Noble gas and radiocarbon constraints on the residence times of groundwater in and around the City of Cape Town

dc.contributor.advisorMiller, Jodie A.en_ZA
dc.contributor.authorHarilall, Zitaen_ZA
dc.contributor.otherStellenbosch University. Faculty of Science. Dept. of Earth Sciences.en_ZA
dc.descriptionThesis (MSc)--Stellenbosch University, 2020.en_ZA
dc.description.abstractENGLISH ABSTRACT: The TMG Aquifer is one of the largest aquifer systems in the country and is currently targeted as a potential source of potable water for the City of Cape Town (CoCT) in times of water stress. This study has aimed to provide proper constraints on turnover time of groundwater in the aquifer system before large-scale abstraction takes place, in order to evaluate the sustainability of the resource. This study has used the 3H/3He system to date modern water (<100 years) and 14C to date older groundwater (>500 years). Groundwater residence times were determined for six aquifers in the Western Cape, namely the alluvial, Witteberg, Bokkeveld, TMG, Cape Granite Suite (CGS) and Malmesbury aquifers. Noble gas and radiocarbon dating of the TMG Aquifer range from 0.3 – 44.6 and <70 – 1 626 years, respectively. Residence times calculated for the alluvial aquifer are also relatively young, ranging from 0.0 – 1 783 years. Good correlation between 3H/3He and 14C ages indicate relatively short residence times for the alluvial and TMG aquifers whereas groundwater from the Witteberg (6 699 years), Bokkeveld (58.5 – 6 038 years), CGS (3.7 – 8 648 years) and Malmesbury (45.5 – 11 146 years) aquifers indicate mixing of older water bodies with modern recharge resulting in distinctly different ages derived from the two dating systems. Noble gas recharge temperatures (9.4 – 28.6°C), 3H and 14C activities suggest that groundwater in the region is primarily recharged at high elevations, but also that rainfall events further down the flow path at lower elevations, make substantial contributions to groundwater recharge. Evaluation of isotopic tracers and basic chemistry have led to the identification of potential proxies for residence time, namely pH, HCO3- concentrations and Ca/Mg ratios. These components can be used to make assumptions on groundwater residence times without the costly process of analysis. Residence times indicate short turnover times for groundwater in the TMG Aquifer (typically <130 years) which suggest that the aquifer would be susceptible to climate change. Projected reductions in precipitation and regular occurrences of droughts would likely diminish groundwater supplies in the aquifer system. If large-scale abstraction does commence, this needs to be factored into abstraction regimes as unsustainable abstraction practices could lead to groundwater depletion.en_ZA
dc.description.abstractAFRIKAANSE OPSOMMING: Geen opsommingaf_ZA
dc.format.extentxii, 134 leaves : illustrations (some color), maps (some color)
dc.publisherStellenbosch : Stellenbosch Universityen_ZA
dc.subjectTMG Aquiferen_ZA
dc.subjectRadiocarbon datingen_ZA
dc.subjectNoble gas datingen_ZA
dc.subjectAquifers -- South Africa -- Western Capeen_ZA
dc.subjectGroundwater ecology -- South Africa -- Western Capeen_ZA
dc.subjectWater-supply -- Cape Town -- Sustainabilityen_ZA
dc.subjectGroundwater recharge -- Measurementen_ZA
dc.titleNoble gas and radiocarbon constraints on the residence times of groundwater in and around the City of Cape Townen_ZA
dc.rights.holderStellenbosch Universityen_ZA

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