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Hydrogeochemistry of pristine basaltic aquifers

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

http://www.sciencedirect.com/science/article/pii/S0883292715300718#fig6

Highlights
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We investigate hydrogeochemistry of pristine basaltic aquifers.
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Groundwater is largely undersaturated with primary silicate minerals.
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We evaluate relative mobility of major and trace elements in groundwater.
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V, U, Zn, and Cr show higher variability in their occurrence and mobility.
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Water–rock interaction, pH, and redox control mobility of elements in groundwater.

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