考虑堆积结构特征的TBM洞渣力学性质三轴试验研究

    Triaxial test study on mechanical properties of TBM muck with consideration of its soil structure

    • 摘要: TBM洞渣因其典型的针片状块石特征,堆置后形成独特的堆积结构,其力学特性与其他土石混合体显著不同。通过倾倒堆积物理模拟和GDS大型三轴试验,揭示了其堆积结构特征,分析了不同含石量和块石定向排列对TBM洞渣变形破坏的影响规律,并探讨了其影响机制。结果表明:①TBM洞渣中典型的针片状块石在倾倒堆积过程中易发生滑移,形成具有块石定向排列和正粒序分布特征的独特堆积结构;②TBM洞渣的相对密度随着含石量的增加呈现先增大后减小的趋势,存在一个最优含石量;③随着含石量的增加,TBM洞渣内部结构发生变化,破坏形式逐渐由单一剪切带破坏转变为“X型”共轭剪切带破坏,抗剪强度先升高后降低,出现明显的强度峰值;④TBM洞渣中的针片状块石主要以面-面接触为主,块石间的咬合与嵌套作用较弱,压缩过程中易发生滑动摩擦,从而导致TBM洞渣整体强度较低,压缩变形量较大;⑤随着围压升高,TBM洞渣中块石定向排列的结构特征抑制了块石间的咬合与嵌套作用,限制了强度的增长,导致其劣势逐渐凸显。

       

      Abstract: TBM muck, a typical needle- and flake-shaped soil-rock mixture, develops a distinctive soil structure during stockpiling. Its deformation and strength characteristics differ markedly from those of other soil-rock mixtures. In this study, the entire dumping and accumulation process of TBM muck is simulated through physical model tests to investigate the resulting soil structure. Using GDS large-scale triaxial tests, we systematically analyze the effects of varying rock block proportions and orientations on mechanical behaviors and failure characteristics of TBM muck. The results indicate that: (1) During the dumping and accumulation, flake-shaped rock blocks are prone to sliding, resulting in significant particle size segregation and formation of a soil structure characterized by oriented rock block alignment and a well-graded distribution. (2) The relative density of TBM muck initially increases and then decreases with increasing rock block proportion, indicating the existence of an optimal rock block proportion. (3) As the rock block proportion increases, the internal structure of TBM muck evolves, and its failure mode transitions from a single shear band to an "X-shaped" conjugate shear band failure. Consequently, the shear strength initially increases, reaches a distinct peak, and then decreases. (4) The needle- and flake-shaped rock blocks in TBM muck primarily exhibit face-to-face contact, with limited interlocking and nesting between particles. Under compression, sliding friction predominates, resulting in a lower overall strength and higher compressive deformation. (5) With increasing confining pressure, the oriented arrangement of rock blocks suppresses the interlocking and nesting effects between particles, thereby limiting strength development and progressively amplifying the material's inherent structural weaknesses.

       

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