大気中の堆積化学の変化に起因する溶解した有機炭素の傾向
Donald T Monteith1, John L Stoddard, Christopher D Evans
1Environmental Change Research Centre, UCL, London, WC1E 6BT, UK. dmonteit@geog.ucl.ac.uk
Nature
|November 23, 2007
まとめ
湖や小川の溶けた有機炭素 (DOC) は,気候変動ではなく,酸性堆積の減少により上昇しています. これは,酸化からの生態系の回復を示し,地域的な炭素バランスに影響を与える.
科学分野:
- 環境科学 環境科学
- エコロジー エコロジー エコロジー
- バイオジオケミストリー バイオジオケミストリー
背景:
- 氷河地帯の地表水における溶解有機炭素 (DOC) の広範な増加が観察されています.
- 既存の仮説は,人為的な強制 (気候変動,窒素堆積,土地利用) または大気中の硫酸塩の減少による工業化以前のレベルへの戻りを含む.
- これらの仮説は,未知の世界的な炭素循環の結果とともに,継続的なDOC上昇を示唆しています.
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