Interfacial reaction between magnesia refractory and “FeO”-rich slag: Formation of magnesiowüstite layer |
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Authors: | Jin Sung Han Jung Ho Heo Joo Hyun Park |
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Affiliation: | 1. Department of Materials Engineering, Hanyang University, Ansan 15588, South Korea;2. Research and Development Center, Hyundai Steel, Dangjin 1480, South Korea;3. Research and Development Center, LS-Nikko Copper, Ulsan 70, South Korea |
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Abstract: | This study investigated the reaction between CaO-SiO2-Al2O3-xFeO-MgO-MnO (CaO/SiO2?=?1.2, x?=?20–50?wt%) slag and magnesia refractory. Using SEM-EDS analysis, we confirmed the formation of a (Mg,Fe)Oss(solid_solution), called magesiowüstite (MW), intermediate layer at the slag-refractory interface. MgO dissolved from refractory and reacted with the bulk slag to form MW layer at the interface. Simultaneously, slag penetrated through micro-pores and reacted with the refractory to form MW layer. In other words, the MW layer built up in both directions from initial refractory-slag interface. The thickness of the MW layer increased as the FeO content in the slag increased, and using EDS line scanning, a Mg and Fe concentration gradient was confirmed within the MW layer. The slag, which penetrated into the refractory, had a chemical composition of the CaO-SiO2-Al2O3-MgO system without FeO, indicating that FeO was consumed by forming a MW layer at the refractory hot face. The slag-refractory interfacial reaction was simulated using thermochemical software, FactSage?7.0. The results predicted a MW monoxide composed of MgO and FeO. A spinel phase was formed when FeO was greater than 40?wt%. These thermochemical computations were comparable to our experimental findings. |
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Keywords: | Magnesia refractory Slag-refractory reaction Magesiowustite layer Slag penetration Thermochemical computation Spinel |
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