Hydrogeological and geochemical characterization of groundwater in the F'Kirina plain (eastern Algeria). (July 2021)

• Record Type: Journal Article
• Authors: Rahal, Omar; Gouaidia, Layachi; Fidelibus, Maria Dolores; Marchina, Chiara; Natali, Claudio; Bianchini, Gianluca
• Is Part Of: Applied geochemistry. Volume 130(2021)
• Publication Date: 2021-07
• Subjects: Groundwater salinization -- Geochemical tracers -- Stable isotopes -- Drought -- Water scarcity -- Endorheic basin; Environmental geochemistry -- Periodicals; Water chemistry -- Periodicals; Geochemistry -- Social aspects -- Periodicals; Geochemistry -- Periodicals; 551.9
• DOI: 10.1016/j.apgeochem.2021.104983
• Languages: English
• ISSNs: 0883-2927

Abstract

Abstract: The F'Kirina plain in eastern Algeria is an endorheic basin suffering water scarcity due to a combination of natural and man-made causes. Its hydrogeological system is complex as made by interconnected aquifers represented by Mesozoic, Cenozoic, and Quaternary lithological units. The combination of drought indicators and water level data shows that a groundwater drought affected the plain during the last 15 years, which reflects on current water quality. The reported geochemical analyses, including major ions and trace elements, indicate that the groundwater resource is suffering from salinization, mainly due to evaporation and leaching of soil salts, a process that is coupled with simultaneous cation-exchange effects. In this framework, we observe a geochemical evolution from the fresh Ca–HCO3 facies, typical of springs bordering the plain, towards more saline groundwater characterized by chloride/sulphate-rich facies in the middle of the plain approaching the sebka. However, geochemical diagrams indicate that in few wells salinization is also influenced by upraising of deep groundwater. The water isotopic composition of the F'Kirina plain samples suggests that they diversely record both recharge and evaporation components. Moreover, the most 18 O and D depleted compositions among the investigated ground-waters suggest recharge contributions by comparatively higher elevation or the involvement of old (fossil) water components. Graphical abstract: Image 1 Highlights: F'Kirina plain (Algeria) aquifer suffers of groundwater scarcity and salinization. Geochemical and isotope tracers show soil soluble component leaching and evaporation. Geochemistry highlights water-sediment interaction and cation-exchange processes. Elemental and isotopic ratios indicate the involvement of deep water components. Isotopes suggest the existence of fossil water end-members recharged in the past.