Effecfs of gravity on interdendritic fluid flow in large remelted ingots

dc.contributor.buuauthorYerebakan, Metin
dc.contributor.departmentMühendislik Fakültesi
dc.contributor.departmentMakine Mühendiliği Bölümü
dc.date.accessioned2023-03-30T10:41:43Z
dc.date.available2023-03-30T10:41:43Z
dc.date.issued1984
dc.description.abstractThis paper presents analytic calculations of the interdendritic fluid-flow in mush zones whose width is small compared to their length, a situation which is caracteristic of large remelted ingots. The flow is found to consist of two main components. The first one is normal to the isotherms which feeds solidifi­cation shrinkage and the second one is parallel to the isotherms which is produced by gravity acting on desity differences in the interdendritic liquid. If the isotherms are not exactly parallel, then the gravity induced flow parallel to the isotherms induces a component normal to it. This companent may cause the freckles that occur in remelted ingots when melting conditions are changed.en_US
dc.identifier.citationYerebakan, M. (1984). "Effecfs of gravity on interdendritic fluid flow in large remelted ingots". Uludağ Üniversitesi Mühendislik Dergisi, 1(1), 43-56.tr_TR
dc.identifier.endpage56tr_TR
dc.identifier.issn2148-4147
dc.identifier.issue1tr_TR
dc.identifier.startpage43tr_TR
dc.identifier.urihttp://hdl.handle.net/11452/32078
dc.identifier.volume1tr_TR
dc.language.isoenen_US
dc.publisherUludağ Üniversitesitr_TR
dc.relation.journalUludağ Üniversitesi Mühendislik Dergisi / Uludağ University Journal of The Faculty of Engineeringtr_TR
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergitr_TR
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectInterdendritic fluid flowen_US
dc.subjectLarge remelted ingotsen_US
dc.titleEffecfs of gravity on interdendritic fluid flow in large remelted ingotsen_US
dc.typeArticleen_US
local.contributor.departmentMühendislik Fakültesi/Makine Mühendiliği Bölümütr_TR

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