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hal.structure.identifierArcelorMittal Maizières Research SA
hal.structure.identifierInstitut de Chimie de la Matière Condensée de Bordeaux [ICMCB]
dc.contributor.authorGOUNÉ, Mohamed
hal.structure.identifierInstitut des Matériaux, de Microélectronique et des Nanosciences de Provence [IM2NP]
dc.contributor.authorMAUGIS, Philippe
hal.structure.identifierArcelorMittal Maizières Research SA
dc.contributor.authorDRILLET, J.
dc.date.issued2012
dc.identifier.issn1005-0302
dc.description.abstractEnThe present study clarifies the role of Mn in cementite on the driving force of cementite dissolution and the growth of austenite. From an experimental study, the effects of manganese composition and temperature on the cementite dissolution were shown. From a theoretical analysis based on thermodynamic and kinetics considerations, a criterion for the change from fast to slow regime of cementite dissolution was proposed. This criterion is in good agreement with the experimental results. It can be easily calculated and can define the composition and temperature ranges where the cementite dissolution is slow or fast.
dc.language.isoen
dc.publisherElsevier
dc.subject.enPhase transformation
dc.subject.enThermodynamics
dc.subject.enKinetics
dc.subject.enCementite dissolution
dc.subject.enSteel
dc.title.enA criterion for the change from fast to slow regime of cementite dissolution in Fe-C-Mn steels
dc.typeArticle de revue
dc.identifier.doi10.1016/s1005-0302(12)60122-4
dc.subject.halChimie/Matériaux
bordeaux.journalJournal of Materials Science and Technology
bordeaux.page728-236
bordeaux.volume23
bordeaux.issue8
bordeaux.peerReviewedoui
hal.identifierhal-00731162
hal.version1
hal.popularnon
hal.audienceInternationale
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-00731162v1
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