冲击地压矿井典型微震信号特征及其判识研究

Characteristics and recognition of typical microseismic signals in rock burst mines

  • 摘要: 准确识别微震信号的类型对于冲击地压矿井动力灾害监测预警与防控具有重要意义。以冲击地压矿井南屯煤矿为工程背景,划分了矿震、爆破、煤岩体破裂、敲击和噪声5种类型微震信号,建立了5种信号类型的样本数据库,分析了最大振幅、持续时间、主频等微震特征参数,建立了微震事件类型的BP神经网络判识模型。研究结果表明:矿震事件与煤层上方高位坚硬岩层破断有关,其能量一般不低于105 J,可触发矿井半数以上传感器,事件具有高最大振幅和高平均振幅的特征(阈值为3×10−4 m/s),持续时间一般在6 s以内、主频一般小于10 Hz;爆破事件能量一般不低于104 J,可触发矿井半数以上传感器,事件具有高最大振幅和高平均振幅的特征,持续时间一般小于2 s;煤岩体破裂事件与采场顶板周期破裂有关,其事件能量一般不高于104 J,可触发矿井40%~65%传感器,该事件具有低最大振幅和低平均振幅的特征,持续时间主要0~1 s、主频分布较为均匀;敲击事件与人为测试有关,其触发传感器数量一般在4个以内,该事件具有高最大振幅和低平均振幅的特征,持续时间较长、主频在0~80 Hz内均匀分布;噪声事件与电磁干扰等相关,绝大多数微震传感器发生无序震动,其触发传感器一般小于6个,该事件具有低最大振幅和低平均振幅的特征,持续时间长、主频不固定。建立的BP神经网络判识模型准确率达88.3%,该方法误判率低,特征参数易获取,为冲击地压矿井微震事件快速准确识别提供了一个新途径。

     

    Abstract: Accurately identifying the type of microseismic signals is of great significance for monitoring, warning, and preventing dynamic disasters in rockburst mines. Leveraging the engineering context of Nantun coal mine, we classify five types of microseismic signals, namely mine earthquakes, blasting, coal-rock fractures, knocking, and noise. We establish a sample database comprising five types of microseismic signals. We analyze the parameters of microseismic events, including maximum amplitude, duration, and main frequency, and develop a BP neural network prediction model for microseismic event types. The results indicate that mine earthquake events are associated with the fracturing of high-hardness rock above the coal seam, and their energy generally exceeds 105 J, which can trigger more than half of the sensors. These events are characterized by high maximum amplitude and high average amplitude (with a threshold of 3×10−4 m/s). Their duration typically does not exceed 6 seconds, and the main frequency is generally below 10 Hz. Blasting events typically have energy levels of not less than 104 J, capable of triggering more than half of the sensors in the mine. These events exhibit high maximum amplitude and high average amplitude, with durations generally less than 2 seconds. Coal-rock fracture events are associated with the periodic rupture of strata, and their energy typically does not exceed 104 J, triggering between 40% and 65% of mine sensors. These events are characterized by low maximum amplitude and low average amplitude, with durations ranging from 0 to 1 seconds, and a relatively uniform distribution of main frequencies. Knocking events are associated with human testing and typically trigger fewer than 4 sensors. These events exhibit high maximum amplitude and low average amplitude, long duration, and a uniform main frequency distribution within the 0-80 Hz range. Noise events are related to electromagnetic interference and other factors. Most microseismic sensors experience erratic vibrations, with generally fewer than 6 sensors being triggered. These events are characterized by low maximum amplitude, low average amplitude, extended duration, and irregular main frequency. The established BP neural network prediction model achieves an accuracy rate of 88.3%. The method boasts a low misjudgment rate and ease of obtaining characteristic parameters, offering a novel approach for rapidly and accurately identifying microseismic events in rock burst mines.

     

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