Background clutter analysis of GPR signal for sedimentary deposit in Urban Infrastructure

Mezgeen A. Rasol, V. Pérez-Gracia, S. Santos-Assunçao, Franziska Schmidt
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Abstract

Soil site studies are crucial in the analysis of seismic hazard in populated areas. Enhancing the analysis of local seismic behaviour studies is based on the understanding of changes in ground materials of the shallow geology. Ground Penetrating Radar (GPR) is used in this study as a non-destructive geophysical method to understand the characterisation of changes in ground material in the sedimentary deposit due seasonal changes of water content in shallow geology of Sant Pau urban area in Barcelona city. The general objective of this research study is focused on enhancing the local seismic soil site analysis. This study employs GPR images to explore changes in the ground materials that can be associated to changes on the seismic soil response. Research procedure is based on real radar images acquired using 25 MHz centre frequency antenna along two different direction (parallel and perpendicular) of the coastline of the Mediterranean Sea of Barcelona city.Radar images are processed using common post-processing techniques, followed by more specific innovative post-processing methodology to support radar images as a complementary approach. A novel comparative study based on Fast Fourier Transform (FFT) is proposed to investigate the background clutter analysis of GPR signal considering background amplitude and centre of frequency to analyse water content in sedimentary deposit. This approach is developed to enhance the quality of GPR images to detect changes in ground materials by an innovative methodology of the radar data processing. The obtained results are mapped and compared to the information based on historical maps.
城市基础设施中沉积物GPR信号背景杂波分析
土壤场地研究是分析人口密集地区地震灾害的关键。加强局部地震行为研究的分析是建立在对浅层地质地层物质变化认识的基础上的。本文利用探地雷达(GPR)作为一种非破坏性的地球物理方法,了解了巴塞罗那市圣保罗城区浅层地质中由于含水量季节性变化而导致的沉积矿床中地面物质变化特征。本研究的总体目标是加强局部地震场地分析。本研究使用探地雷达图像来探索与地震土壤反应变化相关的地面物质变化。研究过程基于使用25 MHz中心频率天线沿着巴塞罗那市地中海海岸线的两个不同方向(平行和垂直)获取的真实雷达图像。雷达图像使用常见的后处理技术进行处理,随后采用更具体的创新后处理方法来支持雷达图像作为补充方法。提出了一种基于快速傅立叶变换(Fast Fourier Transform, FFT)的比较研究方法,对考虑背景幅值和频率中心的GPR信号进行背景杂波分析,以分析沉积物中的含水量。这种方法是通过一种创新的雷达数据处理方法来提高探地雷达图像的质量,以检测地面材料的变化。将获得的结果映射并与基于历史地图的信息进行比较。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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