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Kinetics of Dehydroxylation and Decarburization of Coal Series Kaolinite during Calcination: A Novel Kinetic Method Based on Gaseous Products

机译:煅烧过程中煤系高桥脱羟基化与脱碳动力学:一种基于气态产品的新型动力学方法

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摘要

The analysis of gaseous products reveals the characteristics, mechanisms, and kinetic equations describing the dehydroxylation and decarburization in coal series kaolinite. The results show that the dehydroxylation of coal series kaolinite arises from the calcination of kaolinite and boehmite within the temperature range of 350–850 °C. The activation energy for dehydroxylation is 182.71 kJ·mol−1, and the mechanism conforms to the A2/3 model. Decarburization is a two-step reaction, occurring as a result of the combustion of carbon and the decomposition of a small amount of calcite. The temperature range in the first step is 350–550 °C, and in the second is 580–830 °C. The first step decarburization reaction conforms to the A2/3 mechanism function, and the activation energy is 160.94 kJ·mol−1. The second step decarburization reaction follows the B3 mechanism function, wherein the activation energy is 215.47 kJ·mol−1. A comparison with the traditional methods proves that the kinetics method utilizing TG-FTIR-MS is feasible.
机译:气态产物的分析揭示了描述煤系列高岭土中脱羟基化和脱碳的特征,机构和动力学方程。结果表明,煤系列高岭石的脱羟基化由高岭土和勃姆石的煅烧,温度范围为350-850℃。脱羟基化的活化能量为182.71 kJ·mol-1,该机制符合A2 / 3模型。脱碳是两步反应,由于碳燃烧和少量方解石的分解而发生的两步反应。第一步中的温度范围为350-550℃,第二步是580-830℃。第一步脱碳反应符合A2 / 3机构功能,活化能量为160.94kJ·mol-1。第二步脱碳反应遵循B3机制功能,其中活化能量为215.47kJ·mol-1。与传统方法的比较证明了利用TG-FTIR-MS的动力学方法是可行的。

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