ISIJ International
Online ISSN : 1347-5460
Print ISSN : 0915-1559
ISSN-L : 0915-1559
Regular Article
Activities of FeO1.33 in the FeOx–CaO–SiO2 and FeOx–CaO–SiO2–Al2O3 Slags at 1573 K Under Oxygen Partial Pressures between 10−6 and 10−2 atm
Yoshitaka KatahiraMiyuki Hayashi
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2016 Volume 56 Issue 7 Pages 1164-1170

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Abstract

Qualities of sinters such as reducibility and strength are controlled by morphologies and mineral phases in iron ore sinters. Main mineral phases are hematite, magnetite and calcium ferrite. Slag phases are also included in sinters, which have been mainly liquid phases during the sintering process. Since iron ions in slags are hardly reduced to metallic irons in a blast furnace, iron oxides such as hematite and magnetite and calcium ferrite should be precipitated from molten slags during the sintering process. Precipitation of iron oxides and calcium ferrites from molten slags depends on the activity of FeOx in molten slags from the thermodynamic view point. Therefore, the activities of FeO1.33 have been measured over the wide ranges of chemical compositions in the single liquid phases of the FeOx–CaO–SiO2 and FeOx–CaO–SiO2–Al2O3 slags at 1573 K under oxygen partial pressures between 10−6 and 10−2 atm. It has been found that the aFeO1.33 values have maximum at the CaO/SiO2(mass%) ratios of 0.9–1.0 and 1.3–1.4 for the samples with 35 mass%FeOx equilibrated at PO2 = 1.0×10−2 atm and 1.0×10−4 atm, respectively. For the samples at PO2 = 2.5×10−6 atm, on the other hand, aFeO1.33 monotonically increases with increasing the CaO/SiO2 ratio within the compositional range of the single liquid region. As for the effect of the Al2O3 addition on the activities, the dependency of the activity on the CaO/SiO2 ratio becomes moderate with increasing the Al2O3 addition on the sample at PO2 = 2.5×10−6 atm.

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© 2016 by The Iron and Steel Institute of Japan
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