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Characterization and Reduction Behavior of Mill Scale

机译:轧机氧化皮的表征和还原行为

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This paper presents an initial part of a project devoted to the recycling of mill scale in the form of self-reducing briquettes. First chemical and morphological characteristics of mill scale were investigated and next its gaseous reduction behavior was studied by thermogravimetry. The chemical characterization showed that wustite is the major constituent of this waste matter, with small amounts of magnetite, hematite and metallic iron. The microscopic examination of the scale revealed its complex and layered microstructure with three distinct zones. The outer layer is relatively thin and porous. It is mainly composed of hematite and magnetite. The intermediate layer is made of the dense, columnar grains of wustite. The inner layer is a very porous wustite. The gaseous reduction by carbon monoxide has a topochemical character regardless of initial morphology of scale and, depending on temperature and reducing gas composition it produces a porous iron or the iron whiskers. The unreacted shrinking core model with one interface fits quite well the kinetic data and the activation energy of reduction is about 80 kJ/mol.
机译:本文介绍了一个项目的初始部分,该项目致力于以自还原型团块的形式回收工厂规模。首先研究了氧化皮的化学和形态特征,然后通过热重法研究了其气态还原行为。化学特征表明,铁矿石是废料的主要成分,磁铁矿,赤铁矿和金属铁的含量很少。秤的显微镜检查显示出其复杂且分层的微观结构,具有三个不同的区域。外层较薄且多孔。它主要由赤铁矿和磁铁矿组成。中间层由致密的圆柱状的钙铁矿晶粒组成。内层是非常多孔的钙钛矿。一氧化碳进行的气态还原具有拓扑化学特性,而与氧化皮的初始形态无关,并且取决于温度和还原性气体成分,它会生成多孔铁或铁晶须。具有一个界面的未反应的收缩核模型非常符合动力学数据,还原的活化能约为80 kJ / mol。

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