Investigation of the hydrogeochemical processes in an alluvial channel aquifer located in a typical Karoo Basin of Southern Africa

• Published in: Environmental earth sciences 2013-09, Vol.70 (1), p.227-238
• Main Authors: Gomo, M, van Tonder, G. J, Steyl, G
• Format: Article
• Language: English
• Subjects: Alluvial aquifers; Alluvial channels; Aquifer systems; Aquifers; Biogeosciences; Calcite; Dolomite; Dry season; Earth and Environmental Science; Earth Sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Environmental Science and Engineering; Exact sciences and technology; Geochemistry; Geology; Groundwater; Groundwater data; Hydrogeology; Hydrology; Hydrology. Hydrogeology; Hydrology/Water Resources; Ion exchange; Minerals; Original Article; oxides; Pollution, environment geology; Quartz; sediments; silicon; sodium; Spectrometry; spectroscopy; Terrestrial Pollution; Unconsolidated aquifers; Water quality; X-radiation; X-ray diffraction
• ISSN: 1866-6280; 1866-6299
• DOI: 10.1007/s12665-012-2118-9

An investigation was conducted to assess the hydrogeochemical processes of an alluvial channel aquifer located in a typical Karoo Basin of Southern Africa. The investigation was aimed at identifying and describing the groundwater chemistry evolution and its contribution to the overall groundwater quality. X-ray fluorescent spectrometry (XRF) and X-ray diffractometry (XRD) analyses were performed on geological samples to identify and quantify the major element oxides and minerals. The study utilises the conventional Piper diagram, bivariate plots and PHREEQC hydrogeochemical model to analyse groundwater chemistry data obtained during the wet (February and May) and dry seasons (August and December) of 2011. The XRF and XRD results show that the channel deposits are dominated by SiO₂ element oxides and quartz minerals, thus elevated concentrations of silicon (Si⁴⁺) were found in the groundwater. Dolomite and calcite minerals were also detected in the unconsolidated aquifer sediments. The detailed study of the alluvial aquifer system has shown that dissolution of dolomite and calcite minerals and ion exchange are the dominant hydrogeochemical processes influencing the groundwater quality. The groundwater evolves from Ca²⁺–Mg²⁺–HCO₃ ⁻ recharge water that goes through ion exchange with Na⁺ in the clay-silt sediment to give a Na⁺–HCO₃ ⁻ water type. The groundwater is supersaturated with respect to quartz, dolomite and calcite minerals. The study shows the potential usefulness of simple bivariate plots as a complimentary tool to the conventional methods for analyzing groundwater hydrogeochemical processes.