探地雷达数据稀疏表示在岩石裂隙特征提取研究中的应用

Xinjian Tang, W.Z. Ren, T. Sun, Renjun Hou
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引用次数: 0

摘要

由于地下环境复杂,探地雷达探测的回波信号中往往含有大量的杂波,包括直接耦合波、随机噪声和倍数。这些杂波的存在淹没了探地雷达探测到的岩石结构特征信号,因此对它们的抑制往往是岩石特征提取的必要步骤。从探地雷达测量数据信号中提取岩体结构特征,信号的稀疏表示(SR)是一种非常有用的方法,可以利用过完备字典中少量的基本信号。在对探地雷达信号数据进行处理提取岩石结构和裂隙特征时,研究了采用单一曲波变换或匹配追踪(MP)进行直接耦合波杂波抑制和特征提取的方法,并分析了其局限性。通过对探地雷达信号进行稀疏分解,可以获得较好的建模效果。模拟和实测数据的实验结果表明,所提出的稀疏分解方法能够有效地表示信号,并为地质解释提供了判别特征。
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Application of sparse representation of ground penetrating radar data in a study of extracting rock fracture signature
Due to complex subsurface situation, echo signals surveyed with Ground Penetration Radar (GPR) often contain a lot of clutters, including direct-coupling wave, random noises and multiples. Existence of these clutters submerges measured feature signals of rock structures with GPR, so suppression of them is often essential conduct for rock feature extraction. For extracting rockmass structure features from surveyed GPR data signals, sparse representation (SR) of the signals is an invaluable scheme with a small number of elementary signals from over-complete dictionary. In processing GPR signal data for extraction of rock structure and fracture features, this paper investigates sole Curvelet transform or matching pursuit (MP) for directcoupling wave and clutter suppression and feature extraction, and analyzes their limitations. By modeling ground penetrating radar signals with sparse decomposition, the method can achieve better results. Experimental results with simulation as well as real field data show that the proposed sparse decomposition achieves efficient signal representation and yields discriminative features for geological interpretation.
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