2018年のキラウエア火山の噴火中の周期的な溶岩噴出
M R Patrick1, H R Dietterich2, J J Lyons2
1U.S. Geological Survey, Hawaiian Volcano Observatory, Hilo, HI 96720, USA. mpatrick@usgs.gov.
まとめ
火山噴火の速度は,浅いガス排出と深いマグマ供給の波によって周期的に変動します. これらのサイクルを理解することは 活発な火山からの溶岩の流れの危険を予測する鍵です
科学分野:
- 火山学
- 地理学
- 地球科学
背景:
- 溶岩流は活発な火山の近くのコミュニティに重大な脅威をもたらします.
- 溶岩の噴出速度は,溶岩の流れの行動と関連する危険性に影響を与える重要な要因です.
- 噴火速度の変動の原動力や時間軸はよくわかっていない.
研究 の 目的:
- 2018年のキラウエア噴火時の周期的な噴火率の変動の原因を調査する.
- 噴火率の変動をマグマ系内の特定のプロセスと関連付ける.
主な方法:
- 2018年のキラウエア噴火のマルチパラメータデータの分析.
- カルデラ崩壊などの地質学的な出来事との噴火周期の相関関係.
主要な成果:
- 2018年のキラウエア噴火は,短時間 (分) と長時間 (数十時間) の周期的な噴火率を示した.
- 短期的な循環は 浅いマグマの放出によって引き起こされた.
- 長い周期は,山頂のカルデラの崩壊によって引き起こされた圧力によるマグマ供給の急上昇と関連していました.
結論:
- 噴火速度の変動は,明確なマグマプロセスによって直接制御されます.
- 山頂のカルデラの崩壊は 重要なマグマ供給の急上昇を引き起こし 側面の噴火に影響を与えます
- この研究は,噴火のダイナミクスとマグマのシステム行動の関係を明らかにします.
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