富氢气氛下球团矿的热力学计算与物相转变行为
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Thermodynamic calculation and phase transformation behavior of iron ore pellets in hydrogen-rich atmospheres
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    摘要:

    为实现钢铁工业的低碳转型,本文研究了富氢气氛(H2、CO及CO-H2,混合气体)下铁精矿球团的还原过程与 碳沉积行为。结合热力学计算与高温原位X射线行射技术,系统分析了不同气氛与温度条件下球团矿的相变路 径与热力学特征。结果表明,H2还原速率显著高于CO,还原气利用率随温度和H2比例升高而增加。CO气氛在 400~800C区间易引发碳沉积,温度高于900C,析碳受到抑制;Fe3C的生成依赖于气氛碳势与温度,高CO分压 与低氧是有利条件。研究可为富氢直接还原工艺的优化提供理论依据和试验支持。

    Abstract:

    In order to achieve low-carbon transition in the iron and steel industry, the reduction process and carbon deposition behavior of iron ore concentrate pellets in hydrogen-rich atmosphere [H2, CO, and CO-H2 mixtures] were studied in this paper. By combining thermodynamic calculations with high-temperature in-situ X-ray diffraction (XRD), the phase change pathways and thermodynamic characteristics of pellets under different atmospheres and temperature conditions were systematically analyzed. The results indicate that the reduction rate of H2is significantly higher than that of CO, and the utilization efficiency of reducing gas increases with temperature and higher H2 proportions. Carbon deposition is prone to occur within the temperature range of 400–800?°C in a CO atmosphere, while carbon precipitation is suppressed when temperature is above 900?°C; the formation of Fe3C depends on both the carbon potential of the atmospheres and temperature, and high CO partial pressure and low oxygen are favorable conditions. This work provides a theoretical basis and experimental support for the optimization of hydrogen-based direct reduction processes.

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唐世明,孙强超,程红伟.富氢气氛下球团矿的热力学计算与物相转变行为[J].烧结球团,2026,(1):164-175

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  • 在线发布日期: 2026-03-25
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