Abstract:This paper reviews results about free convection near a vertical flat plate embedded in some saturated porous medium. We focus on a third order autonomous differential equation that gives a special class of solutions called similarity solutions. Two cases are under consideration: in the first one we prescribe the temperature on the plate and in the second one we prescribe the heat flux on it. We will also see that the same equation appears in other industrial processes.
In this paper we use a recently elaborated abstract method, for parameter-dependent ODE systems over the interval (0, ∞), to obtain existence results for the problem of self-similar solutions in boundarylayer free convection in porous media. Using a generalization of the method to exponentially decaying solutions, we are able to recover some known results, and to obtain a new branch of solutions in the case of the so-called backward boundary-layer. The arguments involve the derivation of suitable a priori estimates for the solutions of the problem.
In this paper we use a recently elaborated abstract method, for parameter-dependent ODE systems over the interval (0, ∞), to obtain existence results for the problem of self-similar solutions in boundarylayer free convection in porous media. Using a generalization of the method to exponentially decaying solutions, we are able to recover some known results, and to obtain a new branch of solutions in the case of the so-called backward boundary-layer. The arguments involve the derivation of suitable a priori estimates for the solutions of the problem.
“…This gives the second inequality of (9). To obtain the other one, we set l ′ = inf Γ Θ and H − = inf{H + Θ − l ′ ; 0} and proceed in the same way.…”
Section: Let Us Clarify This Point To This End Formentioning
confidence: 99%
“…These boundary value problems have been widely studied, and mathematical results about them can be found, for example, in [1], [3], [4], [5], [6], [7], [8], [9], [10], [11], [12], [17], [18], [20] and [21].…”
“…Then the coefficients become: a 1 = m+1 2 1, a 2 = 0, a 3 = m. In this case, the equation takes the form (Brighi and Hoernel, 2005): As all the forms of the Blasius equation are third order ordinary differential equations (ODE), it is convenient to split it in three first order ODE's before solving. With f = g and f = g = h, the Blasius equation becomes:…”
Section: Flow Over a Wedgementioning
confidence: 99%
“…The nonlinear differential equation can be solved by using different approaches (Brighi and Hoernel, 2005;Zaturska and Banks, 2001). One common method is to convert the boundary value problem to an initial value problem, where the value of the velocity gradient f (0) = h(0) = s is estimated by using a shooting method for which f exists for [ 0,∞) and f (η L ) = g(η L ) = 1; η L is large value of η.…”
Abstract. The Blasius equation describes the properties of steady-state two dimensional boundary layer forming over a semi-infinite plate parallel to a unidirectional flow field. The flow is governed by a modified Blasius equation when the surface is aligned along the flow. In this paper, we demonstrate using numerical solution, that as the wedge angle increases, bifurcation occurs in the nonlinear Blasius equation and the dynamics becomes chaotic leading to nonconvergence of the solution once the angle exceeds a critical value of 22 • . This critical value is found to be in agreement with experimental results showing the development of shock waves in the medium and also with analytical results showing multiple solutions for wedge angles exceeding a critical value. Finally, we provide a derivation of the equation governing the boundary layer flow for wedge angles exceeding the critical angle at the onset of chaos.
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