Cl/Br ratios and chlorine isotope evidences for groundwater salinization and its impact on groundwater arsenic, fluoride and iodine enrichment in the Datong basin, China
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Natural high arsenic, fluoride and iodine groundwater co-occur with saline water.

Groundwater Cl/Br ratio and Cl isotope were used to study saline water.

Groundwater salinization processes retard the groundwater arsenic enrichment.

Intense evapotranspiration could restrict the groundwater fluoride concentration.

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