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Enhancement of Iron Melting Rate under the Co-existence of Graphite and Wüstite

机译:石墨与硅灰石并存下铁熔体速度的提高

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Carburization and melting processes of solid Fe under the co-existence of graphite and wüstite has been investigated based on a confocal laser scanning microscope “in-situ ” observation of the movement of the interface between Fe–C melt and solid Fe at 1523 K. In the experiments, strong stirring flow at the surface of the Fe–C melt is observed. This flow is found to be Marangoni flow and is introduced by the surface tension gradient due to the difference of oxygen concentration between the Fe–C melt interface with graphite and solid iron. The velocity of Marangoni flow is measured from the moving velocities of bubbles at the molten Fe–C surface. The melting rate of Fe is analyzed by computational fluid flow simulations of the Fe–C melt. Based on these results, it is confirmed that the carburization and melting rate of solid Fe can be enhanced by allowing Fe–C melt to come into contact with wüstite and graphite simultaneously.
机译:基于共聚焦激光扫描显微镜“原位”观察了Fe-C熔体与固态Fe之间的界面运动,研究了石墨与白钨共存下固态Fe的渗碳和熔融过程。 1523K。在实验中,观察到在Fe–C熔体表面强烈搅拌。发现该流为马兰戈尼流,并由于与石墨和固态铁的Fe–C熔体界面之间的氧浓度不同而由表面张力梯度引入。 Marangoni流动的速度是根据熔融Fe-C表面气泡的运动速度来测量的。通过计算Fe–C熔体的流体流动模拟来分析Fe的熔化速率。根据这些结果,可以确认,通过使Fe–C熔体同时与辉石和石墨接触,可以提高固体Fe的渗碳和熔融速率。

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