Please use this identifier to cite or link to this item: https://hdl.handle.net/20.500.14279/14226
DC FieldValueLanguage
dc.contributor.authorSarris, Ernestos-
dc.contributor.authorGravanis, Elias-
dc.contributor.authorPapanastasiou, Panos-
dc.date.accessioned2019-07-01T10:29:22Z-
dc.date.available2019-07-01T10:29:22Z-
dc.date.issued2014-07-
dc.identifier.citationTransport in Porous Media, 2014, vol. 103, no. 3, pp. 341-359en_US
dc.identifier.issn15731634-
dc.description.abstractIn this work, we investigate numerically the injection of supercritical carbon dioxide into a deep saline reservoir from a single well. We analyze systematically the sharp-interface evolution in different flow regimes. The flow regimes can be parameterized by two dimensionless numbers, the gravity number, Γ and the mobility ratio, λ. Numerical simulations are performed using the volume of fluid method, and the results are compared with the solutions of the self-similarity equation established in previous works, which describes the evolution of the sharp interface. We show that these theoretical solutions are in very good agreement with the results from the numerical simulations presented over the different flow regimes, thereby showing that the theoretical and simulation models predict consistently the spreading and migration of the created CO2 plume under complex flow behavior in porous media. Furthermore, we compare the numerical results with known analytic approximations in order to assess their applicability and accuracy over the investigated parametric space. The present study indicates that the self-similar solutions parameterized by the dimensionless numbers λ, Γ are significant for examining effectively injection scenarios, as these numbers control the shape of the interface and migration of the CO2 plume. This finding is essential in assessing the storage capacity of saline aquifers. © 2014 Springer Science+Business Media Dordrecht.en_US
dc.formatpdfen_US
dc.language.isoenen_US
dc.relation.ispartofTransport in Porous Mediaen_US
dc.rights© Springer Natureen_US
dc.subjectPorous mediaen_US
dc.subjectSaline aquiferen_US
dc.subjectVOF methoden_US
dc.titleInvestigation of Self-Similar Interface Evolution in Carbon Dioxide Sequestration in Saline Aquifersen_US
dc.typeArticleen_US
dc.collaborationUniversity of Cyprusen_US
dc.collaborationCyprus University of Technologyen_US
dc.subject.categoryCivil Engineeringen_US
dc.journalsHybrid Open Accessen_US
dc.countryCyprusen_US
dc.subject.fieldEngineering and Technologyen_US
dc.publicationPeer Revieweden_US
dc.identifier.doi10.1007/s11242-014-0304-9en_US
dc.identifier.scopus2-s2.0-84901945729-
dc.identifier.urlhttps://api.elsevier.com/content/abstract/scopus_id/84901945729-
dc.relation.issue3en_US
dc.relation.volume103en_US
cut.common.academicyear2013-2014en_US
dc.identifier.spage341en_US
dc.identifier.epage359en_US
item.fulltextNo Fulltext-
item.cerifentitytypePublications-
item.grantfulltextnone-
item.openairecristypehttp://purl.org/coar/resource_type/c_6501-
item.openairetypearticle-
item.languageiso639-1en-
crisitem.journal.journalissn1573-1634-
crisitem.journal.publisherSpringer Nature-
crisitem.author.deptDepartment of Civil Engineering and Geomatics-
crisitem.author.facultyFaculty of Engineering and Technology-
crisitem.author.orcid0000-0002-5331-6661-
crisitem.author.parentorgFaculty of Engineering and Technology-
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