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This study investigates the geochemical and isotopic characteristics of the Oued Laya aquifer system in Sousse, Tunisia, focusing on groundwater salinity and mineralization processes. Results indicate that salinity is primarily due to mineral dissolution, particularly halite and gypsum, rather than seawater intrusion or increased water extraction. The findings highlight the complexity of groundwater salinization and suggest further research is needed to confirm the contributions of various sources to the aq

Author

aicha.rabah

Language

EN