在水平的Hele-Shaw细胞中,浮力驱动的溶解不稳定性
Kai Li1,2, Ran Hu1,2, Ting Wang3
1State Key Laboratory of Water Resources Engineering and Management, Wuhan University, Wuhan 430072, China.
Langmuir : the ACS journal of surfaces and colloids
|February 15, 2024
概括
岩石断裂中的矿物溶解由于浮力驱动的对流变得不稳定. 这项研究揭示了度边界层的临界厚度,预测了这种不稳定性在地质构造中何时发生.
科学领域:
- 地质化学和水文地质学
- 孔尺度反应式运输反应式运输
背景情况:
- 岩石断裂中的矿物溶解是地质过程的关键.
- 浮力驱动的对流可以导致溶解不稳定性,但孔尺度机制尚不清楚.
- 实验挑战限制了对流量和度场的理解.
研究的目的:
- 研究由浮力驱动的对流驱动的溶解不稳定性的孔尺度机制.
- 用模拟和理论分析辐射水平几何中的溶解.
- 开发一种关于溶解不稳定开始的预测模型.
主要方法:
- 开发并验证了包括重力效应在内的孔尺度建模方法.
- 采用3D孔尺度数值模拟来研究流溶动力学.
- 进行了度边界层和时间尺度相互作用的理论分析.
主要成果:
- 确定了浮力驱动溶解不稳定性的临界长度标准.
- 在有限和半无限域不稳定的政权之间进行区分.
- 证明的不稳定性来自于度边界层的重力不稳定的临界厚度.
结论:
- 建立了一个理论模型,通过模拟和实验验证,以预测溶解不稳定性.
- 增强对辐射水平流中的浮力驱动溶解不稳定性的理解.
- 提供了有关岩水文和地质二氧化碳储存完整性的见解.
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