Hydrogeochemistry of co-occurring geogenic arsenic, fluoride and iodine in groundwater at Datong Basin, northern China
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文摘

Co-mobilization of As, F and I was identified at Datong Basin.

Both As and I are released via reductive dissolution of Fe minerals.

Some amounts of As and I may be sequestered by FeS precipitates.

Intensive evaporation promotes retention of As but mobilization of F and I.

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