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Hydrochemical evolution in the aquifers of the Ksar El Kebir-Larache sectors (Morocco)

dc.contributor.authorBouhmadi, B.
dc.contributor.authorBenavente Herrera, José
dc.contributor.authorHidalgo Estévez, Mari Carmen
dc.date.accessioned2015-03-26T12:35:05Z
dc.date.available2015-03-26T12:35:05Z
dc.date.issued1998
dc.identifier.urihttp://hdl.handle.net/10272/10175
dc.description.abstractThe synthesis of hydrochemical data obtained in the lower basin of the Loukkos river (Morocco) as well as the results of speciation and mass transfer calculations point out that the main processes which influence the groundwater composition of the study area are: a) the dissolution of calcite, dolomite, gypsum and halite, b) the acquisition ofC02 and c) the Ca/Na exchange with clayey sediments, although some mixing with connate saline waters can't be rejected. Thus, a hydrochemical evolution has been identified from low salinity (less than 0.5 g/l) waters of a Ca-HC03 type to others of 7-2 g/l (eventually a few tens of g/l) and Ca and/or Na-CI typeen_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.otherHydrochemistryen_US
dc.subject.otherAlluvial aquiferen_US
dc.subject.otherMineral equilibriaen_US
dc.subject.otherLoukkos riveren_US
dc.subject.otherMoroccoen_US
dc.titleEvolución hidroquímica en los acuíferos del sector Ksar El Kebir-Larache (Marruecos)en_US
dc.titleHydrochemical evolution in the aquifers of the Ksar El Kebir-Larache sectors (Morocco)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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