- Research
- Open access
- Published:
Global and blow-up solutions for quasilinear parabolic equations with a gradient term and nonlinear boundary flux
Journal of Inequalities and Applications volume 2014, Article number: 234 (2014)
Abstract
This work is concerned with positive classical solutions for a quasilinear parabolic equation with a gradient term and nonlinear boundary flux. We find sufficient conditions for the existence of global and blow-up solutions. Moreover, an upper bound for the ‘blow-up time’, an upper estimate of the ‘blow-up rate’ and an upper estimate of the global solution are given. Finally, some application examples are presented.
MSC:35R45, 35K65, 34A12.
1 Introduction
In this paper, we consider the quasilinear parabolic equation with a gradient term
subject to the nonlinear boundary flux and initial conditions
Here () is a bounded domain with a smooth boundary ∂D, is the closure of D, , n is the outer normal vector and T is the maximum existence time of . , and are nonlinear diffusion coefficient, reaction term and boundary flux, respectively. Let , , and suppose that the function , for any , , , , is a nonnegative function, , is a positive function, and the positive function satisfies the compatibility conditions. Under these assumptions, the classical parabolic equation theory [[1], Section 3] ensures that there exists a unique classical solution to problem (1.1)-(1.3) for some , and the solution is positive over . Moreover, by the regularity theorem [[2], Chapter 3], we know .
Equation (1.1) describes the diffusion of concentration of some Newtonian fluids through porous media or the density of some biological species in many physical phenomena and combustion theories (see [3, 4]). The nonlinear Neumann boundary value condition (1.2) can be physically interpreted as the nonlinear radial law (see, e.g., [5, 6]).
In recent years the questions like blow-up and global solvability for nonlinear evolution equations have been investigated extensively by many authors. In particular, for the parabolic equations with a gradient term, we refer to [7–12]etc. For example, Souplet and Weissler [7] studied the semilinear parabolic equation
subject to the homogeneous Dirichlet boundary condition. By using the comparison principle and constructing a self-similar lower solution, they obtained sufficient conditions for global existence and blow-up solutions. Andreu [8] used a similar method to study the quasilinear parabolic equation
Chen [9] considered the following semilinear parabolic equation:
with the homogeneous Dirichlet boundary condition. By estimating the integral of ratio of one solution to the other, the author proved both global existence and blow-up results. Then he used the same method to study a more generalized equation with a gradient term, see [10].
For the nonlinear parabolic equations with Neumann boundary conditions, Lair and Oxley [11] considered the quasilinear parabolic equation without a gradient term
subject to the homogeneous Neumann boundary conditions, and they obtained the necessary and sufficient conditions for the global existence and blow-up solution by the approximation method. Recently, Ding and Gao [12] investigated an initial boundary value problem of the quasilinear parabolic equation with a gradient term
subject to boundary flux , and they obtained sufficient conditions for the global existence and blow-up solution, the upper estimate of global solution and blow-up time.
Motivated by the above works, we construct an appropriate auxiliary function and use the Hopf maximum principle to study problem (1.1)-(1.3). The aim of this paper is to obtain sufficient conditions for the existence of blow-up and global solution, an upper bound for the ‘blow-up time’, an upper estimate of the ‘blow-up rate’ and an upper estimate of the global solution and then to give some examples.
2 Main results and proof
We now state and prove the main results of this paper. Firstly, we give sufficient conditions of the existence of a blow-up solution of problem (1.1)-(1.3).
Theorem 1 Let be a solution of problem (1.1)-(1.3). Assume that the following conditions hold:
-
(1)
For any ,
(2.1) -
(2)
For any ,
(2.2)(2.3) -
(3)
For any ,
(2.4) -
(4)
The constant
(2.5)
where , ;
-
(5)
The integration
(2.6)
then the solution of system (1.1)-(1.3) must blow up in finite time T and
where , , and is the inverse function of Φ.
Proof Consider the auxiliary function
We find that
and
Hence, from (2.11) and (2.12) we have
Using (2.10) leads to
Now substituting (2.14) into (2.13) yields
In fact, from (1.1) we see that
Thus combining (2.15) and (2.16), we arrive at
In view of (2.9), we have
If we substitute (2.18) into (2.17), then it is easy to obtain
From assumptions (2.1)-(2.3), it follows that the right-hand side of (2.19) is nonnegative, i.e.,
Then from (2.4) and (2.5) we have
And as we can see, an explicit calculation
holds on . Thus, by combining (2.20)-(2.22) and using the Hopf maximum principle, we find that the maximum of Ψ on is 0, i.e.,
and by (2.9), it gives
Integrating (2.23) over at the point , where , yields
This together with assumption (2.6) shows that must blow up in finite time T; moreover,
For each fixed x, integrating inequality (2.23) over () leads to
If we let , then formally
therefore
The proof is completed. □
The result on the global solution is stated as Theorem 2 below.
Theorem 2 Let be a solution of problem (1.1)-(1.3). Assume that the following conditions hold:
-
(1)
For any ,
(2.26) -
(2)
For any ,
(2.27)(2.28) -
(3)
For any ,
(2.29) -
(4)
The constant
(2.30)
where , ;
-
(5)
The integration
(2.31)
then the solution of system (1.1)-(1.3) must be a global solution and
where , , and is the inverse function of Ψ.
Proof Consider the auxiliary function
We first replace Ψ and β in (2.20) with Φ and α, respectively, and under assumptions (2.26)-(2.28), we get
In fact, from (2.29) and (2.30) we can see that
Also, on , it gives
By combining (2.34)-(2.36) and using the Hopf maximum principle, we find that the minimum of Φ on is 0, i.e.,
and by (2.33), we can see that
For each fixed x, integrating (2.37) over yields
This together with assumption (2.31) shows that must be a global solution; moreover,
therefore
The proof is completed. □
3 Applications
In what follows, we present several examples to demonstrate the applications of Theorems 1 and 2.
Example 1 Let u be a solution of
where , then we have
It is easy to verify that (2.1)-(2.4) hold. By (2.5), we find
It follows from Theorem 1 that must blow up in finite time T and
and
Example 2 Let u be a solution of
where , then we have
It is easy to verify that (2.26)-(2.29) hold. By (2.30), we find
It follows from Theorem 2 that must be a global solution and
References
Amann H: Quasilinear parabolic systems under nonlinear boundary conditions. Arch. Ration. Mech. Anal. 1986, 92: 153–192.
Sperb RP: Maximum Principles and Their Applications. Academic Press, New York; 1981.
Bebernes J, Eberly D: Mathematical Problems from Combustion Theory. Springer, New York; 1989.
Diaz JI, Thelin FD: On a nonlinear parabolic problem arising in some model related to turbulent flows. SIAM J. Math. Anal. 1994, 25: 1085–1111. 10.1137/S0036141091217731
Filo J: Diffusivity versus absorption through the boundary. J. Differ. Equ. 1992, 99: 281–305. 10.1016/0022-0396(92)90024-H
Levine HA, Payne LE: Nonexistence theorems for the heat equation with nonlinear boundary conditions and for porous medium equation backward in time. J. Differ. Equ. 1974, 16: 319–334. 10.1016/0022-0396(74)90018-7
Souplet P, Weissler FB: Self-similar subsolutions and blowup for nonlinear parabolic equations. J. Math. Anal. Appl. 1997, 212: 60–74. 10.1006/jmaa.1997.5452
Andreu F, Mazón JM, Simondon F, Toledo J: Blow up for a class of nonlinear parabolic problems. Asymptot. Anal. 2002,29(2):143–155.
Chen SH: Global existence and blowup of solutions for a parabolic equation with a gradient term. Proc. Am. Math. Soc. 2001, 129: 975–981. 10.1090/S0002-9939-00-05666-5
Chen SH, Yu DM: Global existence and blowup solutions for quasilinear parabolic equations. J. Math. Anal. Appl. 2007, 335: 151–167. 10.1016/j.jmaa.2007.01.066
Lair AV, Oxley ME: A necessary and sufficient condition for global existence for degenerate parabolic boundary value problem. J. Math. Anal. Appl. 1998, 221: 338–348. 10.1006/jmaa.1997.5900
Ding JT, Guo BZ: Global existence and blow-up solutions for quasilinear reaction-diffusion equations with a gradient term. Appl. Math. Lett. 2011, 24: 936–942. 10.1016/j.aml.2010.12.052
Acknowledgements
This work is supported by the Natural Science Foundation of Shandong Province of China (ZR2012AM018) and the Fundamental Research Funds for the Central Universities (No. 201362032). The authors would like to deeply thank all the reviewers for their insightful and constructive comments.
Author information
Authors and Affiliations
Corresponding author
Additional information
Competing interests
The authors declare that they have no competing interests.
Authors’ contributions
All authors contributed equally to the manuscript and read and approved the final manuscript.
Rights and permissions
Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made.
The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder.
To view a copy of this licence, visit https://creativecommons.org/licenses/by/4.0/.
About this article
Cite this article
Li, C., Sun, L. & Fang, Z.B. Global and blow-up solutions for quasilinear parabolic equations with a gradient term and nonlinear boundary flux. J Inequal Appl 2014, 234 (2014). https://doi.org/10.1186/1029-242X-2014-234
Received:
Accepted:
Published:
DOI: https://doi.org/10.1186/1029-242X-2014-234