Research on in situ stress inversion of deep‐buried tunnel based on pressure/tension axis mechanism and geological structure

Abstract The investigation of the in situ stress distribution has always been a key condition for engineering design of deep tunnels and analysis of surrounding rock stability. In this paper, a comprehensive judgment method coupled with pressure/tension (P/T) axis mechanism and geological structure...

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Main Authors: Guanfu Chen, Xiaoli Liu, Danqing Song
Format: Article
Language:English
Published: Wiley 2023-03-01
Series:Deep Underground Science and Engineering
Subjects:
Online Access:https://doi.org/10.1002/dug2.12025
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author Guanfu Chen
Xiaoli Liu
Danqing Song
author_facet Guanfu Chen
Xiaoli Liu
Danqing Song
author_sort Guanfu Chen
collection DOAJ
description Abstract The investigation of the in situ stress distribution has always been a key condition for engineering design of deep tunnels and analysis of surrounding rock stability. In this paper, a comprehensive judgment method coupled with pressure/tension (P/T) axis mechanism and geological structure is proposed to invert the in situ stress in the Duoxiongla tunnel in Tibet. In the process of TBM tunnel excavation, 3887 groups of microseismic events were collected by means of microseismic monitoring technology. By studying the temporal and spatial distribution of 3887 groups of microseismic events, 42 groups of microseismic data were selected for in situ stress inversion. Then the focal mechanisms of 42 groups of microseisms were inverted. Combined with the analysis of the previous geological survey, the inversion results of the in situ stress were analyzed. According to the focal mechanism of the tunnel area, the linear in situ stress inversion method was used to invert the in situ stress in the source area. Finally, according to the PTGS (pressure/tension axis mechanism and geological structure) comprehensive judgment method proposed in this paper, the in situ stress of the tunnel microseismic region was determined. The results show that there are mainly three groups of fissures and joint surfaces in the tunnel area, and the in situ stress is dominated by the horizontal tectonic stress; the main driving force of the rupture surface in the excavation process of Duoxiongla tunnel is the horizontal tectonic stress; the distribution of the maximum and minimum principal stress obtained by the inversion is consistent with the distribution of the P/T axis; combined with the linear in situ stress inversion method and the comprehensive judgment of PTGS, the azimuth and dip angles of the three principal stresses are finally determined as N90.71°E, 4.06°, N5.35°W, 3.06°, and N8.10W, 85.32°, respectively. The study verifies the feasibility of microseismic inversion of in situ stress.
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spelling doaj.art-5350fdaf59964f72adddd12f8782509d2023-05-17T12:50:26ZengWileyDeep Underground Science and Engineering2097-06682770-13282023-03-0121617310.1002/dug2.12025Research on in situ stress inversion of deep‐buried tunnel based on pressure/tension axis mechanism and geological structureGuanfu Chen0Xiaoli Liu1Danqing Song2State Key Laboratory of Hydroscience and Engineering Tsinghua University Beijing ChinaState Key Laboratory of Hydroscience and Engineering Tsinghua University Beijing ChinaState Key Laboratory of Hydroscience and Engineering Tsinghua University Beijing ChinaAbstract The investigation of the in situ stress distribution has always been a key condition for engineering design of deep tunnels and analysis of surrounding rock stability. In this paper, a comprehensive judgment method coupled with pressure/tension (P/T) axis mechanism and geological structure is proposed to invert the in situ stress in the Duoxiongla tunnel in Tibet. In the process of TBM tunnel excavation, 3887 groups of microseismic events were collected by means of microseismic monitoring technology. By studying the temporal and spatial distribution of 3887 groups of microseismic events, 42 groups of microseismic data were selected for in situ stress inversion. Then the focal mechanisms of 42 groups of microseisms were inverted. Combined with the analysis of the previous geological survey, the inversion results of the in situ stress were analyzed. According to the focal mechanism of the tunnel area, the linear in situ stress inversion method was used to invert the in situ stress in the source area. Finally, according to the PTGS (pressure/tension axis mechanism and geological structure) comprehensive judgment method proposed in this paper, the in situ stress of the tunnel microseismic region was determined. The results show that there are mainly three groups of fissures and joint surfaces in the tunnel area, and the in situ stress is dominated by the horizontal tectonic stress; the main driving force of the rupture surface in the excavation process of Duoxiongla tunnel is the horizontal tectonic stress; the distribution of the maximum and minimum principal stress obtained by the inversion is consistent with the distribution of the P/T axis; combined with the linear in situ stress inversion method and the comprehensive judgment of PTGS, the azimuth and dip angles of the three principal stresses are finally determined as N90.71°E, 4.06°, N5.35°W, 3.06°, and N8.10W, 85.32°, respectively. The study verifies the feasibility of microseismic inversion of in situ stress.https://doi.org/10.1002/dug2.12025deep tunnelfocal mechanismgeological structuremicroseismic monitoringstress inversion
spellingShingle Guanfu Chen
Xiaoli Liu
Danqing Song
Research on in situ stress inversion of deep‐buried tunnel based on pressure/tension axis mechanism and geological structure
Deep Underground Science and Engineering
deep tunnel
focal mechanism
geological structure
microseismic monitoring
stress inversion
title Research on in situ stress inversion of deep‐buried tunnel based on pressure/tension axis mechanism and geological structure
title_full Research on in situ stress inversion of deep‐buried tunnel based on pressure/tension axis mechanism and geological structure
title_fullStr Research on in situ stress inversion of deep‐buried tunnel based on pressure/tension axis mechanism and geological structure
title_full_unstemmed Research on in situ stress inversion of deep‐buried tunnel based on pressure/tension axis mechanism and geological structure
title_short Research on in situ stress inversion of deep‐buried tunnel based on pressure/tension axis mechanism and geological structure
title_sort research on in situ stress inversion of deep buried tunnel based on pressure tension axis mechanism and geological structure
topic deep tunnel
focal mechanism
geological structure
microseismic monitoring
stress inversion
url https://doi.org/10.1002/dug2.12025
work_keys_str_mv AT guanfuchen researchoninsitustressinversionofdeepburiedtunnelbasedonpressuretensionaxismechanismandgeologicalstructure
AT xiaoliliu researchoninsitustressinversionofdeepburiedtunnelbasedonpressuretensionaxismechanismandgeologicalstructure
AT danqingsong researchoninsitustressinversionofdeepburiedtunnelbasedonpressuretensionaxismechanismandgeologicalstructure