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Non-isothermal reduction mechanism and kinetics of high chromium vanadium-titanium magnetite pellets

机译:高铬钒钛磁铁矿球团的非等温还原机理及动力学

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摘要

Non-isothermal reduction kinetics and mechanism of high chromium vanadium-titanium magnetite pellets were studied at 400-1100 degrees C, simulating the lumpy zone of blast furnace conditions. The phase transformation behaviour of valuable elements including Fe, Cr, V and Ti and microstructural changes of reduced pellets were examined by means of X-ray diffraction (XRD) and SEM-EDX. The swelling of reduced pellets was highest at 900 degrees C, while cold crushing strength was highest at 1100 degrees C. Phase transformation behaviour of valuable elements in the lumpy zone is as follows: Fe2O3 -> RFe3O4 -> RFeO -> RFe; Fe2Ti3O9 -> RFe2TiO4 -> RFe5TiO8 -> RFeTiO3; V2O3 -> RVO; (Fe0.6Cr0.4)(2)O-3 -> FeO center dot Cr2O3 -> RCr2O3. By analysing the non-isothermal reduction kinetics of high chromium vanadium-titanium magnetite pellets, based on the evaluation of reaction activation energy calculated according to Coats-Redfern method, gaseous internal diffusion through solid product layer and interfacial chemical reaction are most likely to be the main rate controlling steps in the reduction process.
机译:研究了高铬钒钛磁铁矿球团在400-1100摄氏度下的非等温还原动力学及其机理,模拟了高炉条件下的块状区域。通过X射线衍射(XRD)和SEM-EDX检测了包括Fe,Cr,V和Ti在内的有价值元素的相变行为以及还原球团的微观结构变化。还原粒料的溶胀在900℃下最高,而冷碎强度在1100℃下最高。块状区中有价值元素的相变行为如下:Fe 2 O 3-> RFe 3 O 4-> RFeO-> RFe; Fe2Ti3O9-> RFe2TiO4-> RFe5TiO8-> RFeTiO3; V2O3-> RVO; (Fe0.6Cr0.4)(2)O-3-> FeO中心点Cr2O3-> RCr2O3。通过分析高铬钒钛磁铁矿球团的非等温还原动力学,基于对根据Coats-Redfern方法计算的反应活化能的评估,最有可能是通过固体产物层的气体内部扩散和界面化学反应还原过程中的主要速率控制步骤。

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