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Study of the discharge in Sierra Tejeda Southern sector (Málaga) by means of the correlation and spectral analysis

dc.contributor.authorPérez Ramos, Isaac
dc.contributor.authorJiménez Gavilán, Pablo
dc.contributor.authorAndreo Navarro, Bartolomé
dc.contributor.authorCarrasco Cantos, Francisco
dc.description.abstractFour river basins in Sierra Tejeda area have been studied by means of the correlation and spectral analysis. These river basins are formed by marbles and schists in their upper and lower part, respectively. The water comes from runoff mainly generated in the schists and groundwater from springs in the Sierra Tejeda carbonate aquifer. The application of this method to outflow data shows that the hydrographical basins with more extension of low permeability materials (Rubite and Algarrobo) have a scarce inertial behaviour. While, those river basins with more inertial behaviour (Bermuza and Almanchares basins) present less extension of schists and the most important springs. Consequently, the hydrodynamic behaviour in these rivers are controlled by groundwater and runoff: Bermuza and Almanchares river basins incorporate larger quantity of groundwater than Algarrobo and Rubite basinsen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherSierra Tejedaen_US
dc.subject.otherCorrelation and spectral analysisen_US
dc.subject.otherHydrographical basinen_US
dc.titleEstudio de la descarga de la vertiente meridional de Sierra Tejeda (Málaga) mediante el análisis correlatorio y espectralen_US
dc.titleStudy of the discharge in Sierra Tejeda Southern sector (Málaga) by means of the correlation and spectral analysiseng

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Atribución-NoComercial-SinDerivadas 3.0 España
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