Effect of Addition of Mill Scale on Sintering of Iron Ores

Iron-rich (65 to 70 pct total Fe) mill scale generated during processing by steel mills can be recycled by using it as a ferrous raw material in the sintering process. The effect of mill scale addition on the phase formation of sintered specimens from an industrial sinter blend containing 0 to 15 wt...

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Veröffentlicht in:Metallurgical and materials transactions. B, Process metallurgy and materials processing science Process metallurgy and materials processing science, 2016-10, Vol.47 (5), p.2848-2860
Hauptverfasser: Wang, Zhe, Pinson, David, Chew, Sheng, Monaghan, Brian J., Pownceby, Mark I., Webster, Nathan A. S., Rogers, Harold, Zhang, Guangqing
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Sprache:eng
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Zusammenfassung:Iron-rich (65 to 70 pct total Fe) mill scale generated during processing by steel mills can be recycled by using it as a ferrous raw material in the sintering process. The effect of mill scale addition on the phase formation of sintered specimens from an industrial sinter blend containing 0 to 15 wt pct mill scale was examined, and the mineral phases formed during sintering under various conditions ( T  = 1523 K to 1598 K [1250 °C to 1325 °C] and gas compositions of pO 2  = 0.5, 5 and 21 kPa) were quantitatively measured. For samples sintered in air (pO 2  = 21 kPa), there was negligible effect of mill scale addition on the phases formed. The oxidation of the mill scale was complete, and phases such as Silico-Ferrite of Calcium and Aluminum (SFCA), SFCA-I, and hematite dominated. Under lower oxygen partial pressures (pO 2  = 0.5 or 5 kPa), and throughout the temperature range examined, the mill scale was converted to magnetite, with the extent of reaction controlled by the hematite-magnetite conversion kinetics. When sintered in the gas mixture with pO 2  = 5 kPa, an increase in the mill scale content from 0 to 15 wt pct resulted in a decrease of hematite and total SFCA phases and a corresponding increase in the amount of magnetite which formed. The oxidation of wustite in mill scale to magnetite decreased the local partial pressure of O 2 and increased sintering temperature, which promoted the decomposition of hematite.
ISSN:1073-5615
1543-1916
DOI:10.1007/s11663-016-0738-2