カルボニル硫化物と二硫化炭素は,セントヘレンズ山の噴火からのものです
まとめ
セントヘレンス山からの火山灰は,かなりの量の炭化硫化物と二硫化炭素ガスを放出しました. これは,硫黄に富んだガスが灰の粒子に吸収され,大規模な噴火後に直接平流層に到達することを示唆しています.
科学分野:
- 地質化学 地質化学
- 大気化学 大気化学
- 火山学 火山学とは
背景:
- 火山の噴火は,平流圏のエアロゾール層に影響を及ぼすことが知られている.
- ユンゲ硫酸塩層は,平流圏の重要な構成要素である.
- ストラトスフィアへの硫黄の輸送の正確なメカニズムは,噴火後のさらなる解明を必要としています.
研究 の 目的:
- 周囲の温度で火山灰のガス放出特性を調査する.
- セントヘレン山から炭素硫化物と二酸化炭素が放出されているかどうかを判断する.
- 火山灰を介して平流層に直接硫黄を輸送するメカニズムを提案する.
主な方法:
- セントヘレンス山の火山灰から放出されたガスの分析.
- ガス放出を測定するための室温実験.
主要な成果:
- 1980年のセントヘレンズ山噴火の灰は,室温でかなりの量のカルボニル硫化物 (COS) と二酸化炭素 (CS2) を容易に放出しました.
- これらのガスは,灰の粒子に吸収されることが観察されました.
結論:
- 火山灰の粒子に吸収されたカルボニル硫化物と二硫化炭素は,直接平流層に運ばれます.
- このメカニズムは,硫黄が主要な火山噴火後にユンゲ硫酸塩層を強化するための経路を提供します.
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