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Porewater oxidation, dissolved phosphate and the iron curtain

Iron-phosphorus relations in tidal freshwater marshes

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Abstract

The process of dissolved phosphate removal from aqueous solution, which occurs during oxidation of soluble ferrous compounds to insoluble ferric forms, was examined in soils of two tidal freshwater marshes. Sites of amorphous iron deposition and sorption or co-precipitation of phosphate were found to be in surface soils and along creekbanks, where both ion diffusion and porewater advection move dissolved iron and phosphate from reduced to oxidized regions. Profiles of extractable iron and total phosphorus from creekbank and interior soils were consistent with hypothesized differences between a high and a low marsh. Porewater concentrations of dissolved phosphate were higher in creekbank soils of the high marsh, compared with water actually discharging from the creekbank during tidal exposure. We propose that an iron curtain of ferric hydroxides functions as a barrier to diffusive and advective movement of dissolved phosphate along surfaces of tidal freshwater marshes, and has important implications for the distribution and availability of phosphorus in other types of wetlands and aqueous systems.

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Authors and Affiliations

  1. Department of Environmental Sciences, University of Virginia, Clark Hall, Charlottesville, Virginia, 22903, USA

    Randolph M. Chambers & William E. Odum

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  1. Randolph M. Chambers
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  2. William E. Odum
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Chambers, R.M., Odum, W.E. Porewater oxidation, dissolved phosphate and the iron curtain. Biogeochemistry 10, 37–52 (1990). https://doi.org/10.1007/BF00000891

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