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1.
Centrifuge model test on the face stability of shallow tunnel   总被引:2,自引:2,他引:0  
This paper is an investigation of face stability on a small-scale tunnel model in a geotechnical centrifuge. By making use of symmetry, half of the tunnel cross section was considered. The support at excavation face was provided by a piston, which was adjusted during flight. Some aspects on the collapse at tunnel face are investigated for different overburden pressures: failure mechanism, surface settlement, stress acting at tunnel face, and the required face support counteracting the earth pressure. Ground deformation was observed through a transparent wall and measured by digital image correlation. The results from centrifuge model tests were compared with theoretical models.  相似文献   

2.
吕玺琳  周运才  李冯缔 《岩土力学》2016,37(11):3324-3328
通过开展离心模型试验,对干粉砂及饱和粉砂中盾构隧道开挖面的失稳破坏特性和极限支护压力进行了研究。通过远程控制开挖面土体位移,获得了支护压力与开挖面位移间的关系曲线及开挖面达到主动极限平衡状态时的破坏模式。2组干砂离心模型试验结果表明,当隧道埋深与隧道直径比从0.5增大到1时,开挖面破坏模式从整体坍塌破坏转变为烟囱状,但极限支护压力变化较小。饱和砂土中的试验表明,开挖面水平方向破坏范围相比在相同埋深干砂中的范围扩大,极限支护压力显著增加。对开挖面破坏过程进行三维弹塑性有限元数值模拟,获得了开挖面极限支护压力和破坏机制,所得结果与试验吻合较好。进一步通过数值模拟,分析了土体强度参数、隧道埋深及渗流对极限支护压力的影响规律。结果表明,渗流条件下开挖面破坏区域及极限支护压力均大于无渗流情况,极限支护压力随内摩擦角增大而减小,随隧道埋深增大而减小。  相似文献   

3.
于丽  吕城  段儒禹  王明年 《岩土力学》2020,41(1):194-204
浅埋土质隧道的稳定性研究一直是隧道工程的关键问题,而孔隙水压力的存在影响着浅埋土质隧道的安全。构建了隧道顶部为圆弧形的浅埋土质隧道的三维塌落机制,基于非线性Mohr-Coulomb破坏准则和极限分析上限法,并考虑孔隙水压力的作用,推导出浅埋土质隧道的塌落范围及支护力的最优上限解计算公式。通过与既有研究进行对比,验证了所提方法的合理性。分析了不同参数对塌落范围、塌落土体的重力及支护力的影响,结果表明:孔隙水压力对浅埋土质隧道的塌落范围、塌落土体的重力及支护力有着显著的影响;孔隙水压力对塌落范围、塌落土体重力的影响比较复杂,而支护力都随着孔隙水压力系数的增大而增大;不同参数对浅埋土质隧道的塌落范围、塌落土体的重力及支护力的影响规律不同。新方法可为浅埋土质隧道的设计优化提供理论支撑。  相似文献   

4.
王俊  王闯  何川  胡雄玉  江英超 《岩土力学》2018,39(8):3038-3046
采用?800 mm模型土压盾构开展室内掘进试验,以探究砂卵石中土压盾构隧道掌子面失稳诱发地层变形特征。同时,补充开展三维离散元仿真以挖掘室内试验难以获取的掌子面失稳信息,并研究隧道埋深对掌子面稳定性的影响规律。研究结果表明:砂卵石地层中盾构隧道掌子面失稳发展到地表后,沉降曲面呈上大下小逐步收缩的沙漏状,影响范围小于砂土地层。考虑盾构动态掘进过程后,卵石颗粒接触关系变化十分剧烈,掌子面稳定性被削弱,极限支护压力随之增大。掌子面极限支护压力随隧道埋深基本呈线性增加,极限支护压力与初始支护压力之比则随埋深增大而减小。掌子面失稳机制可根据隧道埋深划分为3种模式。与既有研究相比,考虑了盾构动态掘进过程与实际工程更加接近,可为确保砂卵石地层土压盾构隧道施工掌子面稳定提供参考。  相似文献   

5.
Controlling the face stability of shallow shield tunnels is difficult due to the inadequate understanding of face failure mechanism. The failure mechanism and the limit support pressure of a tunnel face in dry sandy ground were investigated by using discrete element method (DEM), which has particular advantages for revealing mechanical properties of granular materials. The contact parameters of the dry sand particles were obtained by calibrating the results of laboratory direct shear tests. A series of three-dimensional DEM models for different ratios of the cover depth to the diameter of the tunnel (C/= 0.5, 1, and 2; i.e., relative depth) were then built to simulated the process of tunnel face failure. The limit support pressure, failure zone and soil arching were discussed and compared with other methods. The results of DEM simulations show that the process of tunnel face failure can be divided into two stages. With the increase of the horizontal displacement of the tunnel face, the support pressure decreases to the limit support pressure and then increases to the residual support pressure. The limit support pressure increases with the rise of relative depth and then tends to be constant. In the process of tunnel face failure, the failure zone is gradually enlarged in size and expands to the ground surface. The numerical results also demonstrate that soil arching occurs in the upper part of the failure zone and the soil becomes loosened in the failure zone. Consequently, the comprehensive analysis of tunnel face failure may help to guarantee safe construction during tunneling.  相似文献   

6.
隧洞拱冠砂土位移与破坏的离心模型试验研究   总被引:9,自引:1,他引:8  
通过离心模型试验,对隧洞拱冠以上地层位移与隧洞内支护压力的关系及临界支护压力进行了研究。结果表明:在砂土中开挖隧洞,由于砂土抗剪强度的发挥,隧洞拱冠以上砂土在远小于原位上覆土压力的支护压力下仅发生一定的位移而不致塌落;因此,若允许地表面发生少许沉降,隧洞内支护压力可以比原位上覆土压力有较大程度的降低。  相似文献   

7.
This paper investigates tunnel face stability in soft rock masses via coupled limit and reliability analyses. Specifically, a 3D face collapse mechanism was first constructed. Then the Hoek–Brown failure criterion was introduced into the limit analysis via the tangential technique. Taking the variability of rock mass parameters and loads into consideration, a reliability model was established. The collapse pressure and failure range of tunnel faces were determined. In addition, the required factor of safety (FS) and supporting pressure under three safety levels were obtained, and the corresponding safety level graphs for support design were presented. Comparison of the obtained results with previous work demonstrates the rationality of the 3D collapse mechanism and the validity of the results. A decrease in the geological strength index, Hoek–Brown parameter mi, and uniaxial compressive strength or an increase in the disturbance factor results in a nonlinear increase of the collapse pressure and an enlargement of the failure zone. Such changes also lead to a nonlinear increase of the required support pressure under a certain safety level. By contrast, the FS does not exhibit any obvious change when these parameters vary. Therefore, when a rock mass is of poor quality or heavily disturbed, the advance support should be enlarged from upper front to right above the tunnel face. Moreover, as the safety level increases, both the required FS and supporting pressure of the tunnel face increase nonlinearly at a higher rate.  相似文献   

8.
This paper investigates the face stability of shield-driven tunnels shallowly buried in dry sand using 1-g large-scale model tests. A half-circular tunnel model with a rigid front face was designed and tested. The ground movement was mobilized by pulling the tunnel face backwards at different speeds. The support pressure at tunnel face, settlement at ground surface, and internal movement of soil body were measured by load cells, linear variable differential transducers, and a camera, respectively, and the progress of face failure was observed through a transparent lateral wall of model tank. The tests show that, as the tunnel face moves backwards, the support pressure at the tunnel face drops sharply initially, then rebounds slightly, and tends to be stabilized at the end. Similarly, the ground surface settlement shows a three-stage variation pattern. Using the particle image velocimetry technique, the particle movement, shear strain, and vortex location of soil are analyzed. The variation of support pressure and ground surface settlement related to the internal movement of soil particles is discussed. The impact of the tunnel face moving speed on the face stability is discussed. As the tunnel face moves relatively fast, soil failure originates from a height above tunnel invert and an analytical model is developed to analyze such failure.  相似文献   

9.
当土压平衡盾构穿越高水位地层(如穿越江河)时,地下水与土舱之间的高水压差会产生过大的渗透力,导致开挖面失稳。为了研究渗流条件下开挖面失稳问题,开发了一套隧道离心模型试验装置,主要包括刚性模型箱、模型盾构、开挖面伺服加载系统、水位控制系统、储水箱。针对饱和砂质粉土地层,开展了一系列不同水位高度的稳态渗流开挖面失稳模型试验。结果显示,开挖面失稳过程中随着开挖面位移的增加,有效支护压力迅速下降;在达到最小值 之后缓慢回升并趋于稳定;极限有效支护压力 与水头压力 呈线性关系。  相似文献   

10.
为解决上覆流沙层隧道开挖面极易发生坍塌破坏的技术难题,以典型该地质条件下的青岛地铁M2号线啤苗区间(啤酒城站至苗岭路站)为研究对象,基于开挖面的实际破坏特征建立了开挖面失稳破坏力学模型,从功能转化平衡角度,进行了隧道开挖面稳定性上限分析,并利用强度折减与重力加载两种方式,提出了隧道开挖面安全系数,得到了不同开挖面土体黏聚力、摩擦角、重度、隔水层厚度及隧道开挖高度下的临界土体破裂范围及破裂模式。理论研究表明:随着开挖面土体黏聚力、摩擦角、隔水层厚度等参数的增加,开挖面安全系数不断增大,稳定性不断提高;随着土体重度、隧道开挖高度增加,开挖面安全系数不断减小,稳定性不断降低。通过建立不同工况的数值模型验证了理论研究的正确性,得到了上覆流沙层地质条件下开挖面的典型破坏模式和临界参数,并提出了相应工程建议。研究成果为青岛地铁M2号线的顺利贯通及该类地质条件下的隧道施工提供了理论指导和科学对策。  相似文献   

11.
程红战  陈健  胡之锋  黄珏皓 《岩土力学》2018,39(8):3047-3054
采用传统研究方法对盾构开挖面稳定性的分析多基于土体是均质、各向同性材料的假设,显然与其本身的非均质性相违背。为此,开展了考虑土体抗剪强度参数的空间变异性对盾构开挖面稳定性的影响研究。在随机场理论的基础上,采用协方差矩阵分解法建立了描述砂土内摩擦角空间变异性的三维随机场模型,借助于数值分析软件平台研究了内摩擦角的变异系数、自相关距离对开挖面失稳模式、极限支护应力的影响规律,并采用概率分析法探讨了极限支护应力特征值的选取。结果表明:砂土内摩擦角的空间变异性对开挖面稳定性有重要的影响;随内摩擦角的变异系数的增大,极限支护应力的概率分布离散性越大;开挖面失稳模式与自相关距离的大小密切相关,当自相关距离与隧道直径比较接近时,开挖面可能出现局部失稳;提出了开挖面极限支护应力特征值的概念,并结合失稳概率给出了其初步确定方法。  相似文献   

12.
Zeng  Sheng    Xilin  Huang  Maosong 《Acta Geotechnica》2019,14(6):1643-1652

The failure mechanism and limit support pressure are essential factors for the stability assessment of tunnel face during shield tunneling. Previous studies were mostly based on the assumption that soil fails when the plastic limit is reached. The static liquefaction of saturated sand at pre-failure state often largely reduces shear strength; a stable tunnel face could be destabilized and even collapses abruptly. This paper aims to explore the static liquefaction failure of tunnel face in saturated sands by 3D discrete element simulation. The particle shape is considered by using clump composed of two identical spheres, and the micro-material parameters are calibrated by fitting against triaxial tests. The tunnel face is initially supported by the earth pressure at rest, and then the pressure is reduced by applying a displacement on the free surface until soil body completely collapses. The second-order work during the unloading process is calculated, and a negative value denotes the initiation of static liquefaction. The distribution of negative second-order work point shows the initiation and propagation of static liquefaction. The ultimate failure mode is shown to be composed of a sliding wedge and an overlying chimney, and the chimney is confined to a local area for soil arching. The experienced stress path of tunnel face verifies the existence of static liquefaction instability, indicating the stability analysis should consider static liquefaction rather than simply using the conventional plastic limit state analysis.

  相似文献   

13.
成都地铁卵石层中盾构施工开挖面稳定性研究   总被引:4,自引:0,他引:4  
随着我国社会经济的发展,越来越多的城市开始规划和修建地铁,在此期间,部分城市在地铁建设中遇到了地质条件非常复杂的砂卵石土层,特别是正在建设中的成都地铁1、2号线,区间隧道几乎全部从卵石土层中穿越,根据设计,成都地铁1、2号线部分区间隧道采用加泥式土压平衡盾构法施工。利用土压平衡式盾构施工时,开挖面支护土压力控制是保证掘进顺利进行的关键,目前国内外在这方面的研究主要集中于砂土和黏性土,关于卵石土盾构隧道开挖面变形与破坏的研究很少。基于此,根据卵石土具有强烈离散特性的特点,利用颗粒离散元数值方法,对卵石土层土压平衡式盾构施工中开挖面支护应力不足引起开挖面的变形及破坏问题进行了分析研究,探讨了隧道开挖面变形及破坏问题。研究结果显示:(1)开挖面极限支护应力远小于土体原位静止土压力;(2)开挖面失稳后,开挖面前部的滑动块为一曲面体。这为卵石土地层中盾构开挖面控制压力的确定提供参考。  相似文献   

14.
Tsunami runup and drawdown can cause liquefaction failure of coastal fine sand slopes due to the generation of high excess pore pressure and the reduction of the effective over burden pressure during the drawdown. The region immediately seaward of the initial shoreline is the most susceptible to tsunami-induced liquefaction failure because the water level drops significantly below the still water level during the set down phase of the drawdown. The objective of this work is to develop and validate a numerical model to assess the potential for tsunami-induced liquefaction failure of coastal sandy slopes. The transient pressure distribution acting on the slope due to wave runup and drawdown is computed by solving for the hybrid Boussinesq—nonlinear shallow water equations using a finite volume method. The subsurface pore water pressure and deformation fields are solved simultaneously using a finite element method. Two different soil constitutive models have been examined: a linear elastic model and a non-associative Mohr–Coulomb model. The numerical methods are validated by comparing the results with analytical models, and with experimental measurements from a large-scale laboratory study of breaking solitary waves over a planar fine sand beach. Good comparisons were observed from both the analytical and experimental validation studies. Numerical case studies are shown for a full-scale simulation of a 10-m solitary wave over a 1:15 and 1:5 sloped fine sand beach. The results show that the soil near the bed surface, particularly along the seepage face, is at risk to liquefaction failure. The depth of the seepage face increases and the width of the seepage face decreases with increasing bed slope. The rate of bed surface loading and unloading due to wave runup and drawdown, respectively, also increases with increasing bed slope. Consequently, the case with the steeper slope is more susceptible to liquefaction failure due to the higher hydraulic gradient. The analysis also suggests that the results are strongly influenced by the soil permeability and relative compressibility between the pore fluid and solid skeleton, and that a coupled solid/fluid formulation is needed for the soil solver. Finally, the results show the drawdown pore pressure response is strongly influenced by nonlinear material behavior for the full-scale simulation.  相似文献   

15.
刘克奇  丁万涛  陈瑞  侯铭垒 《岩土力学》2020,41(7):2293-2303
为明确盾构施工掌子面滑移破坏机制并确定掌子面支护力的合理范围,基于滑移线理论和极限分析上限定理,利用空间离散技术提出了一种盾构施工掌子面三维滑移破裂模型。依据大主应力拱理论计算滑移区顶部竖向土压力值,并以此作为滑移破坏区上部的竖向荷载计算掌子面极限支护力。研究表明,土拱效应显著影响掌子面前方土体竖向应力的大小及分布规律;将本模型与已有研究方法进行比较,验证了本模型获取的掌子面极限支护力极限分析上限解在黏性土地层以及摩擦土地层中的适用性。同时本模型构建的掌子面破坏区域形态更加贴近离心试验结果与数值计算结果。  相似文献   

16.
Upper bound analysis of tunnel face stability in layered soils   总被引:3,自引:3,他引:0  
The working face of tunnel constructions has to be kept stable during tunneling to prevent large soil deformations or fatal failure. In layered soils with lower cohesion, failures happen more often and more abrupt than in cohesive soils. Therefore, the maintenance of a proper support pressure at the tunnel working face is of high importance. In this paper, an upper bound analysis is introduced to investigate the minimum support pressure for the face stability in layered soils. A three-dimensional kinematically admissible mechanism for the upper bound analysis is improved to model potential failure within different soil layers. An analytical solution for the support pressure assessment is achieved. The influence of the crossing and cover soil on the face stability is analyzed, respectively. This solution provides an analytical estimation of the minimum support pressure for the face stability. It may be used as a reference for projects under similar conditions.  相似文献   

17.
The kinematic approach in combination with numerical simulation is used to examine the effect of pore water pressure on tunnel face stability. Pore water pressure distribution obtained by numerical calculations using FLAC3D is used to interpolate the pore water pressure on a 3D rotational collapse mechanism. Comparisons are made to check the present approach against other solutions, showing that the present approach improves the existing upper bound solutions. Results obtained indicate that critical effective face pressure increases with water table elevation. Several normalized charts are also presented for quick evaluation of tunnel face stability. At the end of the paper, the influence of anisotropic permeability on tunnel face stability is also discussed, showing that the isotropic model leads to an overestimation of the necessary tunnel face pressure for anisotropic soils. Copyright © 2016 John Wiley & Sons, Ltd.  相似文献   

18.
The undrained tunnel face stability in clay with a linearly increasing shear strength with depth was investigated by three-dimensional finite element analysis. Three parametric studies were performed to study the effects of the cover depth ratio, overburden stress factor and linear strength gradient ratio on the load factor of the undrained tunnel face stability. The influence of the linear strength gradient ratio on the predicted failure mechanism of the undrained face stability was discussed and examined. An approximate closed-form solution was proposed for three-dimensional undrained tunnel face stability in clays with constant or linearly increasing shear strength profiles with depth.  相似文献   

19.
粉砂土反复冻胀融沉特性试验研究   总被引:3,自引:0,他引:3  
严晗  王天亮  刘建坤 《岩土力学》2013,34(11):3159-3165
针对深季节冻土区的特殊环境,通过室内试验研究了粉砂土在不同初始含水率、干密度、荷载、冻融次数条件下的反复冻胀、融沉特性。研究结果表明:粉砂土的冻结温度为-1.03 °C;其冻胀融沉变形随冻融次数的增加呈现波浪式起伏变化,并最终趋于稳定状态;经历多次冻融后,干密度较大试样整体表现为膨胀,干密度较小试样整体表现为压密;上部荷载在抑制冻胀的同时加大了试样的整体融沉变形,却降低了每次冻融的冻胀率和融沉系数;存在一个最优初始含水率,该含水率条件下,试样经历多次冻融后的高度不发生变化;由于外界水源的补给,冻融后试样内部含水率均大于初始含水率;干密度和顶端荷载的增大均有效地抑制了外界水源的补给;4次冻融循环后,粉砂土的冻胀率、融沉系数均逐渐趋于稳定。  相似文献   

20.
刘泉维  杨忠年 《岩土力学》2014,35(8):2255-2260
在泥水平衡盾构施工过程中,如何确保施工安全并减少对周边环境的影响受到国内外学者的广泛关注,地层土体稳定性问题显得尤为重要,但对于砂质地层开挖面稳定性的失稳机制及其稳定性分析尚处于经验阶段。利用大尺寸模型试验,研究了不同水头高度(无水、0.9 m和1.1 m)下两种地层中开挖面主动破坏的发展模式和受力情况。试验中分析了不同水头高度对开挖面主动破坏的影响,研究结果表明:砂质土层中盾构隧道开挖面失稳时,存在土拱效应,使得地表对开挖面主动破坏的响应存在滞后效应;根据水头高度不同,可将砂质地层中开挖面主动破坏发展模式划分为无水模式、低水头模式和高水头模式;在形成泥膜和提供支护力的过程中,会在砂质土层中产生超孔隙水压力,在确定支护力时,应在静止土压力和静水压力的基础上,考虑超孔隙水压力的影响。研究结果对确定开挖面极限支护压力有重要的指导意义。  相似文献   

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