• 全国中文核心期刊
  • 中国科技核心期刊
  • 美国工程索引(EI)收录期刊
  • Scopus数据库收录期刊
杨忠平, 张益铭, 蒋源文, 李滨, 崔芳鹏. 采动作用下含深大岩溶结构面坡体裂隙扩展及变形破坏规律[J]. 岩土工程学报, 2022, 44(8): 1397-1405. DOI: 10.11779/CJGE202208004
引用本文: 杨忠平, 张益铭, 蒋源文, 李滨, 崔芳鹏. 采动作用下含深大岩溶结构面坡体裂隙扩展及变形破坏规律[J]. 岩土工程学报, 2022, 44(8): 1397-1405. DOI: 10.11779/CJGE202208004
YANG Zhong-ping, ZHANG Yi-ming, JIANG Yuan-wen, LI Bin, CUI Fang-peng. Propagation of fissures and deformation and failure laws of karst slopes with deep and large structural plane mining action[J]. Chinese Journal of Geotechnical Engineering, 2022, 44(8): 1397-1405. DOI: 10.11779/CJGE202208004
Citation: YANG Zhong-ping, ZHANG Yi-ming, JIANG Yuan-wen, LI Bin, CUI Fang-peng. Propagation of fissures and deformation and failure laws of karst slopes with deep and large structural plane mining action[J]. Chinese Journal of Geotechnical Engineering, 2022, 44(8): 1397-1405. DOI: 10.11779/CJGE202208004

采动作用下含深大岩溶结构面坡体裂隙扩展及变形破坏规律

Propagation of fissures and deformation and failure laws of karst slopes with deep and large structural plane mining action

  • 摘要: 中国西南高陡岩溶山区崩滑灾害频发,长期地下采矿活动是该区域崩滑灾害的重要诱因之一。采动作用下,坡体后缘深大结构面扩展演化控制着高陡岩溶坡体稳定性和失稳破坏模式。在野外地质调查基础上,结合室内物理模型试验和离散元数值模拟,揭示了地下开采扰动下覆岩裂隙扩展演化规律,阐明了深大结构面对边坡稳定性的控制作用,讨论了坡体变形的破坏模式。结果表明:地下开采扰动对斜坡体稳定性的影响主要表现在地下采动卸荷引起覆岩应力重分布、山体变形诱使裂隙扩展;地下采空后,斜坡体在二维剖面上形成类似“悬臂梁结构”,坡体原有深大结构面控制坡体稳定性;下行开采条件下,采空范围在断层之前,山体高度较小,在自重作用下“悬臂梁结构”岩层向断层及采空区方向协同变形,不会产生大量离层裂隙,煤层顶板仅发生断裂坍塌并充填采空区,采空至断层后,左侧山体已发生塌落,山体应力重分布,覆岩在自重作用下形成大量张拉裂隙,直接顶塌落高度与裂隙带高度也随采空区范围增加而增加。其变形破坏演化过程可概化为:地下开采卸荷-应力重分布→覆岩断裂下沉-裂隙扩展→坡体裂隙贯通-悬臂破坏→坡中变形挤出-岩桥剪断→坡体整体失稳破坏。

     

    Abstract: Collapse and slide disasters frequently occur in high and steep karst mountainous areas in Southwest China. Long-term underground mining activities are one of the important inducements of the collapse and slide disasters in these areas. Under the action of mining, the expansion and evolution of deep and large structural plane at the back edge of the slope controls the stability and instability failure mode of high and steep karst slopes. On the basis of field geological survey, combined with indoor physical model tests and discrete element numerical simulation, the propagation and evolution laws of overlying rock fractures under underground mining disturbance are revealed, the control effects of deep and large structural plane on slope stability are expounded, and the failure modes of slope deformation are discussed. The results show that the influences of underground mining disturbance on slope stability are mainly reflected in the redistribution of overburden stresses caused by underground mining unloading and the propagation of fissures induced by mountain deformation. After underground mining, the slope body forms a "cantilever structure" on the two-dimensional section, and the original deep and large structural plane of the slope body controls the stability of the slope body. Under downward mining, the goaf range is in front of the fault, and the mountain height is small. Under the action of self weight, the "cantilever structure" rock stratum cooperates to deform towards the fault and goaf, and will not produce a large number of separation fissures. The coal seam roof only breaks and collapses and fills the goaf. After the goaf reaches the fault, the mountain at the left has collapsed and the mountain stresses are redistributed. The overburden forms a large number of tension fissures under the action of self weight, and the direct roof collapse height and fracture zone height also increase with the increase of goaf range. The evolution process of deformation and failure can be generalized as follows: underground mining unloading-stress redistribution→overburden fault subsidence-fissure propagation→slope fissure penetration-cantilever failure→deformation extrusion in the slope-rock bridge shear→overall instability failure of the slope.

     

/

返回文章
返回