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dc.contributor.authorFraser, Michael
dc.date.accessioned2012-10-30T12:58:05Z
dc.date.available2012-10-30T12:58:05Z
dc.date.issued2012-10-30
dc.identifier.urihttp://hdl.handle.net/10222/15667
dc.description.abstractIt has been demonstrated that nitrogen fixation is a source of hydrogen (H2) to the ocean and therefore measurements of H2 concentrations may be used as a possible indicator of nitrogen fixation (Moore, Punshon, Mahaffey, & Karl, 2009). However, the limited number and sparse distribution of measurements of dissolved hydrogen and nitrogen fixation rates made in the open ocean in the past have made it difficult to quantify the relationship between them. Toward this end, a new method of equilibrating seawater samples for H2 measurement was employed along the 13,000 km Atlantic Meridional Transect (AMT20) from UK to Chile, allowing H¬2 to be measured from underway samples every 3.5 minutes and thereby considerably increasing the number and resolution of H2 measurements made in the open ocean.These high-resolution measurements reveal two regions with high H¬2 concentrations, one in the North Atlantic and one in the South Atlantic.en_US
dc.language.isoenen_US
dc.subjectNorth Atlanticen_US
dc.subjectSouth Atlanticen_US
dc.subjecthydrogenen_US
dc.subjectindicatoren_US
dc.subjecttrace gasesen_US
dc.subjectnitrogen fixationen_US
dc.titleHydrogen supersaturations in the North and South Atlantic - a possible indicator of nitrogen fixation.en_US
dc.date.defence2012-09-18
dc.contributor.departmentDepartment of Oceanographyen_US
dc.contributor.degreeMaster of Scienceen_US
dc.contributor.external-examinerDr Maurice Levasseuren_US
dc.contributor.graduate-coordinatorDr Daniel Kelleyen_US
dc.contributor.thesis-readerDr John Cullenen_US
dc.contributor.thesis-readerDr Markus Kienasten_US
dc.contributor.thesis-supervisorDr Robert Mooreen_US
dc.contributor.ethics-approvalNot Applicableen_US
dc.contributor.manuscriptsNot Applicableen_US
dc.contributor.copyright-releaseNot Applicableen_US
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