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dc.contributor.authorAlmenningen, Stian
dc.contributor.authorGraue, Arne
dc.contributor.authorErsland, Geir
dc.date.accessioned2022-01-31T13:21:15Z
dc.date.available2022-01-31T13:21:15Z
dc.date.created2021-03-02T09:31:05Z
dc.date.issued2021
dc.identifier.issn0887-0624
dc.identifier.urihttps://hdl.handle.net/11250/2976024
dc.description.abstractSequestration of CO2 in natural gas hydrate reservoirs may offer stable long-term deposition of a greenhouse gas while benefiting from CH4 gas production. In this paper, we review old and present new experimental studies of CH4–CO2 exchange in CH4 hydrate-bearing sandstone core plugs. CH4 hydrate was formed in Bentheim sandstone core plugs to prepare for subsequent lab-scale CH4 gas production by CO2 replacement. The effect of temperature, diffusion length, salinity, water saturation, CH4 hydrate saturation, and co-injection of chemicals (N2 and monoethanolamine) with the injected CO2 were measured. The measurements prove the critical role of water saturation in these processes: formation of CO2 hydrate severely reduced the injectivity for water saturations above 0.1 fractions. The results presented in this paper are important when assessing natural gas hydrate reservoirs as candidates for CO2 injection with concurrent CH4 gas production.en_US
dc.language.isoengen_US
dc.publisherAmerican Chemical Societyen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleExperimental Investigation of Critical Parameters Controlling CH4− CO2 Exchange in Sedimentary CH4 Hydratesen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2021 American Chemical Societyen_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.doi10.1021/acs.energyfuels.0c03841
dc.identifier.cristin1894772
dc.source.journalEnergy & Fuelsen_US
dc.source.pagenumber2468-2477en_US
dc.identifier.citationEnergy & Fuels. 2021, 35 (3), 2468-2477.en_US
dc.source.volume35en_US
dc.source.issue3en_US


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