Journal
HYDROGEOLOGY JOURNAL
Volume -, Issue -, Pages -Publisher
SPRINGER
DOI: 10.1007/s10040-023-02594-w
Keywords
Water supply; Numerical modelling; Africa
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A data-driven modelling approach was used to assess the potential groundwater yield from crystalline basement aquifers in West Africa. The study identified seven major geological domains based on lithological, stratigraphic, and structural characteristics. By calibrating the numerical simulations to match measured yields, the researchers found that about 50% of well-sited boreholes could sustain yields exceeding 0.5 L/s, and 25% could sustain the yield required for small irrigation systems (> 1.0 L/s). The study also highlighted regional differences in productivity ranges and the importance of water table depth and aquifer extent.
A data-driven modelling approach was applied to quantify the potential groundwater yield from weathered crystalline basement aquifers in West Africa, which are a strategic resource for achieving water and food security. To account for possible geological control on aquifer productivity, seven major geological domains were identified based on lithological, stratigraphic, and structural characteristics of the crystalline basement. Extensive data mining was conducted for the hydrogeological parameterisation that led to the identification of representative distributions of input parameters for numerical simulations of groundwater abstractions. These were calibrated to match distributions of measured yields for each domain. Calibrated models were then applied to investigate aquifer and borehole scenarios to assess groundwater productivity. Considering the entire region, modelling results indicate that approximately 50% of well-sited standard 60-m-deep boreholes could sustain yields exceeding 0.5 L/s, and 25% could sustain the yield required for small irrigation systems (> 1.0 L/s). Results also highlighted some regional differences in the ranges of productivities for the different domains, and the significance of the depth of the static water table and the lateral extent of aquifers across all geological domains. This approach can be applied to derive groundwater maps for the region and provide the quantitative information required to evaluate the potential of different designs of groundwater supply networks.
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