過去と将来の大気中のCO2に対する非線形草原の反応 ((2))
Richard A Gill1, H Wayne Polley, Hyrum B Johnson
1Department of Biology, Duke University, Durham, NC 27708-0340, USA. rgill@wsu.edu
Nature
|May 17, 2002
まとめ
土壌の有機物質は炭素を貯蔵できるが,その容量は限られている. 大気中の二酸化炭素 (CO2) の増加は,歴史的に植物の成長と土壌の炭素を増加させたが,将来の増加は窒素の利用により制限される可能性がある.
科学分野:
- 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
- 気候科学 気候科学
背景:
- 大気中の二酸化炭素 (CO2) の濃度上昇は,土壌の炭素収縮によって緩和される可能性があります.
- 土壌の炭素貯蔵は,CO2に対する植物の反応と栄養素の利用可能性によって影響を受けます.
研究 の 目的:
- 大気中のCO2の過去および将来の増加に対する土壌の炭素貯蔵と窒素循環の反応性を調査する.
- 草原植物の生理学と土壌の炭素動態に対する高濃度のCO2の影響を理解する.
主な方法:
- 大気中のCO2濃度の連続的なグラデントを持つ草原の生態系を利用した (200〜550マイクロモルモル ((-1)).
- 測定された光合成速度,植物組織化学,土壌の炭素プール (旧・新),窒素の利用度.
主要な成果:
- 高濃度のCO2は,光合成の速度を高め,植物組織化学を変化させた.
- 土壌の炭素は低CO2で失われ,高CO2では古い炭素と新しい炭素のダイナミクスを相殺したため安定したままである.
- CO2グラデントに沿って,窒素の利用可能性が非線形で3倍に減少することが観察されました.
結論:
- 土壌の炭素貯蔵と窒素循環は,予測される将来のレベルよりも,過去のCO2増加に敏感です.
- 将来の CO2 の上昇の下での栄養素の制限の増加は,炭素吸収体として作用する土壌の能力を制限する可能性があります.
- 過去の土壌における炭素結合は有意であったかもしれないが,将来の可能性は栄養素の利用可能性によって制限されている.
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