- Research Article
- Open Access

# Blowup Analysis for a Semilinear Parabolic System with Nonlocal Boundary Condition

- Yulan Wang
^{1}and - Zhaoyin Xiang
^{2}Email author

**2009**:516390

https://doi.org/10.1155/2009/516390

© Y. Wang and Z. Xiang. 2009

**Received:**23 July 2009**Accepted:**26 October 2009**Published:**22 November 2009

## Abstract

This paper deals with the properties of positive solutions to a semilinear parabolic system with nonlocal boundary condition. We first give the criteria for finite time blowup or global existence, which shows the important influence of nonlocal boundary. And then we establish the precise blowup rate estimate for small weighted nonlocal boundary.

## Keywords

- Global Existence
- Comparison Principle
- Nonlocal Boundary
- Blowup Rate
- Blowup Solution

## 1. Introduction

In this paper, we devote our attention to the singularity analysis of the following semilinear parabolic system:

with nonlocal boundary condition

and initial data

where
is a bounded connected domain with smooth boundary
and
are positive parameters. Most physical settings lead to the default assumption that the functions
defined for
are nonnegative and continuous, and that the initial data
,
are nonnegative, which are mathematically convenient and currently followed throughout this paper. We also assume that
satisfies the compatibility condition on
, and that
and
for any
for the sake of the meaning of*nonlocal boundary*.

Over the past few years, a considerable effort has been devoted to studying the blowup properties of solutions to parabolic equations with*local boundary conditions*, say Dirichlet, Neumann, or Robin boundary condition, which can be used to describe heat propagation on the boundary of container (see the survey papers [1, 2]). For example, the system (1.1) and (1.3) with homogeneous Dirichlet boundary condition

has been studied extensively (see [3–5] and references therein), and the following proposition was proved.

- (i)All solutions are global if , while there exist both global solutions and finite time blowup solutions depending on the size of initial data when (See [4]). (ii) The asymptotic behavior near the blowup time is characterized by

For the more parabolic problems related to the local boundary, we refer to the recent works [6–9] and references therein.

On the other hand, there are a number of important phenomena modeled by parabolic equations coupled with nonlocal boundary condition of form (1.2). In this case, the solution could be used to describe the entropy per volume of the material [10–12]. Over the past decades, some basic results such as the global existence and decay property have been obtained for the nonlocal boundary problem (1.1)–(1.3) in the case of scalar equation (see [13–16]). In particular, for the blowup solution of the single equation

under the assumption that , Seo [15] established the following blowup rate estimate

for any . For the more nonlocal boundary problems, we also mention the recent works [17–22]. In particular, Kong and Wang in [17], by using some ideas of Souplet [23], obtained the blowup conditions and blowup profile of the following system:

subject to nonlocal boundary (1.2), and Zheng and Kong in [22] gave the condition for global existence or nonexistence of solutions to the following similar system:

with nonlocal boundary condition (1.2). The typical characterization of systems (1.8) and (1.9) is the complete couple of the nonlocal sources, which leads to the analysis of simultaneous blowup.

To our surprise, however, it seems that there is no work dealing with singularity analysis of the parabolic system (1.1) with nonlocal boundary condition (1.2) except for the single equation case, although this is a very classical model. Therefore, the basic motivation for the work under consideration was our desire to understand the role of weight function in the blowup properties of that nonlinear system. We first remark by the standard theory [4, 13] that there exist local nonnegative classical solutions to this system.

Our main results read as follows.

Theorem 1.2.

Suppose that . All solutions to (1.1)–(1.3) exist globally.

It follows from Theorem 1.2 and Proposition 1.1(i) that any weight perturbation on the boundary has no influence on the global existence when , while the following theorem shows that it plays an important role when . In particular, Theorem 1.3(ii) is completely different from the case of the local boundary (1.4) (by comparing with Proposition 1.1(i)).

Theorem 1.3.

Once we have characterized for which exponents and weights the solution to problem (1.1)–(1.3) can or cannot blow up, we want to study the way the blowing up solutions behave as approaching the blowup time. To this purpose, the first step usually consists in deriving a bound for the blowup rate. For this bound estimate, we will use the classical method initially proposed in Friedman and McLeod [24]. The use of the maximum principle in that process forces us to give the following hypothesis technically.

(H)*There exists a constant*
*, such that*

However, it seems that such an assumption is necessary to obtain the estimates of type (1.5) or (1.10) unless some additional restrictions on parameters are imposed (for the related problem, we refer to the recent work of Matano and Merle [25]).

Here to obtain the precise blowup rates, we shall devote to establishing some relationship between the two components and as our problem involves a system, but we encounter the typical difficulties arising from the integral boundary condition. The following theorem shows that we have partially succeeded in this precise blowup characterization.

Theorem 1.4.

where are both positive constants.

Remark 1.5.

which improves the estimate (1.7). Moreover, we relax the restriction on .

Remark 1.6.

By comparing with Proposition 1.1(ii), Theorem 1.4 could be explained as the small perturbation of homogeneous Dirichlet boundary, which leads to the appearance of blowup, does not influence the precise asymptotic behavior of solutions near the blowup time and the blowup rate exponents and are just determined by the corresponding ODE system . Similar phenomena are also noticed in our previous work [18], where the single porous medium equation is studied.

The rest of this paper is organized as follows. Section 2 is devoted to some preliminaries, which include the comparison principle related to system (1.1)–(1.3). In Section 3, we will study the conditions for the solution to blow up and exist globally and hence prove Theorems 1.2 and 1.3. Proof of Theorem 1.4 is given in Section 4.

## 2. Preliminaries

In this section, we give some basic preliminaries. For convenience, we denote We begin with the definition of the super- and subsolution of system (1.1)–(1.3).

Definition 2.1.

A supersolution is defined with each inequality reversed.

Lemma 2.2.

Proof.

Set . Since , by continuity, there exists such that for all . Thus .

We claim that will lead to a contradiction. Indeed, suggests that or for some . Without loss of generality, we suppose that .

In addition, it is clear that on boundary and at the initial state . Then it follows from the strong maximum principle that in , which contradicts to .

If , we shall have a contradiction:

In the last inequality, we have used the facts that for any and for any , which is a direct result of the previous case.

Therefore, the claim is true and thus , which implies that on .

Remark 2.3.

If and for any in Lemma 2.2, we can obtain in under the assumption that for . Indeed, for any , we can conclude that in as the proof of Lemma 2.2. Then the desired result follows from the limit procedure .

From the above lemma, we can obtain the following comparison principle by the standard argument.

Proposition 2.4.

Let ) and be a subsolution and supersolution of (1.1)–(1.3) in , respectively. If for , then in .

## 3. Global Existence and Blowup in Finite Time

In this section, we will use the super and subsolution technique to get the global existence or finite time blowup of the solution to (1.1)–(1.3).

Proof of Theorem 1.2.

We consider the following auxiliary problem:

where is the measure of and . It follows from [13, Theorem ] that exists globally, and indeed (see [13, Theorem ]).

Our intention is to show that is a global supersolution of (1.1)–(1.3). Indeed, a direct computation yields

It is clear that and . Therefore, we get is a global supersolution of (1.1)–(1.3) and hence the solution to (1.1)–(1.3) exists globally by Proposition 2.4.

- (i)
Let be the solution to the homogeneous Dirichlet boundary problem (1.1), (1.4), and (1.3). Then it is well known that for sufficiently large initial data the solution blows up in finite time when (see [4]). On the other hand, it is obvious that is a subsolution of problem (1.1)–(1.3). Henceforth, the solution of (1.1)–(1.3) with large initial data blows up in finite time provided that .

- (ii)
We consider the ODE system:

- (iii)

where is a positive constant such that . We remark that and ensure the existence of such .

Let

Here we used . The above inequalities show that is a supsolution of problem (1.1)–(1.3) whenever . Therefore, system (1.1)–(1.3) has global solutions if and , for any .

## 4. Blowup Rate Estimate

In this section, we derive the precise blowup rate estimate. To this end, we first establish a partial relationship between the solution components and , which will be very useful in the subsequent analysis. For definiteness, we may assume . If , we can proceed in the same way by changing the role of and and then obtain the corresponding conclusion.

Lemma 4.1.

Proof.

where is a function of and and lies between and .

When , on the other hand, we have

For the initial condition, we have

Summarily, if we take , then it follows from Theorem in [13] that , that is,

which is desired.

Using this lemma, we could establish our blowup rate estimate. To derive our conclusion, we shall use some ideas of [3].

Proof of Theorem 1.4.

For , we have from the boundary conditions that

On the other hand, the hypothesis (H) implies that

Hence, from (4.9)–(4.13) and the comparison principle (see Remark 2.3), we get

Let Then and are Lipschitz continuous and thus are differential almost everywhere (see e.g., [24]). Moreover, we have from equations (1.1) that

We claim that

From (4.15), (4.18), and (4.19), we can confirm our claim (4.17).

for some positive constant . Thus we have established the upper estimates for .

To obtain the lower estimate for , we notice that (4.16) and (4.18) lead to

Finally, we give the lower estimate for . Indeed, using the relationship (4.16), (4.23) and (4.25), we could prove that is bounded from below; that is, there exists a positive constant such that

which would contradict to (4.25) as is large enough since as .

## Declarations

### Acknowledgments

The authors are very grateful to the anonymous referees for their careful reading and useful suggestions, which greatly improved the presentation of the paper. This work is supported in part by Natural Science Foundation Project of CQ CSTC (2007BB2450), China Postdoctoral Science Foundation, the Key Scientific Research Foundation of Xihua University, and Youth Foundation of Science and Technology of UESTC.

## Authors’ Affiliations

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