鉄と鋼
Online ISSN : 1883-2954
Print ISSN : 0021-1575
ISSN-L : 0021-1575
各種合成クロマイトの炭素還元挙動
片山 博徳田 昌則
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1979 年 65 巻 3 号 p. 331-340

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The chromites shown below were prepared synthetically and reduced by graphite powder under a CO atmosphere: FeCr2O4 (Sp 1), MgCr2O4 (Sp 2), (Fe0.5Mg0.5) Cr2O4 (Sp 3), (Fe0.5Mg0.5) (Cr0.8Al0.2) 2O4 (Sp 4), and Mg (Cr0.6Al0.4) 2O4 (Sp 5).
The results obtained are as follows:
1) In the case of the pure iron chromite Sp 1, the reduction of FeO component preceded that of Cr2O3. With the progress of the reduction, the metallic products changed in the following order: Austenite→austenite+ (Fe, Cr) 3C→ (Fe, Cr) 3C+ (Cr, Fe) 7C3→ (Cr, Fe) 7C3.
2) The reduction of complex chromites containing iron oxide (Sp 3 and Sp 4) took place in two stages. In the first stage with the reduction of the FeCr2O4 component, FeO and Cr2O3 were reduced simultaneously at temperatures higher than 1150°C, although the reduction of FeO preceded at lower temperatures. The reduction of the MgCr2O4component (the second stage) required higher temperatures. It started at 1200°C and proceeded rapidly at temperatures higher than 1250°C in the case of Sp 2 and Sp 3. The rapid progress of the reduction of MgCr2O4 component of Sp 4 and Sp 5 which contained Al2O3was only encountered at temperatures higher than 1330°C.
3) The metallic product of the chromites Sp 3 and Sp 4 was (Cr, Fe) 7C3in either reduction stage of the FeCr2O4 and MgCr2O4 components. The final product of the reduction of the chromites Sp 2 and Sp 5 was Cr3C2, while an unidentified phase appeared during the course of the reduction and was considered to be chromium oxycarbide.

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