进行模拟实验,研究堤内的岩混合
Tegan A Havard1, Thomas J Jones2, Janine L Kavanagh1
1Department of Earth, Ocean and Ecological Sciences, University of Liverpool, Liverpool, L69 3GP UK.
概括
在堤式系统中,岩的混合比在腔室式系统中更有效,特别是当岩具有类似的特性时. 这项研究有助于理解火山喷发和岩上升的复杂性.
科学领域:
- 地质化学 地质化学
- 火山学 火山学是一门学科.
- 流体动力学 流体动力学
背景情况:
- 火山管道系统中的岩混合影响了喷发风格和危险.
- 之前的研究使用了管状或状几何体,限制了对堤的推断.
- 堤几何形状是裂火山系统的特征.
研究的目的:
- 为了研究高比例堤几何体内的岩混合动力学.
- 为了比较堤和室式系统之间的混合效率.
- 了解对岩运输和财产演化的影响.
主要方法:
- 利用模拟实验,使用代表岩石的可混合流体对来进行模拟实验.
- 采用高比例的实验设置模拟堤.
- 分析了流量本地化,接口动态和混合率.
主要成果:
- 最初的流量定位在中心,在流体接口的混合向侧扩散.
- 当流体属性相似时,混合更快,接口更大.
- 与室内几何学相比,Dyke几何学促进了更大的混合.
结论:
- 堤几何学显著提高了岩混合效率.
- 混合动力学在岩上升过程中影响晶体和扩散交换.
- 实验结果与Kīlauea 2018年火山爆发的地化学数据一致,为真实世界的火山过程提供了洞察力.
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