不同含石量条件下TBM渣料剪切特性研究

    STUDY ON SHEAR CHARACTERISTICS OF TBM EXCAVATED MATERIALS UNDER DIFFERENT ROCK BLOCK PROPORTIONS

    • 摘要: TBM渣料主要由细砂和针片状碎块石组成,属于不良级配土,含石量变化大,土体结构独特,变形强度特征有别于其他类型的土石混合体。本文依托喜马拉雅东部多雄拉隧道TBM弃渣场,通过现场调查和三维激光扫描技术量化渣料形状和结构特征,提出适用于TBM渣料的离散元直剪模型构建方法,结合室内大型直剪试验和PFC3D离散元数值模拟,揭示不同含石量条件下TBM渣料宏观力学规律和细观变形破坏机制。研究结果表明:TBM渣料中碎块石形状近似于刀盘状、条棒状和圆盘状,在人工堆置过程中,碎块石长轴方向与水平面之间的夹角主要分布在0°~20°,土体结构表现出显著的空间定向性;随着含石量的增加,TBM渣料结构由悬浮密实型结构向骨架密实型结构过渡,最终转变为骨架空隙型结构,块石颗粒间咬合、嵌套、自锁作用显著增强,块石旋转自由度大大受限,其宏观变形特征由“剪缩”向“剪胀”转变,抗剪强度及其指标均呈现出先缓慢增长再轻微降低,最后大幅度提升的趋势,其内部颗粒运动形式由“土石联动”向“土绕石”转变,力链数量线性减少,平均力链强度增长幅度逐渐加大,强力链逐渐在模型内部起到支撑作用,整体上剪切带从“S”型分布逐步趋近于呈“一”字型分布,剪切带厚度明显变薄。研究成果将弥补当前对针片状土石混合体研究的不足,为TBM弃渣场稳定性分析和风险评价工作提供理论支撑。

       

      Abstract: TBM excavated materials are mainly composed of fine sand and needle-flake-shaped rock blocks. The deformation and strength characteristics of TBM excavated materials,which belong to poor graded soil,with large variation in rock block proportion,unique soil structure,are quite different from other types of soil-rock mixtures. Based on the field surveys and 3D laser scanning technology,the shape and structural characteristics of the TBM excavated materials from the Duoxiongla Tunnel in the eastern Himalayas were quantified. This paper proposes a discrete element direct shear model construction method,which is suitable for TBM excavated materials. The large-scale indoor direct shear test combined with PFC3D discrete element numerical simulation were used to reveal the macroscopic mechanical behavior and mesoscopic deformation and failure mechanism of TBM excavated materials under different rock block proportions. The results show that the shape of rock blocks in the TBM excavated materials is similar to cutter disk,bar,and disc. After the manual stacking process,the angle between the long axis direction of the rock blocks and the horizontal plane is mainly distributed in 0°~20°,and the soil structure shows significant spatial orientation. With the increase of rock content,the structure of TBM excavated materials transforms from suspended dense structure to skeleton dense structure,and finally transforms into the skeleton void structure,resulting in a significant increase in the occlusion,nesting,and self-locking between the rock blocks. Therefore,the rotational freedom of the rock is greatly limited. The macroscopic deformation characteristics of specimen change from shear shrinkage to shear dilatation,and its shear strength shows a trend of slow growth at first,then a slight decrease,and finally a large increase. In addition,according to PFC3D simulation results,the internal particle movement form has changed from "soil-rock linkage" to "soil-rock around" with the increase of rock content. The number of force chains decreases linearly,and the mean force chain strength increases gradually. The strong force chain gradually played a supporting role in the model. On the whole,the distribution of the shear zone also gradually approaches from the "S"-shaped distribution to the linear distribution,and the thickness of the shear zone becomes thinner obviously. Overall,this paper will make up for the insufficiency of the current research on the needle-flake-shaped soil-rock mixture,and provides theoretical support for the stability analysis and risk assessment of the TBM waste dump.

       

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