{"title":"On GPR signal polarity reversal","authors":"D. Campo","doi":"10.1109/iwagpr50767.2021.9843176","DOIUrl":null,"url":null,"abstract":"Ground Penetrating Radar (GPR) signal amplitude is the main signal attribute used for GPR data interpretation as, by observing its variations, it is possible to identify buried targets or material changes. 180-degree phase shifts, commonly referred to as polarity reversal, are also used to infer the material nature (e.g., voids). This paper presents an analysis of the polarity reversal occurrence through the definition of the reflection and transmission coefficient for perpendicular and parallel polarization of the electric field, showing different scenarios with the help of Finite Difference Time Domain (FDTD) numerical modelling in ideal lossless conditions as well as lossy/dispersive environments. Real radargrams are also presented to corroborate the forward modelling findings.","PeriodicalId":170169,"journal":{"name":"2021 11th International Workshop on Advanced Ground Penetrating Radar (IWAGPR)","volume":"92 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2021-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"2021 11th International Workshop on Advanced Ground Penetrating Radar (IWAGPR)","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/iwagpr50767.2021.9843176","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1

Abstract

Ground Penetrating Radar (GPR) signal amplitude is the main signal attribute used for GPR data interpretation as, by observing its variations, it is possible to identify buried targets or material changes. 180-degree phase shifts, commonly referred to as polarity reversal, are also used to infer the material nature (e.g., voids). This paper presents an analysis of the polarity reversal occurrence through the definition of the reflection and transmission coefficient for perpendicular and parallel polarization of the electric field, showing different scenarios with the help of Finite Difference Time Domain (FDTD) numerical modelling in ideal lossless conditions as well as lossy/dispersive environments. Real radargrams are also presented to corroborate the forward modelling findings.
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关于探地雷达信号的极性反转
探地雷达(GPR)信号振幅是用于GPR数据解释的主要信号属性,因为通过观察其变化,可以识别埋地目标或物质变化。180度相移,通常称为极性反转,也用于推断材料的性质(例如,空洞)。本文通过定义电场垂直和平行极化的反射和透射系数,分析了极性反转的发生,并借助时域有限差分(FDTD)数值模拟,展示了理想无损条件下和有损/色散环境下的不同情况。真实的雷达图也被提出,以证实正演模拟的结果。
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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