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近直立煤层冲击危险静动态评价方法研究

陈建强, 宋大钊, 常博, 李振雷, 潘鹏志, 兰世瑞, 朱红伟, 杨华康

陈建强,宋大钊,常 博,等. 近直立煤层冲击危险静动态评价方法研究[J]. 煤炭科学技术,2023,51(9):24−34. DOI: 10.12438/cst.2022-1256
引用本文: 陈建强,宋大钊,常 博,等. 近直立煤层冲击危险静动态评价方法研究[J]. 煤炭科学技术,2023,51(9):24−34. DOI: 10.12438/cst.2022-1256
CHEN Jianqiang,SONG Dazhao,CHANG Bo,et al. Static-dynamic rockburst risk assessment method in near-vertical coal seams[J]. Coal Science and Technology,2023,51(9):24−34. DOI: 10.12438/cst.2022-1256
Citation: CHEN Jianqiang,SONG Dazhao,CHANG Bo,et al. Static-dynamic rockburst risk assessment method in near-vertical coal seams[J]. Coal Science and Technology,2023,51(9):24−34. DOI: 10.12438/cst.2022-1256

近直立煤层冲击危险静动态评价方法研究

基金项目: 

国家自然科学基金资助项目(51904019,52011530037)

详细信息
    作者简介:

    陈建强: (1970—),男,山东临沂人,教授级高级工程师。E-mail:499234655@qq.com

    通讯作者:

    李振雷: (1988—),男,山东菏泽人,副教授。E-mail:lizhenlei@ustb.edu.cn

  • 中图分类号: TD324

Static-dynamic rockburst risk assessment method in near-vertical coal seams

Funds: 

National Natural Science Foundation of China(51904019,52011530037)

  • 摘要:

    现有冲击地压危险评价方法以采掘前揭露的地质条件和开采技术条件为依据,属于静态评价,评价结果与真实情况存在差距,如何与采掘过程中的监测数据相结合得到更加符合实际的评价结果是需要进一步解决的问题。为此,综合地质及开采条件和监测数据,提出了一种冲击地压危险静动态耦合评价方法,并在典型近直立煤层工作面进行了应用。首先,通过改进综合指数法提出工作面采掘前静态评价方法,包括将综合指数法包含的评价指标进行线性归一化得到单指标危险指数,利用层次分析法对各评价指标赋权,通过加权求和分别得到地质因素和开采技术因素确定的危险指数,然后将两个危险指数加权平均得到静态评价危险指数;其次,利用监测数据构建了采掘过程中动态评价方法,包括根据微震和钻孔应力监测特点及其与冲击危险性的关系,构建了微震能量密度和钻孔应力变化率作为动态评价指标,将评价指标线性归一化分别得到震动场评价指数和应力场评价指数,将两者加权平均得到动态评价危险指数;最后,利用加权平均法将静态评价危险指数和动态评价危险指数进行耦合叠加得到耦合评价危险指数,根据该指数来确定危险等级和危险区域。上述方法在乌东煤矿+450B3+6工作面的应用结果显示,静态评价方法在工作面回采前划定4个中等冲击危险区和1个弱冲击危险区,动态评价方法判定工作面回采过程中岩柱侧具有较高冲击危险性,静动态耦合评价将静态评价的部分弱冲击危险区再评价为中等冲击危险区;通过工作面回采过程的支架压力监测数据、数值模拟结果和冲击地压显现事件对评价结果进行了检验,发现静动态耦合评价结果更符合现场实际。研究成果为冲击地压危险评价提供了一种新方法和新思路。

    Abstract:

    The existing rockburst risk assessment methods generally belong to static assessment method which normally depends on the geological and mining conditions that are revealed prior to mining. There is commonly a certain gap between the assessment results and the real situation. How to combine with the monitoring data in the mining process to get more realistic evaluation results is a problem that needs to be further solved. To this end, this work proposes a static-dynamic coupling rockburst risk assessment method taking into account the geological and mining conditions as well as the monitoring data, and the method has been being applied in typical panels in near-vertical coal seams. Firstly, a static evaluation method used before mining based on the improved comprehensive index method is proposed. The evaluation indicators contained in the comprehensive index method are linearly normalized to obtain the single indicator risk index. The AHP method is used to assign weights to each evaluation indicator, and the weighted summation of all indicator risk indexes is calculated to obtain the risk indexes determined by geological factors and mining technology factors, respectively. Then the weighted mean of the two risk indexes is used as the static evaluation risk index. Secondly, a dynamic evaluation method used during mining by utilizing the monitoring data is constructed. According to the characteristics of microseismic monitoring and borehole stress monitoring and their relationship with rockburst risk, the dynamic evaluation indicators are constructed based on the microseismic energy density and borehole stress variation. The evaluation indicators are linearly normalized to obtain two evaluation indexes. The weighted mean of the two indexes is used as the dynamic evaluation risk index. Finally, the two proposed methods are combined to get a static-dynamic coupling evaluation model. The coupling evaluation risk index is obtained by weighted average of the static evaluation risk index and the dynamic evaluation risk index, and then the risk grade and risk area are determined. The method is applied in +450B3+6 panel of Wudong Coal Mine. Results show that the static evaluation method demarcates 4 medium risk areas and 1 weak risk area before the mining of the panel, the dynamic evaluation method determines that the rock pillar side has high risk level in the mining process of the panel, and the static dynamic coupling evaluation re-evaluates the weak risk area of the static evaluation to the medium risk area. By investigating the monitoring data of support pressure, the numerical simulation results and the rockburst occurrence on site during the mining process of the panel, the evaluation results are verified, and it is found that the static and dynamic coupling evaluation results are more consistent with the actual situation. This work provides a new method and a new idea for the risk assessment of rock burst.

  • 图  1   乌东煤矿南区各水平工作面示意

    Figure  1.   Diagram of the working face at each level in the South Area of Wudong Mine

    图  2   冲击危险性静态评价模型流程示意

    Figure  2.   Diagram of the rockburst static evaluation model process

    图  3   +450B3+6工作面区域对照

    Figure  3.   +450B3+6 Workface area comparison

    图  4   +450B3+6工作面冲击危险性区域划分结果

    Figure  4.   Rock burst hazard zone results of +450B3+6 Working Face

    图  5   +450B3+6工作面冲击地压危险性动态评价结果

    Figure  5.   Results of dynamic evaluation of the rockburst hazard on the +450B3+6 Working Face

    图  6   +450B3+6面冲击地压静动态耦合危险性评价结果

    Figure  6.   +450B3+6 Working Face rockburst static and dynamic coupling hazard evaluation results

    图  7   +450B3+6工作面支架压力分布

    Figure  7.   +450B3+6 Working Face support pressure distribution

    图  8   +450B3+6工作面开采过程围岩应力分布

    Figure  8.   +450B3+6 mining process stress distribution of the surrounding rock

    表  1   冲击地压危险静态评价危险分级

    Table  1   Static evaluation risk classification of rock burst hazard

    冲击危险等级冲击危险状态综合危险指数Wj
    I<0.25
    II0.25~0.50
    III中等0.50~0.75
    IV>0.75
    下载: 导出CSV

    表  2   不同区域冲击危险指标因素及权重对照

    Table  2   Comparison of factors and weights for each indicator of rockburst in different regions

    区域参数A参数B
    参数危险性指数权重参数危险性指数权重
    A1 0.66 0.14 B1 0 0.24
    A2 0.54 0.20 B2 0.50 0.22
    A3 0.53 0.19 B3 0.98 0.17
    A4 0.98 0.12 B4 1.00 0.13
    A5 0.53 0.12 B5 1.00 0.09
    A6 0 0.07 B6 1.00 0.15
    A7 1.00 0.16
    区域②A1 0.66 0.16 B1 0.33 0.21
    A2 0.54 0.18 B2 0.50 0.16
    A3 0.53 0.18 B3 0.87 0.17
    A4 0.98 0.12 B4 0 0.22
    A5 0.53 0.21 B5 1.00 0.12
    A6 0 0.07 B6 1.00 0.12
    A7 1.00 0.08
    区域③ A1 0.66 0.17 B1 0.33 0.19
    A2 0.54 0.12 B2 0.50 0.24
    A3 0.53 0.15 B3 0.87 0.08
    A4 0.98 0.19 B4 0 0.14
    A5 0.53 0.22 B5 1.00 0.13
    A6 0 0.07 B6 1.00 0.22
    A7 1.00 0.08
    区域④ A1 0.66 0.11 B1 0 0.16
    A2 0.54 0.15 B2 0.50 0.18
    A3 0.53 0.17 B3 0.98 0.09
    A4 0.98 0.09 B4 1.00 0.16
    A5 0.53 0.16 B5 1.00 0.19
    A6 0 0.14 B6 1.00 0.22
    A7 1.00 0.18
    区域⑤ A1 0.66 0.17 B1 0 0.22
    A2 0.54 0.07 B2 0.50 0.15
    A3 0.23 0.20 B3 0.87 0.24
    A4 0.98 0.13 B4 0.50 0.16
    A5 0.53 0.14 B5 0.66 0.11
    A6 0 0.20 B6 0.33 0.12
    A7 1.00 0.09
    下载: 导出CSV

    表  3   +450B3+6工作面不同区域冲击危险性综合指数

    Table  3   Combined index of rockburst for different regions of the +450B3+6 Working Face

    区域地质因素指数开采技术因素指数综合指数冲击危险性
    区域①0.6420.6470.64中等
    区域②0.6070.5370.57中等
    区域③0.6390.6020.62中等
    区域④0.5970.7480.67中等
    区域⑤0.4880.4760.48
    下载: 导出CSV

    表  4   微震危险性系数与冲击危险等级对照

    Table  4   Comparison between microseismic risk index and rockburst risk level

    危险等级危险状态微震危险性系数
    I无冲击危险Rw<0.25
    II弱冲击危险0.25≤Rw<0.50
    III中等冲击危险0.50≤Rw<0.75
    IV强冲击危险0.75≤Rw<1
    下载: 导出CSV

    表  5   应力危险性系数与冲击危险等级对照

    Table  5   Comparison between stress risk index and rockburst risk level

    危险等级危险状态应力危险性系数
    I无冲击危险Rl<0.25
    II弱冲击危险0.25≤Rl<0.50
    III中等冲击危险0.50≤Rl<0.75
    IV强冲击危险0.75≤Rl<1
    下载: 导出CSV

    表  6   冲击危险性动态评价危险分级

    Table  6   Risk classification for dynamic evaluation of rockburst

    危险等级危险状态冲击危险综合指数Wd
    I无冲击危险<0.25
    II弱冲击危险0.25~0.50
    III中等冲击危险0.50~0.75
    IV强冲击危险>0.75
    下载: 导出CSV

    表  7   静动态耦合冲击危险分级指标

    Table  7   Static and dynamic coupling rockburst classification index

    危险等级危险状态耦合危险性指数
    I无冲击危险Wz<0.25
    II弱冲击危险0.25≤Wz<0.50
    III中等冲击危险0.50≤Wz<0.75
    IV强冲击危险0.75≤Wz<1
    下载: 导出CSV
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出版历程
  • 收稿日期:  2022-08-04
  • 网络出版日期:  2023-07-30
  • 刊出日期:  2023-09-18

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