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    基于热重分析的炼焦煤热解过程中的挥发分逸出规律研究

    Study on the law of volatile matter release during the pyrolysis process of typical coking coals

    • 摘要: 炼焦煤热解过程中的挥发分析出对其成焦特性及焦炭结构具有重要影响。采用热重分析方法研究了8种典型炼焦煤热解过程中的挥发分析出行为,对特定温度区间的挥发分析出量参数、挥发分析出速率特征参数、DTG曲线解叠后的子峰特征参数与变质程度参数进行了深入分析,探讨不同变质程度炼焦煤热解活化能参数的差异性。结果表明:特定温度及区间的挥发分析出量可反映典型炼焦煤热解过程中挥发分析出的阶段性特征,绝对挥发分析出量Vx 与变质程度参数Vdaf呈现显著的线性关系(R2>0.8),而相对挥发分析出量VN-x体现煤种差异化的挥发分析出行为。在特定温度区间内,挥发分析出量参数多数与变质程度参数Vdaf呈现多项式关系。DTG曲线提取的温度特征参数TonsetTmaxTend和挥发分析出速率特征参数DTGmaxvar与变质程度参数Vdaf表现出良好的线性关系。子峰2、3、4的峰位温度和积分面积与变质程度关系明显,且子峰3、4在积分面积上的主导地位说明Cal—Cal和Car—Cal键断裂是形成挥发分快速析出的主要原因。采用Coasts-Redfern方法计算得到的表观活化能E虽与变质程度参数Vdaf展现出多项式关系,但相关性较差,说明活化能受多因素共同影响。黏结性指标与挥发分析出行为之间的关系有待进一步研究。

       

      Abstract: The volatile matter release during pyrolysis process of coking coals has a significant influence on its coking characteristics and coke structure. Thermogravimetric analysis was used to study the volatile matter release behavior during pyrolysis of eight typical coking coals. A meticulously comprehensive and profound analysis has been rigorously executed on the parameters associated with the evolution quantity of volatile matter, the characteristic parameters of the volatile matter evolution rate, the sub - peak characteristic parameters resultant from the deconvolution of the DTG (Differential Thermogravimetry) curve, and the metamorphic degree parameters within a precisely demarcated temperature regime. In addition, this research has delved deeply into the variances in the pyrolysis activation energy parameters of coking coals at diverse stages of metamorphism, with the aim of elucidating the underlying mechanisms governing the thermal decomposition behaviors of these coals. The results showed that, The amount of volatile matter evolved at specific temperatures and within specific temperature ranges can mirror the stage-by-stage characteristics of volatile matter evolution during the pyrolysis of typical coking coals. There is a remarkable linear correlation (R2>0.8) between the absolute volatile matter evolution amount Vx and the metamorphic degree parameter Vdaf. On the other hand, the relative volatile matter evolution amount VN-x reflects the differential volatile-matter-evolution behaviors among various coal types. Notably, within specific temperature ranges, the majority of volatile matter evolution amount parameters exhibit a polynomial relationship with the metamorphic degree parameter Vdaf. The temperature characteristic parameters Tonset, Tmax, Tend and the volatile matter release rate characteristic parameters DTGmax, va, r extracted mainly from the DTG curve exhibited a good linear relationship with the coal rank parameter Vdaf, and the correlation R2 was above 0.8. Decomposition of the DTG curve into six sub-peaks showed that the peak temperatures and integral areas of sub-peaks 2, 3, and 4 were significantly related to the coal rank. The dominance of sub-peaks 3 and 4 in the integral area indicated that cleavage of the Cal—Cal and Car—Cal bonds was the main reason for the formation of rapid release of volatile matter. The apparent activation energy E calculated using the Coasts-Redfern method displayed a polynomial relationship with the coal rank parameter Vdaf, but the correlation was poor, indicating that the activation energy was jointly influenced by multiple factors. The relationship between the thermoplastic index and volatile matter release behavior needs to be further studied.

       

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