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OVERVIEW OF THE IMPACT OF MINING ON THE ... - IIED pubs

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D7-13 Premier Diamond – kimberlite Operating Large Medium<br />

D7-14 Kameeldrift Clay minerals Operating Small Very low<br />

D7-15 Boekenhoutkloof Clay minerals Operating Medium Low<br />

D7-17 Fortsig Chrysotile asbestos Operating Small Very low<br />

D7-19 Donkerhoek Glass sand Operating Small Very low<br />

D7-20 Mooiplaas Limestone / Dolomite Operating Medium Low<br />

D7-21 Puntlyk Glass sand Operating Small Very low<br />

D7-22 Samancor Lyttleton Limestone / Dolomite Operating Medium Low<br />

D7-23 Noel Lancaster Glass sand Operating Small Very low<br />

D7-25 Grootfontein Clay minerals Operating Medium Low<br />

D7-31 Hippo Olifantsfontein Limestone / Dolomite Operating Medium Low<br />

D7-37 Bourke Fluorspar Closed Small Very low<br />

D7-38 Rust de Winter Fluorspar Closed Small Very low<br />

4.14.3 Alluvial mining<br />

None known or anticipated.<br />

4.14.4 Monitoring systems<br />

The Department of Water Affairs and Forestry (DWAF) operate a comprehensive monitoring system of flow<br />

measurements and water quality measurements in the sub-catchment. In addition, DWAF also regulate the<br />

quantity and quality of all effluent discharges through a system of effluent discharge permits or licences. Each<br />

licensed effluent discharger is required to carry out a routine monitoring programme of the flow and quality of<br />

their effluent and supply this to DWAF. The Department then conducts a randomised series of audit samples to<br />

check the veracity of the effluent returns submitted by each discharger.<br />

4.14.5 Water quality data<br />

The Department of Water Affairs and Forestry have provided data for the main stem of the Crocodile River at<br />

three points along its length (Table 4.15). These data reveal that the water quality in the Crocodile River is very<br />

poor in the upper reaches due to contamination from effluents and seepage. There is a minor improvement in<br />

orthophosphate (PO4-P) concentrations in Hartbeespoort Dam, but further deterioration occurs downstream,<br />

probably as a result of irrigation return flows and discharges containing fertilizers. Concentrations of total<br />

dissolved salts and pH values increase downstream, indicating progressive salinization. No details of specific<br />

agricultural return flows or effluent discharges could be obtained in time for this report. This information is also<br />

regarded as very sensitive and normally has to be dealt with confidentially.<br />

Table 4.15: Water quality data for three sampling stations along the Crocodile River (Annual averages, in<br />

mg/litre, provided by Department of Water Affairs and Forestry).<br />

cclv

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