高填方边坡工程中多粒级土岩混合物的大型直接剪切试验研究

Chao Zheng, Shuxiang Song, Nan Zhang, Kangwei Xiong
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摘要

土岩混合物是由多种粒度矿物颗粒组成的多相天然地质材料,具有显著的多尺度材料群天然特征。为了研究多粒级土岩混合物在填土工程中原位条件下的抗剪强度特征和变形破坏特征,制备了多粒级土岩混合物原位条件下的样品,并在自然条件和水浸泡条件下进行了大规模原位直接剪切试验。试验结果表明,土岩混合物的抗剪强度较高,经水浸泡饱和后,抗剪强度明显下降,主要表现为内摩擦角减小,而内聚力基本保持不变。多粒径土石混合物的内聚力主要由土石混合物中砾石等粗颗粒的剪切破坏内聚力提供,其发挥程度受土石混合物的级配特征和颗粒形态控制,并受制约因素影响。多粒径土岩混合物在浸水饱和后抗剪强度显著下降的原因可以解释为:粗颗粒表面覆盖的粘土膜在浸水后变得松软,导致粗颗粒与粘土膜之间的滑动摩擦阻力以及粗颗粒之间通过粘土膜界面旋转传递产生的闭塞摩擦阻力显著下降。
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Study on large scale direct shear test on soil-rock mixture with multiple grain grades in high fill slope engineering
Soil-rock mixtures are multiphase natural geological materials composed of mineral particles of multiple grain sizes, and have significant natural characteristics of multiscale material groups. In order to investigate the shear strength characteristics and deformation failure characteristics of soil-rock mixtures with multiple grain sizes under in-situ conditions in fill engineering, samples of soil-rock mixtures with multiple grain sizes under in-situ conditions were prepared, and large-scale in-situ direct shear tests were conducted under natural and water-soaked conditions. The test results showed that the shear strength of soil-rock mixtures is relatively high, and after saturated by water immersion, its shear strength decreases significantly, mainly manifested in the decrease of internal friction angle while the cohesion remains basically unchanged. The cohesion of soil-rock mixtures with multiple grain sizes is mainly provided by the shear-breaking cohesion of coarse particles such as gravel in the soil-rock mixture, and its degree of exertion is controlled by the grading characteristics and particle morphology of the soil-rock mixture and affected by constraints. The reason for the significant decrease in shear strength of soil-rock mixtures with multiple grain sizes after water-soaked saturation can be explained as follows: the clay film covering the surface of coarse particles becomes soft after water immersion, resulting in a significant decrease in the sliding friction resistance between coarse particles and the clay film, as well as the occlusion friction resistance generated by the rotation transfer between coarse particles through the clay film interface.
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