Ángela Vallejos Izquierdo, Antonio Pulido Bosch, Francisco Sánchez Martos, Wenceslao Martín Rosales
From data obtained in several wells of Sierra de Cador, the main hydrochemical characteristic of groundwater are stablished. Using different diagrams it's possible to define some hydrochemical processes taking place into the aquifer. Processes of ionic exchange -direct or indirect- provoke changes in the original composition of the groundwater
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