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Dynamics of particulate phosphorus in a shallow eutrophic lake

We tested the hypothesis that in shallow, eutrophic Lake Kasumigaura, the concentration of particulate phosphorus (PP) is controlled by biogenic P (P in living or dead phytoplankton and bacterial cells), rather than by resuspension of inorganic P in sediment. Increases in wind velocity and turbidity...

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Bibliographic Details
Published in:The Science of the total environment 2016-09, Vol.563-564, p.413-423
Main Authors: Shinohara, Ryuichiro, Imai, Akio, Kohzu, Ayato, Tomioka, Noriko, Furusato, Eiichi, Satou, Takayuki, Sano, Tomoharu, Komatsu, Kazuhiro, Miura, Shingo, Shimotori, Koichi
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Language:English
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Summary:We tested the hypothesis that in shallow, eutrophic Lake Kasumigaura, the concentration of particulate phosphorus (PP) is controlled by biogenic P (P in living or dead phytoplankton and bacterial cells), rather than by resuspension of inorganic P in sediment. Increases in wind velocity and turbidity were associated with bottom shear stress exceeding the critical value for the lake (τc=0.15Nm−2); this increased turbidity was due to sediment resuspension. However, concentrations of PP; HCl-extractable, reactive P in PP (P-rP); and HCl-extractable, non-reactive P in PP (P-nrP) were not correlated with wind velocity (PP vs. wind velocity: r=0.40, p>0.05). Rather, the P-nrP concentration accounted for approximately 79% of PP, and the concentrations of PP, P-rP, and P-nrP were correlated with the particulate organic carbon (POC) concentration (POC vs. PP: r=0.90, p
ISSN:0048-9697
1879-1026
DOI:10.1016/j.scitotenv.2016.04.134