Abstract

To reveal the growth behavior and size characterization of iron particles in coal-based reduction, we reduced oolitic hematite–coal composite briquettes at various temperatures, durations and ore size fractions. The degree of metallization and microstructure of the reduced briquettes and the characteristic of iron particle size were investigated through chemical composition analysis, scanning electron microscopy, energy dispersive spectroscopy, and Bgrimm process mineralogy analysis. Results showed that iron oxides in the oolitic hematite ore were reduced to metallic iron from outer to inner layers; these oxides gradually grew into quasi-spherical iron particles with random distribution in the gangue. As reduction continued, iron grains agglomerated occurred, and iron particle clusters were formed in the form of quasi-spherical, chained, blocky, and clavate when they were viewed in the cross section. The boundaries among the iron grains of the iron particle cluster continuously faded and disappeared, and an iron particle with increased size and homogeneity was finally produced. The reduction temperature, time, and ore size fraction influenced the reduction of composite briquettes and iron particle size. The degree of metallization increased as reduction temperature was increased, reduction time was extended, or ore size fraction was decreased until the equilibrium of reaction was achieved. Moreover, the iron particle size gradually increased as reduction temperature was increased, reduction time was extended, or ore size fraction was decreased.

Highlights

  • Oolitic hematite ore is a significant existing form of iron ores, which are widely distributed in France, Germany, the United States, Canada, Pakistan, China, and other countries [1,2]

  • To investigate the growth behavior and particle size of iron particles in the reduction of oolitic hematite–coal composite briquette, we operated under the following conditions: reduction temperatures of 1423, 1473, 1523, and 1548 K; reduction times of 20, 30, 40, and 50 min; and ore size fractions of −0.1, −1.0, −2.0, and −4.0 mm

  • During the fusion of iron grains, C and P converted from a slag phase into a metal phase, and based on the standard Gibbs free energy changes (∆Gθ ), we considered that Reactions (5) and (6) occurred during fusion (Table 4) [3]

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Summary

Introduction

Oolitic hematite ore is a significant existing form of iron ores, which are widely distributed in France, Germany, the United States, Canada, Pakistan, China, and other countries [1,2]. As one of the most refractory iron ores in the world, oolitic hematite ore possesses complex composition, microstructure, and embedded relationship [4,5], contains some metallic minerals, such as hematite (Fe2 O3 ), siderite (FeCO3 ), and limonite (Fe2 O3 ·nH2 O), and comprises some non-metallic minerals, such as quartz (SiO2 ), chamosite [(Fe,Mg) (Fe,Fe)3 [AlSi3 O10 ](OH)3 ], and collophanite (Ca3 P2 O8 ·H2 O). These ultra-fine-grained minerals cement together to form a disseminated oolitic structure. Phosphorus removal was disregarded in this study to focus on metallic iron particles

Materials
Composite
Analysis and Characterization
Degree of Metallization
Growth Behavior
Effect of Reduction Temperature on Iron Particle Size
Effect of Reduction Time on Iron Particle Size
Effect of Ore Size Fraction on Iron Particle Size
Conclusions
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