C. Leduc et al., RECHARGE OF THE CONTINENTAL TERMINAL WATE R-TABLE (NIAMEY, NIGER) ESTIMATED FROM TRITIUM MEASUREMENTS AND MODELING, Comptes rendus de l'Academie des sciences. Serie II. Sciences de la terre et des planetes, 323(7), 1996, pp. 599-605
As often in the Sahelian belt, recharge of the Continental Terminal wa
ter table near Niamey, Niger, is essentially due to rainfall infiltrat
ion through numerous temporary pools. Tritium content in rain over the
past 40 years is reconstructed and used by a simple model to calculat
e the groundwater renewal rate according to measurements throughout th
e aquifer. This isotopic estimate (25 mm per year) is close to the hyd
rodynamical estimate.