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流体惯性控制矿物沉和孔隙堵塞,以网络规模的流量
Weipeng Yang1, Michael A Chen1, Sang Hyun Lee1
1Department of Earth and Environmental Sciences, College of Science and Engineering, University of Minnesota, Minneapolis, MN 55455.
概括
流体惯性控制矿物沉和在流量交叉点上的堵塞. 不同的流动模式 (雷诺德数) 决定了降水模式,影响了从碳矿化到微流体的过程.
科学领域:
- 地质化学 地质化学
- 流体动力学 流体动力学
- 化学工程是化学工程的重要组成部分.
背景情况:
- 液体混合过程中的矿物沉对于自然和工程系统至关重要.
- 了解水流下的降水动态是必不可少的,但具有挑战性.
研究的目的:
- 研究流体惯性在矿物沉和流交点堵塞中的作用.
- 为了阐明受流动力学和雷诺兹数影响的降水模式.
主要方法:
- 进行了微流体实验.
- 使用了三维反应式运输模拟.
- 对各种雷诺兹数 (Re) 的降水量进行了分析.
主要成果:
- 流体惯性控制流量交叉点的沉和堵塞,即使在层流中也是如此.
- 低Re (<10) 会导致接口沉和关闭;高Re (>50) 会导致快速堵塞.
- 不均的流量注入导致对称性破坏,导致下游通道的降水量增加.
结论:
- 惯性效应在交叉点和网络尺度上显著影响矿物沉.
- 这些发现为优化涉及混合诱导矿物沉的过程提供了一个框架.
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