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The Well-Posedness of the Problem (FBP)

In this section we formulate sufficient conditions for the existence of a solution to the problems (P) and (FBP) and discuss cases of non-existence. The process described by these problems is, in general, driven by forces acting in opposite directions. A typical example is characterized by the boundary conditions and at (see [38,39,44]). Whereas the homogeneous boundary condition for and the positive velocity Q cause a dissolution effect, the positive inflow of prevents or hinders that process. This interaction of opposite influences distinguishes the considered problem from classical Stefan-like problems. Depending on the relation between the boundary conditions, pathological cases of degeneration or ill-posedness of the problem are possible as well as a well-posed dissolution problem. In the transformed problem (FBP), the right-hand side of the differential equation, g, represents the effect of the chemical reaction causing a consumption of u, since g is nonnegative. The flux function represents the difference, , between the imposed boundary conditions and the inflow, , which would be necessary to keep the chemical equilibrium in the whole domain.

If in the special case or if then is negative, i.e., the inflow is high enough to prevent the dissolution. In this case, the maximum principle forces the solution, u, to be negative in and the free boundary condition requires a monotone decreasing boundary function, . This means that zone I does not appear. Moreover, the boundary conditions are incompatible with the equilibrium state in zone II, i.e. the problem is ill-posed in this case.

In the other case the maximum principle does not yield any global statements about the sign of u or the monotony of s. The condition is sufficient to ensure the local solvability of the problem. If , the dissolution process is continuous. We prove the well-posedness of the problem in a more general case, admitting a non-monotonicity of the free boundary as a result of the interaction between dissolution and precipitation. In the following we present some existence, uniqueness and stability results. These results can be proved using a classical embedding technique and applying Schauders fixed point theorem to a integral representation for the free boundary function, The main idea of these methods was first presented in 1951 by Evans [13] and was employed and extended in numerous papers and monographes, e.g., [23], [24], [9], [40].





next up previous
Next: Solvability of problem Up: Dissolution Effects in Transport Previous: Reduction to a



Angela Pawell
Tue Aug 13 09:40:45 MET DST 1996