在基岩岩的解压过程中直接观察脱气
Barbara Bonechi1, Margherita Polacci1, Fabio Arzilli2
1Department of Earth and Environmental Sciences, University of Manchester, Manchester, UK.
Science advances
|August 16, 2024
概括
了解火山喷发风格需要研究气溶合. 这项研究揭示了基岩岩中的泡动态,这对于预测喷发过渡和改善危险评估至关重要.
科学领域:
- 火山学 火山学是一门学科.
- 地质化学 地质化学
- 地质物理学 地质物理学
背景情况:
- 火山喷发的风格取决于在上升过程中气体-岩脱.
- 了解气泡动力学是预测爆炸性喷发和岩喷泉之间的过渡的关键.
研究的目的:
- 在自然条件下观察和量化玄武岩的气泡生长和凝聚.
- 为了研究岩粘度在火山上升期间对气体-融合的影响.
主要方法:
- 利用了X射线放射学与一种新型的高压/高温装置相结合.
- 从100 MPa到表面条件的压力范围实时量化泡动态.
主要成果:
- 在低粘度的岩中,气泡迅速凝聚起来,并在3秒内恢复球形.
- 粘度较高的岩具有较长的泡恢复时间,促进连接的泡通路.
结论:
- 在低粘度的岩石中,气融合会持续到管道上升的最后一百米,有利于岩喷泉.
- 开发的装置为岩过程提供了新的见解,增强了火山危险评估和风险减轻.
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