The Analytical and a Higher-Accuracy Numerical Solution of a Free Boundary Problem in a Class of Discontinuous Functions

A newmethod is suggested for obtaining the exact and numerical solutions of the initial-boundary value problem for a nonlinear parabolic type equation in the domain with the free boundary. With this aim, a special auxiliary problem having some advantages over the main problem and being equivalent to the main problem in a definite sense is introduced. The auxiliary problem allows us to obtain the weak solution in a class of discontinuous functions. Moreover, on the basis of the auxiliary problem a higher-resolution numerical method is developed so that the solution accurately describes all physical properties of the problem. In order to extract the significance of the numerical solutions obtained by using the suggested auxiliary problem, some computer experiments are carried out.


Introduction
It is known that many practical problems such as distribution of heat waves, melting glaciers, and filtration of a gas in a porous medium, and so forth, are described by nonlinear equations of the parabolic type.
In 1 , at first the effect of localization of the solution of the equation describing the motion of perfect gas in a porous medium is observed and the solution in the traveling wave form is structured.Then, the mentioned properties of the solution for the nonlinear parabolic type equation are studied in 2, 3 , and so forth.
These problems are also called free boundary problems.Therefore, it is necessary to obtain the moving unknown boundary together with the solution of a differential problem.Its nature raises several difficulties for finding analytical as well as numerical solutions of this problem.
The questions of the existence and uniqueness of the solutions of the free boundary problems are studied in 4, 5 .In 5 , Oleȋnik introduced the notion of a generalized solution of the Stefan problem whose uniqueness and existence were guaranteed in the class of measurable bounded functions.In 4 , Kamenomostskaya considered the classical quasilinear heat conduction equation and constructed the generalized solution by the use of an explicit difference scheme.
In the literature there are some numerical algorithms homogeneous schemes which are approximated by finite differences of the differential problem without taking into account the properties occurring in the exact solution 6-8 .

Traveling Wave Solution of the Main Problem
We consider the equation conditions, where R 2 I × 0, T .Here, μ 0 and n are real known constants.In order to study the properties of the exact solution of the problem 2.1 -2.3 for the sake of simplicity the case ϕ u u σ is considered.It is clear that the function ϕ u satisfies the following conditions: ii ϕ u ≥ 0, for u ≥ 0 and σ ≥ 2, iii for σ ≥ 2, ϕ u have alternative signs on the domain when u x, t / 0. It is easily shown that the problem 2.1 -2.3 has the solution in the traveling wave form as

2.4
Via simple calculation we get the following: 1 the function u x, t and w x, t −∂u σ x, t /∂x Du x, t are continuous in

2.8
Changing the order of integration in the first integral and then applying the integration by parts to the inner integrals of the first and second terms in the last expression with respect to t and x, respectively, we have If we reapply integration by parts to the inner integrals in the first term and second term by t and x, respectively, we prove that the solution in the form 2.4 satisfies the integral relation 2.7 .

Auxiliary Problem and Its Exact Solution
In order to find the weak solution of the problem 2.1 -2.3 , according to 9, 10 the special auxiliary problem Here, the function v 0 x is any solution of the equation The problem 3.1 -3.3 has the solution in the traveling wave form 9 .As is seen from 3.5 , the differentiability property of the function v x, t is more than the differentiability property of the solution u x, t .In addition to this, from 3. The auxiliary problem has the following advantages.
i The function v x, t is smoother than u x, t .
ii The function v x, t is an absolutely continuous function.
iii In the process of finding the solution u x, t , one does not need to use the first and second derivatives of u x, t with respect to x.
The graphs of the function structured by the formulas 2.4 , 3.5 , and 3.6 are shown in the Figures 1 a , 1 b , and 2 a , respectively.

Developing a Numerical Algorithm in a Class of Discontinuous Functions
In this section we investigate an algorithm for finding a numerical solution of the problem 2.1 -2.3 .At first, we cover the region D t by a special grid: where τ is the step of the grid with respect to t variable.Now, we will develop a numerical algorithm as follows.Since the function ∂u σ /∂x is continuous, we can approximate the problem 3.1 -3.3 by the following finite differences schemes: and the grid function U i,k 1 defined by 4.5 is a solution of the nonlinear system of algebraic equations:

4.7
Here, V i,k and U i,k are the approximation values of v x, t and u x, t at any point x i , t k of the grid ω τ .For the sake of simplicity we introduce the notations

Convergence
In this section we will investigate some properties of the numerical solution and of the question of convergence of the numerical solution to the weak exact solution.Suppose that ε i,k , δ i,k , and η i,k are the errors of approximations of the functions ∂v/∂x, ∂v/∂t, and ∂ϕ/∂x by finite differences, respectively.Then, we can write 3.1 in the following form: where At first, we show that the finite difference scheme 4.2 is consistent; that is, γ i,k 1 approaches zero when τ → 0. It is known that the suitable characteristic of continuity of any function f x on the any interval a, b is its modulus continuity: Finally, Proof.At first, let us write 4.2 in the following form:

4.14
Assume that V i,k 1 is not constant and V i,k 1 takes the greatest value at some point of the grid ω τ rather than at boundary nodes of γ τ .Then, there is such a point x 1 , t 1 ∈ ω τ that V takes the maximal value and even some neighborhood points V x 1 , t 1 less than V x 1 , t 1 .
If V x 1 ,t 1 > V x 1 ,t 1 , because the function ϕ u u σ is monotone, the left part of the relation 4.14 is positive, but the right part is negative.Hence we arrive to inconsistency.We arrive to the same inconsistency if V ± x 1 , t 1 > V x 1 , t 1 .Similarly, we can prove that V does not take a minimal value at the inner nodes of the grid ω τ .
From Theorem 4.1, it follows that the solution of the problem 4.2 -4.4 converges to the solution of problem 3.1 -3.3 pointwise, that is, It can be easily seen that the solution of the mentioned problem is continuously dependent on initial data.Now, we will prove convergence of the U i,k to the solution of the main problem.To this end, by subtracting 4.2 from 4.9 and taking 4.5 into account, we have where R v i,k 1 − V i,k 1 .By multiplying the last equation with R and summing with respect to i and k, we get

4.18
Here, the symbol f, g denotes the differences analogy of the scalar product of the functions of f and g in L 2 ω τ sense:

4.19
With some algebra we have

4.20
It follows that the numerical solution U i,k converges in mean to u i,k .

Numerical Experiments
In order to extract the significance of the suggested method, the numerical solution obtained using the proposed auxiliary problem is compared with the exact solution of the problem 2.1 -2.Comparing Figures 1 a and 3 b shows that the numerical and the exact solutions of the main problem 2.1 -2.3 coincide.Moreover, the graphs of the functions v x, t and V i,k coincide, too.
Thus, the numerical experiments carried out show that the suggested numerical algorithms are efficient and economical from a computer point of view.The proposed algorithms permit us to develop the higher-resolution methods where the obtained solution correctly describes all physical features of the problem, even if the differentiability order of the solution of the problem is less than the order of differentiability which is required by the equation from the solution.
The finite differences scheme 4.2 -4.4 has the first-order approximation with respect to t.But using the different versions of Runge-Kutta's methods we can increase the order of the algorithms mentioned previously.

Conclusions
The new method is suggested for obtaining the regular weak solution for the free boundary problem of the nonlinear parabolic type equation.
The auxiliary problem which has some advantages over the main problem is introduced and it permits us to find the exact solution singular properties.
The auxiliary problem introduced previously allows us to develop the higher-resolution method where the obtained solution correctly describes all physical features of the problem, even if the differentiability order of the solution of the problem is less than the order of differentiability which is required by the equation from the solution.

Figure 1 :Figure 2 :
Figure 1: a The exact solution of the main problem.b The exact solution of the auxiliary problem.

Theorem 4 . 1
Maximum Principle .The solution of problem 4.2 -4.4 takes its maximum (or minimum) value on the boundary of the domain of definition of the solution, that is,

Figure 3 :
Figure 3: a Numerical solution of the problem 4.2 -4.4 .b Numerical solution of the main problem obtained by using the solution of the problem 4.2 -4.4 .
3 on an equal footing.With this aim, firstly, computer experiments are performed on the algorithm 4.2 -4.4 with the values σ 3, T 2, 4, and 6.The graphs of the obtained numerical solutions are presented in Figure 3 a .The numerical solutions of the main problem 2.1 -2.3 obtained by using the algorithm 4.2 -4.4 are shown in Figure 3 b .The numerical solution of the main problem obtained using the algorithm 4.6 -4.7 is demonstrated in Figure 2 b .
< σ < 2 the u t and u x exist, but u xx does not exist.Therefore when σ > 2, we must only consider the weak solution for the problem 2.1 -2.3 .As it is seen from the formula 2.4 , when n 1/ σ − 1 , the solution is equal to zero at holds for every test functions f x, t from o C1,1 D t and f x, T 0.Because the function u x, t and w x, t −∂u σ x, t /∂x are continuous in the domain D t , the integral involving 2.7 exists in the Riemann sense.Now, we show that the solution defined by the formula 2.4 satisfies the integral equality 2.7 ; that is, u x, t is the weak solution of the problem 2.1 -2.3 .According to the definition of the weak solution, we can write 0 1, 2, . . .; k 0, 1, 2, . . . .Here, h Dτ and v 0 x i is any grid function of 3.4 .It can be easily shown that