まとめ
大気中の窒素と水との雷による反応により,酸化窒素,窒素酸塩,窒素酸塩が生成されます. このプロセスは,原始的な海洋に窒素を供給し,潜在的に100万年以内にそれを満たす可能性があります.
科学分野:
- 大気化学 大気化学
- 地質化学 地質化学
- 海洋学 海洋学 海洋学
背景:
- 稲妻放電の近くの窒素と水の反応は,大気中の重要なプロセスです.
- これらの反応を理解することは,初期の地球環境における栄養源の推定に極めて重要です.
研究 の 目的:
- 稲妻の間に窒素と水の反応から酸化窒素の生成を定量化するために.
- 溶解性ニートリートとニトラートの発生源を推定する.
- 原始的な海洋窒素濃度に対する雷の寄与を評価する.
主な方法:
- 雷の周囲で発生する大気中の化学反応の分析.
- 異なる大気組成下での窒素化合物の産出量の推定.
- 原始的な海洋における窒素堆積のモデリング.
主要な成果:
- 稲妻は,酸素濃度が低い場合でも,かなりの量の酸化窒素を生成します.
- 溶性ナイトライトと窒素酸塩の関連源が推定されました.
- 稲妻は,年間10^6トンの窒素を,海に窒素酸塩として供給することができる.
結論:
- 雷とそれに続く大気化学は,原始的な海洋にとって実質的な窒素酸塩源を表しています.
- この海洋の窒素供給は100万年以内に現在の水準に達する可能性がある.
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