赤铁矿裂解还原动力学

F. Adam, F. Jeannot, B. Dupré, C. Gleitzer
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引用次数: 1

摘要

赤铁矿晶体在低温还原成磁铁矿过程中的开裂,提出了在诱导期可能延长后的s型动力学曲线分析的问题。我们已经记录了这样的曲线,CO/CO2 = 2080从350°C到600°C,并使用了不同的模型:-经典的收缩核心模型,只适用于600°C,而不是低于600°C, -噼啪核心模型,除了在反应开始时。令人惊讶的是,这些模型的速率常数和活化能的屈服值都是相当一致的。
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Kinetics of the cracking reduction of hematite

The cracking of hematite crystals during their low-temperature reduction to magnetite raises the question of the analysis of sigmoidal kinetic curves after an induction period which may be prolonged.

We have recorded such curves with CO/CO2 = 2080 from 350 to 600 °C, and used different models: - the classical Shrinking Core Model which should apply only at 600 ° C and not below, - the Crackling Core Model, except for at the beginning of reaction.

Surprisingly these models each yield values for the rate constant and its activation energy which are in reasonable agreement.

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