深部硐室长期稳定性的两个力学问题

王明洋 徐天涵 邓树新 陈昊祥

王明洋, 徐天涵, 邓树新, 陈昊祥. 深部硐室长期稳定性的两个力学问题[J]. 爆炸与冲击, 2021, 41(7): 071101. doi: 10.11883/bzycj-2021-0023
引用本文: 王明洋, 徐天涵, 邓树新, 陈昊祥. 深部硐室长期稳定性的两个力学问题[J]. 爆炸与冲击, 2021, 41(7): 071101. doi: 10.11883/bzycj-2021-0023
WANG Mingyang, XU Tianhan, DENG Shuxin, CHEN Haoxiang. Mechanical problems for the long-term stability of rocks surrounding deep level underground tunnels[J]. Explosion And Shock Waves, 2021, 41(7): 071101. doi: 10.11883/bzycj-2021-0023
Citation: WANG Mingyang, XU Tianhan, DENG Shuxin, CHEN Haoxiang. Mechanical problems for the long-term stability of rocks surrounding deep level underground tunnels[J]. Explosion And Shock Waves, 2021, 41(7): 071101. doi: 10.11883/bzycj-2021-0023

深部硐室长期稳定性的两个力学问题

doi: 10.11883/bzycj-2021-0023
基金项目: 国家自然科学基金重大科研仪器研制项目(51527810);国家自然科学基金青年科学基金(51909120)
详细信息
    作者简介:

    王明洋(1966- ),男,博士,教授,博士生导师,wmyrf@163.com

    通讯作者:

    徐天涵(1995- ),男,博士研究生,martinxu41@126.com

  • 中图分类号: O389; TD322

Mechanical problems for the long-term stability of rocks surrounding deep level underground tunnels

  • 摘要: 在陈宗基院士关于地下硐室长期稳定性力学问题研究的基础上,采用Sadovsky院士关于复杂地质岩体的等级构造学说,围绕深部岩体非均匀构造与封闭应力固有的统计力学属性,研究了岩体非均匀变形与封闭应力特性,以及深部硐室围岩的长期稳定性等两个力学问题。给出了岩体非均匀构造与封闭应力的数学表征;根据质量守恒定律得到了计算深部硐室围岩长期变形的一般公式;得到了围岩变形中劈裂扩容变形占主要部分的结论,并且阐明了深部围岩卸荷时更易出现劈裂破坏的原因。给出了劈裂破坏形态的演进序列与扩容位移的计算方法。将围岩松动圈范围、破裂区位置和边壁位移的计算结果与锦屏一级电站厂房现有监测数据进行了对比,两者相当吻合。
  • 图  1  岩体的构造等级示意图

    Figure  1.  Sketch of hierarchical structure of rock blocks

    图  2  n级非均匀构造单元的变形阶段

    Figure  2.  The deformation stages of the nth non-uniform structure

    图  3  硐室开挖前后侧墙围岩应力状态的变化[1]

    Figure  3.  The change of stress state of surrounding rocks before and after the tunneling[1]

    图  4  硐室开挖前后侧墙围岩应力圆[1]

    Figure  4.  The stress circles of surround rocks before and after the tunneling

    图  5  三向应力状态时的强度准则

    Figure  5.  Strength criterion at triaxial stress state

    图  6  锦屏大理岩真三轴实验结果

    Figure  6.  The true triaxial test results of the marble in Jinping.

    图  7  体积变形与剪切变形的关系

    Figure  7.  The relationship between bulk and shear deformations

    图  8  塑性区围岩位移示意图

    Figure  8.  The deformation of surrounding rocks in the plastic zone

    图  9  地下硐室围岩劈裂示意图[1]

    Figure  9.  The schematic diagram of spalling of rocks surrounding deep level tunnels[1]

    图  10  深部围岩劈裂示意图

    Figure  10.  The splitting of deep surrounding rocks

    图  11  深部围岩分区破裂示意图

    Figure  11.  Diagram of zonal disintegration of deep surrounding rocks

    图  12  分区破裂半径计算与监测结果对比[25]

    Figure  12.  A comparison between the in-situ and theoretical radii of zonal disintegration[25]

    表  1  分区破裂区半径ci/a与能量因子k之间的关系[25]

    Table  1.   The relationship between the radii of zonal disintegration ci/a and the energy factor k[25]

    ci/ak
    exp(1/2)1.4×10−6
    exp(1)1.0×10−7
    exp(3/2)1.0×10−8
    exp(2)1.4×10−9
    下载: 导出CSV

    表  2  围岩变形理论与现场实测结果对比

    Table  2.   Comparison of the theoretical and in-situ results

    硐室等效半径/mψΔ理论扩容变形/mm理论剪切变形/mm理论总变形/mm实测变形/mm
    主变室[18]14.170.5×10−2 60.937.0 97.9233.4
    1.0×10−2121.7158.7
    1.5×10−2182.6219.6*
    2.0×10−2243.5280.5
    主厂房[17]23.820.5×10−2102.362.2164.5上游220.0
    下游247.0
    1.0×10−2204.6266.8*
    1.5×10−2307.0369.2
    2.0×10−2409.3471.5
    尾调室[17]17.50 0.5×10−2 75.245.7120.9*125.0
    1.0×10−2150.3196.0
    1.5×10−2225.5271.2
    2.0×10−2300.7346.4
     注:表中数据加*号的阶段为与实际最接近的变形阶段。
    下载: 导出CSV
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  • 收稿日期:  2021-01-18
  • 修回日期:  2021-04-27
  • 网络出版日期:  2021-06-17
  • 刊出日期:  2021-07-05

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