Reduction Process of High Phosphorus Oolitic Hematite

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Abstract:

The changing characteristics of iron mineral along with the reduction time in reduction of a high phosphorus oolitic hematite by carbon were discussed in the paper. The grain growth of metallic iron was investigated in detail. The results showed that the iron mineral in reduction of the oolitic hematite changed as Fe2O3→Fe3O4→FeO→Fe, and finally was reduced to metallic iron. As the reduction time elongated, the small grain of metallic iron gathered toward the larger one and grew up. The metallic iron existed in the reduction products in the form of larger grains of metallic iron.

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242-245

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January 2012

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© 2012 Trans Tech Publications Ltd. All Rights Reserved

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[1] Yiming Zhao and Chengsi Bi: Mineral Deposits, Vol. 19 (2000), p.350.

Google Scholar

[2] Shufei Li, Yongsheng Sun and Yuexin Han: Advanced Materials Research, Vol. 158 (2011) p.106.

Google Scholar

[3] Jicheng Zhou, Zhengliang Xue and Zongqiang Li: Journal of Wuhan University of Science and Technology (Natural Science Edition), Vol. 30(2007), p.458.

Google Scholar

[4] Zhuqing Gong, Sheng Gong and Baizheng Chen: Journal of Central South University(Science and Technology), Vol. 37(2006), p.703.

Google Scholar