周子涵, 陈忠辉, 包敏, 年庚乾, 张伟. 顺倾断续节理岩质边坡的稳定性突变[J]. 煤炭学报, 2020, 45(S1): 161-172. DOI: 10.13225/j.cnki.jccs.2019.0958
引用本文: 周子涵, 陈忠辉, 包敏, 年庚乾, 张伟. 顺倾断续节理岩质边坡的稳定性突变[J]. 煤炭学报, 2020, 45(S1): 161-172. DOI: 10.13225/j.cnki.jccs.2019.0958
ZHOU Zihan, CHEN Zhonghui, BAO Min, NIAN Gengqian, ZHANG Wei. Stability of rock slope with bedding intermittent joints based on catastrophe theory[J]. Journal of China Coal Society, 2020, 45(S1): 161-172. DOI: 10.13225/j.cnki.jccs.2019.0958
Citation: ZHOU Zihan, CHEN Zhonghui, BAO Min, NIAN Gengqian, ZHANG Wei. Stability of rock slope with bedding intermittent joints based on catastrophe theory[J]. Journal of China Coal Society, 2020, 45(S1): 161-172. DOI: 10.13225/j.cnki.jccs.2019.0958

顺倾断续节理岩质边坡的稳定性突变

Stability of rock slope with bedding intermittent joints based on catastrophe theory

  • 摘要: 基于顺倾断续节理岩质边坡二维平面滑动失稳力学模型,建立自重应力作用下断续节理岩质边坡失稳的尖点突变理论力学模型。根据该突变模型,探讨断续节理长度(节理连通率)、节理倾角、节理摩擦角以及黏聚力等因素对边坡稳定性的影响规律,推导边坡的临界失稳高度,提出节理边坡失稳的判据条件,最后利用有限差分法(FLAC3D)数值模拟方法研究不同节理连通率和节理倾角条件下顺倾断续节理岩质边坡的破坏形态,结果表明:节理连通率和节理倾角越大,节理摩擦角、节理黏聚力、岩石摩擦角以及岩石黏聚力越小,边坡失稳的可能性越高;当节理连通率较小时,岩石摩擦角和岩石黏聚力是影响边坡稳定性的主要因素,随着节理连通率的不断增大,节理摩擦角和节理黏聚力对边坡稳定性的影响愈发显著,逐渐成为控制边坡稳定性的主要因素;顺倾断续节理岩质边坡在自重应力作用下主要发生滑移—倾倒型混合渐进式破坏,且节理岩桥的贯通破坏是由于节理尖端形成的剪切裂纹与既有节理的扩展贯通所致,下部岩桥先贯通并逐渐向上延伸,进而形成局部或整体性贯通滑动面。将理论计算与数值模拟计算结果进行对比发现,利用提出的理论失稳判据条件评价该类边坡的稳定性具有较好的可适用性,为节理边坡岩体稳定性评价与失稳预判提供了一定的理论支持。

     

    Abstract: Based on the two-dimensional plane sliding instability mechanical model of rock slope with bedding intermittent joints,the cusp catastrophe theory model of the instability of jointed slope under gravity stress was established.According to the catastrophe model,the effects of the lengths of intermittent joints (joint connection rate),the inclination angle of joints,the friction angle and cohesion of joints on slope stability were discussed,and the critical instability height of slope was deduced. Then,the criterion conditions of slope instability were put forward. Finally,the finite difference method (FLAC3D) was used to simulate the failure form of rock slope with intermittent joints under the conditions of different joint connection rates and inclination angles. The results show that the greater the joint connection rate and the inclination angle of joint,and the smaller the friction angle and cohesion of joint and the friction angle and cohesion of rock,the higher the possibility of the slope instability. When the connectivity of the joints is small,the rock friction angle and cohesion are the main factors affecting the slope stability. However,with the continuous increase of the connectivity of the joints,the effects of joint friction angle and joint cohesion on slope stability become more and more significant and gradually become the main factors to control the slope stability. Sliding-block toppling mixed progressive failure of the rock slope with bedding intermittent joints occurs under gravity stress and the penetration failure of the joint rock bridge is caused by the propagation of the shear cracks formed at the tip of joints and existing joints. The failure of the lower rock bridges first occurs and the formed shear cracks gradually extend upward,and then form a local or integral sliding surface. By comparing the results of theoretical calculation and numerical simulation,it is found that it is applicable to evaluate the stability of the kind of slope by using the proposed theoretical instability criterion,which provides some theoretical supports for the rock mass stability evaluation and instability prediction of jointed rock slope.

     

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