Characteristic microseismicity during the development process of intermittent rockburst in a deep railway tunnel
文献类型：期刊论文
| 作者 | Feng, Guang-Liang; Feng, Xia-Ting ; Xiao, Ya-Xun; Yao, Zhi-Bin; Hu, Lei; Niu, Wen-Jing; Li, Tong
|
| 刊名 | INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES
 |
| 出版日期 | 2019 |
| 卷号 | 124页码:- |
| 关键词 | Rock mechanics Rockburst Microseismicity Warning Deep tunnel |
| ISSN号 | 1365-1609 |
| DOI | 10.1016/j.ijrmms.2019.104135 |
| 英文摘要 | During deep tunnel excavation, more than one rockburst sometimes occur in a particular area which seriously threatens construction safety. In this work, the characteristic microseismicity occurring during the development process of intermittent rockburst (more than one rockburst occurring in a particular area) and single rockburst (only one rockburst occurring in a particular area) and the associated mechanism of formation are studied. Data was collected during the construction of a railway tunnel in southwestern China. Microseismicity was recorded and analyzed before and after each rockburst (for both intermittent and single rockbursts). The Schmidt number declines heavily with time, the cumulative apparent volume rises sharply with time, and the Seismic activity is high before the rockburst. However, this characteristic microseismicity can also be found with no rockburst occurrence. Between each rockburst in an intermittent rockburst, the MS events mostly have low MS energy, i.e. whose logarithm (measured in Joules) is smaller than 3.5, and the energy stored in the rockmass of the rockburst zone is not adequately released. Therefore, there is likely to be another rockburst after the blast when high in situ stress is present. After the last rockburst of an intermittent rockburst and the single rockburst, some MS events of high MS energy, i.e. whose logarithm (measured in Joules) is larger than 3.5, occur in the deep surrounding rockmass and the energy stored in the rockmass of the rockburst zone is gradually released to a certain degree. The stress is transferred to the deep surrounding rockmass whose stability is relatively high. As a result, a subsequent rockburst is hardly likely to occur again. |
| WOS研究方向 | Engineering ; Mining & Mineral Processing |
| 语种 | 英语 |
| WOS记录号 | WOS:000499079300015 |
| 源URL | [http://119.78.100.198/handle/2S6PX9GI/14810]  |
| 专题 | 岩土力学所知识全产出_期刊论文 国家重点实验室知识产出_期刊论文 |
| 作者单位 | 1.Chinese Acad Sci, Inst Rock & Soil Mech, State Key Lab Geomech & Geotech Engn, Wuhan 430071, Hubei, Peoples R China; 2.Northeastern Univ, Minist Educ Safe Min Deep Met Mines, Key Lab, Shenyang 110819, Liaoning, Peoples R China |
| 推荐引用方式 GB/T 7714 | Feng, Guang-Liang,Feng, Xia-Ting,Xiao, Ya-Xun,et al. Characteristic microseismicity during the development process of intermittent rockburst in a deep railway tunnel[J]. INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES,2019,124:-. |
| APA | Feng, Guang-Liang.,Feng, Xia-Ting.,Xiao, Ya-Xun.,Yao, Zhi-Bin.,Hu, Lei.,...&Li, Tong.(2019).Characteristic microseismicity during the development process of intermittent rockburst in a deep railway tunnel.INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES,124,-. |
| MLA | Feng, Guang-Liang,et al."Characteristic microseismicity during the development process of intermittent rockburst in a deep railway tunnel".INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES 124(2019):-. |
入库方式： OAI收割
来源：武汉岩土力学研究所
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