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An Integrative Approach for Monitoring Water Movement in the Vadose Zone

机译:渗流带水流监测的综合方法

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摘要

Electrical resistivity tomography (ERT), during the past few years, has emerged as a potentially cost-effective, noninvasive tool for imaging changes of moisture content in the vadose zone. The accuracy of ERT surveys, however, has been the subject of debate because of its nonunique inverse solution and spatial variability in the constitutive relation between resistivity and moisture content. In this paper, an integrative inverse approach for ERT, based on a stochastic information fusion concept of Yeh and imnek, was developed to derive the best unbiased estimate of the moisture content distribution. Unlike classical ERT inversion approaches, this new approach assimilates prior information about the geological and moisture content structures in a given geological medium, as well as sparse point measurements of the moisture content, electrical resistivity, and electric potential. Using these types of data and considering the spatial variability of the resistivity–moisture content relation, the new approach directly estimates three-dimensional moisture content distributions instead of simply changes in moisture content in the vadose zone. Numerical experiments were conducted to investigate the effect of uncertainties in the prior information on the estimate. The effects of spatial variability in the constitutive relation were then examined on the interpretation of the change in moisture content, based on the change in electrical resistivity from the ERT survey. Finally, the ability of the integrative approach was tested by directly estimating moisture distributions in three-dimensional, heterogeneous vadose zones. Results show that the integrative approach can produce accurate estimates of the moisture content distributions and that incorporating some measurements of the moisture content is essential to improve the estimate.
机译:在过去的 几年中,电阻层析成像(ERT)已经成为一种具有成本效益的,非侵入性的 工具,用于对渗流带中水分含量的变化进行成像。 sup> 然而,ERT测量的准确性一直是 争论的主题,因为其非唯一的反解和电阻率之间本构关系的空间 可变性< sup> 和水分含量。在本文中,基于Yeh和imnek的随机信息融合概念 ,开发了一种用于ERT的集成逆 方法,以得出最佳的无偏 估计水分含量分布。与经典的 ERT反演方法不同,此新方法吸收了给定地质介质中稀疏的地质和水分含量结构的先前信息。水分,电阻率和电势的点测量 。使用这些类型的数据并考虑电阻率与水分含量关系的空间 可变性, 新方法直接估算三维水分 含量分布而不是简单地改变渗流区水分 的含量。 进行了数值实验,以研究先验信息 中的不确定性对估计的影响。然后根据电阻率的变化 检查了本构关系中空间变异性对水分含量变化 的解释。来自ERT调查。最后,通过直接估算三维非均质渗流区中的水分分布 来测试综合 方法的能力。结果表明 该综合方法可以得出准确的含水量分布估计值 ,合并 一些水分含量测量值对于改善< sup> 估计。

著录项

  • 来源
    《Vadose Zone Journal》 |2004年第2期|681-692|共12页
  • 作者

    Shuyun Liu; Tian-Chyi J. Yeh;

  • 作者单位

    Burgess & Niple, 5025 E. Washington St., Phoenix, AZ 85034;

    Dep. of Hydrology and Water Resour., John W. Harshbarger Bldg., The Univ. of Arizona, Tucson, AZ 85721;

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  • 正文语种 eng
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