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Updated: Feb 24, 2026

The Benthic Exchange of O2, N2 and Dissolved Nutrients Using Small Core Incubations
10:11

The Benthic Exchange of O2, N2 and Dissolved Nutrients Using Small Core Incubations

Published on: August 3, 2016

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河川段階の変動が,河川廊下の窒素酸化物源と沈殿地の動態に及ぼす影響

Lin Zhang1, Tianyuan Zheng1, Bo Guo2

  • 1Key Laboratory of Marine Environment and Ecology, Ministry of Education of China, Ocean University of China, Qingdao 266100, China; College of Environmental Science and Engineering, Ocean University of China, Qingdao 266100, China; Shandong Provincial Key Laboratory of Marine Environment and Geological Engineering, Ocean University of China, Qingdao 266100, China.

Water research
|February 22, 2026
PubMed
まとめ

河川段階の変動,特にダムによる変動は,河岸地帯を窒素酸化物 (N2O) の沈殿所から水源に変える可能性があります. これらの変化は,酸化還元条件と輸送プロセスを変化させることで,窒素循環とN2O排出に影響を及ぼします.

キーワード:
バイオジオケミカルプロセスハイポレイクスの交換酸化窒素酸化窒素は,酸化窒素の定期的な河川段階の変動.ソースとシンク.

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