1887

Abstract

Groundwater exploration in the lower Okavango Delta to the west of Maun in northern Botswana has focussed on<br>the search for shallow fresh-water aquifers in Kalahari sediments. While surface water flow in the delta is fresh,<br>much of the shallow groundwater is saline and deep (~100m) groundwater is almost invariably saline, due to a<br>combination of evaporation, evapotranspiration and poor drainage. The target aquifers comprise thick packages of<br>coarser sands characterised by high porosity and permeability, allowing for annual flushing and recharge. For<br>these reasons, finer-grained, clay-rich sands are poorer targets.

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/content/papers/10.3997/2214-4609-pdb.143.18.1
2001-10-09
2024-09-12
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