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Origin and fate of phosphorus in the Seine watershed (France): Agricultural and hydrographic P budgets
Author(s) -
Némery Julien,
Garnier Josette
Publication year - 2007
Publication title -
journal of geophysical research: biogeosciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2006jg000331
Subject(s) - soil water , environmental science , drainage basin , hydrography , surface runoff , hydrology (agriculture) , particulates , sediment , drainage , watershed , phosphorus , eutrophication , estuary , nutrient , geology , soil science , ecology , oceanography , chemistry , geography , geomorphology , biology , geotechnical engineering , organic chemistry , machine learning , computer science , cartography
Phosphorus (P) sources (point and diffuse) in the human‐impacted Seine basin (64,840 km 2 ) were evaluated for the year 2000. An agricultural P budget showed that fertilizers represented 59% (20–25 kgP ha −1 ) of P inputs to the soils. A P surplus (2.5 kg P ha −1 y −1 ) contributed to P enrichment of the agricultural soils whose stocks amounted to 1800–5000 kgP ha −1 . A hydrographic P budget showed that runoff (0.39–0.51 kgP ha −1 ) dominated the diffuse sources. These losses represented a very low percentage (0.01%) of the P stocks in soils and contributed to 19–25% of the total P inputs to the drainage network. Point sources remained the main source of P (75–81%), particularly in the downstream urbanized zone. Phosphorus retention in the river drainage network accounted for 9–15% of the total P inputs, indicating that it must not be ignored in large river P budget calculations. The Seine basin exported 8000 tP y −1 (44% as particulate P) to its estuary. The annual mean particulate P in suspended sediment at the outlet (2.9 gP kg −1 ) was fourfold greater than in headwaters and in rural zones. The similar increase of the particulate inorganic P/particulate organic P ratio in suspended sediment along the river continuum clearly indicated the increasing pressure of point sources. The close relation between P content of suspended sediment during the high‐flow period and the P content of agricultural soils resulted in proposing a novel method to calculate the PP losses from runoff.

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