18O, Br y el origen de la salinización en los acuíferos costeros de Martíl-Alila y Smir (Tetuán, Marruecos)
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Abstract
The analysis of the occurrence of isotope (O18) in relation to other ions (Cl and Br) in the groundwater of
the Martil-Alila and Smir aquifers revels that the process of salinization is caused by intruding seawater and
polluted waters, coming from river Martil and M’diq city
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