Ángela Vallejos Izquierdo, Juan Gisbert, Francisco Sánchez Martos, Luis Molina Sánchez, Antonio Pulido Bosch, Wenceslao Martín Rosales
The stable isotopes of rainwater, measured in samples at locations with different altitude, show a distinctive altitudinal distribution. Analysis of the precipitation indicates the dominant source and direction of the air masses. The local meteoric water line that is established indicates a primarily Mediterranean origin for the precipitation recharging the aquifers
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