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Impact of floodwaters on vertical water fluxes in the deep vadose zone of an alluvial aquifer in a semi-arid region
Authors:Manel Boughanmi  Lotfi Dridi  Monji Hamdi  Rajouene Majdoub
Institution:1. Département du Génie des Systèmes Horticoles et du Milieu Naturel, Université de Sousse, Institut Supérieur Agronomique de Chott Meriem, Sousse, Tunisia;2. Université de Strasbourg, CNRS, LHyGeS UMR 7517, Strasbourg, France;3. UR Hydrosciences Appliquée, Université de Gabès, Institut Supérieur des Sciences et Techniques des Eaux, Gabès, Tunisia
Abstract:The spatial and temporal variation of moisture distribution, overall water balance and quantity of infiltrated water in the vadose zone of the Sidi Bouzid Plain (Tunisia) during successive flooding events is quantified in this study. The variation in water content in response to environmental factors such as evaporation and water root uptake is also highlighted. One-dimensional flow simulations in the deep vadose zone were conducted at three spreading perimeters located near Wadi El Fekka. The hydraulic boundary conditions of a time-dependent water blade applied to the soil surface were determined from measured flood hydrographs. For the chosen wet year, the successive flooding events contributed to a significant artificial recharge of the natural groundwater. Although the soil hydraulic parameters did not vary strongly in space, flow simulations showed significant differences in the overall water balance of approximately 9–16% for the various spreading perimeters.
Keywords:artificial recharge  vertical water flux  evaporation  water root uptake  flood hydrograph  numerical simulation  vadose zone  Sidi Bouzid Plain
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