Roles of Weight Functions to a Nonlocal Porous Medium Equation with Inner Absorption and Nonlocal Boundary Condition
Abstract
This work is concerned with an initial boundary value problem for a nonlocal porous medium equation with inner absorption and weighted nonlocal boundary condition. We obtain the roles of weight function on whether determining the blowup of nonnegative solutions or not and establish the precise blow-up rate estimates under some suitable condition.
1. Introduction
Many natural phenomena have been formulated as nonlocal diffusive equation (1.1), such as the model of non-Newton flux in the mechanics of fluid, the model of population, biological species, and filtration (we refer to [1, 2] and the references therein). For instance, in the diffusion system of some biological species with human-controlled distribution, u(x, t), Δum, up∫Ωuq(y, t)dy, and −k represent the density of the species, the mutation, the human-controlled distribution, and the decrement rate of biological species at location x and time t, respectively. Due to the effect of spatial inhomogeneity, the arising of nonlocal term denotes that the evolution of the species at a point of space depends not only on the density of species in partial region but also on the total region (we refer to [3–5]). However, there are some important phenomena formulated as parabolic equations which are coupled with weighted nonlocal boundary conditions in mathematical models, such as thermoelasticity theory. In this case, the solution u(x, t) describes entropy per volume of the material (we refer to [6, 7]).
- (a)
If 1 ≤ q < r, then the solution of the problem exists globally.
- (b)
If q > r ≥ 1, the problem has solutions blowing up in finite time as well as global solutions. That is,
- (i)
if ∫Ωf(x, y)dy ≤ 1, and u0(x)≤(α/|Ω|) 1/(r−q), then the solution exists globally;
- (ii)
if ∫Ωf(x, y)dy > 1, and u0(x)>(α/(|Ω | − α)) 1/r (|Ω | > α), then the solution blows up in finite time;
- (iii)
for any f(x, y) ≥ 0, there exists a2 > 0 such that the solution blows up in finite time provided that u0(x) > a2ϕ(x), where ϕ(x) is the corresponding normalized eigenfunction of −Δ with homogeneous Dirichlet boundary condition, and ∫Ωϕ(x)dx = 1.
- (i)
- (c)
If q = r > 1.
- (i)
The solution blows up in finite time for any f(x, y) ≥ 0 and large enough u0.
- (ii)
If ∫Ωf(x, y)dy < 1, the solution exists globally for u0(x) ≤ a1Φ(x) for some a1 > 0, where Φ(x) solves the following problem:
(1.12)
- (i)
In addition, for the initial boundary value problem of (1.11) with weighted nonlinear boundary condition and Dirichlet boundary condition, we refer to [15, 16] and references therein, respectively.
The aim of this paper is to obtain the sufficient condition of global and blow-up solutions to problem (1.1)–(1.3) and to extend the results of the semilinear equation (1.11) to the quasilinear ones. The difficulty lies in finding the roles of weighted function in the boundary condition and the competitive relationship of nonlocal source and inner absorption on whether determining the blowup of solutions or not. Our detailed results are as follows.
Theorem 1.1. Suppose that p + q > r. If ∫Ωf(x, y)dy ≥ 1 for x ∈ ∂Ω, and the initial data u0(x)>(k/(|Ω| − k)) 1/(p+q) (|Ω | > k), then the solution of problem (1.1)–(1.3) blows up in finite time.
Remark 1.2. There may exist a global solution of problem (1.1)–(1.3) for small enough initial data under the condition of Theorem 1.1. Unfortunately, since the weight function satisfies the condition ∫Ωf(x, y)dy ≥ 1 on the boundary, we cannot construct a suitable supersolution of problem (1.1)–(1.3).
Theorem 1.3. Suppose that p + q > r, if ∫Ωf(x, y)dy ≤ 1 for x ∈ ∂Ω, then the solution of problem (1.1)–(1.3) exists globally for the initial data u0(x)<(k/|Ω|) 1/(p+q−r). If p + q ≥ max {m, r}, then the solution of problem (1.1)–(1.3) blows up in finite time for large enough initial data and arbitrary f(x, y) > 0.
Theorem 1.4. Suppose that p + q < r,then the solution of problem (1.1)–(1.3) exists globally for arbitrary f(x, y) > 0.
Theorem 1.5. Suppose that p + q = r. ∫Ωf(x, y) ≤ ρ < 1 for x ∈ ∂Ω, where ρ is a positive constant and ρ < 1.
- (1)
If m > p + q, then every nonnegative solution of problem (1.1)–(1.3) exists globally.
- (2)
If m = p + q, then for |Ω | < k + (δ/M1)(1 − ρm), the solution of problem (1.1)–(1.3) exists globally, where δ, M1 > 0 are as defined in (3.13).
- (3)
If m < p + q, the solution of problem (1.1)–(1.3) exists globally for sufficient small initial data while it blows up in finite time for large enough initial data.
- (C1)
, for x ∈ Ω;
- (C2)
there exists a constant δ′ > 0, such that
(1.13)
Theorem 1.6. Suppose that p + q > max {m, r}, ∫Ωf(x, y)dy ≤ 1 for x ∈ ∂Ω, and the initial data satisfies the conditions (C1)-(C2), then
The rest of our paper is organized as follows. In Section 2, with the definitions of weak upper and lower solutions, we will give the comparison principle of problem (1.1)–(1.3), which is an important tool in our research. The proofs of results of global existence and blow-up of solutions will be given in Section 3. And in Section 4, we will give the blow-up rate estimate of the blow-up solutions.
2. Comparison Principle and Local Existence
In this section, we establish a suitable comparison principle for problem (1.1)–(1.3). Let , and ST = ∂Ω × (0, T). Firstly, we start with the precise definitions of upper solution and lower solution of problem (1.1)–(1.3).
Definition 2.1. Suppose that is nonnegative and satisfies
Similarly, a nonnegative function is an upper solution if it satisfies (2.1)–(2.3) in the reverse order. We say u(x, t) is a solution of problem (1.1)–(1.3) in QT if it is both an upper solution and a lower solution of problem (1.1)–(1.3) in QT which is called classical solution.
The following comparison principle plays a crucial role in our proofs which can be obtained by establishing suitable test function and Gronwall’s inequality.
Proposition 2.2 (comparison principle). Suppose that and are the nonnegative subsolution and supersolution of problem (1.1)–(1.3), respectively. Moreover , and in , then in .
Proof. Let ψ(x, t) ∈ C2,1(QT) be a nonnegative function with ψ = 0 on ST. Multiplying the inequality in (2.1) by ψ(x, t) and integrating it on QT, we get
For x ∈ ∂Ω, y ∈ Ω, t > 0,
Next, we state the local existence and uniqueness theorem without proof.
Theorem 2.3 (local existence and uniqueness). Suppose that the nonnegative initial data satisfies the compatibility condition. Then, there exists a constant T* > 0 such that the problem (1.1)–(1.3) admits nonnegative solution for each T < T*. Furthermore, either T* = ∞ or
Remark 2.4. The existence of local nonnegative solutions in time to problem (1.1)–(1.3) can be obtained by using the fixed point theorem (see [18]) or the regular theory to get the suitable estimate in a standard limiting process (see [19, 20]). By the previous comparison principle, we can get the uniqueness of solution to the problem (1.1)–(1.3) in the case of p + q ≥ 1, r ≥ 1.
3. Global Existence and Blowup of Solutions
Comparing problems with the general homogeneous Dirichlet boundary condition, the existence of weight function on the boundary has a great influence on the global and nonglobal existence of solutions.
Proof of Theorem 1.1. Consider the following problem:
It is obvious that the solution of problem (3.1) is a lower solution of problem (1.1)–(1.3) when ∫Ωf(x, y)dy ≥ 1 and u0(x) > v0. By Proposition 2.2, u(x, t) is a blow-up solution of problem (1.1)–(1.3).
Proof of Theorem 1.3. (1) The case of p + q > r. Let . It is easy to show that if ∫Ωf(x, y)dy < 1 and is the upper solution of problem (1.1)–(1.3), then we can draw the conclusion.
(2) The case of p + q ≥ max {m, r}. We need to establish a self-similar blow-up solution in order to prove the blow-up result. We first suppose that , and ω(x) is not identically zero, and ω(x)|∂Ω = 0. Without loss of generality, we assume that 0 ∈ Ω and ω(0) > 0.
Let , and ξ = |x | (T − t) −μ, where A > 1, 0 < T < 1, γ and μ > 0. We know that
It is easy to see that V′(ξ) ≤ 0 and V < 1, and
If x ∈ ∂Ω, ω(0) > 0, and ω is continuous, it is known that there exist positive ε and ρ such that ω ≥ ε for x ∈ B(0, ρ). We can get B(0, RTσ) ⊂ B(0, ρ) ⊂ Ω if T is small enough. Then, on ∂Ω × (0, T). It follows from (3.3) that for sufficiently large K0. Therefore, one can observe that the solution to (1.1)–(1.3) exists no later than t = T provided that u0 ≥ K0ω(x). This implies that the solution blows up in finite time for large enough initial data.
Proof of Theorem 1.4. Suppose that λ1 > 0 is the first eigenvalue of −Δ with homogeneous Dirichlet boundary condition, and ϕ(x) is the corresponding eigenfunction. Let M∫Ω(1/(ϕ(y) + ε))dy ≤ 1 for some 0 < ε < 1, where
Now, we assume that um = v, then (1.1)–(1.3) becomes that
Set , where C is determined later, then it follows that
For x ∈ ∂Ω, t > 0,
Proof of Theorem 1.5. Suppose that Φ(x) solves the following problem:
Set ω(x, t) = A(ρm/(1 − ρm) + Φ(x)/M1) 1/m, here A > 0 will be determined later and 0 < ρ < 1,
- (1)
If m > p + q, choosing A = max {max |u0(x)|, (|Ω | − k)(M/δ)(1/(1 − ρm)) (p + q)/m}, we have
(3.16) - (2)
If m = p + q, selecting |Ω | < k + (δ/M1)(1 − ρm), and A = max u0(x), we get
(3.17) - (3)
If m < p + q, we choose max u0(x) ≤ A ≤ (|Ω | − k)(M1/δ)(1/(1 − ρm)) −(p + q)/m such that
(3.18)For x ∈ ∂Ω,(3.19)
For the blow-up case of m < p + q, it holds clearly from the second part of the proof of Theorem 1.3.
4. Blow-Up Rate Estimates
Next, we will get the following precise blow-up rate estimates for slow diffusion case under some suitable conditions.
Suppose that v(x, t) is the blow-up solution of problem (*)–(***) in finite time T, and set
Proof of Theorem 1.6. (1) We can easily know that V(t) is Lip continuous and differential almost everywhere,
(2) Next, we set , where δ > 0, then
Since p1 + q1 > r1, we get p1 + 2q1 − n > q1 + 1 − n and p1 + q1 − r1 > 0, then by (4.7)-(4.8),
For (x, t) ∈ ST, because of , we then have
Integrating it over (t, T), we have
Acknowledgments
This work is supported by the Natural Science Foundation of Shandong Province of China (ZR2012AM018). The authors would like to deeply thank all the reviewers for their insightful and constructive comments.