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dc.contributor.advisorJovanovic, Nebo
dc.contributor.authorMajola, Kwazikwakhe Alfred
dc.date.accessioned2014-09-23T13:27:40Z
dc.date.available2014-09-23T13:27:40Z
dc.date.issued2008
dc.identifier.urihttp://hdl.handle.net/11394/3691
dc.descriptionMagister Scientiae - MScen_US
dc.description.abstractThe objectives of this study were: To review and understand flow and transport processes in unsaturated zones. In this study, particular emphasis is placed on understanding mechanisms that cause non-uniform (preferential) flow for two casestudies, namely the Cape Flats sandy environment and the Mpumalanga Highveld fractured rock environment. To evaluate the adequacy of models, in particular MACRO 5.0, in simulating flow and transport in the vadose zone, by making use of two case study sites (Cape Flats and Mpumalanga Highveld). Of particular importance is the evaluation of transfer coefficients to represent fluid and solute exchange between macropores and matrix. To run a sensitivity analysis with MACRO 5.0 in order determine which input model parameters are the most relevant in describing the effects of preferential flow in water and solute transport.en_US
dc.language.isoenen_US
dc.subjectPreferential flowen_US
dc.subjectModellingen_US
dc.subjectVadose zoneen_US
dc.subjectPorous sandsen_US
dc.subjectClaysen_US
dc.subjectMacro 5.0en_US
dc.subjectCape flats districten_US
dc.subjectMpumalanga highveld (Secunda)en_US
dc.subjectGroundwater vulnerabilityen_US
dc.titlePreferential flow modelling in a vadose zone using macro 5.0 – Cape flats porous sands and Mpumalanga highveld clays case studiesen_US
dc.rights.holderuwcen_US


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