太陽光は,淡水と海洋の窒素酸化物の非生物的形成を促す
Elizabeth Leon-Palmero1,2, Rafael Morales-Baquero1, Bo Thamdrup2
1Departamento de Ecología, Universidad de Granada, Granada, Spain.
まとめ
太陽光は水中の窒素酸化物 (N2O) を生成する新しい経路である光化学窒素化を駆動する. この未知のN2Oの源は,世界の温室効果ガス予算とオゾン層の枯渇に大きな影響を与える可能性があります.
科学分野:
- 環境科学
- 大気化学
- 海洋学
背景:
- 窒素酸化物 (N2O) は重要な温室効果ガスであり,オゾン層を破壊する物質である.
- 大気中のN2Oの正確な源は,まだ完全に理解されていません.
- 既存の N20 予算は,既知のすべての生産経路を考慮していない.
研究 の 目的:
- 水環境におけるN2O生産の新たな経路を特定し,特徴づけること.
- 太陽光によるプロセスのN2O排出量への貢献を定量化する.
- グローバル N20 予算の文脈におけるこの新しい経路の重要性を評価する.
主な方法:
- 異なる条件下でのN2O生産の実験調査
- N2Oの生産率と基質の起源を決定するために同位体トレーサを使用した.
- 光化学的N2Oの生成速度を測定し,放射線量と相関させた.
主要な成果:
- 新しいN2O生産経路を発見し,命名しました.
- 淡水と海水における酸素と無生物の条件下で,実質的なN2Oの生産が実証されている.
- 主要な基質としてニートリットを特定し,ニートリートは光還元によっても貢献しています.
- 観測されたN2Oの生成率は,放射線量と強く相関している.
- 光化学的なN2O生産は,地表水における生物学的N2O生産を上回った.
結論:
- 光化学窒素化は,以前見過ごされていた大気中のN2Oの重要な源です.
- このプロセスは,淡水と海洋の表面水の両方で発生し,世界のN2O排出量に貢献しています.
- この結果は,現在の温室効果ガス予算とオゾン層の破壊モデルを再評価することを必要としています.
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