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What are the different types of phosphorus found in sediment in rivers and lakes? 


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Phosphorus in sediment in rivers and lakes exists in various forms. In the southern Caspian Sea, sediment phosphorus is mainly present as calcium-bound P (CaP), with minor fractions of loosely bound P (LP), reductant soluble P (FeP), and metallic oxide-bound P (AlP) . In Baiyangdian lake, inorganic P dominates, while organic P is mainly in the form of orthophosphate monoesters . Sediments under fish farms in Jakkimvaara Bay contain labile phosphorus, influenced by seasonal feeding habits of rainbow trout . In the Pasikhan river watershed, P sources include degraded rangelands, forests, rice fields, tea gardens, and gullies, with clay particles facilitating P transfer . River sediments in a German basin have labile, moderately labile, and stable P fractions, influenced by iron and aluminum contents and land use .

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Labile phosphorus is one type found in sediment, influenced by fish farming. It can accumulate and release back into the water column, impacting aquatic ecosystems. Other types are not specified.
In river sediments, phosphorus types include contributions from degraded rangelands, gullies, rice fields, and tea gardens, with clay particles playing a significant role in phosphorus transfer.
Phosphorus fractions in sediment include loosely bound P (LP), reductant soluble P (FeP), metallic oxide-bound P (AlP), and calcium carbonate-bound P (CaP), influencing bioavailability in aquatic ecosystems.
The phosphorus fractions found in river sediments are labile (NaOH-P), moderately labile, and stable (H2SO4-P), influencing P dynamics and potentially causing eutrophication in water bodies.
In sediment samples from Baiyangdian lake, inorganic phosphorus (dominant), orthophosphate monoesters (organic source when redox changes), and phosphorus bound to Fe, Al, and Mn oxides were identified.

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