This study proposes a simple method for assessing the potential
available monthly and annual recharge in a small crystalline
basement aquifer catchment, taking into consideration the rainfall
and the physical characteristics of the catchment. By studying the
geology, land use and rainfall, and applying different techniques
for estimating recharge, it has been deduced that occurrence of
groundwater recharge, and hence the potential for recharge, is
controlled by the rainfall regime and evaporative fluxes, whilst
the geology and vegetation characteristics of a catchment influence
the mechanism and magnitude of actual recharge.
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