Abstract

The effects of mixed convection on the classical Falkner–Skan similarity solutions are considered, now involving a mixed convection parameter $$\lambda $$ as well as the exponent m associated with the outer flow. The forced convection solutions indicate a singularity in the temperature field as $$m \rightarrow 0.070722$$ . Numerical solutions for $$m>0$$ show the existence of a critical value $$\lambda _\mathrm{c}$$ with $$\lambda _\mathrm{c}<0$$ and solutions only for $$\lambda \ge \lambda _\mathrm{c}$$ . The nature of the solution for $$\lambda \gg 1$$ is investigated. For $$m=0$$ , there are solutions for all $$\lambda <0$$ , opposing flow, and only for a finite range of $$\lambda $$ in aiding flow with the asymptotic solution as $$\lambda \rightarrow -\infty $$ also being considered. Solutions for $$m<0$$ are obtained in the cases when there is a solution to the Falkner–Skan system and for a value of m when no solution to this system exists. In the former case, two completely separate parts to the solution are seen, whereas in the latter case, a solution exists only in aiding flow for a limited range of $$\lambda $$ . The variation of solution with the exponent m is also treated for both aiding and opposing flows. In both cases, a solution is seen to exist for all $$m>0$$ , which, however, is limited to a relatively small range of m when $$m<0$$ .

Highlights

  • The original work by Falkner and Skan [1] presented a classical boundary-layer similarity solution, their results being extended by Hartree [2], see Rosenhead [3]

  • Our aim is to examine how the solution to this modified Falkner–Skan system behaves over the m − λ parameter plane, paying particular attention to those ranges of the mixed convection parameter λ where a solution can exist, finding that these depend to a large extent on the exponent m

  • Λc A significant feature of the results shown in Figs. 2, 3 and 4 is the existence of a critical value λc with dual solutions arising from the saddle–node bifurcation at λ = λc

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Summary

Introduction

The original work by Falkner and Skan [1] presented a classical boundary-layer similarity solution, their results being extended by Hartree [2], see Rosenhead [3]. A free stream U∞(x) ∝ xm flows over a fixed impermeable surface, where x measures distance along the bounding surface. This form for the outer flow allows the problem to be reduced to a similarity system, more usually characterized by the parameter β = 2m/(m + 1). The singular nature of the lower branch solutions as β → 0 from below was derived by Brown and Stewartson [5] Further solutions to this basic problem have been obtained by Craven and Peletier [6] for β > 1 (in the present notation) some exhibiting several regions of reversed flow. There can be branching solutions when β < βc as exhibited by Oskham

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