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Hydrogeology and siting of micro-dams around Léo Burkina Faso

Hydrogeology and siting of micro-dams around Léo ... - SamSamWater

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<strong>Hydrogeology</strong> <strong>and</strong> <strong>siting</strong> <strong>of</strong> <strong>micro</strong>-<strong>dams</strong> <strong>around</strong> <strong>Léo</strong>, <strong>Burkina</strong> <strong>Faso</strong>14 June 2010Figure 3 From left to right: granito-gneiss outcrop, laterite <strong>and</strong> clayThe fractured top part <strong>of</strong> the underlying crystalline basement forms a deeper aquifer. Since the waterwill only be stored <strong>and</strong> transported trough fractures, this aquifer is discontinuous, has a lowpermeability <strong>and</strong> very low storage capacity. Most (all?) boreholes (“forages”) are constructed in thisaquifer.Figure 4 From left to right: a scoophole, an uncovered (h<strong>and</strong> dug) well <strong>and</strong> a borehole withh<strong>and</strong> pumpAccording to the geophysical measurements carried out in 2010 by DEC Ltd the top <strong>of</strong> the crystallinebasement near the river varies between a few meters <strong>and</strong> about 20 m below ground level. Moredetails on the geophysical measurements <strong>and</strong> geology (drill logs) can be found in the reports “Travauxde realization de dix (10) forages positives equips de pompe volonta dans les communes de Bieha,Kassou, Leo en Tho, Provinces de la Sissili et du Ziro - Rapport de fin de travaux“ (CREDO / BESER Sarl,2009) <strong>and</strong> “Rapport d'investigations geophysiques sur cinq (5) sites de <strong>micro</strong>-barrages dans laProvince de la Sissili pour le compte de CREDO “ (DEC Ltd, 2010).6

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