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 |
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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. |
doi_str_mv | 10.1016/j.envpol.2008.02.006 |
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Mobilisation of phosphorus in floodplain wetland soils can be predicted with easily measurable soil characteristics.</description><identifier>ISSN: 0269-7491</identifier><identifier>EISSN: 1873-6424</identifier><identifier>DOI: 10.1016/j.envpol.2008.02.006</identifier><identifier>PMID: 18359542</identifier><identifier>CODEN: ENVPAF</identifier><language>eng</language><publisher>Kidlington: Elsevier Ltd</publisher><subject>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</subject><ispartof>Environmental pollution (1987), 2008-11, Vol.156 (2), p.325-331</ispartof><rights>2008 Elsevier Ltd</rights><rights>2009 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c476t-c0ebe1b90c7d84c51bc6e5aa8b552f82d72dc808b68d070e02ad619c2df249fc3</citedby><cites>FETCH-LOGICAL-c476t-c0ebe1b90c7d84c51bc6e5aa8b552f82d72dc808b68d070e02ad619c2df249fc3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0269749108001000$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3537,27901,27902,65534</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=20818541$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/18359542$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Loeb, Roos</creatorcontrib><creatorcontrib>Lamers, Leon P.M.</creatorcontrib><creatorcontrib>Roelofs, Jan G.M.</creatorcontrib><title>Prediction of phosphorus mobilisation in inundated floodplain soils</title><title>Environmental pollution (1987)</title><addtitle>Environ Pollut</addtitle><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.</description><subject>alluvial soils</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Ecology - methods</subject><subject>Engineering and environment geology. Geothermics</subject><subject>Eutrophication</subject><subject>Exact sciences and technology</subject><subject>Flooding</subject><subject>floodplains</subject><subject>Floods</subject><subject>Forecasting</subject><subject>Freshwater</subject><subject>Geochemistry</subject><subject>iron</subject><subject>Marine and continental quaternary</subject><subject>mineral soils</subject><subject>Mineralogy</subject><subject>Models, Chemical</subject><subject>Netherlands</subject><subject>P fractionation</subject><subject>Phosphorus</subject><subject>Phosphorus - analysis</subject><subject>Pollution, environment geology</subject><subject>prediction</subject><subject>rivers</subject><subject>Silicates</subject><subject>Soil - analysis</subject><subject>soil chemical properties</subject><subject>Soil Pollutants - analysis</subject><subject>soil pore water</subject><subject>Surficial geology</subject><subject>Water geochemistry</subject><subject>Water Pollutants, Chemical - analysis</subject><subject>water pollution</subject><subject>Water storage</subject><subject>Wetland creation</subject><subject>wetland soils</subject><subject>Wetlands</subject><issn>0269-7491</issn><issn>1873-6424</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2008</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><recordid>eNqFkVur1DAQgIMonvXoPxDdF31rnVyapi-CLN7ggIKe55AmE82SbWrSHvDfm7WLvikkM5D5Zki-EPKUQkuBylfHFqe7OcWWAagWWAsg75EdVT1vpGDiPtkBk0PTi4FekUelHAFAcM4fkiuqeDd0gu3I4XNGF-wS0rRPfj9_T6XuvJb9KY0hhmJ-l8J5rZMzC7q9jym5OZp6WFKI5TF54E0s-OSSr8ntu7dfDx-am0_vPx7e3DRW9HJpLOCIdBzA9k4J29HRSuyMUWPXMa-Y65mzCtQolYMeEJhxkg6WOc_E4C2_Ji-3uXNOP1Ysiz6FYjFGM2Fai6ZDp3gN_wcFcKqAV1BsoM2plIxezzmcTP6pKeizZX3Um2V9tqyB6Wq5tj27zF_HE7q_TRetFXhxAUyxJvpsJhvKH46BoqoTtHLPN86bpM23XJnbLwwoB9rXh0hRidcbgVXsXcCsiw042fppGe2iXQr_vusvjnKm3g</recordid><startdate>20081101</startdate><enddate>20081101</enddate><creator>Loeb, Roos</creator><creator>Lamers, Leon P.M.</creator><creator>Roelofs, Jan G.M.</creator><general>Elsevier Ltd</general><general>Elsevier</general><scope>FBQ</scope><scope>IQODW</scope><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>C1K</scope><scope>SOI</scope><scope>7QH</scope><scope>7TV</scope><scope>7U6</scope><scope>7U7</scope><scope>7UA</scope><scope>F1W</scope><scope>H97</scope><scope>L.G</scope></search><sort><creationdate>20081101</creationdate><title>Prediction of phosphorus mobilisation in inundated floodplain soils</title><author>Loeb, Roos ; Lamers, Leon P.M. ; Roelofs, Jan G.M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c476t-c0ebe1b90c7d84c51bc6e5aa8b552f82d72dc808b68d070e02ad619c2df249fc3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2008</creationdate><topic>alluvial soils</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Ecology - methods</topic><topic>Engineering and environment geology. Geothermics</topic><topic>Eutrophication</topic><topic>Exact sciences and technology</topic><topic>Flooding</topic><topic>floodplains</topic><topic>Floods</topic><topic>Forecasting</topic><topic>Freshwater</topic><topic>Geochemistry</topic><topic>iron</topic><topic>Marine and continental quaternary</topic><topic>mineral soils</topic><topic>Mineralogy</topic><topic>Models, Chemical</topic><topic>Netherlands</topic><topic>P fractionation</topic><topic>Phosphorus</topic><topic>Phosphorus - analysis</topic><topic>Pollution, environment geology</topic><topic>prediction</topic><topic>rivers</topic><topic>Silicates</topic><topic>Soil - analysis</topic><topic>soil chemical properties</topic><topic>Soil Pollutants - analysis</topic><topic>soil pore water</topic><topic>Surficial geology</topic><topic>Water geochemistry</topic><topic>Water Pollutants, Chemical - analysis</topic><topic>water pollution</topic><topic>Water storage</topic><topic>Wetland creation</topic><topic>wetland soils</topic><topic>Wetlands</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Loeb, Roos</creatorcontrib><creatorcontrib>Lamers, Leon P.M.</creatorcontrib><creatorcontrib>Roelofs, Jan G.M.</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>Medline</collection><collection>MEDLINE</collection><collection>MEDLINE (Ovid)</collection><collection>MEDLINE</collection><collection>MEDLINE</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Environment Abstracts</collection><collection>Aqualine</collection><collection>Pollution Abstracts</collection><collection>Sustainability Science Abstracts</collection><collection>Toxicology Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 3: Aquatic Pollution & Environmental Quality</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Environmental pollution (1987)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Loeb, Roos</au><au>Lamers, Leon P.M.</au><au>Roelofs, Jan G.M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Prediction of phosphorus mobilisation in inundated floodplain soils</atitle><jtitle>Environmental pollution (1987)</jtitle><addtitle>Environ Pollut</addtitle><date>2008-11-01</date><risdate>2008</risdate><volume>156</volume><issue>2</issue><spage>325</spage><epage>331</epage><pages>325-331</pages><issn>0269-7491</issn><eissn>1873-6424</eissn><coden>ENVPAF</coden><abstract>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.</abstract><cop>Kidlington</cop><pub>Elsevier Ltd</pub><pmid>18359542</pmid><doi>10.1016/j.envpol.2008.02.006</doi><tpages>7</tpages></addata></record> |
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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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