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A novel method for wideband pulsed electromagnetic wave propagation characteristic analysis in layered medium

机译:层状介质中宽带脉冲电磁波传播特性分析的新方法

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Ultra wideband pulsed ground penetrating radar (GPR) detects buried object or underground medium characteristic by emitting and receiving pulsed electromagnetic waves. Establishing underground medium equivalent model and studying the electromagnetic wave propagation characteristic in media are very important to GPR data processing and underground object detecting. This paper introduces the actual pulse electromagnetic wave emitted by GPR as the wavelet, and presents a pulsed electromagnetic wave propagation characteristic analyzing method in layered medium. First, a underground equivalent layered medium model is established. Then the pulse electromagnetic wave emitted by GPR is decomposed into frequency components by Fourier-transform. For each frequency component, the reflected waves and the transmission waves from each interface of underground media are calculated respectively. Finally all of the reflection waves are transformed by Fourier-inverse-transform and recombined into the full GPR echo in time-domain. By using the GPR actual emitting wavelet to implement the propagation characteristic analyzing, we can precisely restore the echoes received by GPR. This method can also consider the electromagnetic wave dispersion and multiple reflections by frequency-domain analyzing approach. The time-domain echoes combining can effectively solve the electromagnetic wave coherence problem. Hence, the method mentioned in this paper have great advantages in studying GPR pulsed electromagnetic wave propagation characteristic in underground layered medium.
机译:超宽带脉冲地面穿透雷达(GPR)通过发射和接收脉冲电磁波来检测地下物体或地下介质的特征。建立地下介质等效模型,研究电磁波在介质中的传播特性,对GPR数据处理和地下物体的探测具有十分重要的意义。本文介绍了由GPR发出的实际脉冲电磁波作为小波,并提出了在分层介质中的脉冲电磁波传播特性分析方法。首先,建立地下等效层状介质模型。然后,通过傅立叶变换将GPR发射的脉冲电磁波分解为频率分量。对于每个频率分量,分别计算地下介质每个界面的反射波和透射波。最后,所有反射波都通过傅立叶逆变换进行变换,并在时域中重组为完整的GPR回波。通过使用GPR实际发射小波进行传播特性分析,可以精确地恢复GPR接收到的回波。该方法还可以通过频域分析方法考虑电磁波的色散和多次反射。时域回波组合可以有效解决电磁波相干问题。因此,本文研究的方法在研究GPR脉冲电磁波在地下层状介质中的传播特性方面具有很大的优势。

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