Instability of an intersecting fault-dyke system during deep rock excavation

Intersecting discontinuities are often encountered in rock engineering and sometimes associated with damaging geohazards. Our understanding of intersecting discontinuities instability remains vastly insufficient due to difficulties in comprehensively monitoring the failure process. Here we use micro...

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Main Authors: Huang, Xiao, Xu, Nuwen, Wu, Wei, Xiao, Peiwei, Dong, Linlu, Li, Biao
Other Authors: School of Civil and Environmental Engineering
Format: Article
Language:English
Published: 2022
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Online Access:https://hdl.handle.net/10356/162194
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Institution: Nanyang Technological University
Language: English
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spelling sg-ntu-dr.10356-1621942022-10-10T00:59:18Z Instability of an intersecting fault-dyke system during deep rock excavation Huang, Xiao Xu, Nuwen Wu, Wei Xiao, Peiwei Dong, Linlu Li, Biao School of Civil and Environmental Engineering Engineering::Civil engineering Underground Excavation Microseismic Monitoring Intersecting discontinuities are often encountered in rock engineering and sometimes associated with damaging geohazards. Our understanding of intersecting discontinuities instability remains vastly insufficient due to difficulties in comprehensively monitoring the failure process. Here we use microseismic (MS) monitoring to virtualize the MS events in the rock masses surrounding a powerhouse crown and investigate the effect of geological features on the occurrence of MS events. We subsequently build a three-dimensional numerical model and validate this model using the in-situ measurements by multipoint displacement meters. The numerical results demonstrate how the displacements of surrounding rock masses near the fault and the dyke increase and reveal possible causes, such as stress condition as well as geometry and orientation of rock discontinuities. We also discuss the correlation between the tempo-spatial distribution of MS events and the failure pattern of rock masses and confirm the weakened dyke as the main cause of the rock collapse. This study highlights that the stability of intersecting discontinuities can be controlled by both the geometrical and mechanical properties of individual discontinuities, and attentions should be paid to key properties favorable for rock instability. This work was supported by the Science Foundation for Distinguished Young Scholars of Sichuan Province (Grant No. 2020JDJQ0011) and the National Natural Science Foundation of China (Grant No. 51809221). 2022-10-10T00:59:18Z 2022-10-10T00:59:18Z 2022 Journal Article Huang, X., Xu, N., Wu, W., Xiao, P., Dong, L. & Li, B. (2022). Instability of an intersecting fault-dyke system during deep rock excavation. International Journal of Rock Mechanics and Mining Sciences, 153, 105087-. https://dx.doi.org/10.1016/j.ijrmms.2022.105087 1365-1609 https://hdl.handle.net/10356/162194 10.1016/j.ijrmms.2022.105087 2-s2.0-85126274500 153 105087 en International Journal of Rock Mechanics and Mining Sciences © 2022 Elsevier Ltd. All rights reserved.
institution Nanyang Technological University
building NTU Library
continent Asia
country Singapore
Singapore
content_provider NTU Library
collection DR-NTU
language English
topic Engineering::Civil engineering
Underground Excavation
Microseismic Monitoring
spellingShingle Engineering::Civil engineering
Underground Excavation
Microseismic Monitoring
Huang, Xiao
Xu, Nuwen
Wu, Wei
Xiao, Peiwei
Dong, Linlu
Li, Biao
Instability of an intersecting fault-dyke system during deep rock excavation
description Intersecting discontinuities are often encountered in rock engineering and sometimes associated with damaging geohazards. Our understanding of intersecting discontinuities instability remains vastly insufficient due to difficulties in comprehensively monitoring the failure process. Here we use microseismic (MS) monitoring to virtualize the MS events in the rock masses surrounding a powerhouse crown and investigate the effect of geological features on the occurrence of MS events. We subsequently build a three-dimensional numerical model and validate this model using the in-situ measurements by multipoint displacement meters. The numerical results demonstrate how the displacements of surrounding rock masses near the fault and the dyke increase and reveal possible causes, such as stress condition as well as geometry and orientation of rock discontinuities. We also discuss the correlation between the tempo-spatial distribution of MS events and the failure pattern of rock masses and confirm the weakened dyke as the main cause of the rock collapse. This study highlights that the stability of intersecting discontinuities can be controlled by both the geometrical and mechanical properties of individual discontinuities, and attentions should be paid to key properties favorable for rock instability.
author2 School of Civil and Environmental Engineering
author_facet School of Civil and Environmental Engineering
Huang, Xiao
Xu, Nuwen
Wu, Wei
Xiao, Peiwei
Dong, Linlu
Li, Biao
format Article
author Huang, Xiao
Xu, Nuwen
Wu, Wei
Xiao, Peiwei
Dong, Linlu
Li, Biao
author_sort Huang, Xiao
title Instability of an intersecting fault-dyke system during deep rock excavation
title_short Instability of an intersecting fault-dyke system during deep rock excavation
title_full Instability of an intersecting fault-dyke system during deep rock excavation
title_fullStr Instability of an intersecting fault-dyke system during deep rock excavation
title_full_unstemmed Instability of an intersecting fault-dyke system during deep rock excavation
title_sort instability of an intersecting fault-dyke system during deep rock excavation
publishDate 2022
url https://hdl.handle.net/10356/162194
_version_ 1749179201906278400