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Assessments of Potential Spatial‐temporal Variations in Phosphorus Distribution and Fractionation in River Bed Sediments
Author(s) -
Wang Jingyu,
Pant Hari K.
Publication year - 2011
Publication title -
clean – soil, air, water
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 66
eISSN - 1863-0669
pISSN - 1863-0650
DOI - 10.1002/clen.201000088
Subject(s) - sediment , environmental science , fractionation , bioavailability , hydrology (agriculture) , watershed , environmental chemistry , phosphorus , geology , chemistry , geomorphology , bioinformatics , geotechnical engineering , organic chemistry , machine learning , computer science , biology
Sediment characteristics influence the distribution and bioavailability of phosphorus (P) in river sediments. In this study, we analyzed different P fractions in the sediments of the Bronx River, New York City, NY, using sequential extraction. The results showed that the average P pool rank order was HCl−P > NaOH−P > NaHCO 3 −P > residue−P, and their relative proportions were 3.7: 2.0: 1.4: 1 in sediments collected in 2006, while HCl−P > NaOH−P > residue−P > NaHCO 3 −P, with their relative proportions of 27.8:6.2:2.7:1 in the sediments obtained in 2007. The strong correlation between microbial P and organic P (OP), along with the changes in microbial P over time indicate that most of the OP in the river bed sediments is potentially bioavailable. The sediment transport, deposition, assimilation, the exchange of P between sediments and water columns, the land use changes, raw sewer discharge, gas spill, construction, fertilizer application, etc., as well as the hydro‐climatic changes could result in the spatial and temporal variations in P bioavailability in the river bed sediments. The estimations of P pools and their bioavailability in river bed sediments could help determine the spatial and temporal variations in P transport and impacts of land use on water quality, in turn, help regulate P in the river's watershed.