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Ocean release of fossil fuel CO2: A case study

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dc.contributor.author Drange, Helge eng
dc.contributor.author Alendal, Guttorm eng
dc.contributor.author Johannessen, Ola M. eng
dc.date.accessioned 2005-04-26T13:04:29Z
dc.date.available 2005-04-26T13:04:29Z
dc.date.issued 2001-07-01 eng
dc.identifier.citation Geophysical Research Letters 28(13): 2637-2640
dc.identifier.issn 0094-8276 eng
dc.identifier.uri http://hdl.handle.net/1956/657
dc.description.abstract The natural ocean uptake of the greenhouse gas CO2 can be accelerated by collecting and liquefying the gas from point sources, and by pumping it into the ocean at appropriate locations and at sufficient depths. Results from a numerical modelling system indicate that injection sites located at about 1,000 m depth in the eastern Norwegian Sea lead to efficient and long term sequestration in the abyss Atlantic. For a release rate corresponding to the CO2 emissions from a 220 MW gas power plant, it is found that the volume of the near-source water with a pH-reduction ≥ 0.1 is ~0.5 km³. These findings, together with available technology and feasible economics, indicate that the Norwegian Sea represents a possible location for large scale demonstration of operational ocean release of CO2. en
dc.format.extent 337551 bytes eng
dc.format.mimetype application/pdf eng
dc.language.iso eng eng
dc.publisher American Geophysical Union eng
dc.subject Global Change: General or miscellaneous eng
dc.subject Oceanography: Biological and chemical eng
dc.subject Carbon cycling eng
dc.subject Modeling eng
dc.title Ocean release of fossil fuel CO2: A case study eng
dc.type Journal article eng
dc.rights.holder Copyright 2001 by the American Geophysical Union
dc.type.version publishedVersion eng
bora.peerreviewed Peer reviewed eng
bora.journalTitle Geophysical Research Letters eng
bibo.volume 28 eng
bibo.issue 13 eng
bibo.pageStart 2637 eng
bibo.pageEnd 2640 eng
bibo.doi http://dx.doi.org/10.1029/2000GL012609 eng
dc.identifier.doi http://dx.doi.org/10.1029/2000GL012609


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