Kinetics of the cracking reduction of hematite

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

Abstract

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.

赤铁矿裂解还原动力学
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。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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