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An examination of direct ground wave soil moisture monitoring over an annual cycle of soil conditions

机译:在一年一度的土壤条件下检查直接地波土壤湿度的方法

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摘要

Direct ground wave (DGW) measurements obtained with ground-penetrating radar have been used in a number of previous studies to estimate volumetric water content in the shallow soil zone; however, these studies have generally involved controlled field experiments or measurements collected across limited natural ranges of soil moisture conditions. To further investigate the capacity of this method, we have undertaken an extensive field study using multifrequency (i.e., 225, 450, and 900 MHz) DGW measurements to monitor a complete annual cycle of soil water content variations typical of midlatitude climates at three sites with different soil textures. The use of common-midpoint surveys allowed us to understand the nature and evolution of the near-surface electromagnetic wavefields and their impact on DGW moisture predictions. We present the novel characterization of a wide-range of seasonal moisture dynamics including soil freezing and thawing process using multifrequency DGW measurements for a range of soil textures. These data showed significant temporal variations in both the near-surface wavefield and multifrequency DGW velocities corresponding to both seasonal and shorter-term variations in soil conditions. Although all of the measurement sites displayed similar temporal responses, the rate and magnitude of these velocity variations corresponded to varying soil water contents, which were controlled by the soil textural properties. Although there were no observed systematic differences in DGW velocities due to frequency dispersion for the 225-900 MHz range, the DGW measurements obtained using higher-frequency antennas was less impacted by near-surface wavefield interference due to their shorter signal pulse duration. DGW velocity measurements combined with an appropriate dielectric mixing formula provided quantitative predictions of soil water content that accurately replicated the soil sample data over the annual cycle of moisture conditions.
机译:以前的许多研究已使用通过探地雷达获得的直接地波(DGW)测量来估算浅土带中的体积水含量。但是,这些研究通常涉及在有限的自然湿度范围内进行的田间控制实验或测量。为了进一步研究这种方法的能力,我们进行了广泛的现场研究,使用多频(即225、450和900 MHz)DGW测量来监测三个地点的中纬度气候典型的土壤水含量变化的完整年度周期,不同的土壤质地。使用共中点测量,我们可以了解近地表电磁波场的性质和演化及其对DGW湿度预测的影响。我们介绍了多种季节性水分动力学的新颖特征,包括使用多频DGW测量得出的一系列土壤质地的土壤冻结和解冻过程。这些数据表明,近地表波场和多频DGW速度均存在明显的时间变化,这与土壤条件的季节性变化和短期变化都相对应。尽管所有测量点都显示出相似的时间响应,但这些速度变化的速率和幅度对应于变化的土壤含水量,而土壤含水量则受土壤质地的控制。尽管没有观察到由于225-900 MHz范围内的频率分散而导致DGW速度出现系统性差异,但是使用高频天线获得的DGW测量值由于其较短的信号脉冲持续时间而受到近地表波场干扰的影响较小。 DGW速度测量值与适当的介电混合公式相结合,提供了土壤含水量的定量预测,可以准确地复制年度湿度条件下的土壤样品数据。

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  • 来源
    《Water resources research》 |2010年第11期|p.W11533.1-W11533.16|共16页
  • 作者单位

    Department of Earth andEnvironmental Sciences, University of Waterloo, Waterloo, ON N2L3G1, Canada;

    Department of Earth andEnvironmental Sciences, University of Waterloo, Waterloo, ON N2L3G1, Canada;

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