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首页> 外文期刊>Powder Technology: An International Journal on the Science and Technology of Wet and Dry Particulate Systems >Research on the characteristics and kinetics of direct reduction of limonite ore fines under CO atmosphere in a rotary drum reactor
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Research on the characteristics and kinetics of direct reduction of limonite ore fines under CO atmosphere in a rotary drum reactor

机译:旋转滚筒反应器CO气氛下褐铁矿矿石直接减少特征和动力学研究

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The behaviors of reduction and carbon deposition during the isothermal reduction of porous limonite ore fines by CO-N-2 gas mixtures were investigated using a rotary drum reactor in the temperature range of 750-900 degrees C. As the results suggested, the CO level and reaction temperature significantly impacted the reduction degree and the rate of reduction. It was found that in pure CO atmosphere at 750 degrees C, the reduction of iron oxides occurred with the carbon deposition reaction, which formed filamentous carbon before 60 min reduction. While with the extension of reduction time, the filamentous carbon disappeared, and the porous graphite clusters were formed due to the elevating level of deposited carbon in the reduced particles. A new mechanism including eight steps was proposed to clarify this phenomenon. Yet at 900 degrees C, the reduced particles gradually showed a sponge-like structure with reduction proceeded, and the iron whiskers precipitated on the particle surface and spread out significantly in 50 vol% CO-N-2 atmosphere. As the mathematical modeling of the experimental data suggested, the overall reduction of Fe2O3 to Fe could be presented by a 3D diffusion model in the whole temperature range investigated. The value of apparent activation energy for the reduction of limonite to metallic iron was found to be nearly 104.4 kJ/mol. (C) 2019 Elsevier B.V. All rights reserved.
机译:通过在750-900℃的温度范围内,研究了CO-N-2气体混合物的多孔褐岩矿矿石细胞等温降低期间的减少和碳沉积的行为。随着结果的提出,CO水平反应温度显着影响降低程度和减少速度。发现在750℃的纯CO气氛中,在碳沉积反应中发生氧化铁的还原,在60分钟内形成丝状碳。虽然随着还原时间的延伸,但由于减少颗粒中的沉积碳的升高,形成多孔石墨簇。提出了一种新机制,包括八个步骤,以澄清这种现象。然而,在900摄氏度下,减少的颗粒逐渐显示出具有缩小的海绵状结构,并且铁晶须在颗粒表面上沉淀并在50体积%的CO-N-2气氛中显着展开。随着所提出的实验数据的数学建模,可以通过研究的全温范围内的3D扩散模型来呈现FE2O3至Fe的总体减少。发现明显活化能量的值为降低褐铁矿到金属铁的值为近104.4kJ / mol。 (c)2019年Elsevier B.V.保留所有权利。

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