Please use this identifier to cite or link to this item: http://archives.univ-biskra.dz/handle/123456789/624
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dc.contributor.authorBRINS, NAFAA-
dc.contributor.authorBOUDOUKHA, ABDERRAHMANE-
dc.date.accessioned2013-12-30T13:53:33Z-
dc.date.available2013-12-30T13:53:33Z-
dc.date.issued2013-12-30-
dc.identifier.urihttp://archives.univ-biskra.dz/handle/123456789/624-
dc.description.abstractThe plain of El-Outaya is in arid zone in southern Algeria. The groundwater are characterized by an Important and variability in its salinity. This work is presented to improve knowledge on these waters by proceeding to their statistical and hydrochemical classifications. Method C.A.H (hierarchical ascending classification) takes of three tendencies based on the importance of the mineralization. The salt rocks are responsible of this height salinity. Concerning the hydrochemical synthesis, the statistical information is confirmed. There is three dominant groups.en_US
dc.language.isofren_US
dc.subjectGroundwateren_US
dc.subjectHierarchical Ascending Classification (C.A.H)en_US
dc.subjectHydrochemistryen_US
dc.subjectSalinityen_US
dc.subjectchemical groupsen_US
dc.subjectPlain of El-Outayaen_US
dc.titleCLASSIFICATION STATISTIQUE ET HYDROCHIMIQUE DES EAUX SOUTERRAINES DE LA PLAINE D'EL-OUTAYA. (W) DE BISKRA-ALGÉRIEen_US
dc.typeArticleen_US
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