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Advanced Ground Penetrating Radar Signal Processing Techniques

机译:先进的探地雷达信号处理技术

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摘要

Ground penetrating radar (GPR) is a non-destructive geophysical method that uses electromagnetic waves to image the subsurface. A typical GPR system has three main components: transmitter and receiver, directly connected to the transmitting and receiving antennas, and a control unit. Electromagnetic pulses are transmitted into the subsurface and the earth response is recorded. The GPR method is characterized by the rapidly decaying amplitude of the electromagnetic waves, together with the loss of the relevant higher frequency harmonics. Thus, GPR data are highly non-stationary and processing is inherently a challenge.
机译:探地雷达(GPR)是一种无损地球物理方法,使用电磁波对地下进行成像。典型的GPR系统具有三个主要组件:直接连接到发射和接收天线的发射器和接收器,以及控制单元。电磁脉冲被传输到地下,并记录地面响应。 GPR方法的特点是电磁波的振幅迅速衰减,同时损失了相关的高频谐波。因此,GPR数据非常不稳定,处理本身就是一个挑战。

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  • 来源
    《Signal processing》 |2017年第3期|197-200|共4页
  • 作者单位

    Applied Geophysics Lab School of Mineral Resources Engineering Technical University of Crete Polytechnioupolis, Kounoupidiana, Chania, Crete, Greece;

    SP4TE - Signal Pro cessing for Telecommunications and Economics Laboratory, University of ROMA TRE, Via Vito Volterra 62, 00146 Rome, Italy;

    Institut de Physique du Globe de Strasbourg Ecole et Observatoire des Sciences de la Terre University of Strasbourg, 5 rue Rene Descartes, 67084 Strasbourg Cedex, France;

    Department of Geophysics, National and Kapodistrian University of Athens Panepistimiopoli, Zografou 15784, Greece;

    Weeks Chair of Environmental Geology Department of Earth & Environmental Science Temple University, Philadelphia, PA 19122, USA;

    Geophysical Research Zipser, Strasse I, 76227 Karlsruhe, Germany;

    Applied and Environmental Geophysics Group School of Physical and Geographical Sciences Keele University Staffordshire, UK;

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