热源埋藏深度对采空区遗煤传热效能的影响实验研究

Experimental Study on The Influence of Heat Source Burial Depth on Heat Transfer Efficiency of Left Coal in Goaf

  • 摘要: 采空区自然发火作为严重影响煤矿安全生产的因素之一,其发生需满足采空区遗煤堆积这一必要条件,而不同的生产地质条件下,不同埋藏深度时采空区遗煤高温点的传热效果是引发火灾并采取防治措施的关键所在。本文以高传热性能薄皮装煤方箱模拟采空区遗煤堆积,以不同功率恒温热源模拟煤堆内部高温点,利用红外热成像技术探测表面温度变化规律,得出埋藏深度对遗煤传热效能的影响规律。结果表明:热源埋藏深度分别在100~300 mm和500~700 mm之间时,温升速率整体分别呈现出下降和上升趋势,采空区自燃防治过程中应该重点关注的遗煤厚度在300~500mm的区域;热源与煤堆表面温度差距越大,平均温度变化梯度也越大,而对于同一埋藏深度的热源来讲,越靠近热源中心,则煤堆内部的平均温度梯度越小,其在指向煤堆表面的方向上逐渐升高;井下采空区高温区域及其温度实际判定时可根据工作面丢煤图谱进行判定遗煤堆积厚度,进而根据拟合规律关系式得出平均温度梯度值,结合遗煤厚度即可推算出中心高温点温度值,进而采取精准防控措施。

     

    Abstract: Natural spontaneous combustion in goaf areas, as one of the critical factors severely impacting coal mine safety production, requires the essential condition of coal residue accumulation in the goaf. Under varying production geological conditions and at different burial depths, the heat transfer efficiency of hightemperature points in goaf coal residues is pivotal in triggering fires and implementing preventive measures. This study simulates goaf coal residue accumulation using thin-walled coal-filled square boxes with high heat transfer performance, models internal high-temperature points with constant-temperature heat sources of different powers, and employs infrared thermal imaging technology to detect surface temperature variation patterns, thereby revealing the influence of burial depth on coal residue heat transfer efficiency. Results indicate: when the heat source burial depth ranges between 100–300 mm and 500–700 mm, the temperature rise rate generally exhibits decreasing and increasing trends, respectively. During goaf spontaneous combustion prevention, priority should be given to coal residue thickness within the 300–500 mm range. A greater temperature gap between the heat source and coal pile surface corresponds to a larger average temperature gradient. For heat sources at the same burial depth, the closer to the heat source center, the higher the average temperature gradient inside the coal pile, which gradually decreases toward the surface direction. For underground goaf high-temperature zones and their actual temperature assessment, the coal residue accumulation thickness can be determined based on the working face coal loss diagram. Subsequently, the average temperature gradient value can be derived from the fitted correlation relationship, and combined with the coal residue thickness, the temperature of the central high-temperature point can be calculated to implement precise prevention measures.

     

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