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Multi-isotopes (δD, δ18Owater, 87Sr/86Sr, δ34S and δ18Osulfate) as indicators for groundwater salinization genesis and evolution of a large agricultural drainage lake basin in Inner Mongolia, Northwest China

HydrogeologyEngineeringWater ResourcesInner MongoliaNorthwest ChinaIsotope GeochemistryGeochemistryHydrogeologic SystemGroundwater HydrogeochemistryGroundwater Salinization GenesisHydrologyEarth Science