首页|探地雷达早期信号探测深度数值研究与应用

探地雷达早期信号探测深度数值研究与应用

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近地工作的地面耦合天线产生的雷达早期信号具有到达早、能量强、波形稳定、相位清晰等特点,其持续时间约为一个信号周期,对同时段内近地表介质的反射、绕射、散射等信号构成强烈干扰.人工构筑物通常设计为层厚固定的层状结构.通过在层状介质模型中设置一系列不同埋深的垂向裂缝,数值研究了不同主频天线雷达早期信号的探测深度,及其探测深度范围内介质介电常数与雷达早期信号振幅强度之间的关系.研究结果表明:与多偏移距测量方法相比,固定偏移距剖面法能更方便、更直观的测量雷达早期信号的探测深度;雷达早期信号的探测深度与天线的主频成反比关系,即天线的主频越低,其雷达早期信号的探测深度越深;此外,雷达早期信号的振幅强度与其探测深度范围内介质的介电常数密切相关,介质的介电常数越大,其对应的雷达早期信号振幅强度越小,与实测雷达数据相吻合.本研究为利用探地雷达早期信号的振幅强度,判断其探测深度范围内介质的介电常数异常变化提供了重要依据.
Numerical study and application for detection depth of gpr early-time signal
The Ground Penetrating Radar(GPR)Early-Time Signals(ETS)generated by ground-coupled antennas operating in close proximity to the ground exhibit characteristics such as early arrival,strong energy,stable waveform,and clear phase.Their duration is approximately one signal cycle,causing significant interference with signals such as reflections,diffractions,and scatterings from near-surface media occurring within the same time frame.Artificially constructed structures are typically designed as layered structures with fixed layer thicknesses.To this end,a series of vertical cracks with different burial depths are set up in a layered medium model to numerically investigate the detection depth of GPR ETS from antennas with different operating frequencies,as well as the relationship between the dielectric constant of the medium within the detection depth and the amplitude intensity of the GPR ETS.The research results indicate that,compared to multi-offset measurement methods,the fixed-offset profiling method provides a more convenient and intuitive approach to measuring the detection depth of GPR ETS.The detection depth of GPR ETS is inversely proportional to the operating frequency of the antenna,meaning that a lower operating frequency results in a deeper detection depth.Furthermore,the amplitude intensity of GPR ETS is closely related to the dielectric constant of the medium within the detection depth;the higher the dielectric constant,the lower the corresponding amplitude intensity of the GPR ETS,which aligns with the verification results obtained from actual radar data.This study provides an important basis for utilizing the amplitude intensity of GPR ETS to judge abnormal changes in the dielectric constant of media within the detection depth.

Ground Penetrating Radar(GPR)Early-Time Signal(ETS)Amplitude intensityEffective detection depthNumerical simulation

范永亮、郭士礼、梁栋、代公正、于明羽

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河南高速公路试验检测有限公司,郑州 450121

河南工程学院环境与生物工程学院,郑州 451191

贵州黔通工程技术有限公司,贵阳 550014

探地雷达 早期信号 振幅强度 探测深度 数值模拟

2024

地球物理学进展
中国科学院地质与地球物理研究所 中国地球物理学会

地球物理学进展

CSTPCD北大核心
影响因子:1.761
ISSN:1004-2903
年,卷(期):2024.39(5)