Prediction of phosphorus mobilisation in inundated floodplain soils

After flooding, iron reduction in riverine wetlands may cause the release of large quantities of phosphorus. As phosphorus is an important nutrient causing eutrophication in aquatic systems, it is important to have a tool to predict this potential release. In this study we examined the P release to...

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Veröffentlicht in:Environmental pollution (1987) 2008-11, Vol.156 (2), p.325-331
Hauptverfasser: Loeb, Roos, Lamers, Leon P.M., Roelofs, Jan G.M.
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container_end_page 331
container_issue 2
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container_title Environmental pollution (1987)
container_volume 156
creator Loeb, Roos
Lamers, Leon P.M.
Roelofs, Jan G.M.
description After flooding, iron reduction in riverine wetlands may cause the release of large quantities of phosphorus. As phosphorus is an important nutrient causing eutrophication in aquatic systems, it is important to have a tool to predict this potential release. In this study we examined the P release to the soil pore water in soil cores from floodplains in the Netherlands and from less anthropogenically influenced floodplains from Poland. During the inundation experiment, concentrations of P in the pore water rose to 2–90 times the initial concentrations. P release was not directly related to the geographic origin of the soils. An important predictor variable of P release was found in the ratio between the concentration of iron-bound P and amorphous iron. This ratio may provide a practical tool for the selection of new areas for wetland creation, and for impact assessment of plans for riverine wetland restoration and floodwater storage. Mobilisation of phosphorus in floodplain wetland soils can be predicted with easily measurable soil characteristics.
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As phosphorus is an important nutrient causing eutrophication in aquatic systems, it is important to have a tool to predict this potential release. In this study we examined the P release to the soil pore water in soil cores from floodplains in the Netherlands and from less anthropogenically influenced floodplains from Poland. During the inundation experiment, concentrations of P in the pore water rose to 2–90 times the initial concentrations. P release was not directly related to the geographic origin of the soils. An important predictor variable of P release was found in the ratio between the concentration of iron-bound P and amorphous iron. This ratio may provide a practical tool for the selection of new areas for wetland creation, and for impact assessment of plans for riverine wetland restoration and floodwater storage. Mobilisation of phosphorus in floodplain wetland soils can be predicted with easily measurable soil characteristics.</description><subject>alluvial soils</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Ecology - methods</subject><subject>Engineering and environment geology. 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subjects alluvial soils
Earth sciences
Earth, ocean, space
Ecology - methods
Engineering and environment geology. Geothermics
Eutrophication
Exact sciences and technology
Flooding
floodplains
Floods
Forecasting
Freshwater
Geochemistry
iron
Marine and continental quaternary
mineral soils
Mineralogy
Models, Chemical
Netherlands
P fractionation
Phosphorus
Phosphorus - analysis
Pollution, environment geology
prediction
rivers
Silicates
Soil - analysis
soil chemical properties
Soil Pollutants - analysis
soil pore water
Surficial geology
Water geochemistry
Water Pollutants, Chemical - analysis
water pollution
Water storage
Wetland creation
wetland soils
Wetlands
title Prediction of phosphorus mobilisation in inundated floodplain soils
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