Experimental study on face instability of shield tunneling in saturated sands at various cover depths

IF 4.9 2区 工程技术 Q3 ENGINEERING, ENVIRONMENTAL
Wantao Ding, Zhipeng Zhong, Zhou Li, Wenhu Wang, Minghui Zhang, Yiran Wen
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Abstract

Strict control of the support pressure is critical for shield tunneling in urban metro projects. However, due to an insufficient understanding of the three-dimensional failure mechanism in saturated sands, the limit support pressure is difficult to determine, and an improper selection can easily lead to face instability. In this study, a series of model tests on face instability were conducted in saturated sands at four different cover depths. The test results indicate that: (1) The support pressure and displacement curve exhibits a four-stage characteristic. As the cover-to-diameter ratio increases, the soil arching effect becomes more significant. For deep tunnels, the maximum ground settlement is only 1/80 of that for shallow tunnels. (2) Face instability induces stress redistribution in the surrounding soil. For shallow tunnels, the failure zone develops more rapidly and propagates to the ground surface, whereas for deep tunnels, the failure zone has a wider horizontal extent, and its height stabilizes at 3 to 4 times the tunnel diameter. The inclination angle of the wedge in the failure zone decreases as the cover-to-diameter ratio increases. (3) Compared to dry sands, the ratio of the limit support pressure to the initial support pressure is larger in saturated sands. The overburden load sustained by the soil arching effect is reduced, and the normalized displacement required to reach the critical settlement Scr increases significantly, indicating a delay in the formation and failure of the soil arch. These findings are primarily applicable to medium-dense, well-graded, saturated medium-to-coarse sands.

饱和砂中不同覆盖深度盾构隧道工作面失稳试验研究
在城市地铁施工中,严格控制支护压力是盾构施工的关键。然而,由于对饱和砂土的三维破坏机制认识不足,极限支撑压力难以确定,选择不当容易导致面失稳。本文对饱和砂土在4种不同覆盖深度下的工作面失稳进行了一系列模型试验。试验结果表明:(1)支护压力与位移曲线呈四阶段特征。随着覆盖径比的增大,土拱效应更加显著。对于深埋隧道,最大地面沉降量仅为浅埋隧道的1/80。(2)工作面失稳引起周围土体应力重分布。浅埋隧道破坏区发展较快,并向地表扩散;深埋隧道破坏区水平范围更广,破坏高度稳定在隧道直径的3 ~ 4倍。楔体在破坏区内的倾角随覆盖径比的增大而减小。(3)与干砂相比,饱和砂的极限支撑压力与初始支撑压力之比更大。土拱效应所承受的覆盖层荷载减小,达到临界沉降Scr所需的归一化位移显著增加,表明土拱的形成和破坏延迟。这些发现主要适用于中致密、级配良好、饱和的中粗砂岩。
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来源期刊
Bulletin of Engineering Geology and the Environment
Bulletin of Engineering Geology and the Environment 工程技术-地球科学综合
CiteScore
7.10
自引率
11.90%
发文量
445
审稿时长
4.1 months
期刊介绍: Engineering geology is defined in the statutes of the IAEG as the science devoted to the investigation, study and solution of engineering and environmental problems which may arise as the result of the interaction between geology and the works or activities of man, as well as of the prediction of and development of measures for the prevention or remediation of geological hazards. Engineering geology embraces: • the applications/implications of the geomorphology, structural geology, and hydrogeological conditions of geological formations; • the characterisation of the mineralogical, physico-geomechanical, chemical and hydraulic properties of all earth materials involved in construction, resource recovery and environmental change; • the assessment of the mechanical and hydrological behaviour of soil and rock masses; • the prediction of changes to the above properties with time; • the determination of the parameters to be considered in the stability analysis of engineering works and earth masses.
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