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Updated: Jul 27, 2025

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The Diffusion of Passive Tracers in Laminar Shear Flow
Published on: May 1, 2018
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一个新的离散模型,在有限体积点稀释方法中更好地考虑沿钻井孔的标记物分布
Nataline Simon1, Serge Brouyère1, Pierre Jamin2
1Department Urban and Environmental Engineering, Hydrogeology and Environmental Geology, University of Liege, Building B52, Sart Tilman 4000, Belgium.
Journal of contaminant hydrology
|June 8, 2023
概括
有限体积点稀释方法 (FVPDM) 量化地下水流量. 一个新的离散模型解释了不完美的标记物混合,提高了长井和透性含水层的准确性.
科学领域:
- 水文地质学 水文地质学
- 环境科学 环境科学
- 地质物理学 地质物理学
背景情况:
- 有限体积点稀释法 (FVPDM) 是一种标准的单井追踪技术,用于量化地下水流量.
- 当前的FVPDM模型假设在测试井间隔内有完美的标记物同质化.
- 这种假设在长井或高度透的构造中可能会失败,导致不准确的流量估计.
研究的目的:
- 为FVPDM开发和验证一个新的离散模型,该模型明确纳入回流流量.
- 评估非完美的追踪剂混合对FVPDM结果和地下水流量计算的影响.
- 为在非理想的混合条件下提供准确的流量估计方法.
主要方法:
- 引入一种新的离散模型,以计算FVPDM的回流流量.
- 使用现场测量对离散模型的验证.
- 灵敏度分析,以评估混合流速对标记器分布的影响.
主要成果:
- 不均的标记物分布发生在循环回流与地下水流相比不足时.
- 经典的FVPDM解决方案在不完美的混合条件下高估了地下水流.
- 新的离散模型准确地估计了地下水流量,并评估了痕迹分布.
结论:
- 开发的离散模型提高了FVPDM在具有挑战性的水文地质环境中的可靠性.
- 它允许在不完美的混合条件下获得的现场数据的正确解释.
- 这种进步扩大了FVPDM可以测量的地下水流量范围.
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