论文标题
通过减少铁矿石的氢血浆的可持续钢:工艺,动力学,微观结构,化学
Sustainable steel through hydrogen plasma reduction of iron ore: process, kinetics, microstructure, chemistry
论文作者
论文摘要
Fe-和钢制造是最大的单个工业二氧化碳发射极,占地球上所有二氧化碳排放量的6.5%。这一事实挑战了当前的技术以实现碳钢铁的产量,并与在2050年左右在所有CO2排放中大幅度降低80%的要求一致。因此,必须实施替代的还原技术来从其矿石中提取铁。基于H的直接还原已被探索为减轻CO2排放的可持续途径,其中中间氧化物产物Fexo Wustite的减少动力学是该过程的限制步骤。总反应具有吸热净能量平衡。基于H血浆的减少可能会提供有吸引力的替代方案。在这里,我们介绍了使用H血浆减少赤铁矿的研究。在几个中间状态下研究了化学组成和相变的演变。我们发现赤铁矿还原动力学取决于初始输入质量和电弧功率之间的平衡。对于优化的输入质量 - ARC功率比,在暴露于H血浆的15分钟内获得了完全降低。钢铁石还原也是朝着完全降低的速率限制步骤。但是,还原反应是放热的,其速率与基于H的直接降低中的速率相当。化学和微观结构分析表明,通过能量分散光谱和原子探针层析成像探测到其余氧化物区域的脉动元件分区。在基丁岩的Fayalite结构域,钢石/Fe杂音互联面和Fe内主要固化的氧化物颗粒中观察到了Si-endichment。但是,随着降低的降低,这些元素逐渐从样品中删除,以使最终的铁产品几乎没有与甘甘脉相关的杂质。
Fe- and steelmaking is the largest single industrial CO2 emitter, accounting for 6.5% of all CO2 emissions on the planet. This fact challenges the current technologies to achieve carbon-lean steel production and to align with the requirement of a drastic reduction of 80% in all CO2 emissions by around 2050. Thus, alternative reduction technologies have to be implemented for extracting iron from its ores. The H-based direct reduction has been explored as a sustainable route to mitigate CO2 emissions, where the reduction kinetics of the intermediate oxide product FexO wustite into Fe is the rate-limiting step of the process. The total reaction has an endothermic net energy balance. Reduction based on a H plasma may offer an attractive alternative. Here, we present a study about the reduction of hematite using H plasma. The evolution of both, chemical composition and phase transformations was investigated in several intermediate states. We found that hematite reduction kinetics depends on the balance between the initial input mass and the arc power. For an optimized input mass-arc power ratio, complete reduction was obtained within 15 min of exposure to the H plasma. The wustite reduction is also the rate-limiting step towards complete reduction. Nonetheless, the reduction reaction is exothermic, and its rates are comparable with those found in H-based direct reduction. Chemical and microstructure analysis revealed that the gangue elements partition to the remaining oxide regions, probed by energy dispersive spectroscopy and atom probe tomography. Si-enrichment was observed in the interdendritic fayalite domains, at the wustite/Fe hetero-interfaces and in the primarily solidified oxide particles inside the Fe. With proceeding reduction, however, such elements are gradually removed from the samples so that the final iron product is nearly free of gangue-related impurities.