2018
DOI: 10.1007/s12517-018-3773-2
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Conceptual model for karstic aquifers by combined analysis of GIS, chemical, thermal, and isotopic tools in Tuniso-Algerian transboundary basin

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Cited by 39 publications
(17 citation statements)
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“…It is filled up by the rare, irregular rainfall, by the leakage from deep aquifers, and by the surplus of irrigation water (Kamel 2013; Besser et al, 2017). It is characterized by high salinity, and it is used generally in water shortage periods (Kamel, 2013; Hamed et al, 2014; Hamad et al, 2018); The CT aquifer: It is hosted in the carbonate formations of the Upper Cretaceous formations in the detrital deposits of the Miocene. It constitutes a huge reservoir of about 350.000 km 2 continuous from Algeria to Libya (Edmunds et al, 2003; Hamed et al, 2013).…”
Section: Methodsmentioning
confidence: 99%
“…It is filled up by the rare, irregular rainfall, by the leakage from deep aquifers, and by the surplus of irrigation water (Kamel 2013; Besser et al, 2017). It is characterized by high salinity, and it is used generally in water shortage periods (Kamel, 2013; Hamed et al, 2014; Hamad et al, 2018); The CT aquifer: It is hosted in the carbonate formations of the Upper Cretaceous formations in the detrital deposits of the Miocene. It constitutes a huge reservoir of about 350.000 km 2 continuous from Algeria to Libya (Edmunds et al, 2003; Hamed et al, 2013).…”
Section: Methodsmentioning
confidence: 99%
“…The most important triggering factor influencing the slope stability is the rainfall [39]. The annual average rainfall map was obtained from the inverse distance weight (IDW) interpolation of data from five hydroclimatic stations (Constantine, Hamma Bouziane, Aïn El Bey, Fourchi and Bir Drimil) over a 32-year period.…”
Section: Rainfallmentioning
confidence: 99%
“…This basin presents an increasing water deficit under the combined effect of climatic factors and the growth of needs. In this area, more than 80% of the available water is used for irrigated agriculture and the mining industry (especially for phosphate ore treatment) with relatively poor use efficiency (Hamed et al, 2013(Hamed et al, , 2018Mokadem et al, 2016;Hamad et al, 2018). The overexploitation of groundwater in this region has reinforced the downward trend in the water levels, and the aquifer drawdown has sometimes reached 0.5-10 m/year (Hamed, 2011;Hamed et al, 2014).…”
Section: Introductionmentioning
confidence: 99%