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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Short summary
Exfiltration of anoxic groundwater containing Fe(II) to surface water is an important mechanism controlling P speciation in the lowland catchments. Due to changes in pH and temperature, the Fe(II) oxidation rates were much lower in winter than in summer. This study also shows a fast transformation of dissolved P to structural P during the initial stage of the Fe oxidation process resulting in low dissolved P concentrations in the surface water throughout the year.
Articles | Volume 18, issue 11
Hydrol. Earth Syst. Sci., 18, 4687–4702, 2014
https://doi.org/10.5194/hess-18-4687-2014
Hydrol. Earth Syst. Sci., 18, 4687–4702, 2014
https://doi.org/10.5194/hess-18-4687-2014

Research article 27 Nov 2014

Research article | 27 Nov 2014

Iron oxidation kinetics and phosphate immobilization along the flow-path from groundwater into surface water

B. van der Grift et al.

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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (Editor review) (18 Sep 2014) by Pierre Regnier
AR by Hans Peter Broers on behalf of the Authors (30 Sep 2014)  Author's response    Manuscript
ED: Publish as is (17 Oct 2014) by Pierre Regnier
Publications Copernicus
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Short summary
Exfiltration of anoxic groundwater containing Fe(II) to surface water is an important mechanism controlling P speciation in the lowland catchments. Due to changes in pH and temperature, the Fe(II) oxidation rates were much lower in winter than in summer. This study also shows a fast transformation of dissolved P to structural P during the initial stage of the Fe oxidation process resulting in low dissolved P concentrations in the surface water throughout the year.
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