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Study on Thermal Decomposition and Oxidation Characteristics of Iron Ores

机译:铁矿石的热分解和氧化特性研究

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Thermal decomposition and oxidation characteristics of three typical iron ores were studied with differential thermal analysis and XRD techniques. The results displayed that DSC curve of limonite showed a significant endothermic arc in the range of 605-1150 ℃. It was thought that the decomposition of crystal water in limonite increased the porosity and surface area of limonite, which improved the adsorption capacity of limonite. DSC curve of hematite showed a weak endothermic arc in the range of 312-652 ℃. DSC curve of magnetite showed a significant exotherm arc in the range of 162-915 ℃. It was thought that lots of heat released when Fe_3O_4 in magnetite was oxidized.
机译:利用差热分析和XRD技术研究了三种典型铁矿石的热分解和氧化特性。结果表明,褐铁矿的DSC曲线在605〜1150℃范围内有明显的吸热弧。认为褐铁矿中结晶水的分解增加了褐铁矿的孔隙率和表面积,从而提高了褐铁矿的吸附能力。赤铁矿的DSC曲线在312-652℃范围内显示出较弱的吸热弧。磁铁矿的DSC曲线在162-915℃范围内有明显的放热弧。可以认为,磁铁矿中的Fe_3O_4被氧化时会放出大量的热量。

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