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Three-Dimensional Modeling of Multiple Automated Equilibrium Tension Lysimeters to Measure Vadose Zone Fluxes

机译:多个自动化平衡张力测渗仪的三维建模,以测量渗流区通量

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摘要

Using numerical simulation, we analyzed a novel vadose zone sampling system installed in a vadose zone of volcanic origin in the Lake Taupo catchment, New Zealand. The system comprises 15 Automated Equilibrium Tension Lysimeters (AETLs) installed at five depths. The vacuum in each individual lysimeter is controlled to match the pressure head measured at a reference location in the undisturbed vadose zone. The three-dimensional numerical flow model HYDRUS-3D was used to investigate the impact of flow impediment and shadow effects caused by the installation and operation of the AETLs. The analysis was conducted for steady-state conditions in homogeneous sand, loam, and ignimbrite, as well as in the layered materials present at the experimental site. The hydraulic properties of the different layers were estimated using one-dimensional inverse modeling and global optimization techniques. Horizontal, vertical, and radial two-dimensional sections through the model domain were analyzed for divergence from steady-state conditions. The results suggest that the sampling efficiency of the AETLs is relatively large and the errors caused by the setup and operation of the vadose zone sampler are relatively small. We further utilized a transient HYDRUS-3D model of the vadose zone sampler to simulate transient tensiometric pressure heads using field data. The simulations for the various depths compared favorably with both the measured pressure heads and the simulations of the one-dimensional model. In contrast, the simulated cumulative water fluxes during the evaluation period were larger than the measurements of the corresponding AETLs. These findings highlight the importance of an adequate model structure and information content of the calibration data for the accurate prediction of vadose zone water fluxes.
机译:通过数值模拟,我们分析了安装在新西兰陶波湖流域火山成因渗流带中的新型渗流带采样系统。该系统包括在五个深度安装的15台自动平衡张力测速仪(AETL)。控制每个溶渗仪中的真空度,以匹配在未扰动渗流区的参考位置测得的压头。三维数值流模型HYDRUS-3D用于研究由AETL的安装和操作引起的流动障碍和阴影效应的影响。分析是针对均质砂,壤土和火成岩以及实验现场存在的层状材料中的稳态条件进行的。使用一维逆向建模和全局优化技术估算不同层的水力特性。分析了穿过模型域的水平,垂直和径向二维截面与稳态条件的差异。结果表明,AETL的采样效率相对较高,而渗流区采样器的设置和操作引起的误差相对较小。我们进一步利用了渗流区采样器的瞬态HYDRUS-3D模型来使用现场数据模拟瞬态张力测压头。与所测得的压头和一维模型的仿真相比,各种深度的仿真均具有优势。相反,在评估期间模拟的累积水通量大于相应AETL的测量值。这些发现凸显了正确模型结构和校准数据信息内容对渗流带水通量准确预测的重要性。

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  • 来源
    《Vadose Zone Journal》 |2009年第4期|p.1051-1063|共13页
  • 作者单位

    a Lincoln Environmental Research, Lincoln Ventures Ltd., Ruakura Research Centre, Hamilton 3240, New Zealandb Institute for Hydrology and Meteorology, Dresden Univ. of Technology, Würzburger Str. 46, 01187 Dresden, Germanyc Soil and Groundwater Lab., Tiergartenstr. 48, 01219 Dresden, Germanyd Dep. of Environmental Sciences, Univ. of California, Riverside, CAe Aqualinc Research Ltd, P.O. Box 14-041, Enderley, Hamilton, New Zealand;

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