Aquifer properties are the hydraulic characteristics of aquifers, which we use to describe the aquifer, and understand how groundwater exists and behaves in that aquifer - in other words, the hydrogeology of that aquifer. Key aquifer properties are permeability (or transmissivity); storage; and thickness.
To get reliable information on aquifer properties, aquifer testing must be carried out. Drilling and carrying out controlled test pumping of boreholes allows estimates of aquifer thickness, permeability, transmissivity and storage to be made. Without controlled test pumping, it is not possible to accurately estimate these aquifer properties.
In many parts of Africa, quantitative aquifer properties data are scarce, and surrogate data and information must be used instead in order to characterise aquifers. The most commonly available hydrogeological data are geology; borehole depth; and borehole yield. These have been used to develop the hydrogeology map used in this Atlas.
Classification of aquifer properties
To produce the aquifer properties maps values of aquifer yield, storage type and saturated thickness were divided into significant ranges.
Storage and Flow Type
A semi-quantitative assessment of aquifer storage type can be made based on geology and inferred porosity. The main distinction is whether groundwater is stored in, and flows through, fractures in a consolidated rock; or via intergranular flow in a porous rock or sediment matrix. Storage and flow in unconsolidated sedimentary aquifers is always dominantly intergranular. Younger sedimentary rocks (e.g. Cenozoic and Mesozoic in age) tend to be more loosely consolidated, and groundwater storage and flow is often dominantly intergranular. Older sedimentary rocks tend to be well consolidated, and groundwater storage and flow is typically dominated by fracture flow. Karstic rocks are entirely dominated by rapid fracture flow. Volcanic and intrusive igneous rocks are typically dominated by fracture flow, although some intergranular flow can occur in weathered zones. In Precambrian basement, fracture flow dominates in unweathered rocks, and a mixture of fracture and intergranular flow and storage in weathered basins.
For more information see [[Hydrogeological environments of Africa | hydrogeological environments of Africa].
To develop the hydrogeology map used in this Atlas, borehole yield data were collated for aquifers across Africa (MacDonald et al. 2010). Six yield categories were distinguished and applied to the mapped aquifers, as a proxy for aquifer productivity. The yield values refer to average yields from a single, effectively-sited and developed borehole in the relevant aquifer.
|Aquifer productivity||Yield range (litres/second or l/s)|
|Very high||> 20|
|High||5 - 20|
|Moderate||2 - 5|
|Low to Moderate||0.5 - 2|
|Low||0.1 - 0.5|
|Very low||< 0.1|
In general non-weathered Precambrian basement is mapped to be of the lowest productivity. The more productive aquifers in Africa are the Cretaceous-Tertiary sedimentary basins (Figure 4).
Saturated thickness – four significant ranges of saturated thickness were mapped – Table 3. Greatest saturated thickness is mapped for the major sedimentary basins of Africa (e.g. the Sirte and Kufra Basins in North Africa), whilst shallow weathered basement aquifers have been mapped as the thinnest aquifers (Figure 6).
Typical borehole yields for each [[Hydrogeological environments of Africa | aquifer group] were
namely, typical borehole yields, aquifer storage type (e.g. fracture or intergranular), and saturated aquifer thickness.
- Citations and Links
MacDonald AM and Davies J. 2000. A brief review of groundwater for rural water supply in sub-Saharan Africa. British Geological Survey Technical Report WC/00/033, 30pp.
MacDonald AM, Bonsor HC, Ó Dochartaigh BE and Taylor RG. 2012. Quantitative maps of groundwater resources in Africa. Environmental Research Letters, 7 (2), 024009. 10.1088/1748-9326/7/2/024009
MacDonald AM, Ó Dochartaigh BE, Bonsor HC, Davies J and Key R. 2010. Developing quantitative aquifer maps for Africa. British Geological Survey Internal Report IR/10/103, Nottingham, UK.