盾构对接冻结对邻近隧道极限冻胀影响的模型试验

    Experimental study on influence of extreme frost heave on adjacent tunnels during freeze reinforcement for shield docking construction

    • 摘要: 盾构对接冻结施工引起冻胀效应的影响规律是评价邻近隧道稳定性及采取应对措施的依据,而邻近隧道约束状态直接决定冻胀效应分布特征。依托大直径盾构江底对接工程,设计进行了隧道结构恒载自由移动及固定两种极限边界条件的冻结模型试验,研究冻结过程中地层温度、冻胀力与位移的演化规律,获得邻近隧道的力学响应与位移变化特征。盾构外侧发散布孔条件下,冻结70 d时冻结管与盾构之间土体被冻实,165 d时盾构对接位置冻结壁厚度达到6 m,而平均温度为-16.1℃;盾构外部冻土形成过程引起邻近隧道的最大冻胀位移为9.6 mm,而作用在隧道表面冻胀力的最大增幅约为原始地层压力的14.1%;冻土与隧道间未冻地层压缩变形和冻胀力分散效果是影响隧道结构承受冻胀效应的重要因素,未冻地层平均变形模量随着冻结壁厚度增加而近线性增大,粉质黏土地层平均变形模量介于20.8~49.3 MPa。研究结果表明,邻近隧道的约束状态显著影响冻胀位移及承受冻胀力的变化过程,而未冻地层被压缩过程会吸收部分冻胀效应,从而减小施工的冻胀影响。

       

      Abstract: The influence patterns of frost heave effects caused by shield connection freezing construction are the basis for evaluating the stability of adjacent tunnels and formulating countermeasures, while the constraint state of the surrounding strata on tunnel structures directly determines the distribution characteristics of the frost heave effect. Based on the large-diameter shield underwater connection project, the model tests of freezing reinforcement under two extreme boundary conditions of constant load free movement and fix constraint of the tunnel structure are designed and carried out. The evolution patterns of strata temperature, frost heave force and displacement during the freezing process are investigated, and the mechanical response and displacement change process characteristics of the adjacent tunnel are obtained. Under the condition of scattered boreholes on the outside of the shield, all the space between the freezing pipe and the shield is completely frozen after 70 days of freezing, and the thickness of the frozen wall at the shield connection position could reach 6 m after 165 days, with an average temperature of about -16.1℃. The maximum frost heave displacement of the adjacent tunnel during the formation of frozen soil outside the shield is 9.6 mm, and the maximum increase of the frost heave force acting on the tunnel surface is approximately 14.1% of the stratum's original pressure. The compression deformation and dispersion effect on frost heave force of the unfrozen stratum between the frozen soil and the tunnel are the key factors affecting the tunnel structure's ability to withstand the frost heave effect. The average deformation modulus of the unfrozen stratum slightly increases with the expansion of the frozen soil, and the average deformation modulus of the silty clay stratum is between 20.8 and 49.3 MPa. The research results indicate that the constraint state adjacent to the tunnel significantly influences the process of frost heave displacement and the variation in the borne frost heave force. Meanwhile, the compression process of the unfrozen stratum absorbs part of the frost heave effect, thereby reducing its impact during construction.

       

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