Fundamentals of Silico-Ferrite of Calcium and Aluminium (SFCA) and SFCA-I Iron Ore Sinter Bonding Phase Formation: Effects of MgO Source on Phase Formation during Heating

被引:3
|
作者
Webster, Nathan A. S. [1 ]
Pownceby, Mark, I [1 ]
Fan, Rong [2 ]
Brand, Helen E. A. [3 ]
机构
[1] CSIRO Mineral Resources, Private Bag 10, Clayton, Vic 3169, Australia
[2] CSIRO Mineral Resources, Locked Bag 2, Glen Osmond, SA 5064, Australia
[3] ANSTO, Australian Synchrotron, 800 Blackburn Rd, Clayton, Vic 3168, Australia
关键词
iron ore sinter; in situ synchrotron X-ray diffraction; complex Ca-rich ferrite iron ore sinter bonding phases; dolomite; serpentine; and olivine; SFCA and SFCA-I phase formation; CRYSTAL-STRUCTURE; CRYSTALLIZATION; MINERALOGY; TITANIUM; MAGNESIA;
D O I
10.2355/isijinternational.ISIJINT-2021-502
中图分类号
TF [冶金工业];
学科分类号
0806 ;
摘要
The relative effects of dolomite and serpentine/olivine as MgO flux sources on the formation of SFCA and SFCA-I iron ore sinter bonding phases during heating was investigated using in situ synchrotron X-ray diffraction. Results showed that a sinter mix containing serpentine/olivine as the primary source of MgO is more likely to form high quality sinter due to the higher proportion of SFCA-I being formed compared to SFCA. SFCA-I is the phase thought to impart high strength and good reducibility characteristics to iron ore sinter. For example, in mixtures containing 2 mass% MgO, when dolomite was used the maximum concentrations of SFCA-I and SFCA attained were 19 and 9 mass%, respectively, and when serpentine/olivine was used the maximum concentrations were 20 and 3 mass%, respectively. In mixtures containing 3 mass% MgO, the maximum concentrations were 18 and 4 mass% (dolomite) and 28 and 2 mass% (serpentine/olivine).
引用
收藏
页码:652 / 657
页数:6
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