MHD Natural Convection Slip Flow through Vertical Porous Plates with Time-Periodic Boundary Conditions

dc.contributor.authorAdesanya, Samuel
dc.date.accessioned2022-08-05T12:19:29Z
dc.date.available2022-08-05T12:19:29Z
dc.date.issued2018
dc.description.abstractIn this work, the convective flow of heat generating hydromagnetic fluid through a leaky channel is investigated. Due to channel porosity, the asymmetrical slip conditions are imposed on both walls. The coupled dimensionless partial differential equations are reduced to a system of second-order boundary-value problems based on some flow assumptions and solved by Adomian decomposition method (ADM). Variations in velocity and temperature profiles are presented and discussed in detail. The result of the analysis revealed that increasing Hartmann number decreases the flow velocity while the slip parameters enhance the flow.en_US
dc.identifier.issn1662-9507
dc.identifier.urihttp://dspace.run.edu.ng:8080/jspui/handle/123456789/3560
dc.language.isoenen_US
dc.publisherDefect and Diffusion Forumen_US
dc.relation.ispartofseries388;135-145
dc.subjectMagnetic fielden_US
dc.subjectBuoyancy forceen_US
dc.subjectOhmic heatingen_US
dc.subjectInternal heat generationen_US
dc.subjectAdomian Decomposition Methoden_US
dc.titleMHD Natural Convection Slip Flow through Vertical Porous Plates with Time-Periodic Boundary Conditionsen_US
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