Reduction kinetics of Shougang iron ore sinter
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摘要: 采用熱重法在1173~1373 K、全CO氣氛條件下,對首鋼燒結礦進行還原動力學實驗,確定了還原反應的表觀活化能,進而推斷在還原反應的前期燒結礦還原速率均由界面反應控制,還原反應后期的控制環節為固相擴散.分別由未反應核模型和固相反應動力學模型,分段給出不同溫度下控制環節突變的時間點;通過動力學公式計算,得出不同溫度下的反應速率常數和固相擴散系數.利用光學顯微鏡觀察了燒結礦在各還原階段的微觀形貌,驗證了燒結礦還原動力學的機理,同時也證明了擴散控制階段使用體積縮小的未反應核模型與實際情況是吻合的.Abstract: The reduction kinetics tests of Shougang sintering iron ores were performed from 1173 to 1373 K with 100% CO by thermogravimetric analysis, from which the values of reduction reaction apparent activation energy were determined. It could be predicted that the reduction of iron ore sinter is controlled by interracial chemical reaction at the initial stage, and solid-state diffusion at the final stage. According to the unreacted core model and the kinetic model of solid-state diffusion separately, the mutational timing of each rate controlling step was given at various temperatures by using phasewise analysis. The reaction rate constants and solid diffusion coefficients were derived from the kinetic formulas at various temperatures. Changes in morphology were analyzed with an optical microscope, and the mechanism of reduction kinetics was also verified. At the same time, the use of the volume-dwindled unreacted core model in the diffusion stage was proved to be feasible.
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Key words:
- iron ore sinter /
- reduction /
- reaction kinetics /
- tliermogravimetric analysis /
- mineralogy
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