Open Access
Issue
Wuhan Univ. J. Nat. Sci.
Volume 30, Number 6, December 2025
Page(s) 523 - 528
DOI https://doi.org/10.1051/wujns/2025306523
Published online 09 January 2026

© Wuhan University 2025

Licence Creative CommonsThis is an Open Access article distributed under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

0 Introduction

Let ΩRN be a bounded domain with sufficiently smooth boundary Ω. The main objective of this article is to investigate the blow-up phenomenon of the following pseudo-parabolic equation with memory and convection terms

{ ( Δ u - | u | p u ) t + Δ u + u q u x 1 + | u | m u = 0 t e - ( t - s ) Δ u d s ,    ( x , t ) Ω T , u ( x , t ) = 0 ,    ( x , t ) S T , u ( x , 0 ) = u 0 ( x ) ,    x Ω ¯ , (1)

where m, p, q and T are four positive parameters, x=(x1, x2,, xN)Ω, ΩT=Ω×(0, T), ST=Ω×(0, T), and u0(x)L(Ω)H01(Ω).

The pseudo-parabolic equations are characterized by the occurrence of mixed third⁃order derivatives, more precisely, second in space variable and first order in time variable. Such equations are used to model heat conduction in two-temperature system[1-2], fluid flow in porous medium[3], two phase flow in porous medium with dynamical capillary pressure[4], and the populations with the tendency to form crows[5-6]. The pseudo-parabolic equations with memory term, like the form (1), can be used to describe the non-stationary process of the electric potential in semiconductors with sources of free-charge currents[7-8]. In this physics content, u(x,t) stands for the electric field potential, the memory term 0te-(t-s)Δuds stands for the memory effect, uqux1 stands for the nonlinear convection of the free electrons, and |u|mu stands for a nonlinear source of the free electric current.

In the past period of time, many mathematicians have focused their attention on the properties of solutions to various pseudo-parabolic equations[9-12]. In particular, Meyvaci[13] considered the problem

{ u t - Δ u t - Δ u - u p u x 1 = | u | 2 m u ,    ( x , t ) Ω T , u ( x , t ) = 0 ,    ( x , t ) S T , u ( x , 0 ) = u 0 ( x ) ,    x Ω ¯ , (2)

and proved that the solution of (2) with p(1,m] and large initial value blows up in finite time. Korpusov and Sveshnikov[14] dealt with the blow-up behavior of the following pseudo-parabolic equation with non-local term

{ ( Δ u - u - | u | p u ) t + Δ u + u x 1 + u u x 1 = Δ u Ω | u | 2 d x ,    ( x , t ) Ω T , u ( x , t ) = 0 ,    ( x , t ) S T , u ( x , 0 ) = u 0 ( x ) ,    x Ω ¯ . (3)

Under some certain conditions, by constructing appropriate auxiliary functions and using differential inequality techniques, the authors gave the sufficient condition for the occurrence of the blow-up phenomenon. Ptashnyk[15] studied the degenerate quasi-linear pseudo-parabolic equation with memory term and variational inequality as the form

{ t b j ( u ) - ( a ( x ) u t ) j - d j ( t , x , u , u ) + M j ( u ) = f j ( u ) ,    ( x , t ) Ω T , u j ( x , t ) = 0 ,    ( x , t ) S T , b j ( u ( x , 0 ) ) = b j ( u 0 ( x ) ) ,    x Ω ¯ , (4)

where the memory operator Mj(u) is defined by

( M j ( t ) ( u ) , v j ) = Ω 0 t K j ( t , s ) g j ( s , x , u ( s , x ) ) d s v j ( t , x ) d x  

for all functions u,vLp(0,T; H01,p(Ω)l) with p2, and (,) means the inner product in the sense of L2(Ω). Under some suitable assumptions on the vector field b, namely, b: RlRl is monotone non-decreasing and a continuous gradient. Ptashnyk[15] obtained the local existence result of the weak solution to problem (4) by using Rothe-Galerkins method. Moreover, he also got the uniqueness of the weak solution for some special cases.

To the best of our knowledge, there is no relevant literature on the blow-up property of the solution to problem (1). Inspired by the works mentioned above, the main goal of this article is to give a criterion for finite time blow-up phenomenon.

1 Preliminaries and Main Result

Throughout this article, we work with the weak solution of problem (1) in the sense of the following definition.

Definition 1   A function u(x,t) with u(x,0)=u0(x) a.e. xΩ¯ is said to be a weak solution of problem (1) if uL2(0,T;H01(Ω))L(0,T;H01(Ω)), |u|puL(0,T;L1(Ω)), (|u|pu-Δu)tL2(0,T;H-1(Ω)), and for any vL2(0,T;H01(Ω)) with vtL2(0,T;H01(Ω))L1(0,T;L(Ω)) and v(x,T)=0, one has

    0 T Ω ( | u | p u v t + u v t ) d x d t - 0 T Ω ( | u 0 | p u 0 v t + u 0 v t ) d x d t + 0 T Ω 0 t e - ( t - s ) u ( x , s ) v ( x , t ) d s d x d t

= 0 T Ω ( u v + 1 q + 1 u q + 1 v x 1 - | u | m u v ) d x d t . (5)

Following a slight modification of the proof of Theorem 3 in Ref. [15], we can obtain the local existence result of the weak solution for problem (1). The main result of this article is the following theorem.

Theorem 1   Suppose that 0<max{p,2q}<m, and the initial data u0(x) satisfies

u 0 m + 2 m + 2 > δ 1 u 0 2 2 + δ 2 u 0 p + 2 p + 2 + δ 3 .

Then

l i m t T - ( 1 2 u 2 2 + p + 1 p + 2 u p + 2 p + 2 ) = + ,

where T- is given by (31), and

δ 1 = 1 + 1 2 ( β α - 1 + γ α - 1 ) , δ 2 = p + 1 p + 2 ( β α - 1 + γ α - 1 ) , δ 3 = C ( β α - 1 + γ α - 1 ) ,

α > 1 , β, γ and C are positive constants, given in Section 2.

2 Proof of the Main Result

In this section, by constructing some appropriate auxiliary functions and using the modified concavity method, we are going to give the proof of Theorem 1.

Proof   First, we denote

G ( t ) = 1 2 u 2 2 + p + 1 p + 2 u p + 2 p + 2 + C (6)

and

H ( t ) = u t 2 2 + ( p + 1 ) Ω | u | p | u t | 2 d x (7)

where C>0 is to be determined. Multiplying both sides of the first equation in (1) by u and ut , respectively, and then integrating over Ω, we have

G ' ( t ) = 0 t Ω e - ( t - s ) u ( x , t ) u ( x , s ) d x d s - u 2 2 + u m + 2 m + 2 (8)

and

H ( t ) = 0 t Ω e - ( t - s ) u t ( x , t ) u ( x , s ) d x d s + 1 m + 2 d d t u m + 2 m + 2 - 1 2 d d t u 2 2 - 1 q + 1 Ω u q + 1 u t x 1 d x (9)

Taking the derivative of G(t) with respect to t, we get

G ' ( t ) = Ω u u t d x + ( p + 1 ) Ω u p + 1 u t d x (10)

Applying the Cauchy-Schwarz inequality, we can conclude that

[ G ' ( t ) ] 2 = [ ( u , u t ) + ( p + 1 u p 2 + 1 , p + 1 u p 2 u t ) ] 2

( u 2 2 + ( p + 1 ) u p + 2 p + 2 ) ( u t 2 2 + ( p + 1 ) Ω | u | p | u t | 2 d x ) ( p + 2 ) G ( t ) H ( t ) , (11)

where (,) is the inner product in the sense of L2(Ω). On the other hand, by virtue of (8) and (9), it is obvious that

H ( t ) = 1 m + 2 G ' ' ( t ) + m + 1 m + 2 0 t Ω e - ( t - s ) u t ( x , t ) u ( x , s ) d x d s

+ 1 m + 2 0 t Ω e - ( t - s ) u ( x , t ) u ( x , s ) d x d s

- m 2 ( m + 2 ) d d t u 2 2 - 1 q + 1 Ω u q + 1 u t x 1 d x - 1 m + 2 u 2 2 (12)

Making use of the Cauchy-Schwarz inequality again, we have

| d d t u 2 2 | ε 0 2 u t 2 2 + 1 2 ε 0 u 2 2 , (13)

and

Ω | u | q + 1 | u t x 1 | d x ε 1 2 u t 2 2 + 1 2 ε 1 u 2 q + 2 2 q + 2 , (14)

where ε0 and ε1 are two positive constants, which will be given later. Moreover, we have

0 t Ω e - ( t - s ) u t ( x , t ) u ( x , s ) d x d s ε 2 2 ( 1 - e - t ) u t 2 2 + 1 2 ε 2 0 t e - ( t - s ) u ( x , s ) 2 2 d s

ε 2 2 u t 2 2 + 1 ε 2 0 t e - ( t - s ) G ( s ) d s , (15)

here ε2>0 will be chosen later. Likewise, we can obtain that

0 t Ω e - ( t - s ) u ( x , t ) u ( x , s ) d x d s 1 2 u 2 2 + 0 t e - ( t - s ) G ( s ) d s . (16)

Combining (12)-(16), we arrive at

             H ( t ) 1 m + 2 G ' ' ( t ) + [ m ε 0 4 ( m + 2 ) + ε 1 2 ( q + 1 ) + ε 2 ( m + 1 ) 2 ( m + 2 ) ] u t 2 2

         + [ 3 2 ( m + 2 ) + m 4 ε 0 ( m + 2 ) ] u 2 2 + 1 2 ε 1 ( q + 1 ) u 2 q + 2 2 q + 2 + [ m + 1 ε 2 ( m + 2 ) + 1 m + 2 ] 0 t e - ( t - s ) G ( s ) d s . (17)

Noticing that m>2q, Young’s inequality can be used to obtain

u 2 q + 2 2 q + 2 m - 2 q m + 2 | Ω | + 2 q + 2 m + 2 u m + 2 m + 2 . (18)

On the other hand, using (8) and (16), we are easy to find that

u m + 2 m + 2 = G ' ( t ) + u 2 2 - 0 t Ω e - ( t - s ) u ( x , t ) u ( x , s ) d x d s

G ' ( t ) + 3 2 u 2 2 + 0 t e - ( t - s ) G ( s ) d s . (19)

From (17), (18) and (19), it follows that

H ( t ) 1 m + 2 G ' ' ( t ) + 1 ε 1 ( m + 2 ) G ' ( t ) + [ 3 2 ( m + 2 ) + m 4 ε 0 ( m + 2 ) + 3 2 ε 1 ( m + 2 ) ] u 2 2

+ [ m ε 0 4 ( m + 2 ) + ε 1 2 ( q + 1 ) + ε 2 ( m + 1 ) 2 ( m + 2 ) ] u t 2 2

  + [ 1 m + 2 + 1 ε 1 ( m + 2 ) + m + 1 ε 2 ( m + 2 ) ] 0 t e - ( t - s ) G ( s ) d s + | Ω | ( m - 2 q ) 2 ε 1 ( m + 2 ) ( q + 1 ) . (20)

Furthermore, the term 0te-(t-s)G(s)ds can be estimated as follows:

0 t e - ( t - s ) G ( s ) d s = e - t 0 t e s G ( s ) d s = G ( t ) - e - t G ( 0 ) - 0 t e - ( t - s ) G ' ( s ) d s G ( t ) - 0 t e - ( t - s ) G ' ( s ) d s . (21)

Now, from the expressions of the constants δi, i=1, 2, 3, it follows that δ1>1, δ2>0 and δ3>0. Then by the assumption u0m+2m+2>δ1u022+δ2u0p+2p+2+δ3, we have u0m+2m+2>u022. This tells us that G'(0)=u0m+2m+2-u022>0. Hence, there exists a t1(0,+) such that G'(t)0 holds for any t[0,t1]. Collecting this fact and (21), we have

0 t e - ( t - s ) G ( s ) d s G ( t ) ,    t [ 0 ,   t 1 ] . (22)

From (6) and (7), it follows that

u t 2 2 H ( t ) , (23)

and

u 2 2 2 G ( t ) - 2 C . (24)

In light of the constraint that p(0,m), one can choose suitable ε0, ε1 and ε2 such that

C 1 = m ε 0 4 ( m + 2 ) + ε 1 2 ( q + 1 ) + ε 2 ( m + 1 ) 2 ( m + 2 ) ( 0 , m - p m + 2 ) ( 0,1 ) .

For the fixed ε0, ε1 and ε2 above, taking

C = ε 0 | Ω | ( m - 2 q ) ( q + 1 ) ( 6 ε 0 + m ε 1 + 6 ε 0 ε 1 ) ,

then (20)-(24) tell us that

( m + 2 ) ( 1 - C 1 ) H ( t ) G ' ' ( t ) + 1 ε 1 G ' ( t ) + ( 4 + m 2 ε 0 + 4 ε 1 + m + 1 ε 2 ) G ( t ) . (25)

Inserting (25) in (11), we have

G ( t ) G ' ' ( t ) - α ( G ' ( t ) ) 2 + β G ( t ) G ' ( t ) + γ G 2 ( t ) 0 ,    t [ 0 , t 1 ] , (26)

where

α = ( m + 2 ) ( 1 - C 1 ) P + 2 > 1 ,   β = 1 ε 1 ,   γ = 4 + m 2 ε 0 + 4 ε 1 + m + 1 ε 2 .

Now, setting Z(t)=G1-α(t)eβt, then (26) tells us that

Z ' ' ( t ) - β Z ' ( t ) - γ ( α - 1 ) Z ( t ) 0 ,    t [ 0 , t 1 ] . (27)

In light of the constraint that the assumption u0m+2m+2>δ1u022+δ2u0p+2p+2+δ3, we have

G ' ( 0 ) > ( β α - 1 + γ α - 1 ) G ( 0 ) > β α - 1 G ( 0 ) . (28)

Then there exists a t2(0,t1] such that, for any t[0,t2], Z'(t)=(α-1)eβtG-α(t)(βα-1G(t)-G'(t))0. The above inequality together with (27), leads to Z''(t)-γ(α-1)Z(t)0,  t[0, t2]. Multiplying both sides of the above inequality by Z'(t) results in Z'(t)Z''(t)-γ(α-1)Z(t)Z'(t)0,  t[0,t2]. Namely,

[ ( Z ' ( t ) ) 2 - γ ( α - 1 ) Z 2 ( t ) ] ' 0 ,    t [ 0 , t 2 ] ,

which implies that

( Z ' ( t ) ) 2 [ Z ' ( 0 ) ] 2 + γ ( α - 1 ) [ Z 2 ( t ) - Z 2 ( 0 ) ]

( α - 1 ) 2 G - 2 α ( 0 ) { [ G ' ( 0 ) - β α - 1 G ( 0 ) ] 2 - γ α - 1 G 2 ( 0 ) } ,    t [ 0 , t 2 ] . (29)

Combining (28) with (29) yields that

Z ' ( t ) - ( α - 1 ) G - α ( 0 ) [ G ' ( 0 ) - β α - 1 G ( 0 ) ] 2 - γ α - 1 G 2 ( 0 ) = B . (30)

Integrating the above differential inequality from 0 to t, we have Z(t)Z(0)-Bt, which implies that G(t)eβα-1tG1-α(0)-Btα-1. That is, G(t) will tend to as

t T - = 1 B G α - 1 ( 0 ) = 1 B ( 1 2 u 0 2 2 + p + 1 p + 2 u 0 p + 2 p + 2 + C ) α - 1 < . (31)

This completes the proof of Theorem 1.

References

  1. Chen P J, Gurtin M E. On a theory of heat conduction involving two temperatures[J]. Zeitschrift Für Angewandte Mathematik und Physik ZAMP, 1968, 19(4): 614-627. [Google Scholar]
  2. Ting T W. A cooling process according to two-temperature theory of heat conduction[J]. Journal of Mathematical Analysis and Applications, 1974, 45(1): 23-31. [Google Scholar]
  3. Barenblatt G I, Zheltov I P, Kochina I N. Basic concepts in the theory of seepage of homogeneous liquids in fissured rocks [strata][J]. Journal of Applied Mathematics and Mechanics, 1960, 24(5): 1286-1303. [Google Scholar]
  4. Cuesta C, van DUIJN C J, Hulshof J. Infiltration in porous media with dynamic capillary pressure: Travelling waves[J]. European Journal of Applied Mathematics, 2000, 11(4): 381-397. [Google Scholar]
  5. Victor P. Sobolev regularization of a nonlinear ill-posed parabolic problem as a model for aggregating populations[J]. Communications in Partial Differential Equations, 1998, 23(3/4): 457-486. [Google Scholar]
  6. Padrón V. Effect of aggregation on population recovery modeled by a forward-backward pseudoparabolic equation[J]. Transactions of the American Mathematical Society, 2004, 356(7): 2739-2756. [Google Scholar]
  7. Korpusov M O, Sveshnikov A G. Blow-up of solutions of strongly nonlinear equations of pseudoparabolic type[J]. Journal of Mathematical Sciences, 2008, 148(1): 1-142. [Google Scholar]
  8. Yushkov E V. On the blow-up of a solution of a non-local system of equations of hydrodynamic type[J]. Izvestiya: Mathematics, 2012, 76(1): 190-213. [Google Scholar]
  9. Korpusov M O. Global solvability conditions for an initial-boundary value problem for a nonlinear equation of pseudoparabolic type[J]. Differential Equations, 2005, 41(5): 712-720. [Google Scholar]
  10. Korpusov M O, Sveshnikov A G. Blow-up of solutions of nonlinear Sobolev type equations with cubic sources[J]. Differential Equations, 2006, 42(3): 431-443. [Google Scholar]
  11. Ding H, Zhou J. Global existence and blow-up for a mixed pseudo-parabolic p-Laplacian type equation with logarithmic nonlinearity[J]. Journal of Mathematical Analysis and Applications, 2019, 478(2): 393-420. [Google Scholar]
  12. Cao Y, Yin J X. An overview of recent studies on the pseudo-parabolic equation[J]. Scientia Sinica (Mathematica), 2024, 54(3): 259-284(Ch). [Google Scholar]
  13. Meyvaci M. Blow up of solutions of pseudoparabolic equations[J]. Journal of Mathematical Analysis and Applications, 2009, 352(2): 629-633. [Google Scholar]
  14. Korpusov M O, Sveshnikov A G. On blowup of a solution to a Sobolev-type equation with a nonlocal source[J]. Siberian Mathematical Journal, 2005, 46(3): 443-452. [Google Scholar]
  15. Ptashnyk M. Degenerate quasilinear pseudoparabolic equations with memory terms and variational inequalities[J]. Nonlinear Analysis: Theory, Methods & Applications, 2007, 66(12): 2653-2675. [Google Scholar]

Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.

Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.

Initial download of the metrics may take a while.