Application of FDEM in the study of large deformation mechanisms in deep-buried soft rock tunnels: A case study

The Hutou Beishan Mega Tunnel frequently experiences significant deformation and instability collapse when passing through weak and fractured rock strata, leading to frequent design modifications and adversely impacting the construction progress and costs. This paper employs the finite-discrete element method (FDEM) to investigate the mechanisms and characteristics of large deformations in soft rock and analyzes the effects of in-situ stress and lateral pressure coefficients on the stability of soft rock tunnels. The results indicate that: (1) Once the compressive stress concentration exceeds the shear strength of the surrounding rock, shear failure occurs, with the resulting cracks predominantly forming X-shaped conjugate fractures. The shape of the excavation damage zone (EDZ) corresponds to the stress state; (2) Under hydrostatic stress conditions, the extent of damage to weak surrounding rock is influenced by the in-situ stress. At lower in-situ stress levels, only a few cracks appear at the edges of the surrounding rock, and deformation is minimal. At higher in-situ stress levels, cracks extend deeper into the tunnel, crushing shallow rock; (3) The failure characteristics of the tunnel vary with different lateral pressure coefficients. As the lateral pressure coefficient changes, the shape of the EDZ also changes, and the concentrated damage zone shifts from the arch waist to the crown as the lateral pressure coefficient increases.

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Publication Details

Journal
Frontiers in Earth Science
Published
2024-12-23
DOI
https://doi.org/10.3389/feart.2024.1517816
Primary Topic
Rock Mechanics and Modeling
Type
article
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article

Application of FDEM in the study of large deformation mechanisms in deep-buried soft rock tunnels: A case study

Yufei Hu, Chengzeng Yan, Jianzhong Qiao, Yanning Wang et al.
Frontiers in Earth Science
Rock Mechanics and Modeling
article

Application of FDEM in the study of large deformation mechanisms in deep-buried soft rock tunnels: A case study

Yufei Hu, Chengzeng Yan, Jianzhong Qiao, Yanning Wang, Zhancheng He, Shaohua Zheng
article en

Abstract

The Hutou Beishan Mega Tunnel frequently experiences significant deformation and instability collapse when passing through weak and fractured rock strata, leading to frequent design modifications and adversely impacting the construction progress and costs. This paper employs the finite-discrete element method (FDEM) to investigate the mechanisms and characteristics of large deformations in soft rock and analyzes the effects of in-situ stress and lateral pressure coefficients on the stability of soft rock tunnels. The results indicate that: (1) Once the compressive stress concentration exceeds the shear strength of the surrounding rock, shear failure occurs, with the resulting cracks predominantly forming X-shaped conjugate fractures. The shape of the excavation damage zone (EDZ) corresponds to the stress state; (2) Under hydrostatic stress conditions, the extent of damage to weak surrounding rock is influenced by the in-situ stress. At lower in-situ stress levels, only a few cracks appear at the edges of the surrounding rock, and deformation is minimal. At higher in-situ stress levels, cracks extend deeper into the tunnel, crushing shallow rock; (3) The failure characteristics of the tunnel vary with different lateral pressure coefficients. As the lateral pressure coefficient changes, the shape of the EDZ also changes, and the concentrated damage zone shifts from the arch waist to the crown as the lateral pressure coefficient increases.

Frontiers in Earth ScienceVol. 12
China University of Geosciences (CN), Tianjin Municipal Engineering Design and Research Institute (CN)
Sustainable cities and communities
Openalex Percentile: Top 73%
Rock Mechanics and Modeling
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Application of FDEM in the study of large deformation mechanisms in deep-buried soft rock tunnels: A case study — Yufei Hu, Chengzeng Yan, et al. · Frontiers in Earth Science (2024) | TGRS Research Map | TGRS