Natural convection in a sinusoidally heated cavity filled with ferrofluid in the presence of partial variable magnetic field

dc.contributor.authorGeridonmez, Pekmen
dc.contributor.authorÖztop, Hakan Fehmi
dc.date.accessioned2026-08-12T18:07:43Z
dc.date.issued2023
dc.departmentFırat Üniversitesi
dc.description.abstractPurpose The purpose of this study is to investigate partial magnetic source (MS) effect on natural convection (NC) flow of a ferrofluid flow in a cavity with sinusoidally heated vertical walls. The combination of ferrohydrodynamics and magnetohydrodynamics due to the variable magnetic field (MF) and magnetite nanoparticles in one part of the cavity, and the classical NC in the other part of the cavity are concerned. Design/methodology/approach The dimensionless equations in stream function-vorticity form are numerically solved by radial basis functions (RBF) based collocation method. Findings A remarkable change in fluid flow and heat transfer is noted if the MS location is close to the left sinusoidally heated wall. In particular, the average Nusselt number is the smallest for the middle centered partial MF through the left wall at a large Hartmann number. Research limitations/implications RBF collocation approach is limited to small geometries due to the obtained solution globally in the entire domain of the problem. Practical implications If the partial restriction of the effect of MF is done in real life, it would be a control parameter at some required/requested areas of the concerned problem. Social implications This is a physical problem. Originality/value If the proposed idea of partial variable MF is able to be applied to a system in real life, it would be a good controller on fluid flow and heat transfer. RBF-based methods are also alternative numerical procedures to solve heat transfer and fluid flow problems.
dc.identifier.doi10.1108/HFF-01-2022-0053
dc.identifier.endpage435
dc.identifier.issn0961-5539
dc.identifier.issn1758-6585
dc.identifier.issue1
dc.identifier.scopus2-s2.0-85133969461
dc.identifier.scopusqualityQ1
dc.identifier.startpage411
dc.identifier.urihttps://doi.org/10.1108/HFF-01-2022-0053
dc.identifier.urihttps://hdl.handle.net/11508/62820
dc.identifier.volume33
dc.identifier.wosWOS:000824267000001
dc.identifier.wosqualityQ1
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherEmerald Group Publishing Ltd
dc.relation.ispartofInternational Journal of Numerical Methods for Heat & Fluid Flow
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.snmzKA_WoS_20260511
dc.subjectRadial basis functions
dc.subjectNatural convection flow
dc.subjectPartial variable magnetic field
dc.subjectSinusoidal temperature distribution
dc.titleNatural convection in a sinusoidally heated cavity filled with ferrofluid in the presence of partial variable magnetic field
dc.typeArticle

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