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Hydrodynamic and hydrochcmical characterization of the Fuente Grande spring (Sierra de la Alfaguara, Granada)

dc.contributor.authorJiménez Gavilán, Pablo
dc.contributor.authorAndreo Navarro, Bartolomé
dc.contributor.authorCarrasco Cantos, Francisco
dc.date.accessioned2014-10-24T11:16:02Z
dc.date.available2014-10-24T11:16:02Z
dc.date.issued2003
dc.identifier.urihttp://hdl.handle.net/10272/8975
dc.description.abstractFuente Grande spring is the main natural discharge point of the carbonate aquifer system of the Sierra de la Alfaguara (Granada, Spain). The hydrodynamic and hydrochemical responses of this spring, with respect to precipitations recorded during the study period (2000-2002), show that the system drained is a fissured system, because slow and little increases in the outflow of the spring, accompanied of a scanty dilution process. The analysis of depletion curves shows that this is a slow process; moreover, the temporal variation of the electrical conductivity of the water and the variation coefficient of this parameter, confirm the low karstification degree of the aquiferen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherCarbonate aquiferen_US
dc.subject.otherFuente Grande springen_US
dc.subject.otherHydrodynamicen_US
dc.subject.otherHydrochemistryen_US
dc.titleCaracterización hidrodinámica e hidroquímica de la Fuente Grande de Alfacar (Sierra de la Alfaguara, Granada)en_US
dc.titleHydrodynamic and hydrochcmical characterization of the Fuente Grande spring (Sierra de la Alfaguara, Granada)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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