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Understanding runoff processes in a semi arid environment through isotope and hydrochemical hydrograph separations

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Figure

Figure 1. Location of the Kaap catchment in the Incomati Basin displaying nearby cities, and DWA and SAWS rain gauges.
Figure 2. (a) Digital elevation model (DEM) of the Kaap catchment with sampling locations and stream and rain gauge locations, (b) land usemap, (c) geological map, (d) contour map of static groundwater levels, (e) aridity index (< 0.03 hyper arid, 0.03–0.2
Table 1. UNESCO-IHE laboratory equipment used in chemical analysis of Kaap catchment samples.
Figure 3. Average monthly precipitation, pan-A evaporation (fromstations X1E006, X1E007, Barberton and Malelane), and maximumand minimum temperatures at Barberton station from 2001 to 2012.
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