挥发性物质在岩室动态中的作用
Herbert E Huppert1, Andrew W Woods
1Institute of Theoretical Geophysics, Department of Applied Mathematics and Theoretical Physics, Silver Street, Cambridge CB3 9EW, UK. heh1@esc.cam.ac.uk
Nature
|December 6, 2002
概括
安地斯火山可以在更长的时间内喷发更多的岩. 一个新的模型表明,岩中的气体可压缩性可以通过释放储存的能量来显著增加喷发的体积和持续时间.
科学领域:
- 火山学 火山学是一门学科.
- 地质物理学 地质物理学
- 地质化学 地质化学
背景情况:
- 安地斯火山经常出现大量喷发,在长时间内释放出大量的岩.
- 观测到的喷发率周期从几个小时到几年不等,受到岩充电和水库压力的影响.
研究的目的:
- 模拟岩中气体压缩能力对喷发动态的影响.
- 调查可能增加喷发持续时间和体积的机制.
主要方法:
- 开发一个数字模型,将气体压缩效应纳入到 magma 中.
- 分析储存的内部能量释放如何影响喷发参数.
主要成果:
- 该模型预测火山爆发的持续时间和体积增加了多达百倍.
- 这种效应由溶解的挥发性物质释放储存的能量而放大.
- 浅层的岩室和富含挥发物质的岩有利于这种能量释放机制.
结论:
- 气体的压缩性是调节和可能放大火山爆发的关键因素.
- 乡村岩石冷却的岩石可以增强能量释放,导致更大的喷发.
- 这些发现为安第西斯火山的长期行为提供了新的见解.
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