2018年基拉韦亚火山爆发期间的周期性岩喷发
M R Patrick1, H R Dietterich2, J J Lyons2
1U.S. Geological Survey, Hawaiian Volcano Observatory, Hilo, HI 96720, USA. mpatrick@usgs.gov.
概括
火山爆发速度因浅层排气和更深层的岩供应激增而周期性波动. 了解这些循环是预测活动火山的岩流危险的关键.
科学领域:
- 火山学
- 地质学
- 地球科学
背景情况:
- 岩流对活火山附近的社区构成重大威胁.
- 卷积喷发率是影响岩流动行为和相关危险的关键因素.
- 喷发率变化的驱动力和时间表尚不清楚.
研究的目的:
- 调查2018年基拉韦亚火山爆发期间周期性喷发率波动的原因.
- 将喷发速度的变化与岩层系统中的特定过程联系起来.
主要方法:
- 分析2018年基拉韦亚火山爆发的多参数数据.
- 喷发周期与地质事件 (如火山口崩) 的相关性.
主要成果:
- 2018年Kīlauea火山爆发在短时间 (几分钟) 和长时间 (几十小时) 的周期性爆发率.
- 短期循环是由浅层岩排气驱动的.
- 长期周期与高峰火山崩事件引发的压力驱动的岩供应激增有关.
结论:
- 喷发速度的波动是由不同的岩层过程直接控制的.
- 顶峰火山崩可能会引发大量的岩供应,影响侧面喷发.
- 这项研究阐明了喷发动态与岩石系统行为之间的关系.
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