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Research on application of ground penetrating radar array method based on plane beam signal in different geological models
The traditional common-offset ground penetrating radar method measures point by point along the survey line with a single transmitter and a single receiver. Due to the influence of the antenna radiation power and the low-pass filtering function of the earth medium, an intense amplitude gain cannot b...
Autores principales: | , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Springer International Publishing
2021
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8514008/ http://dx.doi.org/10.1007/s11600-021-00684-5 |
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author | Cui, Fan Chen, Yi Zhang, Yongqi Du, Yunfei |
author_facet | Cui, Fan Chen, Yi Zhang, Yongqi Du, Yunfei |
author_sort | Cui, Fan |
collection | PubMed |
description | The traditional common-offset ground penetrating radar method measures point by point along the survey line with a single transmitter and a single receiver. Due to the influence of the antenna radiation power and the low-pass filtering function of the earth medium, an intense amplitude gain cannot be obtained when the signal is intercepted. This article addresses a plane beam signal ground penetrating radar array observation method based on high radiation power gain. The transmitting antenna array simultaneously excites the pulse signal with the same centre frequency. All the transmitted signals interfere with each other at the near surface to form a plane beam signal, and the electromagnetic energy is superimposed mutually to increase the radiation power. We applied the plane beam signal ground penetrating radar array method to different geological models constructed by the finite difference time-domain (FDTD) algorithm for numerical simulation in this research. Since there are various offsets in the array ground penetrating radar observation method, we introduce a composite frequency shift-perfect matching layer (CFS-PML) based on the recursive convolution method as the absorbing boundary condition. It eliminates the problem of secondary reflection caused by the angle variation of the incident wave. The research result shows that the plane beam signal illuminates the target uniformly in space, can eliminate the discontinuity in profile data caused by the directivity of the antenna, improve the stability and quality of the echo signal, and enrich the target response parameters. |
format | Online Article Text |
id | pubmed-8514008 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2021 |
publisher | Springer International Publishing |
record_format | MEDLINE/PubMed |
spelling | pubmed-85140082021-10-14 Research on application of ground penetrating radar array method based on plane beam signal in different geological models Cui, Fan Chen, Yi Zhang, Yongqi Du, Yunfei Acta Geophys. Research Article - Applied Geophysics The traditional common-offset ground penetrating radar method measures point by point along the survey line with a single transmitter and a single receiver. Due to the influence of the antenna radiation power and the low-pass filtering function of the earth medium, an intense amplitude gain cannot be obtained when the signal is intercepted. This article addresses a plane beam signal ground penetrating radar array observation method based on high radiation power gain. The transmitting antenna array simultaneously excites the pulse signal with the same centre frequency. All the transmitted signals interfere with each other at the near surface to form a plane beam signal, and the electromagnetic energy is superimposed mutually to increase the radiation power. We applied the plane beam signal ground penetrating radar array method to different geological models constructed by the finite difference time-domain (FDTD) algorithm for numerical simulation in this research. Since there are various offsets in the array ground penetrating radar observation method, we introduce a composite frequency shift-perfect matching layer (CFS-PML) based on the recursive convolution method as the absorbing boundary condition. It eliminates the problem of secondary reflection caused by the angle variation of the incident wave. The research result shows that the plane beam signal illuminates the target uniformly in space, can eliminate the discontinuity in profile data caused by the directivity of the antenna, improve the stability and quality of the echo signal, and enrich the target response parameters. Springer International Publishing 2021-10-13 2021 /pmc/articles/PMC8514008/ http://dx.doi.org/10.1007/s11600-021-00684-5 Text en © Institute of Geophysics, Polish Academy of Sciences & Polish Academy of Sciences 2021 This article is made available via the PMC Open Access Subset for unrestricted research re-use and secondary analysis in any form or by any means with acknowledgement of the original source. These permissions are granted for the duration of the World Health Organization (WHO) declaration of COVID-19 as a global pandemic. |
spellingShingle | Research Article - Applied Geophysics Cui, Fan Chen, Yi Zhang, Yongqi Du, Yunfei Research on application of ground penetrating radar array method based on plane beam signal in different geological models |
title | Research on application of ground penetrating radar array method based on plane beam signal in different geological models |
title_full | Research on application of ground penetrating radar array method based on plane beam signal in different geological models |
title_fullStr | Research on application of ground penetrating radar array method based on plane beam signal in different geological models |
title_full_unstemmed | Research on application of ground penetrating radar array method based on plane beam signal in different geological models |
title_short | Research on application of ground penetrating radar array method based on plane beam signal in different geological models |
title_sort | research on application of ground penetrating radar array method based on plane beam signal in different geological models |
topic | Research Article - Applied Geophysics |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8514008/ http://dx.doi.org/10.1007/s11600-021-00684-5 |
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