Consideraciones sobre el funcionamiento hidrogeológico del acuífero carbonatado de la Alta Cadena (provincia de Málaga, España)

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dc.contributor.authorMudarra Martínez, Matías
dc.contributor.authorAndreo Navarro, Bartolomé
dc.contributor.authorMarín Guerrero, Ana Isabel
dc.date.accessioned2014-06-04T08:03:58Z
dc.date.available2014-06-04T08:03:58Z
dc.date.issued2008
dc.description.abstractThe hydrodinamic and hydrochemical responses of three springs (Villanueva del Rosario, Pita and Parroso) located in the Alta Cadena carbonate aquifer (province of Malaga, South Spain) have been monitored from September 2006 to January 2008. A first interpretation on the hydrogeological functioning and on the karst network development has been performed, which is useful for groundwater protection. Thus, Villanueva del Rosario spring drains a part of the Alta Cadena aquifer more karstified than the catchment area of the other two springs. This means that catchment area of Villanueva del Rosario spring is more vulnerable than the other to the contamination and consequently it needs more strict protection criteriaen_US
dc.identifier.urihttp://hdl.handle.net/10272/8247
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRightsopen access
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherCarbonate (karst) aquiferen_US
dc.subject.otherHydrochemistryen_US
dc.subject.otherHydrodynamicen_US
dc.subject.otherMalaga provinceen_US
dc.titleConsideraciones sobre el funcionamiento hidrogeológico del acuífero carbonatado de la Alta Cadena (provincia de Málaga, España)en_US
dc.titleConsiderations about the hydrogeological functioning of the Alta Cadena carbonate aquifer (Málaga province, Spain)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 44, (2008)