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Hydrogeochemistry of pristine basaltic aquifers


Occurrence and mobility of major and trace elements in groundwater from pristine volcanic aquifers in Jeju Island, Korea


We investigate hydrogeochemistry of pristine basaltic aquifers.

Groundwater is largely undersaturated with primary silicate minerals.

We evaluate relative mobility of major and trace elements in groundwater.

V, U, Zn, and Cr show higher variability in their occurrence and mobility.

Water–rock interaction, pH, and redox control mobility of elements in groundwater.


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