A comparative experimental study on advance geological prediction between TETSP and TSP303

We introduce a new tunnel long distance prediction seismic reflection imaging system called TETSP. We use TETSP and the latest generation TSP303 to advance geological comparison detection in Zhangcun tunnel in Thousand Island Lake-Hangzhou water transfer project. Firstly, we introduce the layout of...

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Main Authors: Liu Yue, Li Jun-jie
Format: Article
Language:English
Published: EDP Sciences 2021-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2021/28/e3sconf_pgsge2021_01034.pdf
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spelling doaj-c97db88a27fd42e38df86fc43d71ef172021-05-04T12:18:36ZengEDP SciencesE3S Web of Conferences2267-12422021-01-012520103410.1051/e3sconf/202125201034e3sconf_pgsge2021_01034A comparative experimental study on advance geological prediction between TETSP and TSP303Liu Yue0Li Jun-jie1Zhejiang Design Institute of Water Conservancy and Hydroelectric PowerZhejiang Design Institute of Water Conservancy and Hydroelectric PowerWe introduce a new tunnel long distance prediction seismic reflection imaging system called TETSP. We use TETSP and the latest generation TSP303 to advance geological comparison detection in Zhangcun tunnel in Thousand Island Lake-Hangzhou water transfer project. Firstly, we introduce the layout of TETSP observation system and data processing flow. Secondly, we expound the differences between TETSP and TSP303 in aspect of geophone coupling and acoustic interference suppression. Lastly, we analyze the characteristics of reflection anomalies in the karst cave zone of the rock mass. The actual tunnel excavation results verify the reliability of the TSP303 and TETSP prediction. Several conclusions are drawn as follow. Firstly, two kinds of seismic reflection technology both can detect whose wave impedance interface exist significant difference in front of tunnel face, but the TSP303 is more accurate. Secondly, the poor integrity of the rock mass is corresponding to the low velocity of P-wave and S-wave.https://www.e3s-conferences.org/articles/e3sconf/pdf/2021/28/e3sconf_pgsge2021_01034.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Liu Yue
Li Jun-jie
spellingShingle Liu Yue
Li Jun-jie
A comparative experimental study on advance geological prediction between TETSP and TSP303
E3S Web of Conferences
author_facet Liu Yue
Li Jun-jie
author_sort Liu Yue
title A comparative experimental study on advance geological prediction between TETSP and TSP303
title_short A comparative experimental study on advance geological prediction between TETSP and TSP303
title_full A comparative experimental study on advance geological prediction between TETSP and TSP303
title_fullStr A comparative experimental study on advance geological prediction between TETSP and TSP303
title_full_unstemmed A comparative experimental study on advance geological prediction between TETSP and TSP303
title_sort comparative experimental study on advance geological prediction between tetsp and tsp303
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2021-01-01
description We introduce a new tunnel long distance prediction seismic reflection imaging system called TETSP. We use TETSP and the latest generation TSP303 to advance geological comparison detection in Zhangcun tunnel in Thousand Island Lake-Hangzhou water transfer project. Firstly, we introduce the layout of TETSP observation system and data processing flow. Secondly, we expound the differences between TETSP and TSP303 in aspect of geophone coupling and acoustic interference suppression. Lastly, we analyze the characteristics of reflection anomalies in the karst cave zone of the rock mass. The actual tunnel excavation results verify the reliability of the TSP303 and TETSP prediction. Several conclusions are drawn as follow. Firstly, two kinds of seismic reflection technology both can detect whose wave impedance interface exist significant difference in front of tunnel face, but the TSP303 is more accurate. Secondly, the poor integrity of the rock mass is corresponding to the low velocity of P-wave and S-wave.
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2021/28/e3sconf_pgsge2021_01034.pdf
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