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- W2769179506 abstract "The karst Tabular Middle Atlas Causses reservoir is the main drinking-water supply of Fez-Meknes region (Saïs Basin) in Morocco. Recent analyses showed a decline in associated groundwater chemical quality and increased turbidity. To understand this hydrosystem, four surveys were undertaken during fall and spring, 2009–2011. Hydrogeochemical studies coupled with isotopic analyses (δ18O, δD and 222Rn) showed that the aquifers between the causses (mountains) and the Saïs Basin are of Liassic origin and at the southern extremities are of Triassic origin. Five recharge zones of different altitudes have been defined, including two main mixing zones in the south. Deuterium excess results suggest local recharge, while a plot of δ18O versus δD characterizes a confined aquifer in the eastern sector. 222Rn results reveal areas of rapid exchanges with an upwelling time of less than 2 weeks. A schematic conceptual model is presented to explain the groundwater circulation system and the behavior of this karst system." @default.
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- W2769179506 date "2017-11-13" @default.
- W2769179506 modified "2023-10-17" @default.
- W2769179506 title "Contraintes hydrochimiques entre les Causses karstiques du Moyen atlas tabulaire et le bassin de Saïs (Maroc): implications de la circulation des eaux souterraines" @default.
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- W2769179506 doi "https://doi.org/10.1007/s10040-017-1675-0" @default.
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