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CO2 Field Lab at Svelvik Ridge: Site Suitability

dc.contributor.authorBakk, Audun
dc.contributor.authorGirard, Jean-Francois
dc.contributor.authorLindeberg, Erik Gøsta Brun
dc.contributor.authorAker, Eyvind
dc.contributor.authorWertz, Frederic
dc.contributor.authorBuddensiek, Maike-Liselotte
dc.contributor.authorBarrio, Maria
dc.contributor.authorJones, David
dc.date.accessioned2016-11-03T06:45:13Z
dc.date.accessioned2017-01-19T14:27:00Z
dc.date.available2016-11-03T06:45:13Z
dc.date.available2017-01-19T14:27:00Z
dc.date.issued2012
dc.identifier.citationEnergy Procedia 2012, 23:306-312nb_NO
dc.identifier.issn1876-6102
dc.identifier.urihttp://hdl.handle.net/11250/2427870
dc.description-nb_NO
dc.description.abstractA field laboratory for monitoring CO2 migration has been established in the Holocene deposit of the Svelvik ridge, located at the sill of the Drammensfjord 50 km south of Oslo. Initial characterization of the site shows that the formation is very suitable for studying migration and associated leakage, particularly within the top 50 m where the sediments consist of relatively homogenous sand. In the deeper part of the deposit, the formation seems to have more structure possibly enabling monitoring of horizontal migration and more complex migration patterns. Copyright © 2012 Published by Elsevier Ltd.nb_NO
dc.language.isoengnb_NO
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/deed.no*
dc.titleCO2 Field Lab at Svelvik Ridge: Site Suitabilitynb_NO
dc.typeJournal articlenb_NO
dc.typePeer reviewednb_NO
dc.date.updated2016-11-03T06:45:13Z
dc.rights.holder© 2012 The Authorsnb_NO
dc.source.pagenumber306-312nb_NO
dc.source.volume23nb_NO
dc.source.journalEnergy Procedianb_NO
dc.identifier.doi10.1016/j.egypro.2012.06.055
dc.identifier.cristin943017


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Attribution-NonCommercial-NoDerivatives 4.0 Internasjonal
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