基于微震监测技术的岩爆预警研究
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  • 英文篇名:Research on Early Warning of Rock Burst Based on Microseismic Monitoring Technology
  • 作者:黄志平 ; 唐春安 ; 李立民 ; 张鹏海
  • 英文作者:HUANG Zhiping;TANG Chun'an;LI Limin;ZHANG Penghai;School of Civil Engineering,Shenyang Jianzhu University;School of Civil Engineering Dalian University of Technology;China Railw ay First Survey and Design Instirute Co.,Ltd.;Center for Rock Instability and Seismicity Research,Northeastern University;
  • 关键词:微震监测 ; 预警机制 ; 深埋隧洞 ; 岩爆 ; 前兆特征
  • 英文关键词:microseismic monitoring;;early warning mechanism;;deep buried tunnel;;rock burst;;precursory characteristics
  • 中文刊名:SYJZ
  • 英文刊名:Journal of Shenyang Jianzhu University(Natural Science)
  • 机构:沈阳建筑大学土木工程学院;大连理工大学土木工程学院;中铁第一勘察设计集团有限公司;东北大学岩石破裂与失稳研究所;
  • 出版日期:2018-07-15
  • 出版单位:沈阳建筑大学学报(自然科学版)
  • 年:2018
  • 期:v.34;No.175
  • 基金:国家自然科学基金项目(51604175);; 中国博士后科学基金项目(2016M601338);; 秦岭输水隧洞越岭段岩爆微震监测技术服务项目(TYY-2017-WZJC-1)
  • 语种:中文;
  • 页:SYJZ201804006
  • 页数:9
  • CN:04
  • ISSN:21-1578/TU
  • 分类号:44-52
摘要
目的通过微震监测系统(MMS)对锦屏二级水电站施工排水洞进行微震监测,对比分析"11·28"极强岩爆灾害实际情况与微震监测结果,探讨岩爆发生的前兆特征及预警预报方法.方法首先对监测隧洞复杂条件下进行微震系统构建,然后进行数据采集、信号过滤与分析,总结微震事件多种指标演化规律.结果提出"多指标、多步骤"综合评价强岩爆、极强岩爆微震预警机制:第一步,确定有效数据,事件数10次/d,能量0.1 k J/次、位置距离临空面小于10 m;第二步,事件聚集度;第三步,突增事件,超过50次/d,能量超过10 k J/次、累积能量超过100 k J/次,是极强岩爆前兆.结论发生强、极强岩爆前具有明显微破裂前兆特征,微震事件空间分布规律由无序、随机分散向有序、集中自组织演变;有效微震事件数目、集中程度、单个事件能量大小及其累计能量释放速率等多个指标是强、极强岩爆预警机制的重要依据.
        It aims to explore the precursory characteristics and early warning method of rockburst,the microseismic monitoring system MMS was used to monitoring the construction drainage tunnel in Jinping Ⅱ hydropower station,by comparing the"11·28"strong rockburst disaster situation and microseismic monitoring results. First,microseismic monitoring system is set up under complexconditions of construction drainage tunnel,then data acquisition and signal filtering and analysis are carried out,the various indicators of microseismic events are summarized. The results showthat "multi-index and multi-steps comprehensive evaluation" is presented as early warning mechanism of strong rockburst and pole-strength rockburst. First step,effective datas are determined which number of events are more than 10 times/d,and energy is more than 0. 1 k J/time,and events distances is less than 10 m from free surface. Second step,event aggregation degree is observed. Third step,when events suddenly increase,the precursor of strong rockburst is judged by the fact which number of events are more than 50 times/d,energy is more than 10 k J/time,and accumulative energy is more than 100 k J/time. The following conclusions are obtained: a lot of obvious micro-rupture precursors arise before rockburst. Spatial distribution lawof microseismic events is subjected from disorder,random distribution to the regional distribution with the increase of microseismic events,and from disorder to order dispersion concentration of self-organization evolution. The analysis of a number of quantitative indicators is adopted according to the number of microseismic events every day,spatial distance away from excavating face,concentration degree,energy released even in per unit time,accumulative energy release rate. Where the basis for the prediction of strong or pole-strong rockburst is provided.
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