二氧化碳通过从日本Usu火山的向导流脱气
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
概括
在2000年爆发之前,Usu火山的岩石二氧化碳 (CO2) 脱气增加. 喷发后,二氧化碳的流量减少,这表明岩堤的释放速度很快.
科学领域:
- 地质化学 地质化学
- 火山学 火山学是一门学科.
- 地球科学 地球科学 地球科学
背景情况:
- 岩石中的二氧化碳 (CO2) 脱气是火山活动的关键指标.
- 了解气体迁移模式对于喷发预测至关重要.
研究的目的:
- 分析2000年乌苏火山爆发之前和之后的二氧化碳脱气模式.
- 研究二氧化碳流变化与火山过程之间的关系.
主要方法:
- 在Usu火山山顶火山口监测二氧化碳流量.
- 结合气体流量数据,对地震观测的分析.
主要成果:
- 在爆发前六个月,二氧化碳的流量从每天120公增加到340公.
- 喷发后三个月,二氧化碳流量显著减少,达到每天39公.
- 地震数据显示,在喷发前,有助力过程控制了气体迁移.
结论:
- 爆发前的二氧化碳流量增加表明气体迁移是有助的.
- 喷发后二氧化碳流量减少可能是由于喷发期间的快速释放造成的.
- 气体迁移动态与岩室过程和堤传播密切相关.
相关概念视频
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