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Interfacial reaction between magnesia refractory and "FeO"-rich slag: Formation of magnesiowiistite layer

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dc.contributor.authorHan, Jin Sung-
dc.contributor.authorHeo, Jung Ho-
dc.contributor.authorPark, Joo Hyun-
dc.date.accessioned2021-06-22T10:02:06Z-
dc.date.available2021-06-22T10:02:06Z-
dc.date.created2021-01-21-
dc.date.issued2019-06-
dc.identifier.issn0272-8842-
dc.identifier.urihttps://scholarworks.bwise.kr/erica/handle/2021.sw.erica/2876-
dc.description.abstractThis 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) O-ss(solid_solution), called magesiowiistite (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 (TM) 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.-
dc.language영어-
dc.language.isoen-
dc.publisherPergamon Press Ltd.-
dc.titleInterfacial reaction between magnesia refractory and "FeO"-rich slag: Formation of magnesiowiistite layer-
dc.typeArticle-
dc.contributor.affiliatedAuthorPark, Joo Hyun-
dc.identifier.doi10.1016/j.ceramint.2019.02.110-
dc.identifier.scopusid2-s2.0-85062098091-
dc.identifier.wosid000465058500100-
dc.identifier.bibliographicCitationCeramics International, v.45, no.8, pp.10481 - 10491-
dc.relation.isPartOfCeramics International-
dc.citation.titleCeramics International-
dc.citation.volume45-
dc.citation.number8-
dc.citation.startPage10481-
dc.citation.endPage10491-
dc.type.rimsART-
dc.type.docTypeArticle-
dc.description.journalClass1-
dc.description.isOpenAccessN-
dc.description.journalRegisteredClassscie-
dc.description.journalRegisteredClassscopus-
dc.relation.journalResearchAreaMaterials Science-
dc.relation.journalWebOfScienceCategoryMaterials Science, Ceramics-
dc.subject.keywordPlusDISSOLUTION RATE-
dc.subject.keywordPlusCORROSION-
dc.subject.keywordPlusMGO-
dc.subject.keywordPlusTEMPERATURE-
dc.subject.keywordPlusCASTABLES-
dc.subject.keywordAuthorMagnesia refractory-
dc.subject.keywordAuthorSlag-refractory reaction-
dc.subject.keywordAuthorMagesiowustite layer-
dc.subject.keywordAuthorSlag penetration-
dc.subject.keywordAuthorThermochemical computation-
dc.subject.keywordAuthorSpinel-
dc.identifier.urlhttps://www.sciencedirect.com/science/article/pii/S0272884219304110?via%3Dihub-
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ERICA 공학대학 (DEPARTMENT OF MATERIALS SCIENCE AND CHEMICAL ENGINEERING)
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