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dc.contributor.authorMartin, Leslie Ann
dc.date.accessioned2014-03-04T03:21:36Z
dc.date.available2014-03-04T03:21:36Z
dc.date.issued2008-05
dc.identifier.othermartin_leslie_a_200805_ms
dc.identifier.urihttp://purl.galileo.usg.edu/uga_etd/martin_leslie_a_200805_ms
dc.identifier.urihttp://hdl.handle.net/10724/24690
dc.description.abstractTurbidity levels at baseflow conditions were examined in relation to a gradient of land use/land cover types, topography, and stream density in 30 drainage basins within the upper Little Tennessee River watershed. Baseflow turbidity at each site was sampled on 11 separate occasions between November 2006 and May 2007. Relationships between baseflow turbidity and 27 independent variables were explored through correlation, linear regression and forward stepwise multiple regression. The watershed variables could be reduced to three components which explained 73% of the variance in baseflow turbidity, with pasture land cover demonstrating the greatest effect. A better understanding of the relationship between basin-scale land use and baseflow turbidity is essential to providing specific guidance on drainage basin alterations most detrimental to stream quality.
dc.languageeng
dc.publisheruga
dc.rightspublic
dc.subjectbaseflow
dc.subjectturbidity
dc.subjectsuspended sediment
dc.subjectland use
dc.subjectland cover
dc.subjectBlue Ridge
dc.subjectLittle Tennessee River
dc.titleBaseflow turbidity of tributaries to the upper Little Tennessee River, North Carolina and Georgia
dc.typeThesis
dc.description.degreeMS
dc.description.departmentGeography
dc.description.majorGeography
dc.description.advisorDavid Leigh
dc.description.committeeDavid Leigh
dc.description.committeeRhett Jackson
dc.description.committeeGeorge Brook


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