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Natural Stimuli Calibration with Fining Direction Regularization in an Integrated Hydrologic Model

机译:综合水文模型中带有精细化方向正则化的自然激励标定

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摘要

The interaction between surface water and groundwater during flood events is a complex process that has traditionally been described using simplified analytical solutions, or abstracted numerical models. To make the problem tractable, it is common to idealize the flood event, simplify river channel geometry, and ignore bank soil heterogeneity, often resulting in a model that only loosely represents the site, thus limiting its applicability to any specific river cross-section. In this study, we calibrate a site-specific fully-integrated surface and subsurface HydroGeoSphere model using flood events for a cross-section along the South River near Waynesboro, VA. The calibration approach presented in this study demonstrates the incorporation of fining direction regularization with a highly parameterized inversion driven by natural stimuli, to develop several realistic realizations of hydraulic conductivity fields that reflect the depositional history of the system. Specifically, we calibrate a model with 365 unique material zones to multiple flood events recorded in a dense well network while incorporating possible fining sequences consistent with the depositional history of the riverbank. Over 25,000 individual simulations were completed using calibration software and a cloud platform specifically designed for highly parallelized computing environments. The results of this study demonstrate the use of fining direction regularization during model calibration to generate multiple calibrated model realizations that account for the depositional environment of the system.
机译:洪水事件期间地表水与地下水之间的相互作用是一个复杂的过程,传统上已使用简化的分析解决方案或抽象的数值模型对其进行了描述。为了使问题更容易解决,通常是使洪水事件理想化,简化河道的几何形状,而忽略河岸土壤的异质性,通常会导致仅以松散的形式表示该地点的模型,从而将其适用于任何特定的河流横截面。在这项研究中,我们使用弗吉尼亚州韦恩斯伯勒附近的南河沿岸断面的洪水事件,校准了特定地点的完全整合的表面和地下HydroGeoSphere模型。本研究中提出的校准方法表明,精细化方向正则化与由自然刺激驱动的高度参数化反演相结合,可以开发出反映系统沉积历史的水力传导率场的若干实际实现。具体来说,我们针对稠密井网中记录的多个洪水事件校准了一个具有365个独特材料区的模型,同时纳入了与河岸沉积历史相吻合的可能的精细化序列。使用校准软件和专门为高度并行化计算环境设计的云平台,完成了超过25,000个单独的仿真。这项研究的结果表明,在模型校准过程中使用精化方向正则化可以生成考虑到系统沉积环境的多个校准模型实现。

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  • 来源
    《Ground water》 |2019年第1期|21-35|共15页
  • 作者单位

    Univ Waterloo, Dept Earth & Environm Sci, 200 Univ Ave W, Waterloo, ON N2L 3G1, Canada|Aquanty Inc, 564 Weber St N,Unit 2, Waterloo, ON N2L 5C6, Canada;

    DuPont Corp Remediat Grp, 974 Ctr Rd, Wilmington, DE 19805 USA;

    DuPont Corp Remediat Grp, 974 Ctr Rd, Wilmington, DE 19805 USA;

    AECOM, 625 West Ridge Pike,Suite E-100, Conshohocken, PA 19428 USA;

    AECOM, 625 West Ridge Pike,Suite E-100, Conshohocken, PA 19428 USA;

    Univ Waterloo, Dept Earth & Environm Sci, 200 Univ Ave W, Waterloo, ON N2L 3G1, Canada|Aquanty Inc, 564 Weber St N,Unit 2, Waterloo, ON N2L 5C6, Canada;

    Univ Waterloo, Dept Earth & Environm Sci, 200 Univ Ave W, Waterloo, ON N2L 3G1, Canada;

    Aquanty Inc, 564 Weber St N,Unit 2, Waterloo, ON N2L 5C6, Canada;

    Univ Waterloo, Dept Earth & Environm Sci, 200 Univ Ave W, Waterloo, ON N2L 3G1, Canada|Aquanty Inc, 564 Weber St N,Unit 2, Waterloo, ON N2L 5C6, Canada;

    Univ Waterloo, Dept Earth & Environm Sci, 200 Univ Ave W, Waterloo, ON N2L 3G1, Canada|Aquanty Inc, 564 Weber St N,Unit 2, Waterloo, ON N2L 5C6, Canada;

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