煤自燃特征温度与理化特性参数关联性研究

    Study on correlation between coal spontaneous combustion characteristic temperature and physical and chemical characteristic parameters

    • 摘要: 煤自燃特征阶段精细划分是煤火灾害早期预警体系建立的前提,煤的理化特性参数及其变化规律是确定特征温度和划分自燃阶段的关键。为探究煤自燃特征温度与理化特性参数的关联特性,选取甘肃省陈家沟煤矿长焰煤煤样,制备为不同温度(40、60、80、100、120、140、160、180、200 ℃)的氧化煤,开展了工业分析、扫描电子显微镜测试(SEM)、能量色散X射线光谱分析(EDS)、X射线衍射测试(XRD)、红外光谱分析(FTIR)等试验,研究不同氧化阶段煤样理化特性参数随温度的变化规律,确定陈家沟煤样煤自燃特征温度,结合灰色关联度分析法,进一步明确了关键理化特性参数与煤温的关联程度。结果表明:陈家沟矿煤样自燃进程可根据特征温度划分为临界阶段(40~80 ℃)、热解阶段(80~120 ℃)、裂变阶段(140~180 ℃)3个阶段;煤的理化结构参数对煤自燃过程中特征温度的变化具有不同的影响方式和效果,煤样中微观基团中羟基与亚甲基对特征温度阶段关联度较高,关联度分别为0.67530.6926;在临界、热解阶段煤体表面活性结构与氧气分子发生物理、化学吸附,羟基先与氧气反应蓄热,随着温度升高侧链少量断裂导致亚甲基含量升高,而羟基在不断地消耗中也因其他官能团参与反应不断生成,裂解阶段煤中游离水分蒸发完成,结合水开始蒸发,分子内缔合氢键被加速破坏,煤的孔隙度变大,气体吸附能力增强,各类官能团与氧气反应活性提高,煤自燃进程加快;此外,堆积高度、层片直径与煤堆积的体积、表面形态及稳定性有关,堆积高度、层片直径在煤自燃进程初期与特征温度阶段始终具有较高的关联度(0.6689)。

       

      Abstract: The fine division of coal spontaneous combustion characteristic stage is the premise for the establishment of early warning system of coal fire disaster. The physical and chemical properties of coal and their variation laws are the key to determine the characteristic temperature and divide the spontaneous combustion stages. In order to explore the correlation between the characteristic temperature of coal spontaneous combustion and the physical and chemical properties, the long flame coal samples of Chenjiagou Coal Mine in Gansu Province were selected to prepare oxidized coal at different temperature conditions (40 ℃, 60 ℃, 80 ℃, 100 ℃, 120 ℃, 140 ℃, 160 ℃, 180 ℃, 200 ℃). Industrial analysis, scanning electron microscopy (SEM), energy dispersive X-ray spectroscopy (EDS), X-ray diffraction (XRD) and infrared spectroscopy (FTIR) were carried out to study the changes of physical and chemical parameters of coal samples with temperature in different oxidation stages. The characteristic temperature of coal spontaneous combustion in Chenjiagou coal sample was determined. Combined with the grey correlation analysis method, the correlation between the key physical and chemical parameters and coal temperature was further clarified. The results show that the spontaneous combustion process of coal samples in Chenjiagou Mine can be divided into three stages according to the characteristic temperature, namely, the critical stage (40-80 ℃), the pyrolysis stage (80-120℃) and the fission stage (140-180 ℃). The physical and chemical structure parameters of coal have different effects on the change of characteristic temperature in the process of coal spontaneous combustion. The correlation degree of hydroxyl group and methylene group in the micro group of coal sample to the characteristic temperature stage is high, and the correlation degree is 0.6753 and 0.6926 respectively. In the critical and pyrolysis stages, the surface active structure of coal body is physically and chemically adsorbed with oxygen molecules. The hydroxyl group first reacts with oxygen to store heat. As the temperature increases, a small amount of side chain breaks, resulting in an increase in the content of methylene. The hydroxyl group is also continuously consumed due to other functional groups. The reaction continues to generate. In the pyrolysis stage, the free water in the coal evaporates, the bound water begins to evaporate, the intramolecular association hydrogen bond is accelerated, the porosity of the coal becomes larger, the gas adsorption capacity is enhanced, the reactivity of various functional groups with oxygen is improved, and the coal spontaneous combustion process is accelerated. In addition, the stacking height and lamellar diameter are related to the volume, surface morphology and stability of coal accumulation. The stacking height and lamellar diameter always have a high correlation degree (0.668 9) between the initial stage of coal spontaneous combustion process and the characteristic temperature stage.

       

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