首页> 外文会议>Japan-China Symposium on Coal and C1 Chemistry; 20031208-11; Kitakyushu, Fukuoka(JP) >TG-MS STUDY ON THE EVOLVED GASES DURING PYROLYSIS OF MACERALS FROM SHENMU COAL
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TG-MS STUDY ON THE EVOLVED GASES DURING PYROLYSIS OF MACERALS FROM SHENMU COAL

机译:TG-MS研究神木煤热分解过程中析出的气体

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Pyrolysis is a useful tool for the examination of structure and (activity of coal if coal pyrolysis is performed under precisely definite conditions, in particular, non-isothermal pyrolysis at constant heating rate. The mechanistic and khetic data on the decomposition of coal and much valuable information about the formation of numerous single products as a function of temperature could be obtained. Van Heek investigated the possibilities and limitations of experimental and theoretical methods of non-isothermal reaction kinetics applied to the relation between coal structure and pyrolysis behavior. They studied the evolution curves of some evolved gases such as CH_4 C_3H_8 and H_2O during coal pyrolysis and compared with those of model compounds. Das studied the evolution characteristics of gases during pyrolysis of maceral concentrates of different rank Russian coal using TGGC. They found the major constituents of gaseous products were CH_4, CO and H_2. And vitrinite of any rank was found to yield a higher amount of CH_4 and lower amount of CO than fusinite. The previous works on pyrolysis behavior paid much attention on the effect of coal rank, few studies was carried out on the pyrolysis behaviors of individual macerals, especially those separated from the same parent coal. The aim of this work is to study the evolution behavior of evolved gases during pyrolysis of macerals separated from Chinese Shenmu coal and get more information about the relationship between maceral structural characteristic and its pyrolysis behavior.
机译:热解是检查结构和(如果在精确确定的条件下进行煤热解,尤其是在恒定加热速率下进行非等温热解)煤的活性的有用工具。有关煤分解的机理和动力学数据,非常有价值范希克(Van Heek)研究了将非等温反应动力学应用于煤结构与热解行为之间关系的实验和理论方法的可能性和局限性,并研究了其演化过程。煤热解过程中一些析出气体如CH_4 C_3H_8和H_2O的曲线,并与模型化合物进行比较,Das用TGGC研究了不同等级的俄罗斯煤的精矿的热解过程中气体的演化特征,发现了气态产物的主要成分分别是CH_4,CO和H_2。因此,与富锌铁矿相比,生成的CH_4量更高,而CO的含量更低。以前关于热解行为的研究主要关注煤级的影响,很少对单个金属的热解行为进行研究,特别是那些从同一母煤中分离出来的金属。这项工作的目的是研究从神木煤中分离出的黄石的热解过程中析出气体的逸出行为,并获得有关黄石结构特征与其热解行为之间关系的更多信息。

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