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Volume 2009, Article ID 516390,14pages doi:10.1155/2009/516390

Research Article

Blowup Analysis for a Semilinear Parabolic System with Nonlocal Boundary Condition

Yulan Wang

1

and Zhaoyin Xiang

2

1School of Mathematics and Computer Engineering, Xihua University, Chengdu 610039, China

2School of Applied Mathematics, University of Electronic Science and Technology of China, Chengdu 610054, China

Correspondence should be addressed to Zhaoyin Xiang,[email protected] Received 23 July 2009; Accepted 26 October 2009

Recommended by Gary Lieberman

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.

Copyrightq2009 Y. Wang and Z. Xiang. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

1. Introduction

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

ut−Δuvp, vt−Δvuq, x∈Ω, t >0 1.1 with nonlocal boundary condition

ux, t

Ωf x, y

u y, t

dy, vx, t

Ωg x, y

v y, t

dy, x∂Ω, t >0, 1.2

and initial data

ux,0 u0x, vx,0 v0x, x∈Ω, 1.3

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where Ω ⊂ RN is a bounded connected domain with smooth boundary ∂Ω, p and qare positive parameters. Most physical settings lead to the default assumption that the functions fx, y, gx, y defined forx∂Ω, y ∈ Ω are nonnegative and continuous, and that the initial data u0x, v0x ∈ C1Ω are nonnegative, which are mathematically convenient and currently followed throughout this paper. We also assume that u0, v0 satisfies the compatibility condition on∂Ω, and thatfx,·/≡0 andgx,·/≡0 for anyx∂Ωfor 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 containersee the survey papers1,2 . For example, the system1.1and 1.3with homogeneous Dirichlet boundary condition

ux, t vx, t 0, x∂Ω, t >0 1.4

has been studied extensivelysee3–5 and references therein, and the following proposition was proved.

Proposition 1.1. iAll solutions are global ifpq1, while there exist both global solutions and finite time blowup solutions depending on the size of initial data whenpq > 1 (See [4]).iiThe asymptotic behavior near the blowup time is characterized by

C−11 ≤max

x∈Ω ux, tTtp1/pq−1C1, C−12 ≤max

x∈Ω vx, tTtq1/pq−1C2 1.5 for someC1, C2>0 (See [3,5]).

For the more parabolic problems related to the local boundary, we refer to the recent works6–9 and references therein.

On the other hand, there are a number of important phenomena modeled by parabolic equations coupled with nonlocal boundary condition of form1.2. 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 equationsee 13–16 . In particular, for the blowup solutionuof the single equation

ut−Δuup, x∈Ω, t >0, ux, t

Ωf x, y

u y, t

dy, x∂Ω, t >0, ux,0 u0x, x∈Ω,

1.6

under the assumption that

Ωfx, ydy 1, Seo15 established the following blowup rate estimate

p−1−1/p−1

T−t−1/p−1≤max

x∈Ω ux, tC1T−t−1/γ−1 1.7

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for anyγ ∈ 1, p. For the more nonlocal boundary problems, we also mention the recent works17–22 . In particular, Kong and Wang in 17 , by using some ideas of Souplet23 , obtained the blowup conditions and blowup profile of the following system:

ut Δu

Ωumx, tvnx, tdx, vt Δv

Ωupx, tvqx, tdx, x∈Ω, t >0 1.8

subject to nonlocal boundary1.2, and Zheng and Kong in22 gave the condition for global existence or nonexistence of solutions to the following similar system:

ut Δuum

Ωvn y, t

dy, vt Δvvq

Ωup y, t

dy, x∈Ω, t >0 1.9

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 system1.1with nonlocal boundary condition1.2except 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 0< pq1. All solutions to1.1–1.3exist globally.

It follows fromTheorem 1.2andProposition 1.1ithat any weight perturbation on the boundary has no influence on the global existence whenpq≤1, while the following theorem shows that it plays an important role whenpq >1. In particular,Theorem 1.3iiis completely different from the case of the local boundary1.4 by comparing withProposition 1.1i.

Theorem 1.3. Suppose thatpq >1.

iFor any nonnegative fx, yandgx, y, solutions to1.1–1.3blow up in finite time provided that the initial data are large enough.

iiIf

Ωfx, ydy1,

Ωgx, ydy1 for anyx∂Ω, then any solutions to1.1–1.3 with positive initial data blow up in finite time.

iiiIf

Ωfx, ydy <1,

Ωgx, ydy <1 for anyx∂Ω, then solutions to1.1–1.3with small initial data exist globally in time.

Once we have characterized for which exponents and weights the solution to problem 1.1–1.3can or cannot blow up, we want to study the way the blowing up solutions behave

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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 McLeod24 . The use of the maximum principle in that process forces us to give the following hypothesis technically.

HThere exists a constant 0< δ <1, such thatΔu0 1−δvp0 ≥0,Δv0 1−δuq0 ≥0.

However, it seems that such an assumption is necessary to obtain the estimates of type1.5 or1.10unless some additional restrictions on parametersp, qare imposedfor the related problem, we refer to the recent work of Matano and Merle25 .

Here to obtain the precise blowup rates, we shall devote to establishing some relationship between the two componentsuandvas 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. Suppose thatpq >1,p, q1,fx, y gx, y,

Ωfx, ydy ≤1,and assumption (H) holds. If the solutionu, vof1.1–1.3with positive initial datau0, v0blows up in finite time T, then

C1−1≤max

x∈Ω ux, tTtp1/pq−1C1, C2−1≤max

x∈Ω vx, tTtq1/pq−1C2, 1.10

whereC1, C2are both positive constants.

Remark 1.5. Ifq pandu0 v0, thenTheorem 1.4implies that for the blowup solution of problem1.6, we have the following precise blowup rate estimate:

C−11 T−t−1/p−1≤max

x∈Ω ux, tC1T−t−1/p−1, 1.11

which improves the estimate1.7. Moreover, we relax the restriction onf.

Remark 1.6. By comparing with Proposition 1.1ii,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 exponentsp1/pq−1andq1/pq−1are just determined by the corresponding ODE systemut vp, vt uq. Similar phenomena are also noticed in our previous work18 , 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 Theorems1.2and1.3. Proof ofTheorem 1.4is given inSection 4.

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2. Preliminaries

In this section, we give some basic preliminaries. For convenience, we denote QT Ω × 0, T, ST ∂Ω×0, T, QT Ω×0, T.We begin with the definition of the super- and subsolution of system1.1–1.3.

Definition 2.1. A pair of functionsu, vC2,1QT

CQTis called a subsolution of1.1–1.3 if

ut−Δu≤vp, vt−Δv≤uq, x, t∈QT, ux, t

Ωf x, y

u y, t

dy, vx, t

Ωg x, y

v y, t

dy, x, t∈ST, ux,0≤u0x, vx,0≤v0x, x∈Ω.

2.1

A supersolution is defined with each inequality reversed.

Lemma 2.2. Suppose thatc1, c2, f,andgare nonnegative functions. Ifw1, w2C2,1QT CQT satisfy

w1t−Δw1c1x, tw2, w2t−Δw2c2x, tw1, x, t∈QT, w1x, t≥

Ωf x, y

w1 y, t

dy, w2x, t≥

Ωg x, y

w2 y, t

dy, x, t∈ST, w1x,0>0, w2x,0>0, x∈Ω,

2.2

thenw1, w2>0 onQT.

Proof. Set t1 : sup{t ∈ 0, T : wix, t > 0, i 1,2}. Since w1x,0, w2x,0 > 0, by continuity, there existsδ > 0 such thatw1x, t, w2x, t > 0 for allx, t ∈ Ω×0, δ. Thus t1∈δ, T .

We claim that t1 < T will lead to a contradiction. Indeed, t1 < T suggests that w1x1, t1 0 or w2x1, t1 0 for somex1 ∈ Ω. Without loss of generality, we suppose thatw1x1, t1 0infQ

t1w1. Ifx1∈Ω, we first notice that

w1t−Δw1c1w2≥0, x, t∈Ω×0, t1 . 2.3

In addition, it is clear thatw1≥0 on boundary∂Ωand at the initial statet0. Then it follows from the strong maximum principle thatw1≡0 inQt1, which contradicts tow1x,0>0.

Ifx1∂Ω, we shall have a contradiction:

0w1x1, t1

Ωf x1, y

w1

y, t1

dy >0. 2.4

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In the last inequality, we have used the facts thatfx,·/≡0 for anyx∂Ωandw1y, t1>0 for anyy∈Ω, which is a direct result of the previous case.

Therefore, the claim is true and thust1T, which implies thatw1, w2>0 onQT. Remark 2.3. If

Ωfx, ydy ≤ 1 and

Ωgx, ydy ≤ 1 for anyx∂ΩinLemma 2.2, we can obtainw1, w2≥0,0inQTunder the assumption thatw1x,0, w2x,0≥0,0forx∈Ω.

Indeed, for any >0, we can conclude thatw1x, t et, w2x, t et>0,0inQTas the proof ofLemma 2.2. Then the desired result follows from the limit procedure → 0.

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

Proposition 2.4. Let u, v) and u, v be a subsolution and supersolution of 1.1–1.3 in QT, respectively. Ifux,0, vx,0<ux,0, vx,0forx∈Ω, thenu, v<u, vinQT.

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 to1.1–1.3.

Proof ofTheorem 1.2. As 0< pq≤1, there exists, l∈0,1such that 1

pl s, 1

qs

l. 3.1

Then we let φx, y x∂Ω, y ∈ Ω be a continuous function satisfying φx, y ≥ max{fx, y, gx, y}and set

ax

Ωφx, ydy 1−s/s

, bx

Ωφx, ydy 1−l/l

, x∂Ω. 3.2

We consider the following auxiliary problem:

wt Δwkw, x∈Ω, t >0,

wx, t ax bx 1

Ω

φ

x, y 1

|Ω|

w

y, t dy

, x∂Ω, wx,0 1u1/s0 x v1/l0 x, t >0,

3.3

where|Ω|is the measure ofΩandk:1/s1/l. It follows from13, Theorem 4.2 thatwx, t exists globally, and indeedwx, t>1,x, t∈Ω×0,∞ see13, Theorem 2.1 .

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Our intention is to show thatu, v: ws, wlis a global supersolution of1.1–1.3.

Indeed, a direct computation yields

utsws−1Δwkwsws−1Δwws,

Δusws−1Δwss−1ws−2|∇w|2sws−1Δw, 3.4

and thus

ut−Δu≥ws wls/l

vp. 3.5

Here we have used the conclusionw > 1 and inequality3.1. We still have to consider the boundary and initial conditions. Whenx∂Ω, in view of H ¨older’s inequality, we have

ux, t≥axs

Ωφx, ywy, tdy s

Ωφx, ydy 1−s

Ωφx, ywy, tdy s

Ωfx, ydy 1−s

Ωfx, ywy, tdy s

Ω f1−s

x, y1/1−s dy

1−s

Ωfsx, ywsy, t1/sdy s

Ωf1−s x, y

f x, y

w y, ts

dy

Ωf x, y

ws y, t

dy

Ωf x, y

u y, t

dy.

3.6

Similarly, we have also forvthat

vt−Δv≥uq, x∈Ω, t >0, v

Ωg x, y

v y, t

dy, x∂Ω, t >0. 3.7

It is clear that u0x < ux,0 and v0x < vx,0. Therefore, we get u, v is a global supersolution of 1.1–1.3 and hence the solution to 1.1–1.3exists globally by Proposition 2.4.

Proof ofTheorem 1.3. i Let u, v be the solution to the homogeneous Dirichlet boundary problem1.1,1.4, and1.3. Then it is well known that for sufficiently large initial data the

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solutionu, vblows up in finite time whenpq >1see4 . On the other hand, it is obvious thatu, vis a subsolution of problem1.1–1.3. Henceforth, the solution of1.1–1.3with large initial data blows up in finite time provided thatpq >1.

iiWe consider the ODE system:

ft hpt, ht fqt, t >0,

f0 a >0, h0 b >0, 3.8

wherea 1/2minΩu0x, b 1/2minΩv0x. Thenpq >1 implies thatf, hblows up in finite timeT see26 . Under the assumption that

Ωfx, ydy≥1 and

Ωgx, ydy≥1 for anyx∂Ω,f, his a subsolution of problem1.1–1.3. Therefore, byProposition 2.4, we see that the solutionu, vof problem1.1–1.3satisfiesu, v≥f, hand thenu, vblows up in finite time.

iiiLetψ1xbe the positive solution of the linear elliptic problem:

−Δψ1x 0, x∈Ω, ψ1x

Ωf x, y

dy, x∂Ω, 3.9

and letψ2xbe the positive solution of the linear elliptic problem:

−Δψ2x 0, x∈Ω, ψ2x

Ωg x, y

dy, x∂Ω, 3.10

whereois a positive constant such that 0≤ψix≤1i1,2. We remark that

Ωfx, ydy <

1 and

Ωgx, ydy <1 ensure the existence of such0. Let

ux aψ1x, vx bψ2x, 3.11

wherea0p1/pq−1, b0q1/pq−1. We now show thatu, vis a supsolution of problem 1.1–1.3for small initial datau0, v0. Indeed, it follows fromb0 aq, a0 bpthat, for x∈Ω,

ut−Δua0bpvp, vt−Δvb0aquq. 3.12 Whenx∂Ω,

ux a

Ωf x, y

dy

Ωf x, y

1 y

dy

Ωf x, y

uxdy,

vx b

Ωg x, y

dy

Ωg x, y

2 y

dy

Ωg x, y

vxdy.

3.13

Here we usedψix≤1i1,2. The above inequalities show thatu, vis a supsolution of problem1.1–1.3wheneveru0x< aψ1x, v0x< bψ2x. Therefore, system1.1–1.3 has global solutions ifpq >1 and

Ωfx, ydy <1,

Ωgx, ydy <1 for anyx∂Ω.

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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 componentsux, tandvx, t, which will be very useful in the subsequent analysis. For definiteness, we may assumepq≥1. Ifq > p, we can proceed in the same way by changing the role ofuandvand then obtain the corresponding conclusion.

Lemma 4.1. Ifpq,fx, y gx, yand

Ωfx, ydy1 for anyx∂Ω, there exists a positive constantC0 such that the solution u, v of problem 1.1–1.3 with positive initial datau0, v0 satisfies

ux, tC0vp1/q1x, t, x, t∈Ω×0, T. 4.1

Proof. LetJx, t ux, tC0vp1/q1x, t, whereC0 is a positive constant to be chosen.

Forx, t∈Ω×0, T, a series of calculations show that

Jt−ΔJutC0p1

q1vp−q/q1vt−ΔuC0

p1 pq

q12 |∇v|2C0p1

q1vp−q/q1Δv

vpC0p1

q1vp−q/q1uq vp−q/q1

vqp1/q1C0

p1 q1uq

vp−q/q1 1

C0qu−JqC0

p1 q1uq

.

4.2

If we chooseC0such that 1/C0qC0p1/q1, we have

Jt−ΔJvp−q/q1θu, vJ≥0, 4.3

whereθu, vis a function ofuand vand lies betweenC0p1/q1u−JandC0p 1/q1u.

Whenx, t∈∂Ω×0, T, on the other hand, we have

Jx, t

Ωf x, y

u y, t

dyC0

Ωfx, yvy, tdy

p1/q1

. 4.4

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DenoteHx :

Ωfx, ydy ≥ 0,x ∈ ∂Ω. Sincefx,·/≡0 for anyx∂Ω,Hx > 0. It follows from Jensen’s inequality,Hx≤1,andp1/q1≥1 that

Ωf x, y

vp1/q1 y, t

dy

Ωfx, yvy, tdy

p1/q1

Hx

Ωfx, yvy, t dy Hx

p1/q1

Ωfx, yvy, tdy

p1/q1

≥0,

4.5

which implies that

Jx, t

Ωf x, y

u y, t

dyC0

Ωf x, y

vp1/q1 y, t

dy

Ωf x, y

J y, t

dy, x∂Ω.

4.6

For the initial condition, we have

Jx,0 u0x−C0v0p1/q1x≥0, x∈Ω, 4.7

provided thatC0≤infx∈Ω{u0xv−p1/q10 x}.

Summarily, if we takeC0 min{infx∈Ωu0xv−p1/q10 x,q1/p11/q1}, then it follows from Theorem 2.1 in13 thatJx, t≥0, that is,

ux, tC0vp1/q1x, t, x, t∈Ω×0, T, 4.8

which is desired.

Using this lemma, we could establish our blowup rate estimate. To derive our conclusion, we shall use some ideas of3 .

Proof ofTheorem 1.4. For simplicity, we introduceα p1/pq−1, β q1/pq−1.

LetFx, t utδvpandGx, t vtδuq. A direct computation yields

Ft−ΔF≥pvp−1G, Gt−ΔG≥quq−1F, x∈Ω, 0< t < T. 4.9

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Forx, t∈∂Ω×0, T, we have from the boundary conditions that Fx, t utδvp

Ωf x, y

ut y, t

dyδ

Ωfx, yvy, tdy p

Ωf x, y

Fδvp y, t

dyδ

Ωfx, yvy, tdy p

Ωf x, y

F y, t

dyδ

Ωf x, y

vp y, t

dy

Ωfx, yvy, tdy p

.

4.10

It follows from

Ωfx, ydy≤1 and Jensen’s inequality that the difference in the last brace is nonnegative and thus

Fx, t

Ωf x, y

F y, t

dy, x∂Ω. 4.11

By similar arguments, we have

Gx, t

Ωf x, y

G y, t

dy, x, t∈∂Ω×0, T. 4.12

On the other hand, the hypothesisHimplies that

Fx,0≥0, Gx,0≥0 x∈Ω. 4.13

Hence, from4.9–4.13and the comparison principleseeRemark 2.3, we get

Fx, t≥0, Gx, t≥0, x, t∈Ω×0, T. 4.14

That is,

utδvp, vtδuq, x, t∈Ω×0, T. 4.15 LetUt maxx∈Ωux, t, Vt maxx∈Ωvx, t.ThenUtand Vtare Lipschitz continuous and thus are differential almost everywheresee e.g.,24 . Moreover, we have from equations1.1that

Ut≤Vpt, Vt≤Uqt, a.e. t∈0, T. 4.16 We claim that

Vt≥kVqp1/q1t, a.e. t∈0, T 4.17

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for some positive constant k. Indeed, if we letxt, tbe the points at whichv attains its maximum, then relation4.1means that

uxt, tC0Vp1/q1t, t∈0, T. 4.18

At any pointt1of differentiability ofVt, ift2> t1, Vt2Vt1

t2t1vxt1, t2vxt1, t1

t2t1 vtxt1, t1 o1, ast2−→t1. 4.19 From4.15,4.18, and4.19, we can confirm our claim4.17.

Integrating4.17ont, Tyields

VtT−tβk, t∈0, T, 4.20

which gives the upper estimate forVt. Namely, there exists a constantc4>0 such that Vtc4T−t−β, t∈0, T. 4.21

Then by4.16and4.21, we get

Ut≤Vpt≤cp4T−t−pβ, t∈0, T. 4.22

Integrating this equality from 0 tot, we obtain

Utc2T−t−α, t∈0, T 4.23

for some positive constantc2. Thus we have established the upper estimates forUt.

To obtain the lower estimate forUt, we notice that4.16and4.18lead to

Ut≤k2Upq1/p1t 4.24

for a constantk2. Integrating above equality ont, T, we see there exists a positive constant c1such that

Utc1T−t−α, t∈0, T. 4.25

Finally, we give the lower estimate for Vt. Indeed, using the relationship 4.16, 4.23 and 4.25, we could prove that VtTtβ is bounded from below; that is, there exists a positive constantc3such that

Vt≥c3T−t−β. 4.26

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To see this, our approach is based on the contradiction arguments. Assume that there would exist two sequences{tn} ⊂0, TwithtnTand{dn}withdn → 0 asn → ∞such that

VtndnT−tn−β, n1,2,3, . . . . 4.27 Then we could choose a corresponding sequence{sn}such thattnsnkTtn, wherekis a positive constant to be determined later. AsUt≤Vpt, we have

UtnUsn

tn

sn

Vpτdτ. 4.28

From4.23and4.27, we obtain

Utnc2T−sn−αVptntnsn

c2T−sn−αdpnT−tn−βptnsn

c2k1−αT−tn−αkdpnT−tn−α.

4.29

Choosingksuch thatc2k1−αc1/2, one can get Utnc1

2T−tn−αkdnpT−tn−α c1

2 kdpn

T−tn−α, 4.30

which would contradict to4.25asnis large enough sincedn → 0 asn → ∞.

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 CSTC2007BB2450, China Postdoctoral Science Foundation, the Key Scientific Research Foundation of Xihua University, and Youth Foundation of Science and Technology of UESTC.

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