Heat Transfer in MHD Mixed Convection Flow of a Ferrofluid along a Vertical Channel
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作者:
Gul, Aaiza
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Univ Teknol Malaysia, Fac Sci, Dept Math Sci, Utm Skudai, Johor, MalaysiaUniv Teknol Malaysia, Fac Sci, Dept Math Sci, Utm Skudai, Johor, Malaysia
Gul, Aaiza
[1
]
Khan, Ilyas
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Majmaah Univ, Coll Engn, Majmaah, Saudi ArabiaUniv Teknol Malaysia, Fac Sci, Dept Math Sci, Utm Skudai, Johor, Malaysia
Khan, Ilyas
[2
]
Shafie, Sharidan
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Univ Teknol Malaysia, Fac Sci, Dept Math Sci, Utm Skudai, Johor, MalaysiaUniv Teknol Malaysia, Fac Sci, Dept Math Sci, Utm Skudai, Johor, Malaysia
Shafie, Sharidan
[1
]
Khalid, Asma
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Univ Teknol Malaysia, Fac Sci, Dept Math Sci, Utm Skudai, Johor, Malaysia
Sardar Bahadur Khan Womens Univ, Quetta, PakistanUniv Teknol Malaysia, Fac Sci, Dept Math Sci, Utm Skudai, Johor, Malaysia
Khalid, Asma
[1
,3
]
Khan, Arshad
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Univ Teknol Malaysia, Fac Sci, Dept Math Sci, Utm Skudai, Johor, MalaysiaUniv Teknol Malaysia, Fac Sci, Dept Math Sci, Utm Skudai, Johor, Malaysia
Khan, Arshad
[1
]
机构:
[1] Univ Teknol Malaysia, Fac Sci, Dept Math Sci, Utm Skudai, Johor, Malaysia
[2] Majmaah Univ, Coll Engn, Majmaah, Saudi Arabia
This study investigated heat transfer in magnetohydrodynamic (MHD) mixed convection flow of ferrofluid along a vertical channel. The channel with non-uniform wall temperatures was taken in a vertical direction with transverse magnetic field. Water with nanoparticles of magnetite (Fe3O4) was selected as a conventional base fluid. In addition, non-magnetic (Al2O3) aluminium oxide nanoparticles were also used. Comparison between magnetic and magnetite nanoparticles were also conducted. Fluid motion was originated due to buoyancy force together with applied pressure gradient. The problem was modelled in terms of partial differential equations with physical boundary conditions. Analytical solutions were obtained for velocity and temperature. Graphical results were plotted and discussed. It was found that temperature and velocity of ferrofluids depend strongly on viscosity and thermal conductivity together with magnetic field. The results of the present study when compared concurred with published work.
机构:
Univ Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USAUniv Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USA
Borglin, SE
Moridis, GJ
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Univ Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USAUniv Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USA
Moridis, GJ
Oldenburg, CM
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Univ Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USAUniv Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USA
机构:
Univ Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USAUniv Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USA
Borglin, SE
Moridis, GJ
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Univ Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USAUniv Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USA
Moridis, GJ
Oldenburg, CM
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Univ Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USAUniv Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USA