在爆炸性火山活动中,地震震动和岩摇
A Mark Jellinek1, David Bercovici
1Department of Earth and Ocean Sciences, The University of British Columbia, Vancouver, British Columbia, V6T 1Z4, Canada. mjellinek@eos.ubc.ca
Nature
|February 26, 2011
概括
火山震动是爆炸性喷发的关键指标,可以通过一种新的模型来解释,在这种模型中,岩柱在富含气体的环内摇摆. 这解释了在全球不同火山中观察到的一致的震动频率.
科学领域:
- 地质物理学 地质物理学
- 火山学 火山学是一门学科.
- 地震学 地震学
背景情况:
- 火山震动是一种持续的振荡 (0.57赫兹),通常在爆炸性喷发之前发生,并且与气体流和地面变形有关.
- 现有的模型很难解释在各种火山中观察到的一致的震动频率,尽管管道结构和岩组成的变化.
研究的目的:
- 开发一种新的模型来解释火山震频率的普遍性.
- 为了研究驱动火山震荡振荡的物理机制.
主要方法:
- 利用了当代的看法,起的岩作为一个柱状插头在囊泡环内.
- 开发了一种基于柱振荡 ("摇摆") 与环形的"气弹"力相对应的模型.
主要成果:
- 岩摇摆模型解释了震动频率对导体几何和结构相对不敏感.
- 该模型预测火山爆发期间的震动频率和带宽会上升,与爆炸性相关.
结论:
- 对环状气体弹力进行摇摆的岩柱为全球火山震荡的恒定,窄频频率提供了强有力的解释.
- 该模型通过将震动特征与喷发动态和爆炸性联系起来,为喷发预测提供了洞察力.
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