Determination of the origins and recharge rates of the Sfax aquifer system (southeastern Tunisia) using isotope tracers

Author:

Ayadi Rahma,Zouari Kamel,Saibi Hakim,Trabelsi Rim,Khanfir Hafedh,Itoi Ryuichi

Publisher

Springer Science and Business Media LLC

Subject

Earth-Surface Processes,Geology,Pollution,Soil Science,Water Science and Technology,Environmental Chemistry,Global and Planetary Change

Reference49 articles.

1. Bear J (1972) Dynamics of fluids in porous media. Dover, New York, p 764

2. Belgacem A, Kharroubi A, Bouri S, Abida H (2010) Contribution of geostatistical modelling to mapping groundwater level and aquifer geometry, case study of Sfax’s deep aquifer. Tunis Middle East J Sci Res 6(3):305–316

3. Ben Akacha M (2001) Etude géologique de la région d’Agareb-Sfax: évolution géomorphologique néotectonique et paléogéographique. DEA, Fac. Sc., Sfax

4. Ben Brahim F, Bouri S, Khanfir H (2011) Hydrochemical analysis and evaluation of groundwater quality of a Mio-Plio-Quaternary aquifer system in an arid regions: case of El Hancha, Djebeniana and El Amra regions, Tunisia. Arab J Geosci 6:2089–2102. doi: 10.1007/s12517-011-0481-6

5. Ben Hamouda MF, Tarhouni J, Leduc C, Zouari K (2010) Understanding the origin of salinization of the Plio-Quaternary eastern coastal aquifer of Cap Bon (Tunisia) using geochemical and isotope investigations. J Environ Earth Sci 63:889–901

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