まとめ
エル・チホン火山は,硫黄や水銀のような大量に揮発性元素を放出しました. これらの元素,特にヒ素は,より小さな火山灰の粒子に集中していました.
科学分野:
- 地質化学 地質化学
- 大気科学 大気科学
- 火山学 火山学とは
背景:
- メキシコのエル・チホン火山は,1982年に噴火した.
- 火山の羽根には,微量ガス,粒子,および酸性揮発性物質が含まれています.
研究 の 目的:
- El Chichón火山の羽根の微量ガスと微粒子を分析するために.
- 微量元素の排出量とその粒子の大きさの分布を定量化するために.
主な方法:
- 火山の羽根を航空機で採取する.
- 元素濃度のための中性子活性化分析.
- 流量推定のための硫黄排出量率への正常化.
主要な成果:
- 硫化水素は,硫黄ガスの支配的成分でした.
- 揮発性元素 (S,Cl,As,Se,Br,Sb,I,W,Hg) は,高濃度 (60-20,000x) の羽根に含まれていた.
- アルゼン,アンチモン,セレニウムは,小さな粒子 (<3ミクロメートル) で発見されました.
- 激しい噴火からのストラトスフィアの灰は,静かな羽毛物質よりも高い元素濃度 (10-30倍) を示した.
結論:
- 火山からの放射は,大気組成に大きな影響を与える.
- 微量元素を粒子に分割する方法は,元素と粒子のサイズによって異なります.
- 激しい噴火は,平流層の元素負荷により大きな影響を及ぼします.
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