饱和水雾条件下环境温度对不同变质程度煤尘吸水率的影响

    Effect of ambient temperature on water absorption of coal dust with different metamorphic degrees under saturated water mist

    • 摘要: 为研究饱和水雾条件下环境温度对掘进工作面煤尘吸水率的影响,利用自行设计的超声雾化吸水实验系统制造饱和水雾环境,测定不同环境温度下煤尘的吸水能力。研究结果表明:在环境温度为20~40 ℃的饱和水雾条件下,随着温度的升高,同一变质程度煤尘的吸水率先升高后降低;同一环境温度下,随着煤尘变质程度的增大,吸水率逐渐降低;不同变质程度煤尘在饱和水雾环境下,温度为27.5 ℃时煤尘的吸水率最高;随着煤尘变质程度的增大,羟基和羰基的数量不断减少,芳香烃和脂肪烃基团数量不断增加,导致煤尘吸水率降低。

       

      Abstract: In order to study the influence of the ambient temperature on the coal dust absorption rate of the heading face under saturated water mist condition, a self-designed ultrasonic atomization moisture adsorption experiment system was used to create a saturated water mist environment, and the water absorption capacity of coal dust under different environmental temperatures was measured. The results of the study indicate that the ambient temperature has a greater influence on the wettability of coal dust under saturated water mist condition. In the temperature range of 20 ℃ to 40 ℃, as the temperature increases, the water absorption rate of coal dust with the same metamorphic degree increases first and then decreases. Under the same ambient temperature, as the degree of coal dust deterioration increases, the water absorption rate gradually decreases. Coal dust with different degrees of metamorphism has the highest water absorption rate at the temperature of 27.5 ℃ in a saturated water mist environment. As the quality of coal dust increases, the number of hydroxyl groups and carbonyl groups in the molecular structure of coal continues to decrease, the number of aromatic and aliphatic hydrocarbon groups continues to increase, carbon structure functional groups increase, and coal dust water absorption decreases.

       

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