日本,Usu火山からのアドベクティブフローによる二酸化炭素脱ガス
P A Hernández1, K Notsu, J M Salazar
1Laboratory for Earthquake Chemistry, Graduate School of Science, University of Tokyo, Bunkyo-Ku 113-0033, Tokyo, Japan. phdez@iter.rcanaria.es
まとめ
Usu火山でのマグマの二酸化炭素 (CO2) の脱ガス化は,2000年の噴火前に増加した. 噴火後,CO2の流れは減少し,マグマダイクからの急速な放出を示唆しています.
科学分野:
- 地質化学 地質化学
- 火山学 火山学とは
- 地球科学 地球科学 地球科学
背景:
- マグマの二酸化炭素 (CO2) の脱ガス化は,火山活動の重要な指標である.
- ガス移動パターンの理解は,噴火の予測に不可欠です.
研究 の 目的:
- 2000年のウス火山噴火前と後のCO2脱ガスパターンを分析するために.
- 二酸化炭素の流れの変化と火山の過程との関係を調査する.
主な方法:
- Usu火山山頂のカルデラでのCO2フローのモニタリング.
- ガス流量データと組み合わせた地震観測の分析.
主要な成果:
- CO2の流れは,噴火の6ヶ月前に1日120トンから340トンに増加した.
- 噴火後3ヶ月で,CO2フローが1日当たり39メトリックトンに大幅に減少したことが観察されました.
- 地震データは,噴火前のアドベクティブプロセスがガス移動を制御していることを示しました.
結論:
- 噴火前のCO2フロースの増加は,アドベクティブガス移動を示唆しています.
- 噴火後のCO2フルースの減少は,噴火中の急速な放出の結果である可能性が高い.
- ガス移動の動態は,マグマ室のプロセスと堤防の伝播と密接に関連しています.
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