Fundamentals of silico-ferrite of calcium and aluminium (SFCA) and SFCA-I iron ore sinter bonding phase formation: effects of mill scale addition

被引:6
|
作者
Webster, Nathan A. S. [1 ]
Pownceby, Mark I. [1 ]
Pattel, Rachel [1 ]
机构
[1] CSIRO Mineral Resources, Private Bag 10, Clayton, Vic 3169, Australia
关键词
iron ore sinter; mill scale; SFCA and SFCA-I; formation mechanisms; in situ X-ray diffraction; CRYSTAL-STRUCTURE; FORMATION MECHANISMS;
D O I
10.1017/S088571561700080X
中图分类号
TB3 [工程材料学];
学科分类号
0805 ; 080502 ;
摘要
The thermal decomposition of mill scale, and the effect of mill scale addition on the formation and decomposition of Silico-Ferrite of Calcium and Aluminium (SFCA) and SFCA-I iron ore sinter bonding phases, has been investigated using in situ X-ray diffraction. Application of the external standard method of quantitative phase analysis of the in situ data collected during decomposition of the mill scale highlighted the applicability of this method for the determination of the nature and abundance of amorphous material in a mineral sample. Increasing mill scale addition from 2.6 to 10.6 and to 21.2 wt% in an otherwise synthetic sinter mixture composition designed to form SFCA did not significantly affect the thermal stability ranges of SFCA-I or SFCA, nor did it significantly affect the amount of each of SFCA or SFCA-I, which formed. This was attributed to the low impurity (i.e. Mn, Mg) concentration in the mill scale, and also the transformation to hematite during heating of the wustite and magnetite present in the mill scale, with the hematite available for reaction to form SFCA and SFCA-I. (c) 2017 International Centre for Diffraction Data.
引用
收藏
页码:S85 / S89
页数:5
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