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Water availability, demand and reliability of in situ water harvesting in smallholder rain fed agriculture in the Thukela River Basin, South Africa

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Figure

Table 1. Overview of approaches to identify potentially suitable locations of WH. AM is antecedent soil moisture conditions.
Table 2. Dominant land cover classes in the basin derived from theSouth African National Land Cover dataset (CSIR et al., 2002).
Table 3. Major soil types of the basin. Moist bulk density, organic carbon content, hydraulic conductivity and available water capacity arepresented for the top layer of the soil profile (0–30 cm depth).
Table 4. Parameter sensitivity of calibrated parameters in relation to the objective function values for discharge (d), smallholder maizeyield (s), and commercial maize yield (c), respectively
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