IDENTIFICATION OF HYDROGEOCHEMICAL PROCESSES IN A NORTH EASTERN ENDOREIC BASIN UNDER SEMI-ARID CONDITIONS (ALGERIA)

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dc.contributor.authorKenza Kadi
dc.contributor.authorD. Dib
dc.date.accessioned2024-02-28T13:54:32Z
dc.date.available2024-02-28T13:54:32Z
dc.date.issued2017
dc.description.abstractStatistical and geochemical methods were used to identify the factors influencing the behavior of groundwater in the Tarf watershed, characterized by a high water deficit. The chemical facies deduced from the piper diagram and the correlations between different major cations and anions evoked a dominance of the evaporite minerals with respect to the carbonates which are saturated and precipitated. Besides the projection of the results of a few points followed over a period of 4 years (2011-1015) on the Gibbs plot demonstrates the dominance of the processes of evaporation - precipitation with respect to the erosion which is very slowed during the last years due to the fact of lack of effective precipitation.
dc.identifier.issn1112-9867
dc.identifier.urihttp://dspace.univ-khenchela.dz:4000/handle/123456789/2281
dc.language.isoen
dc.publisherJournal of Fundamental and Applied Sciences
dc.titleIDENTIFICATION OF HYDROGEOCHEMICAL PROCESSES IN A NORTH EASTERN ENDOREIC BASIN UNDER SEMI-ARID CONDITIONS (ALGERIA)
dc.typeArticle
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