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dc.contributor.authorBiladeau, Christine
dc.date.accessioned2008-07-18T22:16:15Z
dc.date.available2008-07-18T22:16:15Z
dc.date.issued2008-06-19
dc.identifier.citationKeil R., Kelley D., D'Asaro E., Krembs C., and Collins R.E. [Eds.] 2008. Proceedings from the University of Washington School of Oceanography Undergraduate Thesis Research Expedition to Glacier Bay Alaska, March 2008. 296pp.en
dc.identifier.urihttp://hdl.handle.net/1773/3752
dc.description.abstractThe rate at which sediments accumulate in marine waters affects benthic life and sequestration of organic carbon and PAHs. The instantaneous sediment accumulation in Glacier Bay was measured and found to be slower in March than an earlier study found it in July and August. A greater influx of freshwater in summer is presumed to explain the difference. Glacier Bay, relative to its size, buries six times more organic carbon than is estimated.en
dc.language.isoen_USen
dc.publisherSchool of Oceanography, University of Washingtonen
dc.subjectSedimentation and deposition--Alaska--Glacier Bayen
dc.subjectMarine sediments--analysis--methodologyen
dc.titleInstantaneous sediment accumulation rates in Tarr Inlet, Glacier Bay, Alaskaen
dc.typeOtheren


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