爆破扰动下TBM隧洞时滞型岩爆特征及影响机制研究

全永威, 王军, 熊永润, 姚志宾, 张宇, 胡磊. 爆破扰动下TBM隧洞时滞型岩爆特征及影响机制研究[J]. 水文地质工程地质, 2023, 50(1): 94-103. doi: 10.16030/j.cnki.issn.1000-3665.202202042
引用本文: 全永威, 王军, 熊永润, 姚志宾, 张宇, 胡磊. 爆破扰动下TBM隧洞时滞型岩爆特征及影响机制研究[J]. 水文地质工程地质, 2023, 50(1): 94-103. doi: 10.16030/j.cnki.issn.1000-3665.202202042
QUAN Yongwei, WANG Jun, XIONG Yongrun, YAO Zhibin, ZHANG Yu, HU Lei. A study of the characteristics and influence mechanism of time delayed rockburst in a TBM tunnel under the blasting disturbance[J]. Hydrogeology & Engineering Geology, 2023, 50(1): 94-103. doi: 10.16030/j.cnki.issn.1000-3665.202202042
Citation: QUAN Yongwei, WANG Jun, XIONG Yongrun, YAO Zhibin, ZHANG Yu, HU Lei. A study of the characteristics and influence mechanism of time delayed rockburst in a TBM tunnel under the blasting disturbance[J]. Hydrogeology & Engineering Geology, 2023, 50(1): 94-103. doi: 10.16030/j.cnki.issn.1000-3665.202202042

爆破扰动下TBM隧洞时滞型岩爆特征及影响机制研究

详细信息
    作者简介: 全永威(1980-),男,本科,高级工程师,主要从事水利工程建设管理方面的研究。E-mail:89219636@qq.com
    通讯作者: 胡磊(1988-),男,博士,讲师,主要从事岩爆机理、监测、预警与防控方面的研究。E-mail:hulei@mail.neu.edu.cn
  • 中图分类号: U452.1+1;U459.6

A study of the characteristics and influence mechanism of time delayed rockburst in a TBM tunnel under the blasting disturbance

More Information
  • 时滞型岩爆的发生通常具有很强的随机性,会对施工安全造成巨大的威胁,而开挖扰动、爆破扰动等均会对潜在时滞型岩爆区产生不同程度的影响。依托某隧道掘进机(TBM)引水隧洞,采用理论分析和对比分析法研究了拆机洞爆破开挖期间K54+000—K54+700段发生的5次时滞型岩爆,发现:(1)强烈岩爆和中等岩爆区位于缓倾断层附近,围岩发育短小隐节理和含充填的细密节理,轻微岩爆距断层远或位于正断层附近,除含充填的细密节理外,均至少发育1条含充填物的倾向SW的陡倾结构面;(2)TBM法开挖隧洞时滞型岩爆滞后爆破时间更长,滞后工作面距离更远,且爆破对TBM隧洞的扰动作用相对较小;(3)爆破扰动使得潜在时滞型岩爆区围岩失稳变得容易,从而加速了时滞型岩爆的进程。研究成果可为TBM隧洞时滞型岩爆的预警与防控提供参考。

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  • 图 1  拆机洞纵断面图及横断面图

    Figure 1. 

    图 2  地应力与隧洞的空间关系

    Figure 2. 

    图 3  K54+000—K54+700段即时型岩爆分布示意图

    Figure 3. 

    图 4  K54+000—K54+700段地质展布图

    Figure 4. 

    图 5  K54+000—K54+700段围岩初期支护概况

    Figure 5. 

    图 6  某引水隧洞时滞型岩爆分布示意图

    Figure 6. 

    图 7  时滞型岩爆断面分布情况

    Figure 7. 

    图 8  岩爆区域内的结构面

    Figure 8. 

    图 9  岩爆IV爆堆

    Figure 9. 

    图 10  时滞型岩爆爆坑深度与爆坑中心前后各10 m范围内累计即时型岩爆爆坑深度的关系

    Figure 10. 

    图 11  不同等级时滞型岩爆地质力学模式示意图

    Figure 11. 

    表 1  时滞型岩爆发生信息统计

    Table 1.  Statistics of occurrence information of time delayed rockburst

    岩爆爆坑照片描述
    岩爆Ⅰ发生时间:2021年10月22日
    发生位置:K54+200—K54+213(距工作面769.0 m)
    岩爆等级:强烈岩爆
    爆坑形态:长条深窝型
    爆坑位置:10点钟—2点钟方位
    爆坑尺寸:13 m×6 m×1.2 m(长×宽×深)
    爆坑区域结构面:石英脉+多条灰白色钙质充填细脉
    岩爆前支护措施:随机砂浆锚杆&钢筋网片&混凝土喷层
    岩爆Ⅱ发生时间:2021年10月22日
    发生位置:K54+550—K54+551.2(距工作面430.8 m)
    岩爆等级:轻微岩爆
    爆坑形态:浅窝型
    爆坑位置:9点钟—10点钟方位
    爆坑尺寸:1.2 m×1.5 m×0.1 m(长×宽×深)
    爆坑区域结构面:1条厚0.2~0.4 m的白色钙膜及铁绣色斑充填结构面+多条含钙膜充填的细小节理
    岩爆前支护措施:混凝土喷层
    岩爆Ⅲ发生时间:2021年11月1日
    发生位置:K54+128—K54+131.5(距工作面850.5 m)
    岩爆等级:中等岩爆
    爆坑形态:深窝型
    爆坑位置:9点钟—10点钟方位
    爆坑尺寸:3.5 m×7.5 m ×0.5 m(长×宽×深)
    爆坑区域结构面:大量密集节理,呈共轭相交,伴有白色钙膜充填
    岩爆前支护措施:混凝土喷层
    岩爆Ⅳ发生时间:2021年11月2日
    发生位置:K54+640—K54+642(距工作面340.0 m)
    岩爆等级:轻微岩爆
    爆坑形态:浅窝型,结构面控制边界
    爆坑位置:2点半—4点钟方位
    爆坑尺寸:2.5 m×3.7 m×0.15 m(长×宽×深)
    爆坑区域结构面:1条含5~8 cm墨绿色充填结构面+细小节理集密,伴有钙膜充填
    岩爆前支护措施:混凝土喷层
    岩爆Ⅴ发生时间:2021年11月7日
    发生位置:K54+116—K54+119.5(距工作面862.5m)
    岩爆等级:轻微岩爆
    爆坑形态:V型
    爆坑位置:2点钟—3点半方位
    爆坑尺寸:3.5 m×2.5 m×0.2 m(长×宽×深)
    爆坑区域结构面:2条含充填结构面,厚2~10 cm
    岩爆前支护措施:混凝土喷层
    下载: 导出CSV

    表 2  时滞型岩爆滞后时间及空间信息

    Table 2.  Lag time and spatial information of time delayed rockburst

    岩爆滞后时间及空间岩爆Ⅰ岩爆Ⅱ岩爆Ⅲ岩爆Ⅳ岩爆Ⅴ
    岩爆滞后开挖的天数/d1058111088117
    岩爆滞后拆机洞第二次爆破的天数/d77171823
    岩爆滞后工作面的距离/m769.0430.8850.5340.0862.5
    下载: 导出CSV
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出版历程
收稿日期:  2022-02-04
修回日期:  2022-05-25
录用日期:  2022-05-25
刊出日期:  2023-01-15

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