气泡积累及其在上层地岩库的演变中的作用
A Parmigiani1,2, S Faroughi2,3, C Huber2,3
1Institute of Geochemistry and Petrology, ETH Zurich, Zurich 8092, Switzerland.
Nature
|April 14, 2016
概括
火山爆发释放大量的硫,导致全球冷却. 这项研究揭示了晶体贫乏的岩石中如何积聚挥发性阶段,解释了爆炸性喷发期间的高硫释放.
科学领域:
- 火山学
- 地质化学
- 流体动力学
背景情况:
- 大规模的石爆发会释放硫,导致全球变冷.
- 缺乏晶体的岩石比富含晶体的岩石更容易爆发.
- 观察到的硫释放往往超过了化储存的估计值.
研究的目的:
- 评估浅岩的喷发潜力.
- 确定挥发性释放的理论极限.
- 解释高硫释放在晶体贫乏的喷发.
主要方法:
- 研究了岩层挥发阶段 (MVP) 的流体动力学.
- 分析了富含晶体和缺乏晶体的MVP行为.
- 检查了毛细血管应力和粘度对比的相互作用.
主要成果:
- 磁性挥发性阶段 (MVP) 在富含晶体的岩中有效地迁移.
- MVP积聚在冰晶较少的岩储层中.
- 这种积累解释了爆炸性喷发期间的过度硫释放.
结论:
- 在区域性岩储中,岩挥发阶段的行为是关键.
- 有效的MVP迁移在富含晶体的区域和积累在缺乏晶体的区域是违反直觉的.
- 在缺乏晶体的岩石中积累的MVP导致高硫释放和爆发潜力.
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