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A combined methodology for estimating the potential natural aquifer recharge in an arid environment
Authors:Alberto Carletti  Simona Canu  Andrea Motroni  Giorgio Ghiglieri
Institution:1. Deserti?cation Research Centre (NRD), University of Sassari , Sassari, Italy;2. Department of Chemical and Geological Sciences, University of Cagliari, Cittadella Universitaria di Monserrato , Cagliari, Italy acarletti@uniss.it;4. Department of Meteorology and Climatology, Environmental Protection Agency of Sardinia (ARPA) , Sassari, Italy;5. Department of Chemical and Geological Sciences, University of Cagliari, Cittadella Universitaria di Monserrato , Cagliari, Italy ORCID Iconhttps://orcid.org/0000-0002-6566-7733
Abstract:ABSTRACT

An innovative methodology that combines an indirect physiography-based method for determining the runoff coefficient at a sub-basin scale and a water balance model applied on a daily time scale was developed to calculate the natural groundwater recharge in three watersheds within the Oum Zessar arid area, Tunisia. The effective infiltration was calculated as part of the water surplus by considering the average available water content (AWC) of soil and an average runoff coefficient for each sub-basin. The model indicates that the sub-basins covered mainly by the “artificial” soils of tabias and jessour, characterized by average AWC values greater than 150 mm, did not contribute to natural groundwater recharge over the 10-year period (2003–2012) considered. The estimated volume for the Triassic aquifer amounted to about 4.5 hm3 year?1, which is consistent with previous studies. For the Jurassic and Cretaceous aquifers, the estimated volumes amounted to about 200 dm3 year?1.
Keywords:natural aquifer recharge  hydrogeology  arid environment  Oum Zessar  Tunisia
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