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Impact of nutrient enrichment in a waterchestnut ecosystem at Takahama-Iri Bay of Lake Kasumigaura, Japan

I. Nutrient influx and phytoplankton bloom

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Abstract

The heaviest algal bloom that can be expected in an aquatic system was formed in a waterchestnut ecosystem in Lake Kasumigaura during the summer in 1978 when the water temperature was greater than 30°C, caused by the nutrient discharges from the River Koise and the River Sanno. The heavy bloom not only threatens the steady-state equilibrium of the eutrophic system of the Lake but also must accelerate the Lake transformation into a low moor by forming ooze on the lake bottom with the precipitation of a large amount of dead blue-green algae.

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Seki, H., Takahashi, M. & Ichimura, SE. Impact of nutrient enrichment in a waterchestnut ecosystem at Takahama-Iri Bay of Lake Kasumigaura, Japan. Water Air Soil Pollut 12, 383–391 (1979). https://doi.org/10.1007/BF01047024

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  • DOI: https://doi.org/10.1007/BF01047024

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