单轴压缩下煤岩变形破坏中子辐射响应特征初探
Preliminary investigation on neutron emission characteristics during the failure process of coal and rock under uniaxial compression
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摘要: 为探索矿山动力灾害监测新方法, 本文结合中子辐射信号不受电磁干扰等特点, 选取煤、花岗岩和磁铁矿样品开展单轴压缩试验, 同步监测中子辐射与声发射信号, 对煤、岩失稳过程中的中子辐射信号特征进行初探, 探讨煤、岩失稳破坏的中子辐射预警指标。结果表明: 煤、岩在失稳破坏时中子辐射发生显著变化, 表明中子辐射技术具有作为煤、岩失稳监测新方法的潜力; 在受载过程中样品突然破坏时, 铁元素含量较高的样品更易引发中子辐射, 且其幅值与铁元素含量亦相关; 红庆河强冲击倾向性煤样在失稳时中子辐射信号峰值约为测试环境中子辐射背景信号的13.3倍, 而王楼弱冲击性煤样失稳时中子辐射信号强度始终与测试环境背景信号无显著差异。声发射能够连续刻画损伤累积的全过程, 而中子辐射则在宏观失稳临界点呈现突增特征, 二者在时序与物理机制上形成互补。失稳前中子辐射表现为累计值的非线性增长与变异系数的数量级跃迁, 样品临近失稳时, 变异系数曲线均出现显著突增峰值。Abstract: Neutron emission (NE) has the advantage of electromagnetic interference immunity. To explore a new monitoring method for potential application on the forecast of dynamic hazards in mining, the NE characteristics of coal, granite, and magnetite samples were investigated by performing uniaxial compression experiments. Acoustic emission (AE) signals were synchronously monitored in the experimental process. The early warning indicators of coal and rock were discussed based on the acquired NE and AE data. It was found that the NE signals vary enormously during the failure process, which demonstrates its potential to serve as a novel method for monitoring coal and rock instability. Samples with higher iron contents are more prone to induce NE upon sudden failure, and the amplitude of NE is correlated with the iron content. For the strongly burst-prone coal sample from Hongqinghe Coal Mine, the peak NE intensity at instability is approximately 13.3 times the background NE intensity of the test environment. In contrast, for the weakly burst-prone coal sample from Wanglou Coal Mine, it shows no noticeable difference from the background intensity throughout failure. AE can continuously characterize the entire process of damage accumulation, while NE displays a sharp surge at the critical point of macroscopic instability. The two kinds of signals are complementary in terms of time sequence and physical mechanisms. Prior to instability, NE is characterized by the nonlinear growth of cumulative values and an order-of-magnitude jump in the coefficient of variation. When the samples approach instability, all coefficients of variation curves exhibit a significant sudden surge to the peak value.
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