Progressive failure of water-filled karst cave of stratified tunnel using coupled discontinuous smoothed particle hydrodynamics method

Chengzhi Xia , Zhenming Shi , Liu Liu , Guangyin Lu , Lin Zhou , Chuanyi Tao , Shaoqiang Meng

Underground Space ›› 2025, Vol. 25 ›› Issue (6) : 74 -98.

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Underground Space ›› 2025, Vol. 25 ›› Issue (6) :74 -98. DOI: 10.1016/j.undsp.2024.10.006
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Progressive failure of water-filled karst cave of stratified tunnel using coupled discontinuous smoothed particle hydrodynamics method
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Abstract

Tunnel construction in karst terrain is influenced by water-filled karst caves and stratigraphic layers, which involves failure characteristics of water-resistant structures and complex fluid-solid interaction (FSI) processes. To cope with this challenge, this paper used coupled discontinuous smoothed particle hydrodynamics (CDSPH) method for investigating water inrush of tunnels considering stratigraphic layers and karst cave positions. Hydraulic fracturing test and sliding-induced impulsive wave test were carried out to verify the accuracy of the CDSPH method. Moreover, a comprehensive analysis of inrush events in the field-scale Qiyeshan (QYS) karst tunnel was conducted, considering different layer dip angles and cave positions on the evolution characteristics of inrush disasters, with quantitative parameters proposed for predicting water/mud inrush from local to overall disaster. The simulation results indicate that CDSPH karst model has been verified to faithfully capture the progressive failure of water-resistant structure during inrush in stratigraphic layers. Water/mud inrush in QYS tunnels can be divided into four stages based on vertical/horizontal stress characteristics, encompassing hydraulic fracturing of karst caves, local inrush, rock collapse, and overall inrush. The dip angle of the bedding planes affects the hydraulic failure characteristics of karst caves. When the cave is located at the top of the tunnel, the water-resistant structures with a dip angle (θ) of 45° poses the highest risk, while θ = 0° provides the most stability. Furthermore, the decrease in water pressure and the occurrence of the maximum flow velocity within the cave can serve as vital indexes to predict the transition from local inrush to overall inrush disaster. These findings emphasize the importance of the CDSPH tunnel model considering stratigraphic layers and karst cave positions when predicting water/mud inrush, and provide guidance for the prevention of inrush flow in karst tunnels.

Keywords

Coupled discontinuous smoothed particle hydrodynamics / Stratigraphic layers / Rock tunnel / Water inrush / Karst cave

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Chengzhi Xia, Zhenming Shi, Liu Liu, Guangyin Lu, Lin Zhou, Chuanyi Tao, Shaoqiang Meng. Progressive failure of water-filled karst cave of stratified tunnel using coupled discontinuous smoothed particle hydrodynamics method. Underground Space, 2025, 25(6): 74-98 DOI:10.1016/j.undsp.2024.10.006

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Data availability

The data that support the findings of this study are available from the corresponding author upon reasonable request.

CRediT authorship contribution statement

Chengzhi Xia: Writing - review & editing, Software, Validation, Formal analysis, Writing - original draft, Data curation, Methodology, Visualization. Zhenming Shi: Project administration, Writing - review & editing, Supervision, Writing - original draft. Liu Liu: Writing - review & editing, Supervision, Writing - original draft, Resources, Investigation. Guangyin Lu: Writing - review & editing, Supervision, Funding acquisition, Project administration. Lin Zhou: Writing - review & editing, Formal analysis, Methodology. Chuanyi Tao: Writing - review & editing, Investigation, Software. Shaoqiang Meng: Software, Writing - review & editing, Data curation, Writing - original draft, Conceptualization.

Declaration of competing interest

The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this study.

Acknowledgement

This research was supported by the National Natural Science Foundation for Doctoral Scholars (Grant No. 424B2055) and National Key Research and Development Program of China (Grant No. 2023YFC3008300), the National Natural Science Foundation of China (Grant Nos. 42172296 and 41974148), and the International Exchange Program for Graduate Students of Tongji University. We extend our gratitude to Professor Bo Li from Tongji University for his support with the flume experiments.

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