Review of similarity stretching exact solutions of the Navier-Stokes equations
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Publication:1940542
DOI10.1016/j.euromechflu.2011.05.006zbMath1258.76061OpenAlexW2075987850MaRDI QIDQ1940542
Publication date: 7 March 2013
Published in: European Journal of Mechanics. B. Fluids (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1016/j.euromechflu.2011.05.006
Navier-Stokes equations for incompressible viscous fluids (76D05) Dimensional analysis and similarity applied to problems in fluid mechanics (76M55) Research exposition (monographs, survey articles) pertaining to fluid mechanics (76-02)
Related Items (19)
Entropy optimized flow of hydromagnetic Reiner–Philippoff fluid over a stretching surface ⋮ Extending the traditional Jeffery-Hamel flow to stretchable convergent/divergent channels ⋮ Biorthogonal stretching and shearing of an impermeable surface in a uniformly rotating fluid system ⋮ On an equation arising in the boundary-layer flow of stretching/shrinking permeable surfaces ⋮ Unsteady boundary layer flow over a permeable curved stretching/shrinking surface ⋮ Existence of solutions of a system of 3D axisymmetric inviscid stagnation flows ⋮ Mixed convection in a Falkner-Skan system ⋮ Similarity solution of fractional viscoelastic magnetohydrodynamic fluid flow over a permeable stretching sheet with suction/injection ⋮ Existence and nonexistence of solutions on opposing mixed convection problems in boundary layer theory ⋮ Hiemenz stagnation-point flow impinging on a uniformly rotating plate ⋮ On some new exact solutions of incompressible steady state Navier-Stokes equations ⋮ Stretching or shrinking sheet problem for unsteady separated stagnation-point flow ⋮ The motion induced by a radially stretching membrane in a rotating fluid system ⋮ Multiple similarity solutions in boundary-layer flow on a moving surface ⋮ Multiple solutions of two-dimensional and three-dimensional flows induced by a stretching flat surface ⋮ Stagnation point flow and heat transfer over a non-linearly moving flat plate in a parallel free stream with slip ⋮ The motion induced by the orthogonal stretching and shearing of a membrane beneath a quiescent fluid ⋮ On an equation arising in natural convection boundary layer flow in a porous medium ⋮ Stagnation point flow past a stretching/shrinking sheet driven by arrhenius kinetics
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