Published March 2021 | Version v1
Journal article

Saline groundwater in the Buffels River catchment, Namaqualand, South Africa: A new look at an old problem

  • 1. Department of Earth Sciences, Stellenbosch University, Private Bag X1, Matieland (South Africa)
  • 2. Department of Soil Sciences, Stellenbosch University, Private Bag, X1, Matieland (South Africa)
  • 3. Isotope Climatology and Environmental Research Centre, Debrecen (Hungary)
  • 4. Council for Geoscience, PO Box 572, Bellville 7530 (South Africa)
  • 5. Department of Geological Sciences, University of Cape Town (South Africa)

Description

Highlights: • Evaporation does not appear to be a significant contributor to groundwater salinisation. • Salts are derived from marine aerosols, ion-exchange reactions and weathering processes. • Salts are concentrated in heuweltjies, palaeo-biophysical features, common in Namaqualand. • Heuweltjies may thus be an important unrecognized source of groundwater salts. • Flushing of heuweltjie salts likely controlled by incidence of high volume precipitation events. Namaqualand, South Africa, is a global biodiversity hotspot but local populations are affected by challenging economic conditions largely because of poor access to water. In this study groundwater types are characterised and sources of salts and salinisation processes are identified using hydrochemistry and δ18O, δ2H and 87Sr/86Sr data. Analysis of δ18O and δ2H data suggests that evaporation does not play a major role in salinisation of the groundwater. However, major ion chemistry and 87Sr/86Sr ratios indicate that salts present in the groundwater are linked to dry deposition of marine aerosols and ion-exchange reactions in soils in the alluvial aquifer systems. The hydrochemical variability of the groundwater in the basement aquifer system suggests that there are strong local controls linked to weathering processes in individual basement rock types. The region is also notable for the high density of heuweltjies, biophysical features associated with increased nutrient levels, associated with termite activity. Electromagnetic scanning as well as measurement of water-soluble soil electrical conductivity values on and off heuweltjies, show that heuweltjies are saline with salinity increasing with depth. The level of groundwater salinity correlates with the level of heuweltjie salinity. Precipitation records from the last 150 years provide support for the hypothesis that accumulated salts, and in particular, heuweltjie salts are flushed into the groundwater system during sporadic large volume precipitation events. Thus, heuweltjies and hence termite activity, could potentially represent a previously unrecognized contributor to groundwater salinisation across Namaqualand and in other parts of the world.

Availability note (English)

Available from http://dx.doi.org/10.1016/j.scitotenv.2020.143140

Additional details

Identifiers

DOI
10.1016/j.scitotenv.2020.143140;
PII
S0048969720366705;

Publishing Information

Journal Title
Science of the Total Environment
Journal Volume
762
Journal Page Range
vp.
ISSN
0048-9697
CODEN
STENDL

Optional Information

Copyright
Copyright (c) 2020 Elsevier B.V. All rights reserved.