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dc.contributor.authorHvidevold, Hilde Kristineeng
dc.contributor.authorAlendal, Guttormeng
dc.contributor.authorJohannessen, Trulseng
dc.contributor.authorMannseth, Trondeng
dc.date.accessioned2015-04-10T09:15:08Z
dc.date.available2015-04-10T09:15:08Z
dc.date.issued2013eng
dc.identifier.issn1876-6102en_US
dc.identifier.urihttps://hdl.handle.net/1956/9745
dc.description.abstractThis paper assesses how parameter uncertainties in the model for rise velocity of CO2 droplets in the ocean cause uncertainties in their rise and dissolution in marine waters. The parameter uncertainties in the rise velocity for both hydrate coated and hydrate free droplets are estimated from experiment data. Thereafter the rise velocity is coupled with a mass transfer model to simulate the fate of dissolution of a single droplet. The assessment shows that parameter uncertainties are highest for large droplets. However, it is also shown that in some circumstances varying the temperature gives significant change in rise distance of droplets.en_US
dc.language.isoengeng
dc.publisherElsevieren_US
dc.relation.ispartof<a href="http://hdl.handle.net/1956/11211" target="_blank">Quantifying uncertainties when monitoring marine environments in connection with geological storage of CO2</a>en_US
dc.rightsAttribution-NonCommercial-NoDerivs CC BY-NC-NDeng
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/eng
dc.subjectGeological Storageeng
dc.subjectLeakage to Marine Environmenteng
dc.subjectCO2 Dropletseng
dc.subjectParameter Uncertaintieseng
dc.subjectRise and Dissolution of CO2eng
dc.titleAssessing Model Uncertainties Through Proper Experimental Designen_US
dc.typePeer reviewed
dc.typeJournal article
dc.date.updated2015-04-01T08:22:34Zen_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2013 The Authorsen_US
dc.identifier.doihttps://doi.org/10.1016/j.egypro.2013.06.233
dc.identifier.cristin1051934
dc.source.journalEnergy Procedia
dc.source.4037
dc.source.pagenumber3439-3446


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