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Geometry, piezometry and hydraulic parameters ofthe aquifers ofthe Iower part ofthe Loukkos river basin (Morocco)

dc.contributor.authorBouhmadi, B.
dc.contributor.authorBenavente Herrera, José
dc.contributor.authorCruz Sanjulián, J. J.
dc.description.abstractThe alluvial materials of the Loukkos river (Morocco) downstream from Ksar-El-Kebir present transmissivity values in the 10-3 - 10-2 m2/s range and storativity values of 10-4-10-3 . The adjacent Oulad-Ogbane conglomerate formation drains towards the alluvium and is characterized by Iower T and higher S values. The morphology of the potentiometric surface (April, 1992) shows a general downstream hydraulic gradient ofnear 0.2 0/00 and a well-marked conoid —extending over TO km2 and with its apex slightly below the sea level— induced by the Ksar-El-Kebir supply pumping. The geometry of the substratum indicates a depression —elongated in the NW-SE direction— in the OuIad-Ogbane zone where depths of50 m below the sea leve/ are encounteredes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherAlluvial aquiferses_ES
dc.subject.otherAquifer's geometry and piezometryes_ES
dc.subject.otherPumping testses_ES
dc.subject.otherN. Moroccoes_ES
dc.titleGeometría, piezometría y parámetros hidráulicos de los acuíferos de la cuenca baja del río Loukkos (Marruecos)es_ES
dc.titleGeometry, piezometry and hydraulic parameters ofthe aquifers ofthe Iower part ofthe Loukkos river basin (Morocco)eng

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