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Contribution of tritium content to identify the origin of groundwater: Sierra de Gádor (Almería)

dc.contributor.authorVallejos, Ángela
dc.contributor.authorPulido Bosch, Antonio
dc.contributor.authorMolina, Luis
dc.contributor.authorSánchez Martos, Francisco
dc.contributor.authorGisbert, Josep
dc.contributor.authorMartín Rosales, Wenceslao
dc.description.abstractTritium content of rainwater in Sierra de Gador has been higher than at. 10 TU during the last forty years. Groundwater samples apparently indicate the absence of recent contributions from the precipitation. The mixture with older waters stored inside the aquifer frequently hides the presence of modem recharge. From the content in tritium one can recognize two areas of preferential flow and recharge. One coincides with vulnerable basins to the generation of surface runoff and the other one is bound to a process of marine intrusionen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherMixed wateren_US
dc.titleContribución del contenido en tritio a la identificación del origen del agua subterránea: Sierra de Gádor (Almería)en_US
dc.titleContribution of tritium content to identify the origin of groundwater: Sierra de Gádor (Almería)eng

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