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Nine meteorological stations, distributed between 3 and 996 m of altitude, have been used as basis of an isotopic study of rainwater carried out in the Rif chain (Northern part of Morocco) during the hydrological years 2002 to 2004. The study allowed examining the isotopic variations during the years and defining the relationship between the stable isotopes of water (oxygen-18 and deuterium). The...
Groundwater resources in the Tadla basin stem from surface water recharge and different groundwater inflows, forming a multilayered aquifer system, which hosts one of Morocco’s most important groundwater reservoirs. The hydrodynamic infrastructure; i.e. the relationship between all regional aquifers, recharge, and the residence time of waters poses a serious challenge for current water management...
Groundwater and surface water in Souss–Massa basin in the west-southern part of Morocco is characterized by a large variation in salinity, up to levels of 37gL −1 . The high salinity coupled with groundwater level decline pose serious problems for current irrigation and domestic water supplies as well as future exploitation. A combined hydrogeologic and isotopic investigation using several...
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