Flow and heat transfer characteristics of the boundary layers over a stretching surface with a uniform-shear free stream

DOI10.1016/j.ijheatmasstransfer.2007.11.013zbMath1144.80313OpenAlexW2005160894MaRDI QIDQ927973

Tie-gang Fang

Publication date: 10 June 2008

Published in: International Journal of Heat and Mass Transfer (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1016/j.ijheatmasstransfer.2007.11.013

zbMATH Keywords

similarity solutionstretching surfacepower-law shear flowuniform-shear free stream

Mathematics Subject Classification ID

Related Items (13)

Axisymmetric flow with heat transfer over exponentially stretching sheet: a computational approach ⋮ Thermal boundary layers over a shrinking sheet: an analytical solution ⋮ A new solution branch for the Blasius equation -- a shrinking sheet problem ⋮ A new family of unsteady boundary layers over a stretching surface ⋮ Falkner-Skan boundary layer flow of a power-law fluid past a stretching wedge ⋮ Momentum and heat transfer of the Falkner-Skan flow with algebraic decay: an analytical solution ⋮ MHD slip flow of Newtonian fluid past a stretching sheet with thermal convective boundary condition, radiation, and chemical reaction ⋮ Heat transfer of a generalized stretching/shrinking wall problem with convective boundary conditions ⋮ Analytical prediction of multiple solutions for MHD Jeffery-Hamel flow and heat transfer utilizing KKL nanofluid model ⋮ Momentum and heat transfer of a special case of the unsteady stagnation-point flow ⋮ On similarity solution of heat and mass transfer in MHD Powell-Eyring fluid over a non-linear stretching surface ⋮ Multiple solutions of two-dimensional and three-dimensional flows induced by a stretching flat surface ⋮ Flow, heat, and species transfer over a stretching plate considering coupled Stefan blowing effects from species transfer

Uses Software

• Mathematica

Cites Work

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• The acoustic self-radiation impedance of a rigid oscillating disc near a similar stationary disc
• A method for integrating the boundary-layer equations through a region of reverse flow

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