2018
DOI: 10.1144/sp479.3
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Towards defining a baseline status of scarce groundwater resources in anticipation of hydraulic fracturing in the Eastern Cape Karoo, South Africa: salinity, aquifer yields and groundwater levels

Abstract: Abstract:The Eastern Cape Karoo region is water stressed and will become increasingly so with further climate change. Effective and reliable groundwater management is crucial for a development such as the proposed hydraulic fracturing for shale gas. This is especially critical across this region of agriculture and protected ecosystem services. The research, as part of baseline data gathering, aims to characterize the hydrochemistry for both the shallow groundwater (<500 m) and saline groundwater closer to the … Show more

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Cited by 8 publications
(7 citation statements)
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“…In these areas, possible sources are further determined using isotope analysis [54][55][56]. It was initially proposed that the relatively higher salinity south of the escarpments may be due to low precipitation and limited dilution of groundwater with fresh meteoric water [57]. However, new groundwater samples collected in this area have both 14C (Carbon) and 3H (Tritium) isotope signatures of deep (old) groundwater, usually saline and non-potable, mixed with shallow, modern groundwater, with ca.…”
Section: Hydrocensusmentioning
confidence: 99%
“…In these areas, possible sources are further determined using isotope analysis [54][55][56]. It was initially proposed that the relatively higher salinity south of the escarpments may be due to low precipitation and limited dilution of groundwater with fresh meteoric water [57]. However, new groundwater samples collected in this area have both 14C (Carbon) and 3H (Tritium) isotope signatures of deep (old) groundwater, usually saline and non-potable, mixed with shallow, modern groundwater, with ca.…”
Section: Hydrocensusmentioning
confidence: 99%
“…10 The site is located between Nahoon and Buffalo river catchments and its geology is characterized by dykes and dolerite sheets dating to Jurassic age as well as Beaufort sediment of the Karoo family. 9 Area groundwater flows to the southeast and northeast and is classified as a minor aquifer with low groundwater yields of 1 L/s in most boreholes and a deep depth of >40 m. The area has clayey soils. 9 To evaluate the effect of leachate on groundwater, samples were collected in 3 monitoring boreholes near the landfill facility ( Figure 2).…”
Section: Study Area and Samplingmentioning
confidence: 99%
“…9 Area groundwater flows to the southeast and northeast and is classified as a minor aquifer with low groundwater yields of 1 L/s in most boreholes and a deep depth of >40 m. The area has clayey soils. 9 To evaluate the effect of leachate on groundwater, samples were collected in 3 monitoring boreholes near the landfill facility ( Figure 2). A handheld GARMIN GPS-60 receiver was used to locate the sampling points whose coordinates were georeferenced and documented as shown in Table 1.…”
Section: Study Area and Samplingmentioning
confidence: 99%
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“…However, at the same time, facing these challenges provides an opportunity for new proposed exploration projects to establish suitable monitoring programmes ahead of the start of exploration activities in order to minimize impacts on water resources. In this context, Stroebel et al (2018) present an approach to comprehensive groundwater baseline monitoring across the Eastern Karoo Basin in the context of proposed shale gas extraction in the region.…”
mentioning
confidence: 99%