地球の表面環境における広範囲にわたる岩石窒素源の収束証拠
B Z Houlton1, S L Morford2,3, R A Dahlgren2
1Department of Land, Air and Water Resources, University of California, Davis, CA, USA. bzhoulton@ucdavis.edu.
まとめ
ベッドロックは,大気へのインプットに匹敵する,以前は認識されていない,重要な窒素源です. この地質的な窒素は地球の窒素予算と地球上の炭素吸収に大きく影響します
科学分野:
- 地化学
- 生地化学
- エコロジー
背景:
- 窒素の利用は地球上の炭素の吸収と 地球規模の気候変動に重大な影響を及ぼします
- 伝統的な理解では,大気中の堆積が地上の生態系への主要な窒素供給源である.
研究 の 目的:
- 地上生態系における窒素の潜在源として岩床を調査する.
- 岩石から動員された窒素が世界の窒素予算に与える貢献度を定量化する.
- 地球上の炭素吸収源と気候変動の理解への影響を評価する.
主な方法:
- 全世界の窒素バランスの分析
- 地化学的な代理の試験
- 空間気象モデルの開発と適用
主要な成果:
- 表面に近い岩石から毎年約19〜31テラグラムの窒素が動員されます.
- この動員された窒素の11〜18テラグラムは,現地で化学的に耐候されます.
- この地質学的窒素の輸入は,管理されていない陸上の窒素バランスを8%から26%増加させます.
結論:
- ベッドロックは,大気からの投入に匹敵する,地上の生態系のための主要な窒素源を表しています.
- この発見は,世界の窒素予算の見直しを必要とする.
- 岩底の窒素の動員を理解することは,地上の炭素吸収器の栄養主体の制御を予測するために不可欠です.
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