@article{10272/18115,
year = {1994},
url = {http://hdl.handle.net/10272/18115},
abstract = {The 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 encountered},
publisher = {Sociedad Geológica de España},
keywords = {Alluvial aquifers},
keywords = {Aquifer's geometry and piezometry},
keywords = {Pumping tests},
keywords = {N. Morocco},
title = {Geometría, piezometría y parámetros hidráulicos de los acuíferos de la cuenca baja del río Loukkos (Marruecos)},
title = {Geometry, piezometry and hydraulic parameters ofthe aquifers ofthe Iower part ofthe Loukkos river  basin (Morocco)},
author = {Bouhmadi, B. and Benavente Herrera, José and Cruz Sanjulián, J. J.},
}