The inversion GPR signal by compressing sensing and its application

Z. Zeng, Jing Li, Q. Lu, Kunru Wang, Xuan Feng, S. Xia, Fengshan Liu
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Abstract

GPR signal is essentially a delayed, scaled and distorted version of the transmitted pulse, determined by sparse parameters such as time delays and amplitudes. The time delay indicates the detected target's depth, and the amplitude is the impedance contrast at interface or reflection coefficient. A system for sampling GPR signal at an ultra-low sampling rate based on the Finite Rate of Innovation (FRI) and the estimation of time delays and amplitudes to detect GPR signal is presented in the paper. We build the algorithm and apply it to real GPR data from Northwest of China. The results demonstrate that the inverted impedance and time delay can be used to depict the sandstone and clay layer with high accuracy.
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利用压缩感知反演探地雷达信号及其应用
探地雷达信号本质上是发射脉冲的延迟、缩放和扭曲版本,由时间延迟和幅度等稀疏参数决定。时延表示被探测目标的深度,幅值表示界面处的阻抗对比或反射系数。提出了一种基于有限创新率(FRI)和时延、幅值估计的探地雷达信号超低采样系统,用于探地雷达信号检测。建立了该算法,并将其应用于中国西北地区的真实探地雷达数据。结果表明,利用反向阻抗和时间延迟可以较准确地描述砂岩和粘土层。
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