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计算水平水流通过渗漏含水层的地下水运移时间。

Calculating ground water transit time of horizontal flow through leaky aquifers.

作者信息

Braunsfurth Angelika C, Schneider Wilfried

机构信息

Hamburg University of Technology, Institute of Water Resources and Water Supply, Schwarzenbergstrasse 95, 21073 Hamburg, Germany.

出版信息

Ground Water. 2008 Jan-Feb;46(1):160-3. doi: 10.1111/j.1745-6584.2007.00393.x.

Abstract

The calculation of ground water transit times is one important factor in ground water protection. In this paper, we present an analytical solution for the transit time for a Dupuit-type flow system applicable to saturated flow through a horizontal leaky aquifer discharging to a downgradient fixed-head boundary under steady-state conditions. We investigate the influence of leakage when comparing the resulting travel times of our model based on head-dependent leakage with the commonly used model with no leakage and a simplified model with constant leakage. The results show significant differences in the position of the water divide and transit time, suggesting that leakage cannot be ignored.

摘要

计算地下水运移时间是地下水保护中的一个重要因素。在本文中,我们给出了一个适用于稳态条件下通过水平渗漏含水层向降坡固定水头边界排泄的饱和流的Dupuit型流系统运移时间的解析解。在将基于水头依赖渗漏的模型所得运移时间与常用的无渗漏模型和简化的恒定渗漏模型所得运移时间进行比较时,我们研究了渗漏的影响。结果表明,分水线位置和运移时间存在显著差异,这表明渗漏不能被忽略。

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