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On-line Access: 2024-08-27

Received: 2023-10-17

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Journal of Zhejiang University SCIENCE A

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Experimental investigation on the stability of shield tunnel excavation face with water-rich in upper loose and lower dense strata


Author(s):  Pengfei LI, Chuang WANG, Xiaopu CUI, Qing XU, Zhaoguo GE, Shaohua LI

Affiliation(s):  Key Laboratory of Urban Security and Disaster Engineering, Ministry of Education, Beijing University of Technology, Beijing 100124, China; more

Corresponding email(s):  cxp2021@emails.bjut.edu.cn

Key Words:  Shield tunnel; Upper loose and lower dense strata; Excavation face stability; Water pressure ratio


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Pengfei LI, Chuang WANG, Xiaopu CUI, Qing XU, Zhaoguo GE, Shaohua LI. Experimental investigation on the stability of shield tunnel excavation face with water-rich in upper loose and lower dense strata[J]. Journal of Zhejiang University Science A,in press.Frontiers of Information Technology & Electronic Engineering,in press.https://doi.org/10.1631/jzus.A2400309

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author="Pengfei LI, Chuang WANG, Xiaopu CUI, Qing XU, Zhaoguo GE, Shaohua LI",
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doi="https://doi.org/10.1631/jzus.A2400309"
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%T Experimental investigation on the stability of shield tunnel excavation face with water-rich in upper loose and lower dense strata
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Abstract: 
Maintaining the stability of excavation face is key for ensuring the safety of underwater shield tunnel construction. However, the majority of current studies on the stability of excavation face focus on homogeneous strata, with limited research conducted on strata with upper loose and lower dense. Active instability tests are conducted in this study, in concert with the digital image correlation (DIC) technique, to investigate the effects of different water pressure ratios (α) in water-rich upper loose and lower dense strata. The accuracy of these model tests is verified using numerical simulations. The results indicate that as α decreases, there is an increase in both the peak displacement of surface settlement, and the seepage path range of water ahead of the excavation face expands. In contrast, decreasing α will break the limit equilibrium state of the strata faster, cause the earth pressure on the cutterhead to change more rapidly, and increase the instability range of the strata.

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