窒素添加による土壌炭素の安定性および循環に対する窒素添加の変動効果
Jason C Neff1, Alan R Townsend, Gerd Gleixner
1Earth Surface Processes Team, Geologic Division, US Geological Survey, MS 980, Denver Federal Center, Denver, Colorado 80225, USA. jneff@usgs.gov
Nature
|November 1, 2002
まとめ
窒素肥料は,土壌の炭素分解を軽量分数に加速しますが,より重い分数を安定させます. 大量土壌炭素は変化せず,現在の土壌炭素モデルの限界を示した.
科学分野:
- 土壌科学 土壌科学
- バイオジオケミストリー バイオジオケミストリー
- 環境科学 環境科学
背景:
- 土壌は地球上の炭素を大量に貯蔵しており,これは地球規模の炭素循環を理解する上で極めて重要です.
- 土壌の炭素分解に対する気候の影響は知られているが,窒素の役割は不明である.
- 反応性窒素は,農業と化石燃料から,世界中で増加しています.
研究 の 目的:
- 窒素肥料の土壌炭素動態への影響を調査する.
- 窒素添加に対する異なる土壌の炭素プールの反応を分析する.
主な方法:
- 14C,13C,および化合物固有の分析を用いた.
- 長期窒素肥料のプロットからの土壌炭素の検査.
主要な成果:
- 窒素添加は,土壌の軽い炭素分子の分解を加速した (十年周回).
- 窒素添加により,鉱物に関連した土壌の炭素分子が安定した (数十年から百年の寿命).
- 土壌の大量炭素の有意な変化は観察されなかった.
結論:
- 現在の単一プールモデルでは,環境変化に対する土壌の炭素反応を評価するには不十分です.
- 窒素の利用可能性は,土壌の炭素貯蔵に複雑な影響を及ぼします.
- 高濃度の肥料添加と長期の大気堆積効果を比較するためにさらなる研究が必要である.
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