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Processus et bilan des flux hydriques d'un bassin versant de milieu tropical de socle au Bénin (Donga, haut Ouémé)
Processus et bilan des flux hydriques d'un bassin versant de milieu tropical de socle au Bénin (Donga, haut Ouémé)
Abstract : Hydrodynamic, geochemical, and subsurface geophysical investigations, for two consecutive years with contrasting rainfall conditions, were used to characterize the hydrological processes occurring, and the water balance of a 586-km2 watershed in Benin (Africa). The water table's monitoring shows that recharge occurs by direct infiltration of rainfall, and represents between 5 to 24% of the annual rainfall. Both surface water outflow, limited to the rainy season, and water chemistry indicate a weak groundwater contribution to river discharge. This implies that the calculated variations in annual runoff coefficients (of 14 and 28%) are mainly governed by surface and subsurface flows.
Cited literature [26 references]
https://hal.ird.fr/ird-00165994
Contributor : Guillaume Favreau Connect in order to contact the contributor
Submitted on : Tuesday, July 31, 2007 - 9:35:26 AM
Last modification on : Tuesday, July 5, 2022 - 8:56:12 AM
Long-term archiving on: : Thursday, April 8, 2010 - 9:05:10 PM
Contributor : Guillaume Favreau Connect in order to contact the contributor
Submitted on : Tuesday, July 31, 2007 - 9:35:26 AM
Last modification on : Tuesday, July 5, 2022 - 8:56:12 AM
Long-term archiving on: : Thursday, April 8, 2010 - 9:05:10 PM
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Kamagate_et_al_CRAS_2007.pdf
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