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Resolving precipitation induced water content profiles by inversion of dispersive GPR data: A numerical study

机译:通过分散GPR数据反演降水引起的水分含量分布:数值研究

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Surface-based ground-penetrating radar (GPR) measurements have significant potential for monitoring dynamic hydrologic processes at multiple scales in time and space. At early times during infiltration into a soil, the zone above the wetting front may act as a low-velocity waveguide that traps GPR waves, thereby causing dispersion and making interpretation of the data using standard methods difficult. In this work, we show that the dispersion is dependent upon the distribution of water within the waveguide, which is controlled by soil hydrologic properties. Simulations of infiltration were performed by varying the n-parameter of the Mualem-van Genuchten equation using HYDRUS-1D; the associated GPR data were simulated to evaluate the influence of dispersion. We observed a notable decrease in wave dispersion as the sharpness of the wetting front profile decreased. Given the sensitivity of the dispersion effect to the wetting front profile, we also evaluated whether the water content distribution can be determined through inversion of the dispersive GPR data. We found that a global grid search combined with the simplex algorithm was able to estimate the average water content when the wetted zone is divided into 2 layers. This approach was incapable, however, of representing the gradational nature of the water content distribution behind the wetting front. In contrast, the shuffled complex evolution algorithm was able to constrain a piece-wise linear function to closely match the shallow gradational water content profile. In both the layered and piece-wise linear case, the sensitivity of the dispersive data dropped sharply below the wetting front, which in this case was around 20 cm, i.e., twice the average wavelength, for a 900 MHz GPR survey. This study demonstrates that dispersive GPR data has significant potential for capturing the early-time dynamics of infiltration that cannot be obtained with standard GPR analysis approaches. (C) 2015 Elsevier B.V. All rights reserved.
机译:基于地面的探地雷达(GPR)测量在监视多个时空尺度的动态水文过程方面具有巨大潜力。在渗入土壤的早期,湿润锋线以上的区域可能会充当捕获GPR波的低速波导,从而导致分散并使得使用标准方法解释数据变得困难。在这项工作中,我们表明分散度取决于水在波导中的分布,而水的分布受土壤水文特性控制。通过使用HYDRUS-1D改变Mualem-van Genuchten方程的n参数来进行渗透模拟。模拟相关的GPR数据以评估色散的影响。我们观察到,随着湿润锋线轮廓的清晰度降低,波的色散显着降低。给定分散效应对润湿前轮廓的敏感性,我们还评估了是否可以通过分散GPR数据的反演来确定水含量分布。我们发现,将湿润区域分为2层时,结合单纯形算法的全局网格搜索能够估计平均含水量。然而,这种方法不能代表润湿前沿后面的水含量分布的等级性质。相反,经过改组的复杂演化算法能够约束分段线性函数以紧密匹配浅层次水分含量曲线。在分层和分段线性情况下,色散数据的灵敏度都急剧下降到湿润前沿以下,在这种情况下,对于900 MHz GPR测量,其约为20 cm,即平均波长的两倍。这项研究表明,分散的GPR数据具有捕获渗透的早期动态的巨大潜力,而标准GPR分析方法无法获得这种动态。 (C)2015 Elsevier B.V.保留所有权利。

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