Boundary-layer non-Newtonian flow over vertical plate in porous medium saturated with nanofluid
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Publication:764600
DOI10.1007/s10483-011-1524-7zbMath1382.76006OpenAlexW2046666283MaRDI QIDQ764600
Publication date: 13 March 2012
Published in: Applied Mathematics and Mechanics. (English Edition) (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1007/s10483-011-1524-7
Non-Newtonian fluids (76A05) Free convection (76R10) Boundary-layer theory for compressible fluids and gas dynamics (76N20)
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Mathematical modelling of radiative hydromagnetic thermosolutal nanofluid convection slip flow in saturated porous media ⋮ The influence of slip boundary condition on Casson nanofluid flow over a stretching sheet in the presence of viscous dissipation and chemical reaction ⋮ Thermal dispersion effects on convective heat and mass transfer in an Ostwald de Waele nanofluid flow in porous media ⋮ Non-Newtonian effect on natural convection flow over cylinder of elliptic cross section ⋮ Numerical study for Carreau nanofluid flow over a convectively heated nonlinear stretching surface with chemically reactive species ⋮ Magneto-hydrodynamic mixed convection of a non-Newtonian power-law nanofluid past a moving vertical plate with variable density ⋮ Thermal conductivity variation and heat generation effects on magneto-hybrid nanofluid flow in a porous medium with slip condition
Cites Work
- Thermal conductivity of non-Newtonian nanofluids: experimental data and modeling using neural network
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- The Cheng-Minkowycz problem for natural convective boundary-layer flow in a porous medium saturated by a nanofluid
- Thermal instability in a porous medium layer saturated by a nanofluid
- Buoyancy induced flows in a saturated porous medium adjacent to impermeable horizontal surfaces
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- Conceptions for heat transfer correlation of nanofluids
- Free convection boundary-layer flow along a vertical surface in a porous medium with Newtonian heating
- Free Convection from a Horizontal Surface in a Porous Medium with Newtonian Heating
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