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Deep groundwater characterisation and recharge estimation in the Verlorenvlei catchment

Thesis (MSc)--Stellenbosch University, 2018.

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Main Author: Eilers, Anya
Other Authors: Miller, Jodie A.
Format: Thesis
Language:en_ZA
Published: Stellenbosch : Stellenbosch University 2018
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access_status_str Open Access
author Eilers, Anya
author2 Miller, Jodie A.
author_browse Eilers, Anya
Miller, Jodie A.
author_facet Miller, Jodie A.
Eilers, Anya
author_sort Eilers, Anya
collection Thesis
dc_rights_str_mv Stellenbosch University
description Thesis (MSc)--Stellenbosch University, 2018.
format Thesis
id oai:scholar.sun.ac.za:10019.1/103515
institution Stellenbosch University (South Africa)
language en_ZA
last_indexed 2026-06-10T12:47:14.760Z
license_str Other — see source repository
provenance_str_mv Harvested via OAI-PMH from SUNScholar — Stellenbosch University Repository
publishDate 2018
publishDateRange 2018
publishDateSort 2018
publisher Stellenbosch : Stellenbosch University
publisherStr Stellenbosch : Stellenbosch University
record_format dspace
source_str SUNScholar — Stellenbosch University Repository
spelling oai:scholar.sun.ac.za:10019.1/103515 Deep groundwater characterisation and recharge estimation in the Verlorenvlei catchment Eilers, Anya Miller, Jodie A. Stellenbosch University. Faculty of Science. Dept. of Earth Sciences. Verbrenvlei (South Africa) -- Groundwater characterisation Semi-arid catchments -- Southern Africa Chloride Mass Balance (CMB) technique UCTD Thesis (MSc)--Stellenbosch University, 2018. ENGLISH ABSTRACT: Secondary aquifers are a primary source of water in many semi-arid regions, and understanding groundwater recharge is necessary for the effective management of this resource. The Chloride Mass Balance (CMB) technique provides low-cost recharge estimates, and has successfully been used in many semi-arid catchments in Southern Africa. It is particularly useful along the west coast of South Africa, where physical data is limited. The west coast hosts the Verlorenvlei catchment and its RAMSAR listed wetland, where it is thought that deep groundwater baseflow sustains the wetland during the dry season. Shallow groundwater salinisation and increasing agricultural activity in the catchment has resulted in more deep groundwater abstraction, threatening the long-term health of the wetland. This study describes how major ion and stable isotope chemistry of ground and rain water can be used to calculate recharge to the secondary aquifer using the CMB technique, and its implications for assessing mechanisms of recharge and salinisation in the catchment. To do this, 102 groundwater samples were collected across the catchment over six sampling seasons. Additionally, 94 rain water samples were collected over the period of eighteen months, with daily rainfall collectors located in the valley, and a cumulative collector erected on the Piketberg mountain range, to assess the contribution of recharge from the Table Mountain Group (TMG) aquifer. CMB recharge estimates in the upper catchment indicate that the TMG aquifer contributes between 40 and 53 mm/a (11.4 – 15.2% MAP) recharge to the secondary aquifer, while direct recharge in the upper valley is between 20 and 27 mm/a (4.2 – 5.6% MAP). These estimates are supported by δ18O and δ2H values of rain and groundwater, and correlate well with previous physical methods. δ18O and δ2H values also indicate that the upper catchment is likely to be a gaining stream, with deep groundwater contributing to baseflow. The additional input of salts further down the catchment, due to water-rock interaction and the inflow of other deep groundwater, make CMB recharge estimates unreliable in the lower catchment. Furthermore, pumping-induced discharge from the primary to secondary aquifer during the summer months is responsible for a distinct increase in salinity of the secondary aquifer. This is characteristic of a losing stream, with groundwater contributing little to baseflow. Predictions of increasing temperature and decreasing rainfall along the west coast indicate that pumping-induced discharge could become more common in the lower catchment, increasing the threat of secondary aquifer salinisation and a reduction in groundwater baseflow. Overall, the methodology applied in this study can be used for high resolution, at-point CMB estimates in other small catchments, and contribute to long-term groundwater management in semi-arid catchments affected by salinisation. Keywords: Recharge, Chloride Mass Balance, Verlorenvlei, Deep Groundwater, Semi-arid AFRIKAANS OPSOMMING: Geen opsomming beskikbaar 2018-02-20T09:23:51Z 2018-04-09T06:59:07Z 2018-02-20T09:23:51Z 2018-04-09T06:59:07Z 2018-03 Thesis http://hdl.handle.net/10019.1/103515 en_ZA Stellenbosch University 107 pages : illustrations, maps application/pdf Stellenbosch : Stellenbosch University
spellingShingle Verbrenvlei (South Africa) -- Groundwater characterisation
Semi-arid catchments -- Southern Africa
Chloride Mass Balance (CMB) technique
UCTD
Eilers, Anya
Deep groundwater characterisation and recharge estimation in the Verlorenvlei catchment
title Deep groundwater characterisation and recharge estimation in the Verlorenvlei catchment
title_full Deep groundwater characterisation and recharge estimation in the Verlorenvlei catchment
title_fullStr Deep groundwater characterisation and recharge estimation in the Verlorenvlei catchment
title_full_unstemmed Deep groundwater characterisation and recharge estimation in the Verlorenvlei catchment
title_short Deep groundwater characterisation and recharge estimation in the Verlorenvlei catchment
title_sort deep groundwater characterisation and recharge estimation in the verlorenvlei catchment
topic Verbrenvlei (South Africa) -- Groundwater characterisation
Semi-arid catchments -- Southern Africa
Chloride Mass Balance (CMB) technique
UCTD
url http://hdl.handle.net/10019.1/103515
work_keys_str_mv AT eilersanya deepgroundwatercharacterisationandrechargeestimationintheverlorenvleicatchment