been carried out using water.en_US
dc.language.isoengen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleCO2 Convective Dissolution in Oil-Saturated Unconsolidated Porous Media at Reservoir Conditionsen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.rights.holderCopyright © 2021, Author(s)
dc.description.versionpublishedVersionen_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.doi10.3390/en14010233
dc.identifier.cristin1924833
dc.source.journalEnergiesen_US


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