Abstract:The natural convection boundary-layer flow near a stagnation point on a permeable surface embedded in a porous medium is considered when there is local heat generation within the boundary layer at a rate proportional to The initial-value problem reveals that, for 1 p\2, the nontrivial steady states are stable and the solution evolves to this state at large times. However, for p [ 2 these steady states are unstable and the solution either approaches the trivial state with the local heating dying out or a finite… Show more
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