爆破振动作用下含软弱夹层边坡稳定性及安全判据

马冲 詹红兵 姚文敏 余海兵

马冲, 詹红兵, 姚文敏, 余海兵. 爆破振动作用下含软弱夹层边坡稳定性及安全判据[J]. 爆炸与冲击, 2018, 38(3): 563-571. doi: 10.11883/bzycj-2016-0275
引用本文: 马冲, 詹红兵, 姚文敏, 余海兵. 爆破振动作用下含软弱夹层边坡稳定性及安全判据[J]. 爆炸与冲击, 2018, 38(3): 563-571. doi: 10.11883/bzycj-2016-0275
MA Chong, ZHAN Hongbing, YAO Wenmin, YU Haibing. Stability and safety criterion of a slope with weak interlayer under blasting vibration[J]. Explosion And Shock Waves, 2018, 38(3): 563-571. doi: 10.11883/bzycj-2016-0275
Citation: MA Chong, ZHAN Hongbing, YAO Wenmin, YU Haibing. Stability and safety criterion of a slope with weak interlayer under blasting vibration[J]. Explosion And Shock Waves, 2018, 38(3): 563-571. doi: 10.11883/bzycj-2016-0275

爆破振动作用下含软弱夹层边坡稳定性及安全判据

doi: 10.11883/bzycj-2016-0275
基金项目: 

国家自然科学基金项目 41672317

详细信息
    作者简介:

    马冲(1984-), 男, 博士, 讲师

    通讯作者:

    詹红兵, zhan@geos.tamu.edu

  • 中图分类号: O389;TU457

Stability and safety criterion of a slope with weak interlayer under blasting vibration

  • 摘要: 运用FLAC3D软件建立了顺层台阶边坡数值模型,首先分析爆破振动作用下边坡的振速响应规律,然后通过边坡的位移、剪应变增量分析其稳定性,最后根据边坡稳定性判据,制定爆破振速安全阈值。研究表明,随着爆心距的增大,振速传播规律为近处衰减快、远处衰减慢,坡面存在高程放大效应,临空面中由于软弱夹层的阻隔影响,使得坡脚的振速最大;边坡的变形破坏受软弱夹层控制,其上覆岩体为潜在滑体,破裂面可以根据水平位移云图和塑性区分布图综合确定;边坡的破坏是一个渐进性的累积过程,位移和剪应变的累积会导致岩体的力学参数不断弱化,爆破振动劣化作用后仍有较大安全储备的边坡只会累积产生永久位移,而接近极限平衡状态的边坡将会失稳;当岩层倾角为15°~23°时,边坡振速安全阀值为21 cm/s;当软弱夹层剪出口距离坡顶高度为14 m,倾角分别为24°、29°、31°、34°时,安全阀值分别为10、8、6、5 cm/s。
  • 图  1  矿山现场照片

    Figure  1.  Local pictures of mine

    图  2  边坡动力分析模型和监测点位置分布

    Figure  2.  Dynamic numerical simulation model of the slope and location distribution of monitoring points

    图  3  N1水平和垂直速度曲线与输入波形的比较

    Figure  3.  Horizontal and vertical velocity curves at N1 compared with input wave curves

    图  4  不同时刻的水平速度云图

    Figure  4.  Contour maps of horizontal velocity at different times

    图  5  监测点主振速度

    Figure  5.  Maximum velocity amplitudes of monitoring points

    图  6  爆破后水平位移云图和塑形区分布

    Figure  6.  Plastic zones and horizontal displacement of slope after blasting

    图  7  监测点水平向位移时程曲线

    Figure  7.  Horizontal displacement-time curves of monitoring points

    图  8  监测单元剪应变增量时程曲线

    Figure  8.  Shear-strain increment-time curves of key elements

    图  9  监测点水平向位移时程曲线

    Figure  9.  Time-dependent curves of horizontal displacement of monitoring points

    图  10  监测单元剪应变增量时程曲线

    Figure  10.  Time-dependent curves of shear-strain increment of key elements

    图  11  监测点N7的水平向位移时程曲线

    Figure  11.  Time-dependent curves of horizontal displacement at N7

    图  12  边坡的稳定性系数

    Figure  12.  Stability coefficient of slope

    图  13  塑性区分布图和水平位移云图

    Figure  13.  Plastic zones and horizontal displacement of slope

    图  14  软弱夹层倾角与安全阈值的关系

    Figure  14.  Relationship of weak interlayer inclination and safety threshold

    表  1  物理力学参数

    Table  1.   Physico-mechanical parameters of rock mass

    岩体弹性模量/GPa泊松比内聚力/MPa内摩擦角/(°)重度/(kN·m-3)抗拉强度/MPa
    灰岩70.21.53526.81
    夹层(天然)0.680.30.0429200.016
    夹层(残余)0.680.30.0122200.016
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出版历程
  • 收稿日期:  2016-09-09
  • 修回日期:  2016-12-15
  • 刊出日期:  2018-05-25

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