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Sedimentation and chemical processes on the Lower Mkuze floodplain : implications for wetland structure and function

dc.contributor.authorHumphries, Marc
dc.date.accessioned2010-08-20T10:14:52Z
dc.date.available2010-08-20T10:14:52Z
dc.date.issued2008
dc.descriptionThesis (Ph.D)-University of KwaZulu-Natal, Westville, 2008.en_US
dc.description.abstractThe Mkuze Wetland System, situated in northern KwaZulu-Natal, is South Africa’s largest freshwater wetland area. The system plays a vital role in the functioning of the local landscape and has been identified as an important site for the retention of a number of solutes. The mechanisms through which this retention occurs were investigated through analysis of sediment, groundwater and porewater samples collected from the lower floodplain. Sample analysis was achieved through the use of several techniques, including Inductively Coupled Plasma-Optical Emission Spectroscopy (ICP-OES), X-ray Diffraction (XRD), X-ray Fluorescence (XRF), electron microscopy and sequential extraction.
dc.identifier.urihttp://hdl.handle.net/10413/430
dc.language.isoenen_US
dc.subjectWetland hydrology--KwaZulu-Natal.en_US
dc.subjectWater--Analysis.en_US
dc.subjectTheses--Chemistry.en_US
dc.titleSedimentation and chemical processes on the Lower Mkuze floodplain : implications for wetland structure and functionen_US
dc.typeThesisen_US

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