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The well-posedness problem of an anisotropic porous medium equation with a convection term
Journal of Inequalities and Applications volume 2022, Article number: 108 (2022)
Abstract
The initial boundary value problem of an anisotropic porous medium equation is considered in this paper. The existence of a weak solution is proved by the monotone convergent method. By showing that \(\nabla u\in L^{\infty}(0,T; L^{2}_{\mathrm{loc}}(\Omega ))\), according to different boundary value conditions, some stability theorems of weak solutions are obtained. The unusual thing is that the partial boundary value condition is based on a submanifold Σ of \(\partial \Omega \times (0,T)\) and, in some special cases, \(\Sigma = \{(x,t)\in \partial \Omega \times (0,T): \prod a_{i}(x,t)>0 \}\).
1 Introduction
The well-posedness and regularity of weak solutions to the porous medium equation
or
were addressed from the sixties to eighties in the twentieth century by many mathematicians, one can refer to [3, 6, 17, 18, 21, 22] and the references therein. Later, DiBenedetto [2] and Ziemer [28] studied the regularity to the more general equation
considering suitable assumptions on a⃗ and b. The proofs followed different approaches: DiBenedetto’s proof was based on a parabolic version of De Giorgi’s technique, while Ziemer’s approach was related to Moser’s iteration technique. But, since many reaction-diffusion processes depend on different environments, one should consider a reaction-diffusion equation with anisotropic characteristic, then the anisotropic porous medium equation modeled by
was introduced and studied since 1980s. Actually, Song [19, 20] studied the existence and uniqueness of the very weak solution of the anisotropic porous medium equation with singular advections and absorptions. Henriques [7] established an interior regularity result for the solutions of (1.4). Li [11] developed the finite element method to derive a special analytical solution for anisotropic porous medium equation for time-independent diffusion. Also, several applied models related to an anisotropic porous medium have been introduced recently. The first one is the flow diverter model. Since the explicit modeling of thin wires of simulation of flow diverter (FD) imposes extremely high demand of computational resources and time, such a fact limits its use in time-sensitive presurgical planning. One alternative approach is to model as a homogenous porous medium, which saves time but with compromise in accuracy. Then, Ou et al. [13] proposed a new method to model FD as a heterogeneous and anisotropic porous medium whose properties were determined from local porosity. The second one is a multiple-relaxation-time lattice Boltzmann model for the flow and heat transfer in a hydrodynamically and thermally anisotropic porous medium [8]. The third one arises from computational fluid dynamics (CFD). Doumbia et al. [5] gave a CFD modelling of an animal occupied zone using an anisotropic porous medium model with velocity-dependent resistance parameters. Another model comes from the physical characteristics of cracked rocks. By testing elastic velocities and Thomsen parameters—as a function of crack density for fixed values of aspect ratio—predicted by the model with data acquired from synthetic rock samples, Nascimento et al. [12] introduced a new ultrasonic physical model in an anisotropic porous cracked medium.
Moreover, in the theory of PDE, the anisotropic equation has provoked more people’s attention in recent time. For example, the existence and multiplicity of nontrivial solutions to the anisotropic elliptic equation
has been an active topic in recent years (see [4, 15, 16], etc.), while the anisotropic parabolic equation
In this paper, we consider the well-posedness of weak solutions to the following initial boundary value problem:
with
and
Compared with equation (1.1), we call equation (1.7) an anisotropic medium equation with a convection term. Apart from the anisotropic characteristic of equation (1.7), we are concerned with whether the homogeneous boundary value condition (1.9) is overdetermined or not. In our previous work [27], we made the usual exploration on the following porous medium equation:
We found that if one wants to prove the uniqueness (or the stability) of weak solutions to this equation, the homogeneous boundary value condition (1.9) can be replaced by that \(a(x)=0\), \(x\in \partial \Omega \). Even much earlier, Yin and Wang [23, 24] studied the following equation:
divided the boundary value condition into three parts, and in particular they showed that if \(a(x)=0\), \(f_{i}(x)=0\) when \(x\in \partial \Omega \), then the uniqueness of a weak solution to equation (1.11) can be proved independent of the boundary value condition (1.9). The optimal boundary value condition matching up with equation (1.11) was studied by the author recently in [26].
Instead of \(a(x)|_{x\in \partial \Omega}=0\) in [27], we only assume that \(a_{i}(x,t)>0\), \((x,t)\in \Omega \times (0,T)\) and do not emphasize that
So, for any given \(t\in [0,T]\), both
and
may have a positive \((N-1)\)-dimensional Hausdorff measure in ∂Ω. Naturally, based on past experience [23, 24, 27], we guess that a partial boundary value condition
is enough to ensure the well-posedness of weak solutions to equation (1.7). The further work is to specify the explicit expression of Σ in (1.12). Different from other related references [23, 24, 27] in which Σ is just a cylinder, we found that Σ appearing in (1.12) is a submanifold of \(\partial \Omega \times (0,T)\) and, in some special cases, \(\Sigma = \{(x,t)\in \partial \Omega \times (0,T): \prod a_{i}(x,t)>0 \}\).
Actually, compared with [7, 19, 20], the degeneracy of diffusion coefficient \(a_{i}(x,t)\) has brought more essential difficulties. For example, maybe it is not difficult to construct the fundamental solution of equation (1.4) by Barenblatt’s method, but it is impossible to construct the corresponding fundamental solution of the simplest anisotropic porous medium equation
by a similar method. However, the main aim of this paper is to study the well-posedness of weak solutions to equation (1.7), and we pay no attention to the fundamental solution for the time being. The local integrability \(\nabla u\in L^{\infty}(0,T; L^{2}_{\mathrm{loc}}(\Omega ))\), which was found for the first time in this paper, acts as an important role to overcome the above difficulties.
The remainder of this paper is structured as follows. In Sect. 2, we present the definition of weak solution and the main results. In Sect. 3, the existence of a weak solution is proved. In Sect. 4, the stability of a weak solution to the usual initial boundary value problem is studied. In Sect. 5, the local integrability of ∇u is found and the uniqueness of a weak solution to the usual initial boundary value problem is obtained. In Sect. 6, when \(\prod_{i=1}^{N}a_{i}(x,t)|_{x\in \partial \Omega}=0\), the stability of a weak solution based on a partial boundary value condition is proved. In Sect. 7, we prove the stability of weak solutions under the general condition \(\prod_{i=1}^{N}a_{i}(x,t)\geq 0\).
2 The definition of the weak solution and the main results
The definition of weak solution and the main results of this paper are listed below.
Definition 2.1
A function \(u(x,t)\) is said to be a weak solution of equation (1.7) if
and for any function \(\varphi \in C_{0}^{1} ({Q_{T}})\), there holds
The initial value condition is satisfied in the sense of that
where \(\phi (x)\in C_{0}^{\infty}(\Omega )\). The boundary value condition (1.9) or the partial boundary value condition (1.12) is satisfied in the sense of trace.
Theorem 2.2
If \(\alpha _{i}>0\), \(b_{i}(s,x,t)\) is a \(C^{1}\) function and \(\vert \frac{\partial}{\partial x_{i}}b_{i}(s,x,t) \vert \leq c(M)\) when \(|s|\leq M+1\), \({u_{0}}(x)\) satisfies
\(a_{i}(x,t)\geq 0\) satisfies
then equation (1.7) with initial boundary values (1.8)–(1.9) has a nonnegative solution. Here and the after, M is a constant such that \(\|u_{0}(x)\|_{L^{\infty}(\Omega)}\leq M\).
From Theorem 2.3 to Theorem 2.6, we all assume that \(a_{i}(x,t)>0\), \(x\in \Omega \) and denote that
Theorem 2.3
Let \(u(x,t)\) and \(v(x,t)\) be two solutions of equation (1.7) with the initial value \({u_{0}}(x)\), \(v_{0}(x)\) respectively, and with the boundary value condition (1.9). If \(\alpha _{i}\geq 0\), and there is a constant \(\alpha >\frac{1}{2}(\alpha ^{+}+2)\) such that
then the solution of equation (1.7) is unique.
Theorem 2.4
Let \(u(x,t)\) and \(v(x,t)\) be two nonnegative solutions of equation (1.7) with the initial value \({u_{0}}(x)\), \(v_{0}(x)\) respectively, with the same boundary value condition (1.9). If \(\alpha _{i}\geq 1\),
then
Theorem 2.4 implies that we only can show that the stability of weak solutions is true for a kind of solutions which satisfy (2.7). The following stability theorems are established on a partial boundary value condition.
Theorem 2.5
Let \(u(x,t)\) and \(v(x,t)\) be two solutions of equation (1.7) satisfying
with the initial value \({u_{0}}(x)\), \(v_{0}(x)\) respectively, and with a partial boundary value condition
If \(\alpha ^{-}\geq 1\), \(b_{i}(\cdot ,x,t)\) satisfies
then
Here,
and \(\Omega _{\lambda t}= \{x\in \Omega : \prod_{i=1}^{N}a_{i}(x,t)> \lambda \}\).
Theorem 2.5 is based on the fact that we can show the first order partial derivative to the solution u is with the local integrability
The weakness of Theorem 2.5 is that the expression of Σ, (2.15) seems too complicated. By choosing another test function, we can prove another stability theorem based on a simpler partial boundary value condition.
Theorem 2.6
Suppose \(\alpha ^{-}\geq 1\),
Let \(u(x,t)\) and \(v(x,t)\) be two solutions of equation (1.7) with the initial value \({u_{0}}(x)\), \(v_{0}(x)\) respectively, but without the boundary value condition. If (2.13) is true and
then
We find that the partial boundary value conditions with (2.12) are submanifold of \(\partial \Omega \times (0,T)\), while in the previous works the corresponding partial boundary value conditions are the cylinder domains \(\Sigma _{1}\times (0,T)\), where \(\Sigma _{1}\subseteq \partial \Omega \) is a relatively open subset [9, 10, 23, 25, 27], etc.
Last but not least, once the well-posedness problem has been solved, we can consider the extinction, blow-up phenomena, the positivity, and the large time behavior of the weak solutions of anisotropic porous medium equation (1.7) in the future. However, different from the porous medium equation, because of the anisotropy, these problems are not so easy to be solved, the methods used in the usual porous medium equation (1.1) cannot be extended to the anisotropic porous medium equation (1.13) directly.
3 The existence of weak solution
Proof of Theorem 2.2
We consider the following normalized problem:
where \(a_{in}(u,x,t) \geqslant c(n) > 0\), and
Similar to the porous medium equation (1.1), we can show that problem (3.1) has a nonnegative solution \(u_{n}\), which is called as a viscous solution generally and satisfies
and by comparison theorem, we have
Thus
is well defined. Now, we will prove u is a weak solution of (1.7).
First, multiplying both sides of the first equation in (3.1) by \(\phi = u_{n}-\frac{1}{n}\), denoting that \(Q_{t}=\Omega \times (0,t)\) for \(t\in (0,T)\), then
Since
we have
Thus, from (3.5), we can find that
which implies
By choosing a subsequence, we may assume that
weakly in \(L^{2}(Q_{T})\).
In the second step, we want to show that
For any \(\forall \psi \in C_{0}^{1}(Q_{T})\), we have
Let \(n\rightarrow \infty \). Then
For the right-hand side of (3.9), by the assumption
using the dominated convergent theorem, we have
From (3.9)–(3.11), we obtain (3.8).
In the third step, since \(b_{i}\in C^{1}\), by (3.4), we have
Moreover, by a BV estimate method [9, 10], we can show that
and
Then \(u_{t}\in L^{1}(Q_{T})\) and (2.1) is true, and we can define the trace of u on the boundary ∂Ω. The initial value condition true in the sense of (2.3) can be found in [22] etc.
Thus, u is a solution of equation (1.7) with the initial value (1.8) and the homogeneous boundary value condition (1.9). Theorem 2.2 is proved. □
Finally, we would like to point out that, though the viscous solution \(u_{n}\) satisfies (3.3), we cannot deduce that the solution u of equation (1.7) satisfies
Actually, in the next section, we will show that
4 The uniqueness of weak solution of the usual initial boundary value problem
Proposition 4.1
Let \(u(x,t)\) be a solution of equation (1.7). Then
Proof
Let \(u_{n}\) be the viscous solution of the initial boundary value (3.1)–(3.3). If we choose \((u_{n}-u)\phi \) as the test function, where \(\phi \in C_{0}^{1}(Q_{T})\), then
Let \(n \rightarrow \infty \) in (4.2). We can deduce that
and this equality yields
Due to the arbitrariness of ϕ and \(|u_{n}|^{\alpha _{i}}u_{n x_{i}}\in L^{1} (0,T; L_{\mathrm{loc}}^{2}( \Omega ) )\), there holds
□
Theorem 4.2
If there is β, \(1>\beta >0\), and there is a nonnegative function \(g_{i}(x,t)\) such that
then the nonnegative solution of equation (1.7) is unique.
Proof
For a small positive constant \(\delta >0\), denoting \(D_{\delta}=\{x\in \Omega : w=u-v>\delta \}\), we suppose that the measure \(\mu (D_{\delta})>0\). Let
where \(\delta >2\lambda >0\), \(1>\beta >0\).
Now, by a process of limit, we can choose \(F_{\lambda}(w)=F_{\lambda}(u-v)\) and integrate it over \(Q_{t}\), \(0\leq t< T\), accordingly,
In the first place,
In the second place, by (4.3), (4.4), we have
In the third place, by (4.3), since u and v both are nonnegative,
we have
Last but not least, let \(t_{0}=\inf \{\tau \in (0,t]: w>\lambda \}\). Then
Letting \(\lambda \rightarrow 0\), we get the contradiction. □
Proof of Theorem 2.3
If condition (2.6) is true, then conditions (4.3),(4.4) are true naturally. Thus, we have Theorem 2.3. □
5 The stability of weak solution of the usual initial boundary value problem
For any given positive integer n, let \({g_{n}}(s)=\int _{0}^{s}h_{n}(\tau )\,d\tau \), \(h_{n}(s)=2n ( 1-n| s| )_{+}\). Then \(h_{n}(s)\in C(\mathbb{R})\), and
and
As we have pointed out in the introduction section, for the classical porous medium equation
if \(u(x,t)\) and \(v(x,t)\) are two nonnegative solutions of the initial boundary value problem, by choosing \(g_{n}(u^{m}-v^{m})\) as the test function, we easily show that
Now, for the anisotropic diffusion equation (1.7) considered in this paper, since \(\alpha _{i}\) may be different from one to another, though for every i
we cannot choose \(g_{n}(u^{1+\alpha _{i}}-v^{1+\alpha _{i}})\) as a test function. If we insist on using a similar method to obtain the stability (5.3), then only for a kind of weak solution we can achieve the requirement.
Theorem 5.1
Let \(u(x,t)\) and \(v(x,t)\) be two nonnegative solutions of the initial boundary value problem (1.7)–(1.9) satisfying (2.7). If \(\alpha _{i}\geq 1\),
and
then the stability (5.3) is true.
Proof
By a process of limit, we can choose \({g_{n}}(u- v)\) as the test function, then
Obviously,
By (2.7) and \(\alpha _{i}\geq 1\), using the Lebesgue dominated theorem, we have
We now prove that
In detail, by (5.4), we have
Here, we have used the notation
Let \(n\rightarrow \infty \) in (5.12). Since (5.5),
if \(D_{0}=\{ x \in \Omega :|u- v| = 0\}\) is a set with 0 measure, by that
we have
While \(D_{0}=\{ x \in \Omega :|u - v| = 0\}\) has a positive measure, by that
then
Thus, in both cases, the right-hand side of inequality (5.12) goes to 0 as \(n\rightarrow \infty \).
Moreover,
At last, let \(n\rightarrow \infty \) in (5.6). Then
□
Proof of Theorem 2.4
Since we assume conditions (2.7)–(2.8), conditions (5.4)–(5.5) are true naturally, by Theorem 5.1, we clearly have Theorem 2.4. □
6 The partial boundary value condition based on a submanifold
In this section, we consider equation (1.7) with the initial value condition (1.8) and with a partial boundary value condition (2.12). For a small positive constant \(\lambda >0\) and any \(t\in [0,t)\), let
and set
Proof of Theorem 2.5
If we choose \(\phi g_{n}(u- v)\) as the test function, then
Clearly, we have
and from \(\iint _{Q_{T}}|u_{t}|\,dx\,dt \leq c\), we deduce
Since
by that \(\alpha _{i}\geq 1\), using the Lebesgue dominated theorem, we have
At the same time, if we denote that
then by (2.10) we have
For the convection term, by (6.5) and (2.13), we have
By (2.13), using the homogeneous boundary value condition (2.12), we have
Now, after letting \(n\rightarrow \infty \), let \(\lambda \rightarrow 0\) in (6.2). Then
Theorem 2.5 is proved. □
7 The proof of Theorem 2.6
In this section, we prove Theorem 2.6. For a small positive constant \(\lambda >0\) and any \(t\in [0,t)\), set \(\Omega _{\lambda t}\) and \(\phi (x)\) as (6.1).
Proof of Theorem 2.6
Let \(u(x,t)\), \(v(x,t)\) be two solutions of equation (1.7) with the initial boundary values \(u_{0}(x)\), \(v_{0}(x)\) respectively, but without the partial boundary value condition (2.12). By assumption (2.17), we can choose \({g_{n}}(\phi (u- v))\) as the test function and get
In the first place, we have
Clearly,
and
Since \(a_{i}(x,t)\) satisfies (2.17) and
by that \(\alpha ^{-}\geq 1\) and
using the Lebesgue dominated convergence theorem, we have
In the second place, we have
While by (2.18)
we have
Similarly, we have
In the third place, since (1.13) \(|b_{i}(u,x,t)-b_{i}(v,x,t)|\leq c\sqrt{a_{i}(x,t)}\), we have
Moreover, since (4.1), we clearly have
Now, let \(n\rightarrow \infty \) in (7.1). Then
Theorem 2.6 is proved. □
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The authors would like to express their sincere thanks to the reviewers and the editors.
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The paper is supported by NSFC-52171308, China.
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The first author, Dr. YZ, made the main calculations and accomplished the original manuscript. The corresponding author, Prof. HZ, gave the idea, checked the calculations, and completed the final submission. The needed APC of this paper will be paid by the first author. All authors read and approved the final manuscript.
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Zhi, Y., Zhan, H. The well-posedness problem of an anisotropic porous medium equation with a convection term. J Inequal Appl 2022, 108 (2022). https://doi.org/10.1186/s13660-022-02847-4
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DOI: https://doi.org/10.1186/s13660-022-02847-4
MSC
- 35L65
- 35K55
- 35B05
Keywords
- Anisotropic porous medium equation
- Stability theorem
- Partial boundary condition
- Submanifold