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A two-dimensional analytical solution for groundwater flow in a leaky confined aquifer system near open tidal water

机译:开放式潮水附近泄漏承压含水层系统中地下水流动的二维分析解决方案

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摘要

Groundwater in coastal areas is commonly disturbed by tidal fluctuations. A two-dimensional analytical solution is derived to describe the groundwater fluctuation in a leaky confined aquifer system near open tidal water under the assumption that the groundwater head in the confined aquifer fluctuates in response to sea tide whereas that of the overlying unconfined aquifer remains constant. The analytical solution presented here is an extension of the solution by Sun for two-dimensional groundwater flow in a confined aquifer and the solution by Jiao and Tang for one-dimensional groundwater flow in a leaky confined aquifer. The analytical solution is compared with a two-dimensional finite difference solution. On the basis of the analytical solution, the groundwater head distribution in a leaky confined aquifer in response to tidal boundaries is examined and the influence of leakage on groundwater fluctuation is discussed. Copyright © 2001 John Wiley and Sons, Ltd.
机译:沿海地区的地下水通常受到潮汐波动的干扰。推导了一个二维分析解决方案来描述潮汐水附近的泄漏承压含水层系统中的地下水波动,假设承压含水层中的地下水头随海潮而波动,而上方的无承压含水层中的地下水压头则保持恒定。此处提供的分析解决方案是Sun对密闭含水层中的二维地下水流的求解方法的扩展,以及Jiao和Tang对于渗漏密闭含水层中的一维地下水流的求解方案的扩展。将解析解与二维有限差分解进行比较。在分析结果的基础上,研究了渗漏承压含水层响应潮汐边界的地下水位分布,并探讨了渗漏对地下水波动的影响。版权所有©2001 John Wiley and Sons,Ltd.

著录项

  • 作者

    Jiao, JJ; Tang, Z;

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  • 年度 2001
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  • 原文格式 PDF
  • 正文语种 eng
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