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dc.contributor.authorMcKinley, Robert Ashley
dc.date.accessioned2014-03-04T20:21:47Z
dc.date.available2014-03-04T20:21:47Z
dc.date.issued2011-08
dc.identifier.othermckinley_robert_a_201108_ms
dc.identifier.urihttp://purl.galileo.usg.edu/uga_etd/mckinley_robert_a_201108_ms
dc.identifier.urihttp://hdl.handle.net/10724/27535
dc.description.abstractSediment fingerprinting is a relatively recent technique capable of determining the origin of suspended sediment. The objective of this study was to examine spatial variations in the origin of suspended sediments and to test a streamlined fingerprinting approach which would reduce the cost. Samples were collected from three tributaries, the outlet of the main stem, and at the middle of the main stem. Two methods to collect suspended sediment samples were compared: a mobile continuous flow centrifuge and automated samplers. A relatively small initial tracer suite consisting of 15N, 13C, TN, and TC was employed in tracer selection. Results using a multivariate mixing model showed that banks contributed the majority of sediment throughout all locations sampled. The use of the streamlined approach should allow for the adoption of sediment fingerprinting as an operational tool for state agencies in the Southern Piedmont wishing to utilize it in TMDL/BMP evaluations.
dc.languageeng
dc.publisheruga
dc.rightspublic
dc.subjectSediment Fingerprinting, TMDL, Sediment Load, Uncertainty Analysis
dc.titleInvestigating spatial variations in sediment origin using a streamlined sediment fingerprinting approach in a southern Piedmont watershed
dc.typeThesis
dc.description.degreeMS
dc.description.departmentCrop and Soil Sciences
dc.description.majorCrop and Soil Sciences
dc.description.advisorDavid E. Radcliffe
dc.description.committeeDavid E. Radcliffe
dc.description.committeeMark Risse
dc.description.committeeTodd C. Rasmussen


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