Investigation of transformations of low-grade manganese ore during the roasting process

IF 0.9 Q3 MINING & MINERAL PROCESSING
H. Ali, M. El-Sadek, H. Ahmed
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引用次数: 0

Abstract

ABSTRACT The transformations of low-grade manganese ore were investigated during roasting in the air at different temperatures up to 1200°C. The transformations were followed up by XRD and TGA-DTA. Moreover, the morphology and magnetic properties were determined by SEM and VSM. It was observed that MnO2 transformed to the lower oxide Mn5O8 at 500°C and then to bixbyite (Mn2O3) at 600°C. Finally, the bixbyite decomposed to hausmannite (Mn3O4) at 800°C. Increasing the roasting temperature to 900°C induced a reaction between hematite and hausmannite and led to the formation of a small amount of solid solution of the ferrite spinel MnFe2O4. Further increase in temperature to 1000°C led to the formation of a solid solution of braunite (Mn7SiO12) which decomposed to rhodonite (MnSiO3) at 1200°C. The magnetic susceptibility of the original ore gradually increased with the roasting temperature, from 0.119 × 10−3 at ambient temperature to a maximum value of 80 × 10−3 at 1200°C.
低品位锰矿在焙烧过程中的转化研究
摘要研究了低品位锰矿在1200°C以下不同温度下的空气焙烧过程中的转化过程。通过XRD和TGA-DTA对转化进行了跟踪。此外,通过扫描电镜和VSM测定了其形貌和磁性能。观察到MnO2在500°C时转化为较低的氧化物Mn5O8,然后在600°C时转变为二氧化二钒(Mn2O3)。最后,在800°C下,方镁石分解为锰铝石(Mn3O4)。将焙烧温度提高到900°C会引发赤铁矿和hausmannite之间的反应,并导致形成少量铁氧体尖晶石MnFe2O4的固溶体。温度进一步升高至1000°C,形成了在1200°C分解为菱铁矿(MnSiO3)的黑柱石(Mn7SiO12)固溶体。原始矿石的磁化率随着焙烧温度的升高而逐渐增加,从0.119 × 环境温度为10−3,最大值为80 × 1200°C时为10−3。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
3.50
自引率
0.00%
发文量
6
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