中国安全科学学报 ›› 2026, Vol. 36 ›› Issue (S1): 67-74.doi: 10.16265/j.cnki.issn1003-3033.2026.S1.0011

• 安全技术与工程 • 上一篇    下一篇

近直立特厚煤层破坏过程声电特征研究

闫瑞兵1(), 李康1, 蒋新军1, 宋大钊2, 杜涛涛3   

  1. 1 国能新疆能源化工有限公司, 新疆 乌鲁木齐 830027
    2 北京科技大学 资源与安全工程学院, 北京 100083
    3 中煤科工开采研究院有限公司, 北京 100013
  • 收稿日期:2026-02-05 修回日期:2026-05-10 出版日期:2026-06-30
  • 作者简介:

    闫瑞兵 (1992—),男,陕西西安人,硕士,高级工程师,主要从事矿山压力与灾害防治方面的工作。E-mail:。

    李 康 高级工程师

    蒋新军 高级工程师

    宋大钊 教授

    杜涛涛 研究员

AE and EMR characteristics of failure process of near vertical extra-thick coal seam

Yan Ruibing1(), Li Kang1, Jiang Xinjun1, Song Dazhao2, Du Taotao3   

  1. 1 CHN Energy Group Xinjiang Energy Chemical Co., Ltd., Urumqi Xinjiang 830027, China
    2 School of Resources and Safety Engineering, University of Science and Technology Beijing, ;Beijing 100083, China
    3 CCTEG Coal Mining Research Institute, Beijing 100013, China
  • Received:2026-02-05 Revised:2026-05-10 Published:2026-06-30

摘要:

针对近直立特厚煤层冲击地压以帮鼓为主、现有声电前兆判据多基于近水平/缓倾斜煤层适用性不足的问题,以乌东煤矿倾角87°、平均厚48.87 m的近直立特厚煤层为对象,开展煤岩单轴压缩同步声发射(AE)-电磁辐射(EMR)试验及现场地音、微震(MS)、EMR多参量监测,并与其他典型煤层跨倾角对比。结果表明:实验室尺度AE-EMR幅值与应力正相关,岩样信号集中度高于煤样;冲击显现前,小时级地音能量、脉冲数呈M型双峰演化,峰值达103 J级;天级微震能量、频次呈V型前兆,峰值达105 J级,冲击当日骤升至107 J级;EMR强度随距工作面距离的变化呈M型分布,高值区位于10~30及70 m,煤层EMR强度较顶底板高20%~35%,与帮鼓特征吻合。近直立特厚煤层微震频次与其他煤层相近,但能量V型演化模式显著不同。

关键词: 近直立特厚煤层, 冲击地压, 声发射(AE), 微震, 电磁辐射(EMR)

Abstract:

To address the problems that rock bursts in near vertical extra-thick coal seams are dominated by side heave and that existing acoustic-electromagnetic precursor criteria are mostly derived from near-horizontal or gently inclined coal seams with insufficient applicability, with the near vertical extra-thick coal seam of Wudong Coal Mine (dip angle 87°, average thickness 48.87 m) as the research object, synchronous uniaxial compression experiments combining AE and EMR were conducted on coal and rock samples, together with field multi-parameter monitoring of geoacoustic (GA), microseismic (MS), and EMR signals. Comparisons were also made with other typical coal seams at different dip angles. The results show that at the laboratory scale, AE-EMR amplitudes are positively correlated with stress, and the signal concentration of rock samples is higher than that of coal samples. Before the rock burst occurrence, the hourly GA energy and pulse count exhibit an M-shaped double-peak evolution, with the peak energy reaching the order of 103 J. The daily MS energy and frequency show a V-shaped precursor, with the peak energy reaching the order of 105 J, surging to 107 J on the day of rock burst. The EMR intensity presents an M-shaped distribution with increasing distance from the working face, with high-value zones located at 10-30 m and 70 m. The EMR intensity of the coal seam is 20%-35% higher than those of the roof and floor, consistent with the side heave characteristics. The MS frequency of the near vertical extra-thick coal seam is similar to those of other coal seams, whereas the V-shaped evolution pattern of MS energy is significantly distinct.

Key words: near vertical extra-thick coal seam, rock burst, acoustic emission (AE), microseism, electromagnetic radiation (EMR)

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