Abstract
The present study targets of Tiznit region's water which is a semi-arid zone located in south-western part of Moroccan Anti-Atlas (Coordinates: 29° 42′ 00″ North, 9° 43′ 37″ West). It is concerned with the geochemical study, since the quality of groundwater depends on several factors such as recharge water quality, geology, grade of chemical weathering of the different rock types, a water–rock interface (Emenike et al., 2017; Aly, 2015). This study was carried out using the representations of Piper and Schoeller Berkaloff of water in this region at the first moment. The predominant facies are calcium and magnesium hyperchloride and calcium bicarbonate with a slight preponderance of this latter. The thermodynamic characterization of the scaling power of water in this region is then given, at a second moment. This study was carried out using the method of Legrand-Poirier-Leroy (LPL) (Legrand et al., 1981; Belattar, et al., 2018) and allowed us to determine the position of water in Tiznit region with respect to the calco-carbonic equilibrium and to conclude that this water is calcifying type.
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