TDS load contribution from acid mine drainage to Hartbeespoort Dam, South Africa

Pj Hobbs

doi:10.4314/wsa.v43i4.10

Abstract

Evidence of a mine-water impact on groundwater in the karst aquifer downstream of the actively draining West Rand Goldfield can be traced back to the early 1980s. This is attributed to the dewatering of ‘fissure water’ encountered during mining, and its discharge into the Bloubank Spruit catchment. Rewatering of the subsurface void following the cessation of mining in the late 1990s culminated in mine-water issuing from various point sources (shafts and boreholes) in 2002. The past 6 hydrological years have periodically produced the greatest volume and worst quality of mine-water discharge, causing widespread concern for the receiving aquatic environment. In this regard, the proximal Cradle of Humankind World Heritage Site attracts a much sharper focus than the distal, regionally important Hartbeespoort Dam. Objectivity requires that an assessment of the mine-water impact on the receiving surface water resources must recognise both the subregional and regional scales. The evaluation presented in this communication examines the temporal mine-water impact at both scales, and interprets the results in terms of the influence exerted by the natural hydrosystem in mitigating adverse impacts on the water resources environment. An analysis of the respective contributions of each of the major drainages to the quantity and quality of water impounded in Hartbeespoort Dam indicates that the median total dissolved solids (TDS) load delivered by the Bloubank Spruit system amounted to ~26 kt/a in the past 6 hydrological years. This is ~12% of the regional median total of ~224 kt/a entering the impoundment in the same period. By comparison, the preceding long-term record dating back 30 years to 1979 reflects a 66% lower median annual contribution of 8.6 kt, representing ~10% of a regional median total of ~89 kt/a. Proportionally, therefore, the recent 6-year period of high volume and poor-quality discharge from the Bloubank Spruit catchment represents only a marginally greater TDS load contribution to Hartbeespoort Dam than that which characterises the previous 30 years. Keywords : acid mine drainage, allogenic water, autogenic water, Cradle of Humankind, karst springs, karst terrane, TDS load

Highlights

Located on the southeastern boundary of North west and the Crocodile River (West) Province, South Africa (Fig. 1), Hartbeespoort Dam has regional significance as a supply of water for irrigation, industry and municipal use downstream along the Crocodile River (West)
Completed in 1923, it has a full supply capacity (FSC) of ~195 million m3 (Mm3) after the dam wall was raised by 2.4 m to 59 m in the mid-1960s
The Bloubank Spruit contribution amounts to ~51% in all three assessment periods, despite the considerably greater median aggregate discharge of ~95 Mm3/a delivered in the recent period compared to the ~48 Mm3/a of the whole record, and the ~41 Mm3/a of the truncated long-term record

Summary

Introduction

Located on the southeastern boundary of North West Province, South Africa (Fig. 1), Hartbeespoort Dam has regional significance as a supply of water for irrigation, industry and municipal use downstream along the Crocodile River (West). The Bloubank Spruit contribution amounts to ~51% in all three assessment periods, despite the considerably greater median aggregate discharge of ~95 Mm3/a delivered in the recent period compared to the ~48 Mm3/a of the whole record, and the ~41 Mm3/a of the truncated long-term record.

Results

Conclusion