Iodine budget in surface waters from Atacama: Natural and anthropogenic iodine sources revealed by halogen geochemistry and iodine-129 isotopes
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文摘

Natural waters from the Atacama Desert are strongly enriched in iodine.

Lower Iodine isotopic ratios confirm that most of the iodine derives from a deep fluid.

Higher iodine isotopic ratios indicate the input of anthropogenic meteoric water.

Groundwater was a key agent for iodine remobilization in Atacama.

There is a long-lived continental iodine cycle in the hyperarid Atacama Desert.

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