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• W2167379602 abstract "Abstract Lake Yogo is a small, eutrophic lake located 1.3 km north of Lake Biwa, Japan. The lake, which was originally a natural, closed lake, has a unique water management system. It is replenished with water pumped from Lake Biwa and supplies irrigation water to ≈ 5 km 2 of agricultural fields. As a result, Lake Yogo functions as a water storage dam and is artificially controlled. As seen in most stratified lakes in temperate regions, large amounts of phosphate (PO 4 ) are released from the sediment in the hypolimnetic water layer during the summer stratification period. In order to reduce the impacts of internal phosphorus (P) loading, a destratification aeration system was installed in the lake. Although the stratification was weakened concomitant with a temperature increase in the hypolimnetic layers, anoxic conditions were still observed because of the small scale of the aeration system, with cyanobacterial blooms continuing to occur during the summer and autumn of every year. Although the internal P load at the autumn turnover is probably immediately scavenged by its incorporation into ferric oxyhydroxide colloids, the phytoplankton present at that time would doubtless benefit from the temporary, increased PO 4 supply because of their rapid uptake rates. Although the PO 4 transported continually from the hypolimnetic to the epilimnetic layers by the destratification aeration system should be scavenged as ferric oxyhydroxide colloids, a portion of the PO 4 is probably incorporated into the phytoplankton biomass. As a result, an insufficient level of artificial destratification might support phytoplankton growth during the period of thermal stratification in the lake." @default.
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• W2167379602 creator A5029067544 @default.
• W2167379602 date "2004-09-01" @default.
• W2167379602 modified "2023-10-16" @default.
• W2167379602 title "Water management of Lake Yogo targeting internal phosphorus loading" @default.
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• W2167379602 doi "https://doi.org/10.1111/j.1440-1770.2004.00249.x" @default.
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