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Evaluation of the inorganic water chemistry of the Vaal River

dc.contributor.advisorDennis, I.
dc.contributor.advisorHuizenga, J.M.
dc.contributor.authorMöhr, Angelika
dc.contributor.researchID21907609 - Huizenga, Jan Marten (Supervisor)
dc.contributor.researchID23616857 - Dennis, Ingrid (Supervisor)
dc.date.accessioned2015-11-30T14:18:32Z
dc.date.available2015-11-30T14:18:32Z
dc.date.issued2015
dc.descriptionMSc (Environmental Sciences), North-West University, Potchefstroom Campus, 2015en_US
dc.description.abstractOne of the most essential resources for life on our planet is water. A concern for water resource sustainability has shifted towards the sustainable development of clean water body resource (SWDF, 2009). Data for the Vaal River water chemistry is in abundance. However, research on the historic natural conditions influencing the inorganic water quality, is not as extensive. Inorganic data was obtained from the Department of Water Affairs, for the period 1972 to 2011, for identified monitoring stations along the Vaal River. Water quality was evaluated using various geochemical techniques to analyse the data. The results of the study indicate that the water chemistry of the Vaal River is controlled by: 1. Chemical weathering of siliceous sediment, intrusive igneous rocks and metamorphic rocks (Na+, K+, Mg2+, Ca2+ and (HCO3)-). 2. Anthropogenic influences increasing the sulphate (SO4) concentration There is no major increase in ion concentrations for the stations. However the concentrations of bicarbonate (HCO3)- and SO4 change as it progresses downstream from the first upstream station to the last downstream station. Based on the chemical characterisation, three groups have been identified. (1) Group 1 stations appear to suggest a higher influence in chemical weathering than the group 2 stations. (2) Group 2 stations appear to suggest a greater influence from SO4. (3) Group 3 stations appear to suggest an influence from both the bicarbonate and the SO4 influences. Geographically the chemical weathering is an indication of the three different groups with strong anthropogenic influences in the middle group. The water chemistry for the Vaal River is controlled by two processes, namely chemical weathering and anthropogenic influences. The prominent indication of the difference in these two influences can be seen between group 1 and group 2. A secondary conclusion indicates that a total dissolved solid (TDS) alone is not an accurate representation of anthropogenic influence (or poor water quality) on inorganic water quality of the Vaal River. The natural weathering or geological influences appears to play a more dominant role in certain sections or catchments with lower contributions from anthropogenic influences.en_US
dc.description.thesistypeMastersen_US
dc.identifier.urihttp://hdl.handle.net/10394/15424
dc.language.isoenen_US
dc.publisherNorth-West University
dc.subjectChemical weatheringen_US
dc.subjectHCO3en_US
dc.subjectAnthropogenicen_US
dc.subjectWater qualityen_US
dc.subjectAcid mine drainageen_US
dc.subjectGeochemical influenceen_US
dc.subjectGroundwateren_US
dc.subjectSurface wateren_US
dc.titleEvaluation of the inorganic water chemistry of the Vaal Riveren
dc.typeThesisen_US

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