Oxidation of iron over a

Iron oxidation

Iron oxidation kinetics and phosphate immobilization along the flow-path from groundwater into surface water
B. van der Grift1, 2, J. C. Rozemeijer2, J. Griffioen1, 2, and Y. van der Velde3
1Department of Innovation, Environmental and Energy Sciences – Faculty of Geosciences, Utrecht University, P.O. Box 80115, 3508 TA Utrecht, the Netherlands
2Deltares, P.O. Box 85467, 3508 AL Utrecht, the Netherlands
3Soil Geography and Landscape, Wageningen University and Research Centre, Droevendaalsesteeg 4, 6708 PB Wageningen, the NetherlandsRevised: 30 September 2014 – Accepted: 17 October 2014 – Published: 27 November 2014Abstract. The retention of phosphorus in surface waters through co-precipitation of phosphate with Fe-oxyhydroxides during exfiltration of anaerobic Fe(II) rich groundwater is not well understood. We developed an experimental field set-up to study Fe(II) oxidation and P immobilization along the flow-path from groundwater into surface water in an agricultural experimental catchment of a small lowland river. We physically separated tube drain effluent from groundwater discharge before it entered a ditch in an agricultural field. Through continuous discharge measurements and weekly water quality sampling of groundwater, tube drain water, exfiltrated groundwater, and surface water, we investigated Fe(II) oxidation kinetics and P immobilization processes. The oxidation rate inferred from our field measurements closely agreed with the general rate law for abiotic oxidation of Fe(II) by O2. Seasonal changes in climatic conditions affected the Fe(II) oxidation process. Lower pH and lower temperatures in winter (compared to summer) resulted in low Fe oxidation rates. After exfiltration to the surface water, it took a couple of days to more than a week before complete oxidation of Fe(II) is reached. In summer time, Fe oxidation rates were much higher. The Fe concentrations in the exfiltrated groundwater were low, indicating that dissolved Fe(II) is completely oxidized prior to inflow into a ditch. While the Fe oxidation rates reduce drastically from summer to winter, P concentrations remained high in the groundwater and an order of magnitude lower in the surface water throughout the year. This study shows very fast immobilization of dissolved P during the initial stage of the Fe(II) oxidation process which results in P-depleted water before Fe(II) is completely depleted. This cannot be explained by surface complexation of phosphate to freshly formed Fe-oxyhydroxides but indicates the formation of Fe(III)-phosphate precipitates. The formation of Fe(III)-phosphates at redox gradients seems an important geochemical mechanism in the transformation of dissolved phosphate to structural phosphate and, therefore, a major control on the P retention in natural waters that drain anaerobic aquifers.
Read electro-mechanical engineering blog
You might also like
oxidation of aluminium metal, producing pure iron
oxidation of aluminium metal, producing pure iron
How to Oxidize iron
How to Oxidize iron
Early diagenetic quartz formation at a deep iron oxidation
Early diagenetic quartz formation at a deep iron oxidation ...
L20-14 ChemQuiz: Oxidation of Iron - calculating the
L20-14 ChemQuiz: Oxidation of Iron - calculating the ...
Iron Age Grates Material Finishes and Oxidation
Iron Age Grates Material Finishes and Oxidation
Iron Oxidation & Method to Prevent Oxidation
Iron Oxidation & Method to Prevent Oxidation
Aoyue Aoyue Soldering Iron Tip Cleaner with Brass wire sponge, no water needed
Home Improvement (Aoyue)
  • Cleans Tip without Messy Wet Sponges
  • Uses Low abrasive Brass, no water needed
  • Works with any tip
  • Heat resistant Stainless Steel Case
  • lengthens tip life by reducing oxidation
Related Posts