Past anthropogenic activities offset dissolved inorganic phosphorus retention in the Mississippi River basin
The rapid acceleration of anthropogenic phosphorus (P) loadings to watersheds has fuelled massive freshwater and coastal eutrophication and completely changed the global P cycle. Within watersheds, emitted P is transported downstream towards estuaries. Reservoirs can retain a significant proportion...
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| Veröffentlicht in: | Biogeochemistry 2022-11, Vol.161 (2), p.157-169 |
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| creator | Vilmin, Lauriane Bouwman, Alexander F. Beusen, Arthur H. W. van Hoek, Wim Joost Mogollón, José M. |
| description | The rapid acceleration of anthropogenic phosphorus (P) loadings to watersheds has fuelled massive freshwater and coastal eutrophication and completely changed the global P cycle. Within watersheds, emitted P is transported downstream towards estuaries. Reservoirs can retain a significant proportion of this P. In the long term, this accumulated P can however be re-mobilized, a process lacking in current global P budgets. Here, we include P cycling in a coupled integrated assessment-hydrology-biogeochemistry framework with 0.5 by 0.5-degree spatial resolution and an annual time resolution, and apply it to the Mississippi River basin (MRB). We show that, while reservoirs have aided in the net retention of P, they serve as dissolved inorganic P (DIP) sources due to the transformation of legacy P in sediments. The increasing DIP sourcing in the MRB has been offsetting P retention in streams, especially towards the end of the twentieth century. Due to its bioavailability, DIP is the most likely form to trigger eutrophication. Although P inputs into the MRB have decreased since the 1970s, legacy effects are delaying positive outcomes of remediation measures. |
| doi_str_mv | 10.1007/s10533-022-00973-1 |
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We show that, while reservoirs have aided in the net retention of P, they serve as dissolved inorganic P (DIP) sources due to the transformation of legacy P in sediments. The increasing DIP sourcing in the MRB has been offsetting P retention in streams, especially towards the end of the twentieth century. Due to its bioavailability, DIP is the most likely form to trigger eutrophication. Although P inputs into the MRB have decreased since the 1970s, legacy effects are delaying positive outcomes of remediation measures.</description><identifier>ISSN: 0168-2563</identifier><identifier>EISSN: 1573-515X</identifier><identifier>DOI: 10.1007/s10533-022-00973-1</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Anthropogenic factors ; Bioavailability ; Biogeochemistry ; Biogeosciences ; Coastal zone ; Earth and Environmental Science ; Earth Sciences ; Ecosystems ; Environmental Chemistry ; Estuaries ; Eutrophication ; Freshwater ; Hydrology ; Inland water environment ; Life Sciences ; Phosphorus ; Reservoirs ; Resolution ; Retention ; River basins ; Rivers ; Sediments ; Spatial discrimination ; Spatial resolution ; Streams ; Watersheds</subject><ispartof>Biogeochemistry, 2022-11, Vol.161 (2), p.157-169</ispartof><rights>The Author(s) 2022</rights><rights>The Author(s) 2022. 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We show that, while reservoirs have aided in the net retention of P, they serve as dissolved inorganic P (DIP) sources due to the transformation of legacy P in sediments. The increasing DIP sourcing in the MRB has been offsetting P retention in streams, especially towards the end of the twentieth century. Due to its bioavailability, DIP is the most likely form to trigger eutrophication. 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W.</au><au>van Hoek, Wim Joost</au><au>Mogollón, José M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Past anthropogenic activities offset dissolved inorganic phosphorus retention in the Mississippi River basin</atitle><jtitle>Biogeochemistry</jtitle><stitle>Biogeochemistry</stitle><date>2022-11-01</date><risdate>2022</risdate><volume>161</volume><issue>2</issue><spage>157</spage><epage>169</epage><pages>157-169</pages><issn>0168-2563</issn><eissn>1573-515X</eissn><abstract>The rapid acceleration of anthropogenic phosphorus (P) loadings to watersheds has fuelled massive freshwater and coastal eutrophication and completely changed the global P cycle. Within watersheds, emitted P is transported downstream towards estuaries. Reservoirs can retain a significant proportion of this P. In the long term, this accumulated P can however be re-mobilized, a process lacking in current global P budgets. 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| subjects | Anthropogenic factors Bioavailability Biogeochemistry Biogeosciences Coastal zone Earth and Environmental Science Earth Sciences Ecosystems Environmental Chemistry Estuaries Eutrophication Freshwater Hydrology Inland water environment Life Sciences Phosphorus Reservoirs Resolution Retention River basins Rivers Sediments Spatial discrimination Spatial resolution Streams Watersheds |
| title | Past anthropogenic activities offset dissolved inorganic phosphorus retention in the Mississippi River basin |
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