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Full-Wave Calibration of Time- and Frequency-Domain Ground-Penetrating Radar in Far-Field Conditions

机译:远场条件下时域和频域探地雷达的全波校准

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Full-wave modeling of ground-penetrating radar (GPR) data using Green's functions for wave propagation in planar layered media and antenna characteristic global reflection and transmission functions for describing far-field antenna effects, including antenna-medium interactions, has shown a great potential for nondestructive characterization of soils and materials. The accuracy of the retrieved parameters in the GPR data inversion depends on the accuracy of the GPR external calibration. In this research we studied the stability and the repeatability of two different GPR systems, namely, frequency- and time-domain systems. A combination of a vector network analyzer and 800–5200 MHz horn antenna was used as a frequency-domain GPR (FD-GPR) whereas a GSSI GPR system using a 900 MHz bowtie antenna was used as a time-domain GPR (TD-GPR). Both GPR systems including their antennas were calibrated several times using measurements with the antennas at different heights over a perfect electric conductor (PEC) in the laboratory as well as over a water layer. In addition, measurements were performed over a thin water layer and a relatively thick sandy soil layer as validating medium. The results showed that the FD-GPR is relatively stable while the TD-GPR presents a significant drift which can be accounted for using corrections based on the air direct-coupling waves (free-space measurements). Water- and PEC-based calibrations provided very similar results for the GPR calibration functions. Inversions for the water layer and the sandy soil layer provided reliable results and showed a high degree of the repeatability for both radar systems. The error on the calibration based on inaccurate antenna heights over PEC showed the significant errors on the inversion results for the directive antenna (horn antenna) but less error for the bowtie antenna. This analysis demonstrated the general validity of the proposed far-field radar modeling approach, not only with respect to fre- uency and time domain radars but as well with respect to the calibrating medium.
机译:使用格林在平面分层介质中传播的函数以及用于描述远场天线效应(包括天线与介质之间的相互作用)的天线特性全局反射和传输函数,利用格林函数对探地雷达(GPR)数据进行全波建模已显示出巨大的潜力用于土壤和材料的非破坏性表征。 GPR数据反演中检索到的参数的准确性取决于GPR外部校准的准确性。在这项研究中,我们研究了两种不同的GPR系统(即频域和时域系统)的稳定性和可重复性。矢量网络分析仪和800-5200 MHz喇叭天线的组合被用作频域GPR(FD-GPR),而使用900 MHz领结天线的GSSI GPR系统被用作时域GPR(TD-GPR )。两种GPR系统及其天线均使用在实验室中的完美电导体(PEC)和水层上不同高度的天线进行了多次校准。另外,在薄水层和相对厚的沙土层作为验证介质上进行了测量。结果表明,FD-GPR相对稳定,而TD-GPR则存在明显的漂移,这可以通过使用基于空气直接耦合波的校正(自由空间测量)来解释。基于水和PEC的校准为GPR校准功能提供了非常相似的结果。水层和沙土层的反演提供了可靠的结果,并显示了两种雷达系统的高度可重复性。基于PEC上不正确的天线高度的校准误差显示,定向天线(喇叭天线)的反演结果存在明显误差,而领结天线的误差较小。这项分析证明了拟议的远场雷达建模方法的普遍有效性,不仅对于频域和时域雷达,而且对于校准介质。

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