versão On-line ISSN 1816-7950
versão impressa ISSN 0378-4738
Water SA vol.34 no.1 Pretoria Jan. 2008
W RoetsI; Y XuII; L RaittIII; L BrendonckIV
ISSI Engineers and Environmental Consultants (Pty) Ltd, Postnet suite #200, P/Bag X6590, George 6530, South Africa
IIUniversity of the Western Cape, Department of Earth Sciences, P/Bag X17, Bellville 7535, South Africa
IIIUniversity of the Western Cape, Department of Biodiversity and Conservation Biology, P/Bag X17, Bellville 7535, South Africa
IVLaboratory of Aquatic Ecology, K.U. Leuven, Ch. Deberiotstraat 32, B-3000 Leuven, Belgium
This paper reports on a conceptual model that was developed to describe the different groundwater discharge 'types' from the Table Mountain Group (TMG) aquifer, that contributes to the different components of the flow regime in each of the recognised river reaches for streams and rivers associated with the TMG. This model integrates hydrogeological, ecological and geomorphological understandings into an ecohydrological perspective linking ground- and surface water systems. Through geospatial intersections of existing GIS layers a GIS model was also developed to highlight the quaternary catchments containing sensitive aquatic ecosystems that could be vulnerable to groundwater use from the TMG.
The conceptual model demonstrates the intimate link between groundwater from the TMG aquifer and aquatic ecosystems in the mountain and foothill reaches of streams and rivers in the Cape Folded Mountains in particular. It also identifies two primary zones of interaction between groundwater and surface water in the TMG, namely, the 'TMG aquifer daylight-domain', located in the recharge zone, and the 'TMG aquifer surface water interface-domain', located at the discharge end of the aquifer.
The conceptual model clearly indicates the difference between real groundwater, and perceived groundwater contributions to streamflow in the TMG. It is the lower flows of the flow regime that will be most vulnerable to groundwater use from the TMG aquifer in the 'TMG aquifer daylight-domain', which are unfortunately also the most important flows from an ecological perspective. However, any groundwater use from the TMG aquifer will also affect the discharge end of the aquifer, located far from the higher elevation recharge areas, or the point of groundwater abstraction, in lowland settings in the 'TMG aquifer surface water interface-domain'.
The GIS model integrated the conceptual understanding into a management tool by highlight all quaternary catchments associated with TMG containing sensitive aquatic ecosystems and gave the variable vulnerability for each.
Keywords: ecohydrology, ecosystem dynamics, groundwater abstraction, river basin management, streamflow regime, TMG aquifer
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Received 10 September 2007;
Accepted in revised form 27 November 2007.