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Interfacial Phenomena of Sinter Melt on a Sintered Hematite Substrate–Effects of Temperature and Melt Composition

机译:烧结赤铁矿基质上熔体的界面现象-温度和熔体组成的影响

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In iron ore sintering,interfacial phenomena play a predominant role in sinter melt formation and therefore sinter quality.In this study,a high-temperature visualisation system was used in conjunction with optical and scanning electron microscopy to investigate the effects of temperature and melt composition on the interfacial phenomena and on the interactions of sinter melt with a sintered hematite substrate.The wettability and interactions between monocalcium ferrite melt and the hematite substrate were found to be improved with increasing temperature.Addition of Al2O3 or SiO2 improved the wetting behaviour of the melt on the sintered hematite substrate when their concentration was less than 6 wt.%.However,addition of MgO appeared to make the melt less wetting.Interaction was observed at the interface between the sinter melt and the sintered hematite substrate to a degree depending on respective melt composition.It was essentially dissolution of hematite from the substrate into the melt rather than penetration of the melt into the substrate along the grain boundaries.This could lead to compositional change of sinter melt and changes of sinter melt properties.
机译:在铁矿石烧结中,界面现象在烧结矿熔体的形成和烧结质量中起主要作用。在这项研究中,高温可视化系统与光学和扫描电子显微镜结合使用,研究温度和熔体组成对烧结矿的影响。烧结熔体与赤铁矿基体之间的界面现象以及相互作用;随着温度的升高,单钙铁氧体熔体与赤铁矿基体之间的润湿性和相互作用得到改善; Al2O3或SiO2的加入改善了熔体在硅酸盐上的润湿行为当其浓度低于6 wt。%时,烧结的赤铁矿基体。但是,MgO的加入使熔体的润湿性降低。在烧结熔体和烧结的赤铁矿基体之间的界面处观察到相互作用,其程度取决于各自的熔体基本上是赤铁矿从基质溶解到介质中而不是熔体沿着晶界渗透到基体中。这可能导致烧结矿熔体的成分变化和烧结矿熔体性能的变化。

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