Seasonal movements of phosphorus and iron compounds, dissolved hydrogen sulfide, and others in anoxic seawater at lake hamana.
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概要
- 論文の詳細を見る
The sea bottom in the vicinity of the center of Lake Hamana in Japan forms a sea basin, and anoxic seawater appears in this bottom layer in summer. We examined the seasonal movements of phosphorus and iron compounds, dissolved hydrogen sulfide, and others in this anoxic seawater with a view to investigating their elution processes from the sediments of the sea basin into the anoxic seawater. Some parts of the elution phenomena of these components from the sediments of the sea basin in Lake Hamana into the anoxic seawater in summer will be described in the present work.
- 公益社団法人 日本化学会の論文
著者
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Tamura Hisae
Shizuoka Industrial Research Institurte
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Shimizu Chiaki
Fisheries Laboratory Faculty Of Agriculture University Of Tokyo
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INUI Takuo
Shizuoka Industrial Research Institute of Shizuoka Prefecture
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Okamoto Ken
Fisheries Laboratory Faculty Of Agriculture The University Of Tokyo
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Ichinose Norio
Department of Chemistry, Hamamatsu University School of Medicine
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Adachi Kyoko
Department of Chemistry, Hamamatsu University School of Medicine
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Mitsui Mina
Department of Chemistry, Hamamatsu University School of Medicine
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Kurokura Hisashi
Marine Biological Science Division, Faculty of Applied Biological Science, Hiroshima University
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