Effecfs of gravity on interdendritic fluid flow in large remelted ingots

Publication:
Effecfs of gravity on interdendritic fluid flow in large remelted ingots

dc.contributor.buuauthor	Yerebakan, Metin
dc.contributor.department	Mühendislik Fakültesi
dc.contributor.department	Makine Mühendiliği Bölümü
dc.date.accessioned	2023-03-30T10:41:43Z
dc.date.available	2023-03-30T10:41:43Z
dc.date.issued	1984
dc.description.abstract	This 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.
dc.identifier.citation	Yerebakan, M. (1984). "Effecfs of gravity on interdendritic fluid flow in large remelted ingots". Uludağ Üniversitesi Mühendislik Dergisi, 1(1), 43-56.
dc.identifier.endpage	56
dc.identifier.issn	2148-4147
dc.identifier.issue	1
dc.identifier.startpage	43
dc.identifier.uri	http://hdl.handle.net/11452/32078
dc.identifier.volume	1
dc.language.iso	en
dc.publisher	Uludağ Üniversitesi
dc.relation.journal	Uludağ Üniversitesi Mühendislik Dergisi / Uludağ University Journal of The Faculty of Engineering
dc.relation.publicationcategory	Makale - Uluslararası Hakemli Dergi
dc.rights	info:eu-repo/semantics/openAccess
dc.subject	Interdendritic fluid flow
dc.subject	Large remelted ingots
dc.title	Effecfs of gravity on interdendritic fluid flow in large remelted ingots
dc.type	Article
dspace.entity.type	Publication
local.contributor.department	Mühendislik Fakültesi/Makine Mühendiliği Bölümü