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Abstract. Fe-DGT (Diffusive Gradient in Thin-films), as a measure of in-situ net dissolved Fe production, together with conventional pore water ions, were determined in the upper 40 cm of organic rich sediments from Loch Duich, Scotland. There was an increase in net Fe production towards the base of the apparent Fe-R zone, which was interpreted as either being due to rapidly decreasing dissolved Fe...
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