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Testing a transmission line model for homogeneous subsurface media using ground penetrating radar

机译:使用地面渗透雷达测试同质地下介质的传输线模型

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Ground Penetrating Radars (GPR) process electromagnetic reflections from subsurface interfaces to characterize the subsurface and detect buried targets. Our objective is to test an inversion algorithm that calculates the intrinsic impedance of subsurface media when the signal transmitted is modeled as the first or second derivative of a large bandwidth Gaussian pulse. For this purpose we model the subsurface as a transmission line with multiple segments, each having different propagating velocities and characteristic impedances. We simulate the propagation and reflection of the pulse from multilayered lossless and lossy media, and process the received signal with a rectifier and filter subsystem to estimate the impulse response. We then run the impulse response through the inversion algorithm in order to calculate the relative permittivity of each subsurface layer. We show that the algorithm is able to detect targets using the primary reflections, even though secondary reflections are sometimes required to maintain inversion stability. We also demonstrate the importance of compensating for geometric spreading losses and conductivity losses to accurately characterize each substrate layer and target. Such compensation is not trivial in experimental data where electronic range delays can be arbitrary, transmitted pulses often deviate from the theoretical models, and limited resolution can cause ambiguity in the range of the targets.
机译:地面穿透雷达(GPR)处理来自地下界面的电磁反射,以表征地下并检测掩埋目标。我们的目的是测试一种反演算法,当被发送的信号被建模为大带宽高斯脉冲的第一或第二导数时,计算地下介质的内部阻抗。为此目的,我们将地下模拟了具有多个段的传输线,每个传输线具有不同的传播速度和特征阻抗。我们模拟了来自多层损耗和有损介质的脉冲的传播和反射,并使用整流器和过滤器子系统处理接收信号来估计脉冲响应。然后,我们通过反转算法运行脉冲响应,以便计算每个地下层的相对介电常数。我们表明该算法能够检测使用主要反射的目标,即使有时需要进行二次反射以维持反转稳定性。我们还证明了补偿几何扩展损耗和电导率损耗的重要性,以准确地表征每个基底层和靶标。这种补偿在实验数据中不是琐碎的,其中电子范围延迟可以是任意的,透射脉冲通常偏离理论模型,并且有限的分辨率可能导致目标范围内的模糊性。

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