瓦哈里火山的热喷发是由热水矿物化和岩石气体输入驱动的
Sophie C Pearson-Grant1, Michael J Heap2,3, Adrian E Croucher4
1Earth Sciences New Zealand, Lower Hutt, New Zealand.
概括
气喷发很难预测. 数字模型表明,低透性的密封件捕获气体,导致几个月内喷发,脱气的变化可以信号即将发生的事件.
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
- 水文地质学 水文地质学
背景情况:
- 热喷发是危险的火山事件,很难预测.
- 了解导致喷发的地下条件对于开发预警系统至关重要.
研究的目的:
- 调查热,水力和地质因素导致热喷发的原因.
- 探索驱动这些火山事件的时间尺度和机制.
主要方法:
- 利用热量和流体流动的3维数值模型.
- 纳入来自新西兰瓦哈里/白岛火山的现场和实验室数据.
主要成果:
- 确定了水热矿化,低透性的密封件作为捕获气体的关键特征.
- 证明被困气体的压力可以在几天到几个月内超过岩石的强度,引发喷发.
- 通过二次通风口持续脱气的变化可以表明主管道的压力累积.
结论:
- 提供了对热喷发触发的过程和时间尺度的新见解.
- 为量化解释火山信号提供了一个框架,以评估喷发潜力.
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