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Updated: Jul 12, 2026

The Benthic Exchange of O2, N2 and Dissolved Nutrients Using Small Core Incubations
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Published on: August 3, 2016

pelagic 海洋沈殿物における酸素消費

J W Murray, V Grundmanis

    Science (New York, N.Y.)
    |September 26, 1980
    PubMed
    まとめ

    溶解した酸素は,太平洋の沈殿物の深さに伴い減少し,バイオターバーションによる有機炭素供給の制限により,平準化します. これにより,測定可能な酸素のグラデーションと,堆積物と水の界面を横断する拡散的な流れが生じる.

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