{"title":"超宽带探地雷达管探测的Kirchhoff迁移法","authors":"V. Plakhtii, O. Dumin, O. Pryshchenko","doi":"10.1109/DIPED53165.2021.9552330","DOIUrl":null,"url":null,"abstract":"The problem of subsurface object depth determination is solved by the ultrawideband ground penetrating radar simulation and Kirchhoff migration method. The electromagnetic problem is calculated by the FDTD method. The source of electromagnetic field is a plane electromagnetic wave of nanosecond time duration with normal incidence to the ground plane. A-scans are obtained by measuring the reflected electromagnetic field at the certain height above the air-ground interface. The resulting scattered fields in the form of B-scans are processed by Kirchhoff migration method in order to determine the exact depth of the hidden object.","PeriodicalId":150897,"journal":{"name":"2021 IEEE 26th International Seminar/Workshop on Direct and Inverse Problems of Electromagnetic and Acoustic Wave Theory (DIPED)","volume":"1 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2021-09-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"Kirchhoff Migration Method for Tube Detection with UWB GPR\",\"authors\":\"V. Plakhtii, O. Dumin, O. Pryshchenko\",\"doi\":\"10.1109/DIPED53165.2021.9552330\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The problem of subsurface object depth determination is solved by the ultrawideband ground penetrating radar simulation and Kirchhoff migration method. The electromagnetic problem is calculated by the FDTD method. The source of electromagnetic field is a plane electromagnetic wave of nanosecond time duration with normal incidence to the ground plane. A-scans are obtained by measuring the reflected electromagnetic field at the certain height above the air-ground interface. The resulting scattered fields in the form of B-scans are processed by Kirchhoff migration method in order to determine the exact depth of the hidden object.\",\"PeriodicalId\":150897,\"journal\":{\"name\":\"2021 IEEE 26th International Seminar/Workshop on Direct and Inverse Problems of Electromagnetic and Acoustic Wave Theory (DIPED)\",\"volume\":\"1 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-09-08\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"2021 IEEE 26th International Seminar/Workshop on Direct and Inverse Problems of Electromagnetic and Acoustic Wave Theory (DIPED)\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1109/DIPED53165.2021.9552330\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"2021 IEEE 26th International Seminar/Workshop on Direct and Inverse Problems of Electromagnetic and Acoustic Wave Theory (DIPED)","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/DIPED53165.2021.9552330","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Kirchhoff Migration Method for Tube Detection with UWB GPR
The problem of subsurface object depth determination is solved by the ultrawideband ground penetrating radar simulation and Kirchhoff migration method. The electromagnetic problem is calculated by the FDTD method. The source of electromagnetic field is a plane electromagnetic wave of nanosecond time duration with normal incidence to the ground plane. A-scans are obtained by measuring the reflected electromagnetic field at the certain height above the air-ground interface. The resulting scattered fields in the form of B-scans are processed by Kirchhoff migration method in order to determine the exact depth of the hidden object.