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Assimilation and Mineral Formation during Sintering for Blends Containing Magnetite Concentrate and Hematite/Pisolite Sintering Fines

机译:含磁铁矿精矿和赤铁矿/透晶石烧结粉的共混物在烧结过程中的同化和矿物形成

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摘要

Blends for sintering in China commonly contain domestic magnetite concentrate and imported hematite or/and pisolite sintering fines. Interactions between these ores will, no doubt, have an important impact on sintering performance and sinter quality of these blends. Studies have been carried out to look at assimilation of sintering fines and mineral formation during sintering of such blends. The results show that at given mix composition, pisolite ores are easier to be assimilated than hematite and magnetite ores while magnetite shows the least assimilation. For the same ore, the assimilation depends on melt level and ore porosity. For this reason, higher assimilation was observed for porous ores or ores with high gangue content or when an easy-fusing ore was present in the blend.
机译:在中国,用于烧结的掺合物通常包含国产磁铁矿精矿和进口赤铁矿或/和镁橄榄石烧结粉。毫无疑问,这些矿石之间的相互作用将对这些混合物的烧结性能和烧结质量产生重要影响。已经进行了研究以研究这种混合物的烧结过程中烧结细粉的同化和矿物形成。结果表明,在给定的混合成分下,镁橄榄石矿石比赤铁矿和磁铁矿矿石更容易被同化,而磁铁矿的同化作用最少。对于相同的矿石,同化作用取决于熔融液位和矿石孔隙率。因此,对于多孔矿石或porous石含量高的矿石,或掺混物中存在易熔矿石,观察到较高的同化作用。

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