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Salinisation source(s) and mechanism(s) in shallow alluvial aquifers along the Buffels River, Northern Cape Province, South Africa

Thesis (MSc)--Stellenbosch University, 2015.

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Main Author: Nakwafila, Albertina Nuusiku
Other Authors: Miller, Jodie A.
Format: Thesis
Language:en_ZA
Published: Stellenbosch : Stellenbosch University 2015
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access_status_str Open Access
author Nakwafila, Albertina Nuusiku
author2 Miller, Jodie A.
author_browse Miller, Jodie A.
Nakwafila, Albertina Nuusiku
author_facet Miller, Jodie A.
Nakwafila, Albertina Nuusiku
author_sort Nakwafila, Albertina Nuusiku
collection Thesis
dc_rights_str_mv Stellenbosch University
description Thesis (MSc)--Stellenbosch University, 2015.
format Thesis
id oai:scholar.sun.ac.za:10019.1/96826
institution Stellenbosch University (South Africa)
language en_ZA
last_indexed 2026-06-10T12:46:43.557Z
license_str Other — see source repository
provenance_str_mv Harvested via OAI-PMH from SUNScholar — Stellenbosch University Repository
publishDate 2015
publishDateRange 2015
publishDateSort 2015
publisher Stellenbosch : Stellenbosch University
publisherStr Stellenbosch : Stellenbosch University
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source_str SUNScholar — Stellenbosch University Repository
spelling oai:scholar.sun.ac.za:10019.1/96826 Salinisation source(s) and mechanism(s) in shallow alluvial aquifers along the Buffels River, Northern Cape Province, South Africa Nakwafila, Albertina Nuusiku Miller, Jodie A. Clarke, Catherine E. Stellenbosch University. Faculty of Science. Dept. of Earth Sciences. Aquifers -- South Africa -- Namaqualand Salinisation -- South Africa -- Namaqualand Groundwater -- South Africa -- Namaqualand Stable isotopes UCTD Groundwater recharge -- South Africa -- Namaqualand Buffels River Catchment (South Africa) Thesis (MSc)--Stellenbosch University, 2015. ENGLISH ABSTRACT: Several areas in Namaqualand are affected by elevated levels of salinity; including the shallow alluvial aquifers along the Buffels River catchment. The chemistry of rainwater that recharges these aquifers has low salt-loads, but the groundwater system is very saline. The shallow alluvial aquifers are an important source of water for several communal areas along the river both for domestic and agricultural purposes. Groundwater is also used for the copper and diamond mining activities along the river. Prior to this study, the sources of salinity to the alluvial aquifers and whether salinity can be remediated has not been determined. Possible salinity sources included seawater intrusion, evaporitic salts dissolution, concentrations by evaporation, deep aquifer brines, dissolution of minerals from the aquifer geology as well as salts from anthropogenic activities (i.e. mining). The source(s) of salinity to the groundwater has been determined using the geochemical as well as the isotopic tracers. The ratios of major ions (i.e. Na/Cl) as well the oxygen (18O), hydrogen (2H), 36Cl/Cl, and 87Sr/86Sr isotopes were used in determining the possible solute sources. In addition to these, the chloride mass balance (CMB) method was used to determine the recharge rates to the alluvial aquifers. Furthermore, the groundwater age of the alluvial aquifers was determined using the tritium (3H) isotope. The groundwater samples have high 87Sr/86Sr ratios, which are in the same ranges as the 87Sr/86Sr ratios in the surrounding granitic rocks indicating water-rock interactions. The 36Cl/Cl ratios are low and indicate the dissolution of old salts. The 18O and 2H stable isotopes of groundwater show an evaporative trend with respect to the LMWL, which indicate that groundwater has been evaporated before or during infiltration. Salinity to the shallow alluvial aquifers was found to be mainly derived from the dissolution of rock mass and concentration by evaporation process. The groundwater is relatively young, but there is mixing between old water recharged prior to bomb testing and recently recharged groundwater in some boreholes. The Chloride mass balance (CMB) method assumes atmospheric chloride is the only source of chloride to the aquifers. However, there is additional chloride to these alluvial aquifers from rock mass dissolution. The estimated recharge rates by CMB method (0.1-3.4mm/a) are therefore underestimated. A simulation model was used to determine the recharge rates based on the annual precipitation that will yield the current measured chloride concentrations in the groundwater. Recharge was found to range from 1-5% of the annual precipitation, which is also low. The CMB method therefore gives significant recharge rate estimates, but they are not accurate and need to be supported by another method. AFRIKAANSE OPSOMMING: Geen opsomming beskikbaar. 2015-05-20T09:27:47Z 2015-05-20T09:27:47Z 2015-04 Thesis http://hdl.handle.net/10019.1/96826 en_ZA Stellenbosch University 86 pages : illustrations, maps application/pdf Stellenbosch : Stellenbosch University
spellingShingle Aquifers -- South Africa -- Namaqualand
Salinisation -- South Africa -- Namaqualand
Groundwater -- South Africa -- Namaqualand
Stable isotopes
UCTD
Groundwater recharge -- South Africa -- Namaqualand
Buffels River Catchment (South Africa)
Nakwafila, Albertina Nuusiku
Salinisation source(s) and mechanism(s) in shallow alluvial aquifers along the Buffels River, Northern Cape Province, South Africa
title Salinisation source(s) and mechanism(s) in shallow alluvial aquifers along the Buffels River, Northern Cape Province, South Africa
title_full Salinisation source(s) and mechanism(s) in shallow alluvial aquifers along the Buffels River, Northern Cape Province, South Africa
title_fullStr Salinisation source(s) and mechanism(s) in shallow alluvial aquifers along the Buffels River, Northern Cape Province, South Africa
title_full_unstemmed Salinisation source(s) and mechanism(s) in shallow alluvial aquifers along the Buffels River, Northern Cape Province, South Africa
title_short Salinisation source(s) and mechanism(s) in shallow alluvial aquifers along the Buffels River, Northern Cape Province, South Africa
title_sort salinisation source s and mechanism s in shallow alluvial aquifers along the buffels river northern cape province south africa
topic Aquifers -- South Africa -- Namaqualand
Salinisation -- South Africa -- Namaqualand
Groundwater -- South Africa -- Namaqualand
Stable isotopes
UCTD
Groundwater recharge -- South Africa -- Namaqualand
Buffels River Catchment (South Africa)
url http://hdl.handle.net/10019.1/96826
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