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WANG Linkang,ZHENG Zihan,ZHANG Guangcheng,et al. Test study on the toppling mode of steep bedding rock slope[J]. Bulletin of Geological Science and Technology,2025,44(2):1-15 doi: 10.19509/j.cnki.dzkq.tb20230550
Citation: WANG Linkang,ZHENG Zihan,ZHANG Guangcheng,et al. Test study on the toppling mode of steep bedding rock slope[J]. Bulletin of Geological Science and Technology,2025,44(2):1-15 doi: 10.19509/j.cnki.dzkq.tb20230550

Test study on the toppling mode of steep bedding rock slope

doi: 10.19509/j.cnki.dzkq.tb20230550
More Information
  • <p>There are a large number of steep bedding rock slopes along the left bank of Dahuaqiao Hydropower Station in the middle and upper reaches of Lancang River. The unique engineering geological conditions in the reservoir area provide a good breeding environment for deformation. The landslide deposits formed by the collapse of the toppling deformed body are widely distributed in the reservoir area, which causes great difficulties for the operation and maintenance of the hydropower project. </p></sec><sec><title>Objective

    In this paper, in order to study the evolution process, toppling mode, toppling deformation and failure mechanism of steep bedding rock slope,

    Methods

    we used the slightly weathered slate on the left bank of the reservoir as a reference prototype for the similar material material, then we choose to use the bottom friction test method to analyze the deformation and failure characteristics of slope under different condition of slope angles, plane inclination angles and structural plane occurrences.

    Results

    The results show that: ①The main toppling failure mode of the steep bedding rock slope is the tensile-toppling type. In the early stage of evolution, the rock mass at the foot of the slope is the first to topple due to stress concentration, and gradually develops from the front edge of the slope body to the middle and back. The rock mass in the middle of the slope surface also gradually changes from the forward dip to the upright to the reverse dip state, and accelerates to bend and topple towards the free surface under the action of gravity. When the deformation of rock mass reaches a certain extent, it will fracture along the maximum bending part or structural plane, and eventually slip along the tensile fracture plane or even collapse directly. ②By comparing the slope parameters and deformation characteristics of the test models, the 7 groups of model slopes are roughly divided into 3 categories: near-vertical bedding rock gentle slope, steep dip bedding rock steep slope, near-vertical bedding rock steep slope. Compared with slope Angle, the rock layer dip Angle has more influence on the toppling deformation and failure of the steep bedding rock slope. The gently inclined structural plane that is not perpendicular to the plane is more likely to cause the toppling deformation and failure of the steep bedding slope than the one perpendicular to the plane, and the scale of toppling deformation and failure is larger when the slope body develops the inward structural plane compared with the outward inclined structural plane. ③From the perspective of deformation stage, the deformation evolution process of slope is divided into initial deformation stage, toppling deformation stage and toppling failure stage. ④The toppling deformation and failure process of steep bedding rock slope is divided into stress adjustment stage, flexural-creep stage, flexural-sliding stage and toppling-sliding-collapse fracture stage from the mechanism. According to the deformation degree of the toppling area, the deformed slope can be divided into three zones: a strong toppled zone, a weak toppled zone, and a stable zone.

    Conclusion

    The research results can provide reference for the research of the evolution process, toppling mode, toppling deformation and failure mechanism of steep bedding rock slope.

     

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