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Mineral Composition and Microstructure Changes of Iron Ore Sinter During the Gas-Solid Reduction

机译:矿物固体减少期间铁矿石烧结的矿物成分和微观结构变化

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Characteristics of the gas-solid reduction reaction between iron ore sinter and carbon monoxide (CO) gas at 1273 K were studied with thermogravimetric analyzer. The microstructure, mineral compositions and porosity of sample were investigated prior to reduction, in the 30% reduced sample, in the 70% reduced sample, and in the fully reduced sample. At the reduction degree of 30%, the hematite and calcium ferrite was reduced to 44.4 and 60.4% respectively. At the reduction degree of 70%, all the hematite, calcium ferrite and magnetite were reduced to metal iron, only 36% wustite was left in the core area. The reduction reaction began with the loose structures and spread to the nearby area. In the area of micro-pores, the reducing gas can easily diffuse to the reaction interface to proceed the reduction reaction effectively. So increasing the content of micro-pores is an effective way to improve the reducibility of the sinter.
机译:用热量标注分析仪研究了1273 k下铁矿石烧结和一氧化碳(CO)气体的气体固体还原反应的特征。在减少样品之前研究样品的微观结构,矿物组合物和孔隙率,在70%的样品中,在70%降低的样品中,并在完全减少的样品中。在降低30%的降低程度下,赤铁矿和钙铁氧体分别降至44.4和60.4%。在降低70%的情况下,将所有赤铁矿,钙铁氧体和磁铁矿降低到金属铁,核心区域仅留下36%的沃抗石。还原反应开始源于松散的结构并蔓延到附近的区域。在微孔的区域中,还原气体可以容易地扩散到反应界面中以有效地进行还原反应。因此,增加微孔的含量是提高烧结的还原性的有效方法。

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