まとめ
火山の噴火は,気候とオゾン層に影響を与える,重要な二酸化硫黄 (SO2) を放出します. 噴火前のマグマ蒸気は,赤外線光譜で特定され,この過剰なSO2の主要な源である.
科学分野:
- 地質化学 地質化学
- 火山学 火山学とは
- 大気科学 大気科学
背景:
- 1991年のピナトゥボ山噴火では,大量に二酸化硫黄 (SO2) が放出され,地球温暖化と平流層のオゾンに悪影響を及ぼした.
- 観測されたSO2の質量は,噴火前の溶解量を超えており,追加の噴火源が関与していたことを示しています.
研究 の 目的:
- ピナトゥボ山の噴火中に放出された二酸化硫黄 (SO(2) の過剰の源を特定するために.
- マグマとそのガス含有量の噴火前の状態を調査する.
主な方法:
- クォーツフェノクリスタスのガラスのインクルージョン内の溶けた水と二酸化炭素の赤外線光譜分析.
- 他のサブデュークションに関連する火山の弧からのガス排出データの比較.
主要な成果:
- 噴火前のマグマ内で,SO2を含む別の蒸気相の証拠が見つかりました.
- この蒸気相におけるSO2含有量は,噴火後に観測されたSO2過剰を説明する.
結論:
- 噴火前のマグマ蒸気は,爆発的な火山噴火の間に,以前過小評価されていた二酸化硫黄 (SO2) の重要な源です.
- この発見は,火山が気候や大気化学に与える影響を理解する上で重要な意味を持つ.
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