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Structural and morphological changes during reduction of hematite to magnetite and wustite in hydrogen rich reduction gases under fluidised bed conditions

机译:流化床条件下富氢还原气体中赤铁矿还原成磁铁矿和铁水辉石的结构和形态变化

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摘要

During the reduction of iron ore fines structural changes in particles have a significant influence on the rate of reduction. Investigations regarding porosity, specific surface area and mean pore diameters in the reduction of hematite with hydrogen rich reducing gases were performed by mercury porosimetry. Morphological changes were examined by metallographic analyses of polished sections in reflected light. In the magnetite equilibrium phase, significant influence of temperature on structural parameters and sintering effects were found. For wustite phases, the influence of temperature was less pronounced. For the reduction of hematite to magnetite and magnetite to wustite topochemical phase growth and microporous product layers were observed. In the single step, reduction of hematite to wustite progressive conversion and significant increase in the mean pore diameter were found. The results presented in this work are of high importance for understanding the reaction kinetics of iron ore fines and essential for modelling heterogeneous reactions.
机译:在铁矿石细粉还原过程中,颗粒的结构变化对还原速率有重大影响。通过汞孔隙率法进行了有关用富氢还原气体还原赤铁矿的孔隙率,比表面积和平均孔径的研究。通过金相分析抛光部分在反射光下的形态变化。在磁铁矿平衡阶段,发现温度对结构参数和烧结效果有显着影响。对于镁橄榄石相,温度的影响不太明显。为了将赤铁矿还原为磁铁矿,将磁铁矿还原为铁矾土拓扑化学相,观察到了微孔产物层的生长。在单一步骤中,发现了赤铁矿向铁矾石的逐步转化的减少和平均孔径的显着增加。这项工作中提出的结果对于理解铁矿粉的反应动力学非常重要,对于建模异质反应至关重要。

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