Unsteady three-dimensional boundary layer flow due to a permeable shrinking sheet

DOI10.1007/s10483-010-1372-6zbMath1428.76058OpenAlexW2036194566MaRDI QIDQ618919

Anuar Ishak, Ioan Pop, Norfifah Bachok

Publication date: 17 January 2011

Published in: Applied Mathematics and Mechanics. (English Edition) (Search for Journal in Brave)

Full work available at URL: http://psasir.upm.edu.my/id/eprint/17526/1/Unsteady%20three.pdf

Mathematics Subject Classification ID

Boundary-layer theory, separation and reattachment, higher-order effects (76D10)

Related Items (6)

Melting heat transfer in boundary layer stagnation-point flow towards a stretching/shrinking sheet in a micropolar fluid ⋮ On new numerical techniques for the MHD flow past a shrinking sheet with heat and mass transfer in the presence of a chemical reaction ⋮ Review of similarity stretching exact solutions of the Navier-Stokes equations ⋮ On dual solutions of the three‐dimensional Hiemenz flow over a stretching/shrinking sheet ⋮ Thermo-physical characteristics during the flow and heat transfer analysis of GO-nanoparticles adjacent to a continuously moving thin needle ⋮ A new numerical solution of Maxwell fluid over a shrinking sheet in the region of a stagnation point

Cites Work

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• Effects of slip condition on MHD stagnation-point flow over a power-law stretching sheet
• MHD rotating flow of a viscous fluid over a shrinking surface
• Thermal boundary layers over a shrinking sheet: an analytical solution
• MHD boundary-layer flow due to a moving extensible surface
• Boundary layer flow over a shrinking sheet with power-law velocity
• Exact solutions for self-similar boundary-layer flows induced by permeable stretching walls
• A new solution branch for the Blasius equation -- a shrinking sheet problem
• The three-dimensional flow due to a stretching flat surface
• On Boundary Layers in Fluid Mechanics that Decay Algebraically along Stretches of Wall that are not Vanishingly Small
• Hydromagnetic flow and heat transfer over a stretching sheet
• Viscous flow due to a shrinking sheet

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