首页> 外文期刊>Journal of Hydrology >An explicit approach to capture diffusive effects in finite water-content method for solving vadose zone flow
【24h】

An explicit approach to capture diffusive effects in finite water-content method for solving vadose zone flow

机译:求解渗流区流的有限含水量方法中捕获扩散效应的显式方法

获取原文
获取原文并翻译 | 示例
           

摘要

Vadose zone flow problems are usually solved from the Richards equation. Solution to the Richards equation is generally challenging because the hydraulic conductivity and diffusivity in the equation are strongly non-linear functions of water content. The finite water-content method was proposed as an alternative general solution method of the vadose zone flow problem for infiltration, falling slugs, and vadose zone response to water table dynamics based on discretizing the water content domain into numerous bins instead of the traditional spatial discretization. In this study, we develop an improved approach to the original finite water-content method (referred to as TO method hereinafter) that better simulates diffusive effects but retains the robustness of the TO method. The approach treats advection and diffusion separately and considers diffusion on a bin by bin basis. After discretizing into water content bins, we treat the conductivity and diffusivity in individual bins as water content dependent constant evaluated at given water content corresponding to each bin. For each bin, we can solve the flow equations analytically since the hydraulic conductivity and diffusivity can be treated as a constant. We then develop solutions for each bin to determine the diffusive water amounts at each time step. The water amount ahead of the convective front for each bin is redistributed among water content bins to account for diffusive effects. The application of developed solution is straightforward only involving algebraic manipulations at each time step. The method can mainly improve water content profiles, but has no significant difference for the total infiltration rate and cumulative infiltration compared to the TO method. Although the method separately deals with advection and diffusion, it can account for the coupling effects of advection and diffusion reasonably well. (C) 2016 Elsevier B.V. All rights reserved.
机译:渗流区流动问题通常由Richards方程解决。理查兹方程的求解通常具有挑战性,因为方程中的水力传导率和扩散率是水分的强烈非线性函数。提出了一种有限水含量方法,作为渗流,落块和渗流带对地下水位动态响应的渗流带流动问题的一种替代的一般求解方法,它是基于将含水量域离散化为多个单元,而不是传统的空间离散化。 。在这项研究中,我们开发了一种对原始的有限含水量方法(以下称为TO方法)的改进方法,该方法可以更好地模拟扩散效果,但保留TO方法的鲁棒性。该方法分别处理对流和扩散,并逐个二进制地考虑扩散。在离散化为水含量仓之后,我们将各个仓中的电导率和扩散率视为与水含量相关的常数,该常数是在与每个仓对应的给定水含量下评估的。对于每个仓,我们可以解析地求解流量方程,因为可以将水力传导率和扩散率视为常数。然后,我们为每个垃圾箱开发解决方案,以确定每个时间步的扩散水量。每个水箱在对流前沿之前的水量会在水含量水箱之间重新分配,以解决扩散效应。所开发解决方案的应用非常简单,仅涉及每个时间步的代数运算。该方法主要可以改善含水量,但与总渗透率相比,总渗透率和累积渗透率没有显着差异。尽管该方法分别处理对流和扩散,但是可以很好地解决对流和扩散的耦合效应。 (C)2016 Elsevier B.V.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号