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MAPPING SURFACE SOIL WATER CONTENT WITH THE GROUND WAVE OF GROUND-PENETRATING RADAR

机译:用探地雷达的地波映射表层土壤水含量

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We investigated the accuracy of surface soil water content measurements with the ground wave of GPR. We examined the influence of SWC mapping equipment near the GPR and tested the significance of reported time differences in air and ground wave arrival time at zero antenna offset (t_0). The influence of the equipment on the radar signal was tested by introducing the sleds, odometer and vehicle to pull equipment stepwise. The sleds caused a decrease in the amplitude of the ground wave and all the equipment caused disturbances in the air wave. However, the data quality remained sufficient to pick arrival times automatically. The importance of t_0 was assessed with 20 WARR measurements and a sensitivity analysis based on GPR simulations. We observed a mean t_0 of 0.5231 ns that could not be explained from the GPR simulations. There also was a large variation in t_0, but that could be explained by considering picking error, positional error and soil water content heterogeneity in the sensitivity analysis. We conclude that a t_0 correction in the calculation of soil water content would improve measurements with GPR, but it should be noted that the large variation in to makes it difficult to accurately estimate mean t_0.
机译:我们研究了地表雷达声波测量地表土壤含水量的准确性。我们检查了GPR附近SWC制图设备的影响,并测试了在零天线偏移(t_0)时空中和地面波到达时间所报告的时差的重要性。通过引入雪橇,里程表和车辆逐步拉动设备,测试了设备对雷达信号的影响。雪橇引起了地波振幅的减小,所有设备都引起了空气波的干扰。但是,数据质量仍然足以自动选择到达时间。通过20次WARR测量和基于GPR模拟的灵敏度分析评估了t_0的重要性。我们观察到的平均t_0为0.5231 ns,这无法从GPR仿真中得到解释。 t_0的变化也很大,但可以通过在灵敏度分析中考虑采摘误差,位置误差和土壤水分异质性来解释。我们得出的结论是,对土壤含水量的计算中的t_0校正将改善GPR的测量结果,但应注意,的大变化使得难以准确估计均值t_0。

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