A. E. Rudenchik, L. Volkomirskaya, A. Reznikov, E. Bezrukova
{"title":"天线在两种均匀介质界面处产生的场表面波","authors":"A. E. Rudenchik, L. Volkomirskaya, A. Reznikov, E. Bezrukova","doi":"10.1109/UWBUSIS.2010.5609166","DOIUrl":null,"url":null,"abstract":"In circumstances where the dispersion of the permittivity can be neglected, the tangential component of the surface wave is expressed through the Laplace function of two complex arguments algebraically. This reduces the computation time of the surface wave at a given point to a few milliseconds, and to determine the current in the radiating antenna, as well as the dielectric constant of the underlying surface, for the time of the order of several seconds. Obtain estimates of the surface wave field for the most typical parameters of soils. These calculations can be used to select regularizators inverse GPR for quantitative calculations of the parameters of the soil and for the qualitative interpretation of GPR data.","PeriodicalId":124478,"journal":{"name":"2010 5th International Confernce on Ultrawideband and Ultrashort Impulse Signals","volume":"115 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2010-10-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Presentation of the field surface wave generated by an antenna at the interface of two homogeneous media\",\"authors\":\"A. E. Rudenchik, L. Volkomirskaya, A. Reznikov, E. Bezrukova\",\"doi\":\"10.1109/UWBUSIS.2010.5609166\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"In circumstances where the dispersion of the permittivity can be neglected, the tangential component of the surface wave is expressed through the Laplace function of two complex arguments algebraically. This reduces the computation time of the surface wave at a given point to a few milliseconds, and to determine the current in the radiating antenna, as well as the dielectric constant of the underlying surface, for the time of the order of several seconds. Obtain estimates of the surface wave field for the most typical parameters of soils. These calculations can be used to select regularizators inverse GPR for quantitative calculations of the parameters of the soil and for the qualitative interpretation of GPR data.\",\"PeriodicalId\":124478,\"journal\":{\"name\":\"2010 5th International Confernce on Ultrawideband and Ultrashort Impulse Signals\",\"volume\":\"115 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2010-10-25\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"2010 5th International Confernce on Ultrawideband and Ultrashort Impulse Signals\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1109/UWBUSIS.2010.5609166\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"2010 5th International Confernce on Ultrawideband and Ultrashort Impulse Signals","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/UWBUSIS.2010.5609166","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Presentation of the field surface wave generated by an antenna at the interface of two homogeneous media
In circumstances where the dispersion of the permittivity can be neglected, the tangential component of the surface wave is expressed through the Laplace function of two complex arguments algebraically. This reduces the computation time of the surface wave at a given point to a few milliseconds, and to determine the current in the radiating antenna, as well as the dielectric constant of the underlying surface, for the time of the order of several seconds. Obtain estimates of the surface wave field for the most typical parameters of soils. These calculations can be used to select regularizators inverse GPR for quantitative calculations of the parameters of the soil and for the qualitative interpretation of GPR data.