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Kinetic parameters associated with self-heating of New Zealand coals under adiabatic conditions

机译:绝热条件下与新西兰煤自热相关的动力学参数

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摘要

Adiabatic self-heating tests were carried out on five New Zealand coal samples ranging in rank from lignite to high-volatile bituminous. Kinetic parameters of oxidation were obtained from the self-heating curves assuming Arrhenius behaviour. The activation energy E (kJ mol~(-1)) and the pre-exponential factor A (s~(-1)) were determined in the temperature range of 70-140 deg. The activation energy exhibited a definite rank relationship with a minimum E of 55 kJ mol~(-1) occurring at a Suggate rank of approx 6.2 corresponding to subbituminous C Either side of this rank there was a noticeable increase in the activation energy indicating lower reactivity of the coal. A similar rank trend was also observed in the R_(70) self-heating rate index values that were taken from the initial portion of the self-heating cure from 40 deg to 70 deg. From these results it is clear that the adiabatic method is capable of proving reliable kinetic parameters of coal oxidation.
机译:对五个新西兰煤样品进行了绝热自热测试,煤样品的等级范围从褐煤到高挥发性沥青。氧化的动力学参数是从假设阿伦尼乌斯行为的自热曲线获得的。在70-140度的温度范围内确定了活化能E(kJ mol〜(-1))和指数前因子A(s〜(-1))。活化能表现出确定的等级关系,最低E为55 kJ mol〜(-1),Suggate等级约为6.2,对应于次沥青C。在该等级的任一侧,活化能均显着增加,表明反应性较低煤炭。从自热固化的初始部分从40度到70度的R_(70)自热速率指数值中也观察到类似的等级趋势。从这些结果可以明显看出,绝热方法能够证明煤氧化的可靠动力学参数。

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