Startseite On a strongly damped semilinear wave equation with time-varying source and singular dissipation
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On a strongly damped semilinear wave equation with time-varying source and singular dissipation

  • Yi Yang und Zhong Bo Fang EMAIL logo
Veröffentlicht/Copyright: 18. November 2022

Abstract

This paper deals with the global well-posedness and blow-up phenomena for a strongly damped semilinear wave equation with time-varying source and singular dissipative terms under the null Dirichlet boundary condition. On the basis of cut-off technique, multiplier method, contraction mapping principle, and the modified potential well method, we establish the local well-posedness and obtain the threshold between the existence and nonexistence of the global solution (including the critical case). Meanwhile, with the aid of modified differential inequality technique, the blow-up result of the solutions with arbitrarily positive initial energy and the lifespan of the blow-up solutions are derived.

MSC 2010: 35L05; 35L71; 35A01

1 Introduction

We consider a strongly damped semilinear wave equation with time-varying source and singular dissipative terms:

(1.1) u t t Δ u Δ u t + V ( x ) u t = k ( t ) u p 2 u , ( x , t ) Ω × ( 0 , + ) ,

subject to the null Dirichlet boundary and initial conditions:

(1.2) u ( x , t ) = 0 , ( x , t ) Ω × ( 0 , + ) ,

(1.3) u ( x , 0 ) = u 0 ( x ) , u t ( x , 0 ) = u 1 ( x ) , x Ω ,

where Ω R N ( N > 2 ) is a bounded domain containing the origin 0 with smooth boundary Ω (if the origin is not included, the parallel movement invariance of spatial variables can be used to move the origin to the interior of the region), u 0 ( x ) H 0 1 ( Ω ) , u 1 ( x ) L 2 ( Ω ) and 2 < p < 2 N N 2 . Moreover, the singular coefficient of weak damping is given as follows:

V ( x ) = x s ( 0 s 2 ) ,

and time-dependent coefficients k ( t ) satisfies the following equation:

k ( t ) C 1 ( [ 0 , + ) ) , k ( 0 ) > 0 , k ( t ) 0 , t [ 0 , + ) .

Our model (1.1) is a classical semilinear wave equation with strong or weak damping that often appears in the theory of viscoelasticity. For instance, in one and two space dimensions, when V ( x ) 1 , (1.1) models the transversal vibrations of a homogeneous string and the longitudinal vibrations of a homogeneous bar, respectively. The term Δ u t indicates that the stress is proportional not only to the strain, as with the Hooke law, but also to the strain rate as in a linearized Kelvin-Voigt material. The term V ( x ) u t describes the damping effect, which plays a role in reducing the energy of the wave (cf. [19]). Meanwhile, it is well known that the data k ( t ) u p 2 u may greatly affect the behavior of u ( x , t ) with the development of time. In fact, we assume that k ( t ) is positive and nondecreasing in the source term of (1.1). So the blow-up phenomena of solutions is easy to occur under some conditions.

During the past decades, there have been fruitful results on the well-posedness and qualitative properties of solutions for nonlinear wave equation with strongly damping term. Among them, we are very interested in the Dirichlet initial boundary value problem to the strongly damped semilinear wave equation with time-varying source and singular dissipative term. In order to state our research motivation, we review the advances on (strongly damped) semilinear wave equation with the source term of power type. Webb [24] first considered the following semilinear wave equation with strongly damped term:

u t t Δ u γ Δ u t = f ( u ) , ( x , t ) Ω × ( 0 , + ) ,

where γ 0 , f ( u ) = u p 2 u with 2 < p < + if N = 1 , 2 , or 2 < p 2 N 2 N 2 for γ = 0 and 2 < p 2 N N 2 for γ > 0 if N 3 . He established the well-posedness of strong solutions by virtue of operator theory and obtained the long-time behavior of the solution with the aid of Lyapunov stability techniques. As for the blow-up analysis, Ono [16] derived the conclusion that the solution with negative initial energy blows up at finite time. Ohta [15] derived the result that the solutions with negative initial energy blow up in finite time. In particular, Gazzola and Squassina [5] considered the semilinear strongly damped wave equations with frictional damping:

u t t Δ u ω Δ u t + μ u t = u p 2 u , ( x , t ) Ω × ( 0 , + ) .

By using the potential well method and Levineąŕs concavity technique, they obtained the existence and nonexistence of the solution with E ( 0 ) d and the blow-up result in the case of high initial energy E ( 0 ) > d . In [14], we investigated the Dirichlet initial boundary value problem of a semilinear wave equation with strong damping and logarithmic nonlinear source

u t t Δ u Δ u t = u log u 2 , ( x , t ) Ω × ( 0 , + ) ,

and derived the global solvability, decay estimate, and infinite blow-up results by means of potential well theory and logarithmic Sobolev inequality. Di et al. [3] improved our results to the more general problem with logarithmic source. Recently, Lian and Xu [13] studied the Dirichlet initial boundary value problem of a damped wave equation with logarithmic source term:

u t t Δ u ω Δ u t + μ u t = u ln u , ( x , t ) Ω × ( 0 , + ) .

Combining the contraction mapping principle with the potential well method and differential inequality technique, they proved the local and global existence of the weak solution, energy decay of global solution, and infinite blow-up results with three initial data levels.

In addition, we refer to [7,17] on global existence and smooth attractors of weak solutions to Dirichlet exterior problems of such equations in two-dimensional space and [1] on existence of ground state solutions for a semilinear elliptic problem with critical and subcritical growth.

However, to our knowledge, there is few research on the models with singular space-dependent coefficient of frictional damping V ( x ) u t and time-dependent coefficient of source k ( t ) u p 2 u . Most recently, there are some new advances on the study of hyperbolic equations without strong damping but with weighted weakly damping terms, one can see [8,9,10,19,22,23]. For instance, Pata and Zelik [17] considered the Cauchy problem of the wave equation with space-dependent coefficient of weak damping:

u t t Δ u + V ( x ) u t = 0 , ( x , t ) R N × ( 0 , + ) ,

where V ( x ) = ( 1 + x 2 ) α 2 , 0 α < 1 . He proved that the asymptotic profile of the solution by a solution of the corresponding heat equation in the L 2 sense. Watanabe [23] studied Dirichlet exterior problems of nonlinear wave system with space-time dependent dissipative term:

u t t Δ u + V ( x , t ) u t = F ( u , 2 u ) , ( x , t ) Ω × ( 0 , + ) ,

where Ω = R N Σ , Σ is a star-shaped domain with a smooth and compact boundary Ω . He derived the global existence and decay estimate of the solutions under some appropriate condition by rescaling technique. Ikeda and Sobajima [8] considered the Dirichlet initial boundary value problem for semilinear wave equations with space-dependent coefficient of weak damping and convex source terms:

u t t Δ u + V ( x ) u t = λ u p , ( x , t ) C Σ × ( 0 , T ) ,

in an cone-like domain, where C Σ is a cone-like domain in R N ( N 2 ) defined as C Σ = int { r w R N ; r 0 , w Σ } with a connected open set Σ in S N 1 with smooth boundary Σ . Here, V ( x ) is a nonzero coefficient of t u satisfying V ( x ) V 0 ( 1 + x 2 ) α 2 and α [ 0 , 1 ] , 1 < p < N N 2 , λ C is a fixed constant, they proved the sharp upper lifespan estimates of solutions by a test function method. Recently, this method was extended by Ikehata and Takeda [9] to study the Cauchy problem of semilinear wave equations with scattering space-dependent damping

u t t Δ u + V ( x ) u t = u p , ( x , t ) R N × ( 0 , T ) ,

where V ( x ) = μ ( 1 + x ) β , μ > 0 , β > 2 . Suppose that the initial data f ( x ) , g ( x ) are compactly supported functions, they proved that the upper bound of the lifespan is the same as that of the solution of the corresponding problem without damping. They mainly constructed the test function appropriately. In addition, for the new progresses on parabolic equation (including pseudo-parabolic equation) with singular potential and time-dependent coefficients, we refer the reader to [4,6,12,18,20, 21,25] and the references therein.

In view of the works mentioned earlier, much less effort has been devoted to strongly damped semilinear wave equation with time-varying source and singular dissipation to our knowledge. The main difficulties lie in the following: (i) the treatment of singular damping V ( x ) u t , and (ii) the Nehari manifold, well depth, stable, and unstable sets of corresponding problems Δ u = k ( t ) u p 2 u are time-varying since the existence of time-dependent coefficient k ( t ) . Motivated by these observations, by cut-off technique, multiplier method, and contraction mapping principle, we will establish the local well-posedness of problems (1.1)–(1.3). Meanwhile, we will make some revisions to the classical potential well method and apply Hardy-Sobolev inequality to obtain the global existence, asymptotic behavior and blow-up results (including critical initial energy). Finally, by using the technique of differential inequality, the lifespan estimate of blow-up solutions is established.

The remainder of this paper is organized as follows. In Secttion 2, we present some symbols, definitions, lemmas, potential wells, and series of relative properties. In Sections 3 and 4, we prove well-posedness of local solutions to problems (1.1)–(1.3) and obtain global existence, asymptotic behavior, and blow-up of solutions with initial energy E ( 0 ) d ( ) . In Section 5, we derive the finite time blow-up result with arbitrary positive initial energy E ( 0 ) > 0 . Finally, a lower bound for the blow-up time is obtained in Section 6.

2 Preliminaries

Throughout this paper, we will use C and C i ( i = 1 , ) to denote various constants. For u , v H 0 1 ( Ω ) , in view of Poincare inequality, we have the following inner-product and norm:

( u , v ) H 0 1 ( Ω ) ( u , v ) Ω u v d x , u H 0 1 ( Ω ) u 2 Ω u 2 d x 1 2 .

Meanwhile, we denote < , > as the duality pairing between H 1 ( Ω ) and H 0 1 ( Ω ) , and we set the following Hilbert phase space:

H 0 1 ( Ω ) × L 2 ( Ω ) ,

endowed with norm

( ( u , v ) ) 2 u 2 2 + v 2 2 , ( ( u , v ) ) ,

where ( ( , ) ) represents a pair of functions in H 0 1 ( Ω ) and L 2 ( Ω ) .

Now, we define functionals on H 0 1 ( Ω ) as follows:

J ( u ; t ) 1 2 u 2 2 1 p k ( t ) u p p , I ( u ; t ) u 2 2 k ( t ) u p p ,

and then we have

(2.1) J ( u ; t ) = p 2 2 p u 2 2 + 1 p I ( u ; t ) .

Meanwhile, introducing the following energy functional:

E ( t ) 1 2 u t 2 2 + 1 2 u 2 2 1 p k ( t ) u p p

for t [ 0 , + ) .

Next, we establish potential wells for problems (1.1)–(1.3) and prove a series of relative properties. We proceed to give the definitions of Nehari manifold and potential depth, respectively, as follows:

N ( t ) { u H 0 1 ( Ω ) { 0 } I ( u ; t ) = 0 } , d ( t ) inf u H 0 1 ( Ω ) { 0 } sup λ 0 J ( λ u ; t ) = inf u N ( t ) J ( u ; t ) .

Moreover, we introduce the following stable and unstable sets:

W ( t ) { u H 0 1 ( Ω ) { 0 } I ( u ( t ) ; t ) 0 } , V ( t ) { u H 0 1 ( Ω ) { 0 } I ( u ( t ) ; t ) < 0 } .

Definition 2.1

(Weak solution) u ( x , t ) is called a weak solution of (1.1)–(1.3) on Ω × [ 0 , T ] if u C ( [ 0 , T ] ; H 0 1 ( Ω ) ) with u t C ( [ 0 , T ] ; L 2 ( Ω ) ) and u t t L 2 ( 0 , T ; H 1 ( Ω ) ) satisfying

  1. for any η H 0 1 ( Ω ) and a.e. t ( 0 , T ) ,

    (2.2) u t t , η + ( u , η ) + ( u t , η ) + ( x s u t , η ) = k ( t ) ( u p 2 u , η )

    and 0 t u τ x s 2 2 2 d τ < + .

  2. u ( x , 0 ) = u 0 ( x ) in H 0 1 ( Ω ) ; u t ( x , 0 ) = u 1 ( x ) in L 2 ( Ω ) .

Definition 2.2

(Finite time blow-up) Let u ( x , t ) be a weak solution of problems (1.1)–(1.3). We say that u ( x , t ) blows up in finite time if the maximal existence time satisfying T max < + and

lim t T max u 2 2 + u x s 2 2 2 = + .

Due to the singularity existing in the model equation, we need the following Hardy-Sobolev inequality.

Lemma 2.1

(Hardy-Sobolev inequality) (cf. [2]) Let R N = R k × R N k , 2 k N , and x = ( y , z ) R N = R k × R N k . For given p , s satisfying 1 < p < N , 0 s p , s < k , and m ( s , N , p ) = p ( N s ) N p , there exists a positive constant H = H ( s , N , p , k ) such that for any u W 0 1 , n ( R N ) ,

(2.3) R N u ( x ) m y s d x H R N u p d x N s N p .

Remark 2.1

When m = p = s , this inequality is the classical Hardy inequality. With above inequality, we have u x s 2 2 2 H u 2 2 ( H > 0 ) . In fact, let m = 2 in (2.3), and by m ( s , N , p ) = p ( N s ) N p , we have p = 2 N N s + 2 . For u H 0 1 ( Ω ) , by extending u ( x ) with u ( x ) = 0 in x R N Ω , we have u H 1 ( R N ) , and (2.3) becomes

(2.4) u x s 2 2 2 H Ω u 2 N N s + 2 d x N s + 2 N .

Due to 0 s 2 , then 2 N N + 2 γ 2 . We define γ 2 N N s + 2 , then N s + 2 N = 2 γ . By N > 2 , we know 2 N N + 2 > 1 , and then 1 < γ 2 . By (2.4) and L 2 ( Ω ) L γ ( Ω ) , we obtain

u x s 2 2 2 H Ω u γ d x 2 γ = H u γ 2 H u 2 2 .

Next, we provide the relative properties of potential wells.

Lemma 2.2

Let u H 0 1 ( Ω ) { 0 } for any t [ 0 , + ) , and the potential depth d ( t ) satisfies

(2.5) ( i ) d ( t ) = p 2 2 p 1 k ( t ) B 0 p 2 p 2 > 0 ,

where B 0 is the optimal embedding constant of H 0 1 ( Ω ) L p ( Ω ) , i.e.,

(2.6) 1 B 0 = inf u H 0 1 ( Ω ) { 0 } u 2 u p and u p B 0 u 2 , u H 0 1 ( Ω ) .

(ii) d ( t ) is positive nonincreasing, and there exists d ( ) [ 0 , d ( 0 ) ] such that d ( ) lim t + d ( t ) .

Proof

(i) For any 0 u H 0 1 ( Ω ) and t 0 , let

F ( λ ) J ( λ u ; t ) = λ 2 2 u 2 2 k ( t ) p λ p u p p , λ 0 .

By a simple computation, it can be known that there exists a unique λ u 2 2 k ( t ) u p p 1 p 2 such that F ( λ ) = 0 , F ( λ ) is strictly increasing on ( 0 , λ ) and strictly decreasing on ( λ , + ) . Hence, using the definition of the potential depth d and combining (2.6), we have

d ( t ) = inf u H 0 1 ( Ω ) { 0 } sup λ 0 J ( λ u ; t ) = inf u H 0 1 ( Ω ) { 0 } F ( λ ) = p 2 2 p 1 k ( t ) B 0 p 2 p 2 .

Obviously, it is known from the assumption of k ( t ) , k ( t ) C 1 ( [ 0 , + ) ) is a nondecreasing function satisfying k ( 0 ) > 0 , and for t [ 0 , + ) , well depth d ( t ) > 0 .

(ii) Based on (2.5) and the assumption of k ( t ) , it is easy to verify that d ( t ) is nondecreasing and d ( ) [ 0 , d ( 0 ) ] . The proof of Lemma 2.2 is completed.□

Lemma 2.3

Let u be a solution of problems (1.1)–(1.3), then E ( t ) is nonincreasing with respect to t.

Proof

Multiplying (1.1) by u t , then integrating over Ω × [ 0 , t ] , we arrive at

1 2 u t 2 2 + 1 2 u 2 2 + 0 t u τ 2 2 d τ + 0 t u τ x s 2 2 2 d τ + 1 p 0 t k ( τ ) u p p d τ 1 p k ( t ) u p p = 1 2 u 1 2 2 + 1 2 u 0 2 2 1 p k ( 0 ) u 0 p p .

Utilizing the definition of E ( t ) , which can lead to

(2.7) E ( t ) + 0 t u τ 2 2 d τ + 0 t u τ x s 2 2 2 d τ + 1 p 0 t k ( τ ) u p p d τ = E ( 0 ) ,

and with the assumption of k ( t ) , we have

d d t E ( t ) = u t 2 2 Ω u t 2 x s d x 1 p k ( t ) u p p 0 .

The proof is completed.□

3 Local solvability and regularity

In this section, the existence and uniqueness of local solutions will be proved by applying the Galerkin method and compression mapping principle.

Due to the singularity existing in the model equation, we introduce the following ρ n ( x ) to deal with it

ρ n ( x ) min { x s , n } , n N .

Further, we denote

( v , w ) Ω v w d x + Ω ρ n v w d x , v ( v , v ) v 2 2 + Ω ρ n v 2 d x .

To prove the existence and uniqueness of local solution in time of problems (1.1)–(1.3), we need the following lemma that converts the nonlinear problem into a linear problem.

Lemma 3.1

For some T > 0 and every initial data ( ( u 0 ( x ) , u 1 ( x ) ) ) and every known u n satisfying

u n C ( [ 0 , T ] ; H 0 1 ( Ω ) ) C 1 ( [ 0 , T ] ; L 2 ( Ω ) ) , u n t L 2 ( 0 , T ; H 0 1 ( Ω ) ) ,

there exists a unique solution

v n C ( [ 0 , T ] ; H 0 1 ( Ω ) ) C 1 ( [ 0 , T ] ; L 2 ( Ω ) ) , v n t L 2 ( 0 , T ; H 0 1 ( Ω ) ) , v n t t L 2 ( 0 , T ; H 1 ( Ω ) ) ,

which solves the linear problem

(3.1) v n t t Δ v n Δ v n t + ρ n ( x ) v n t = k ( t ) u n p 2 u n , ( x , t ) Ω × ( 0 , T ) , v n ( x , t ) = 0 , ( x , t ) Ω × ( 0 , T ) , v n ( x , 0 ) = u 0 ( x ) , v n t ( x , 0 ) = u 1 ( x ) , x Ω .

Proof

The standard approach to show this result is the Galerkin method.

Step 1: Approximate problem.

For j N , we choose a complete smooth orthogonal basis { ω j ( x ) } j = 1 + with ω j 2 = 1 in H 0 1 ( Ω ) , which is also orthogonal in L 2 ( Ω ) . We define finite dimensional space W h span { ω 1 , , ω h } , h N , and we construct the approximate solution v n h ( t ) of problem (3.1):

(3.2) v n h ( t ) = j = 1 h γ n j h ( t ) ω j ( x ) ,

admitting to the following Cauchy problem:

(3.3) v ¨ n h , ω j + ( v n h , ω j ) + ( v ˙ n h , ω j ) + ( ρ n ( x ) v ˙ n h , ω j ) = k ( t ) ( u n p 2 u n , ω j ) ,

v n h ( x , 0 ) = j = 1 h γ n j h ( 0 ) ω j ( x ) u 0 ( x ) , h + ,

and

v ˙ n h ( x , 0 ) = j = 1 h γ ˙ n j h ( 0 ) ω j ( x ) u 1 ( x ) , h + ,

where v ¨ n h ( t ) and v ˙ n h ( t ) are derivatives of time variables t .

According to the standard theory for ordinary differential equations, for every j and n , there exists a unique global solution γ n j h C ( [ 0 , T ] ) of the aforementioned Cauchy problem. Therefore, the unique solution v n h solves (3.3). Next, we will prove that { v n h } has convergent subsequences, and its limit v n is the unique weak solution of problem (3.1).

Step 2: A priori estimates.

In (3.3), taking η = v ˙ n h ( t ) and integrating from 0 to t , we obtain

(3.4) 1 2 v ˙ n h 2 2 + 1 2 v n h 2 2 + 0 t v ˙ n h 2 d τ = 1 2 u 1 h 2 2 + 1 2 u 0 h 2 2 + 0 t Ω k ( τ ) u n p 2 u n v ˙ n h d x d τ .

Next we estimate the last term in (3.4). By Hölder’s inequality and the assumption of k ( t ) , we derive

(3.5) 0 t Ω k ( τ ) u n p 2 u n v ˙ n h d x d τ max t [ 0 , T ] k ( t ) 0 t Ω u n p 1 v ˙ n h d x d τ max t [ 0 , T ] k ( t ) 0 t u n p 1 2 N N + 2 v ˙ n h 2 N N 2 d τ C T 0 T u n 2 N ( p 1 ) N + 2 p 1 v ˙ n h 2 N N 2 d τ .

So next we estimate the term v ˙ n h 2 N N 2 in the aforementioned formula. Since H 0 1 ( Ω ) L 2 N N 2 ( Ω ) , we have v ˙ n h 2 N N 2 C v ˙ n h 2 . Meanwhile, due to 2 N ( p 1 ) N + 2 < 2 N N 2 , it follows that the embedding H 0 1 ( Ω ) L 2 N N 2 ( Ω ) L 2 N ( p 1 ) N + 2 ( Ω ) and the estimate:

u n 2 N ( p 1 ) N + 2 p 1 u n 2 p 1 C 1 .

According to the aforementioned estimates, (3.5), and Young’s inequality, (3.4) becomes

(3.6) 1 2 v ˙ n h 2 2 + 1 2 v n h 2 2 + 0 t v ˙ n h 2 d τ 1 2 u 1 h 2 2 + 1 2 u 0 h 2 2 + C T C 1 T 0 t v ˙ n h d τ C ¯ T + 1 2 0 t v ˙ n h 2 d τ ,

where C ¯ T = 1 2 u 1 h ( x ) 2 2 + 1 2 u 0 h ( x ) 2 2 + 1 2 ( C T C 1 T ) 2 T and C ¯ T > 0 is independent of h for every h 1 . By this uniform estimate, we have

v ˙ n h 2 2 + v n h 2 2 + 0 t v ˙ n h 2 d τ C ¯ T , h N .

Therefore, we obtain { v ˙ n h } is uniformly bounded in L ( 0 , T ; L 2 ( Ω ) ) , { v n h } is uniformly bounded in L ( 0 , T ; H 0 1 ( Ω ) ) , and { ρ n ( x ) v ˙ n h } and { v ˙ n h } are uniformly bounded in L 2 ( 0 , T ; L 2 ( Ω ) ) . Further, since

0 t Ω v ˙ n h ( τ ) 2 d x d τ 1 n 0 t Ω ρ n v ˙ n h ( τ ) 2 d x d τ , ρ n = n , R s 0 t Ω ρ v v ˙ n h ( τ ) 2 d x d τ , ρ n = x s ,

which implies { v ˙ n h } is uniformly bounded in L 2 ( 0 , T ; H 0 1 ( Ω ) ) .

Step 3: Pass to the limit.

It follows from the aforementioned priori estimates, that there exist function v n h and a subsequence of { v n h } h = 1 , which we still denote by { v n h } h = 1 for convenience, such that

(3.7) v n h W v n , in L ( 0 , T ; H 0 1 ( Ω ) ) ,

(3.8) v ˙ n h W v ˙ n , in L ( 0 , T ; L 2 ( Ω ) ) ,

(3.9) v ˙ n h W v ˙ n , in L 2 ( 0 , T ; H 0 1 ( Ω ) ) .

Then from Aubin-Lions theorem, we have

(3.10) v n h v n , in C ( [ 0 , T ] ; H 0 1 ( Ω ) ) .

On the other hand, using that u n C ( [ 0 , T ] ; H 0 1 ( Ω ) ) C 1 ( [ 0 , T ] ; L 2 ( Ω ) ) , we obtain u n u , a.e. ( x , t ) Ω × ( 0 , T ) and

u n p 2 u n u p 2 u a.e. ( x , t ) Ω × ( 0 , T ) ,

which implies that

u n p 2 u n W u p 2 u , in L ( 0 , T ; L 2 ( Ω ) ) ,

and

(3.11) v ¨ n h W v ¨ n , in L 2 ( 0 , T ; H 1 ( Ω ) ) .

In view of the aforementioned regularity, we obtain

v n C ( [ 0 , T ] ; H 0 1 ( Ω ) ) C 1 ( [ 0 , T ] ; L 2 ( Ω ) ) .

Therefore, we can pass to the limit in (3.3) and using the initial condition ( ( u 0 h ( x ) , u 1 h ( x ) ) ) ( ( u 0 ( x ) , u 1 ( x ) ) ) in H 0 1 ( Ω ) × L 2 ( Ω ) , we conclude that the existence of the solution v n of problem (3.3) satisfying the condition of (3.1) is proved.

Step 4: Uniqueness.

We suppose that v n and w n are two solutions of problem (3.1), then function z n v n w n verifies

Ω z ¨ n h ω j d x + Ω z n ω j d x + Ω z ˙ n ω j d x + Ω ρ n ( x ) z ˙ n ω j d x = 0 ,

and the initial value ( ( z n ( x , 0 ) , z n t ( x , 0 ) ) ) . Taking z ˙ n = ω j in aforementioned identity, we obtain

1 2 d d t ( z ˙ n 2 2 + z n 2 2 ) + z ˙ n 2 = 0 ,

and integrating from 0 to t , we have

1 2 ( z ˙ n 2 2 + z n 2 2 ) + 0 t z ˙ n 2 d τ = 1 2 ( z n t ( x , 0 ) 2 2 + z n ( x , 0 ) 2 2 ) .

Further, there exists a constant C ¯ such that

z ˙ n 2 2 + z n 2 2 C ¯ ( z n t ( x , 0 ) 2 2 + z n ( x , 0 ) 2 2 ) .

Along with initial conditions z n t ( x , 0 ) 2 2 = z n ( x , 0 ) 2 2 = 0 , we conclude z n = 0 , i.e., v n = w n . The proof of Lemma 3.1 is now complete.□

Theorem 3.1

Let the initial data ( ( u 0 ( x ) , u 1 ( x ) ) ) , then problems (1.1)–(1.3) admit a unique week solution u satisfying

u C ( [ 0 , T ] ; H 0 1 ( Ω ) ) C 1 ( [ 0 , T ] ; L 2 ( Ω ) ) , u t L 2 ( 0 , T ; H 0 1 ( Ω ) ) , u t t L 2 ( 0 , T ; H 1 ( Ω ) ) .

Moreover, at least one of the following statements holds true:

  1. T max = + ;

  2. lim t T max u 2 2 + u t 2 2 = + .

Proof

We will derive existence and uniqueness of local solution to problems (1.1)–(1.3) for appropriate small time T by using contraction mapping theorem. Recalling the definition of ρ n , problems (1.1)–(1.3) become

(3.12) u t t Δ u Δ u t + ρ n ( x ) u t = k ( t ) u p 2 u , ( x , t ) Ω × ( 0 , T ) , u ( x , t ) = 0 , ( x , t ) Ω × ( 0 , T ) , u ( x , 0 ) = u 0 ( x ) , u t ( x , 0 ) = u 1 ( x ) , x Ω .

However, for every n , the aforementioned problem has a correspond solution u n satisfying

(3.13) u n t t Δ u n Δ u n t + ρ n ( x ) u n t = k ( t ) u n p 2 u n , ( x , t ) Ω × ( 0 , T ) , u n ( x , t ) = 0 , ( x , t ) Ω × ( 0 , T ) , u n ( x , 0 ) = u n 0 ( x ) , u n t ( x , 0 ) = u n 1 ( x ) , x Ω .

Take ( ( u n 0 ( x ) , u n 1 ( x ) ) ) , we have u n 0 ( x ) u 0 ( x ) in H 0 1 ( Ω ) and u n 1 ( x ) u 1 ( x ) in L 2 ( Ω ) . Let R 2 = 2 u n 0 ( x ) 2 2 + 2 u n 1 ( x ) 2 2 and for any T > 0 , consider

Q T = { ( u n , u n t ) C ( [ 0 , T ] ; ) : u n ( x , 0 ) = u n 0 ( x ) , u n t ( x , 0 ) = u n 1 ( x ) , max 0 t T u n 2 2 + u n t 2 2 R 2 } .

By Lemma 3.1, we may define v n = Φ ( u n ) as the unique solution to problem (3.1) for any u n Q T .

Next we shall prove a contraction mapping Φ that satisfies Φ ( Q T ) Q T .

(i) Given u n Q T , there must exist a corresponding solution v n = Φ ( u n ) such that for all t ( 0 , T ) the energy identity

1 2 v ˙ n 2 2 + 1 2 v n 2 2 + 0 t v ˙ n 2 d τ = 1 2 u 1 ( x ) 2 2 + 1 2 u 0 ( x ) 2 2 + 0 t Ω k ( τ ) u n p 2 u n v ˙ n d x d τ .

Next we estimate the last term in the aforementioned equation, applying (3.6), Young’s inequality, and Hölder’s inequality, and we obtain that

(3.14) 0 t Ω k ( τ ) u n p 2 u n v ˙ n d x d τ k ( T ) 0 T Ω u n p 1 v ˙ n d x d τ k ( T ) 0 T u n p 1 p 1 v ˙ n p 1 p 2 d τ 1 2 C 2 T k ( T ) R 2 ( p 1 ) + 1 2 0 T v ˙ n h 2 N N 2 d τ 1 2 C 2 T k ( T ) R 2 ( p 1 ) + 1 2 0 T v ˙ n 2 d τ 1 2 C 2 T k ( T ) R 2 ( p 1 ) + 1 2 0 T v ˙ n d τ

for all t ( 0 , T ) . Substituting (3.14) into (3.13) and taking the maximum over ( 0 , T ) provide

v ˙ n 2 2 + v n 2 2 C 3 T k ( T ) R 2 ( p 1 ) + 1 2 R 2 ,

where C 3 is a positive constant independent of T . By choosing sufficiently small T , it suffices to show that T k ( T ) 1 2 C 3 R 2 ( 2 p ) and v ˙ n 2 2 + v n 2 2 R 2 . Thus, we prove Φ ( Q T ) Q T .

(ii) Now, taking ω n 1 Q T and ω n 2 Q T , subtracting the two equations of (3.1) for v n 1 = Φ ( ω n 1 ) and v n 2 = Φ ( ω n 2 ) , and setting v n v n 1 v n 2 , we obtain for any η H 0 1 ( Ω ) and t ( 0 , T ) ,

(3.15) Ω v ¨ n η + v n η + v ˙ n η + ρ n ( x ) v ˙ n η d x = k ( t ) Ω ( ω n 1 p 2 ω n 1 ω n 2 p 2 ω n 2 ) η d x .

Taking η = v ˙ n , we have

(3.16) 1 2 d d t ( v ˙ n 2 2 + v n 2 2 ) + v ˙ n 2 = k ( t ) Ω ( ω n 1 p 2 ω n 1 ω n 2 p 2 ω n 2 ) v ˙ n d x .

Indeed, for every n , we define F ( u ) u p 2 u , and

Ω ( F ( ω n 1 ) F ( ω n 2 ) ) v ˙ n d x = Ω ( ω n 1 p 2 ω n 1 ω n 2 p 2 ω n 2 ) v ˙ n d x .

Let ω n 1 = u n + h and ω n 2 = u n , then h = ω n 1 ω n 2 . By Gateaux derivative and triangle inequality, the aforementioned equation becomes

(3.17) Ω ( ω n 1 p 2 ω n 1 ω n 2 p 2 ω n 2 ) v ˙ n d x = Ω 0 1 d ( F ( u n + ξ h ) ; h ) v ˙ n d ξ d x = Ω 0 1 d d τ ( u n + ξ h + τ h p 2 u n + ξ h + τ h ) τ = 0 v ˙ n d ξ d x = Ω 0 1 ( p 1 ) ω n 2 + ξ ( ω n 1 ω n 2 ) p 2 ( ω n 1 ω n 2 ) v ˙ n d ξ d x Ω ( p 1 ) ( ω n 2 + ω n 1 ) p 2 ω n 1 ω n 2 v ˙ n d x .

Then by substituting (3.17) into (3.16) and integrating over ( 0 , t ) , we can compute

1 2 ( v ˙ n 2 2 + v n 2 2 ) + 0 t v ˙ n 2 d τ C 4 max t [ 0 , T ] k ( t ) T ( p 1 ) R 2 p 4 ω n 1 ω n 2 2 v ˙ n 2 C 4 k ( T ) T ( p 1 ) R 2 p 4 ω n 1 ω n 2 2 v ˙ n 2 ,

where C 4 is independent of T . Therefore, by increasing k ( t ) , as long as T is small enough satisfying

k ( T ) T min 1 2 C 3 R 2 ( 2 p ) , 1 2 ( p 1 ) C 4 R 3 2 p ,

there holds

Φ ( ω n 1 ) Φ ( ω n 2 ) 2 = v n 2 C 4 k ( T ) T ( p 1 ) R 2 p 3 ω n 1 ω n 1 2 1 2 ω n 1 ω n 1 2 .

This proves a contraction mapping Φ that satisfies Φ ( Q T ) Q T . According to contraction mapping theorem, (3.13) defined on ( 0 , T ) has a unique solution u n for every n . Moreover, it follows from u n ( t ) C 1 ( [ 0 , T ] ; H 0 1 ( Ω ) ) and by Arzela-Ascoli Theorem, there exists a subsequence of { u n } (still denoted by { u n } ) and a function u C 1 ( [ 0 , T ] ; H 0 1 ( Ω ) ) such that

u n ( t ) u ( t ) uniformly in C 1 ( [ 0 , T ] ; H 0 1 ( Ω ) ) .

Thus, we obtain the unique solution u to problems (1.1)–(1.3).

Finally, we will use a standard continuation argument to prove the second part of the theorem. Indeed, by contradiction argument, suppose that T max < + and lim t T max u t 2 2 + u 2 2 < + ; then there exists a sequence { t n } n N and a constant K > 0 , such that t n T max as n + and u t 2 2 + u 2 2 < K , n = 1 , 2 , . As we have already shown previously, for each n N , there exists a unique solution of the problems (1.1)–(1.3) with initial data ( u ( t n ) , u ˙ ( t n ) ) on [ t n , t n + T ] , where T > 0 only depends on K . Thus, for n N large enough, we can obtain T max < t n + T . This contradicts the maximality of T max . This completes the proof.□

4 Low initial energy E ( 0 ) d ( )

In this section, we will prove the global existence, finite time blow-up and asymptotic behavior of solutions for problems (1.1)–(1.3) at subcritical energy and critical initial energy.

Theorem 4.1

Let the initial data ( ( u 0 ( x ) , u 1 ( x ) ) ) , E ( 0 ) d ( ) , u 0 ( x ) W ( 0 ) , then problems (1.1)–(1.3) possesses a unique weak global solution, i.e., u ( x , t ) W ( t ) ( 0 t < + ) in the class

u C ( [ 0 , + ) ; H 0 1 ( Ω ) ) C 1 ( [ 0 , + ) ; L 2 ( Ω ) ) , u t L 2 ( 0 , + ; H 0 1 ( Ω ) ) , u t t L 2 ( 0 , + ; H 1 ( Ω ) ) .

Moreover, for 0 t < + , there exists a positive constant C 3 such that the energy functional E ( t ) satisfies polynomial decay estimation: E ( t ) C 3 1 + t .

Proof

The proof of Theorem 4.1 is divided into four steps.

Step 1: Weak solutions for the case of E ( 0 ) < d ( ) .

Recalling the definition of ρ n ( x ) in Section 3, for every n , problems (1.1)–(1.3) become

(4.1) u n t t Δ u n Δ u n t + ρ n ( x ) u n t = k ( t ) u n p 2 u n , ( x , t ) Ω × ( 0 , + ) , u n ( x , t ) = 0 , ( x , t ) Ω × ( 0 , ) , u n ( x , 0 ) = u n 0 ( x ) , u n t ( x , 0 ) = u n 1 ( x ) , x Ω .

Let { η j ( x ) } be a completely orthogonal system in H 0 1 ( Ω ) and construct the approximate solution

u n ( t ) = j = 1 n g j n ( t ) η j ( x ) , n N ,

then we have

(4.2) u n t t , η j + ( u n , η j ) + ( u n t , η j ) + ( ρ n ( x ) u n t , η i ) = k ( t ) ( u n p 2 u n , η i ) , i = 1 , 2 , , n ,

and

u n ( x , 0 ) = j = 1 n g j n ( 0 ) η j ( x ) u 0 ( x ) in H 0 1 ( Ω ) ; u n t ( x , 0 ) = j = 1 n g j n t ( 0 ) η j ( x ) u 1 ( x ) in L 2 ( Ω ) .

Multiplying (4.2) by g i n ( t ) , summing on i = 1 , 2 , , n and integrating with respect to time from 0 to t , we obtain

E ( u n ( t ) ) + 0 t u n τ 2 2 d τ + 0 t Ω ρ n ( x ) u τ 2 d x d τ + 1 p 0 t k ( τ ) u n p p d τ = E ( u n ( 0 ) ) , 0 t < + ,

and it is easy to know E ( u n ( 0 ) ) E ( 0 ) from the initial conditions. For sufficiently large n , we obtain

(4.3) E ( u n ( t ) ) + 0 t u n τ 2 2 d τ + 0 t Ω ρ n ( x ) u n τ 2 d x d τ + 1 p 0 t k ( τ ) u n p p d τ < d ( ) d ( t ) , 0 t < + ,

and

(4.4) E ( u n ( t ) ) = 1 2 u n t 2 2 + J ( u n ; t ) E ( 0 ) < d ( t ) , 0 t < + .

Next, we prove that u n ( x , t ) W ( t ) for t [ 0 , T max ) when E ( 0 ) < d ( ) and u n ( x , 0 ) W ( 0 ) . In fact, we only need to verify that I ( u n ( t ) ; t ) > 0 for t [ 0 , + ) . By contradiction argument, if it is false, then there exists a t 1 > t > 0 such that I ( u n ( t 1 ) ; t 1 ) = 0 and I ( u n ( t ) ; t ) > 0 for t [ 0 , t 1 ) . Then we have J ( u n ( t 1 ) ; t 1 ) d ( t 1 ) by the definition of potential depth d ( t ) , which contradicts with (4.4). Thus, u n ( x , t ) W ( t ) and I ( u n ( t ) ; t ) > 0 for t [ 0 , T max ) .

Now, using the definitions of J ( u ; t ) and I ( u ; t ) , we obtain

(4.5) J ( u n ; t ) = 1 p I ( u n ; t ) + 1 2 1 p u n 2 2 ,

together with I ( u n ; t ) > 0 , (4.2) and (4.4) give

(4.6) 1 2 u n t 2 2 + 1 2 1 p u n 2 2 + 0 t u n τ 2 2 d τ + 0 t Ω ρ n ( x ) u n τ 2 d x d τ + 1 p 0 t k ( τ ) u n p p d τ < d ( ) , 0 t < + ,

from p > 2 , it follows that

(4.7) u n t 2 2 < 2 d ( ) , u n 2 2 < 2 p d ( ) ( p 2 ) , 0 t u n τ 2 2 d τ + 0 t Ω ρ n ( x ) u n τ 2 d x d τ < d ( ) .

Then there exist u and a subsequence still denoted by { u n } n = 1 such that

u n W u , in L ( 0 , + ; H 0 1 ( Ω ) ) , u n t W u t , in L ( 0 , + ; L 2 ( Ω ) ) , u n t W u t , in L 2 ( 0 , + ; H 0 1 ( Ω ) ) , ρ n ( x ) u n t W u t x s , in L 2 ( 0 , + ; L 2 ( Ω ) ) .

Therefore, we take the limit n of the problem (4.1) to obtain a global solution, and u satisfies 0 t u τ x s 2 2 2 d τ < + and we have u ( x , t ) W ( t ) for t [ 0 , + ) .

Step 2: Weak solutions for the case of E ( 0 ) = d ( ) .

Let κ η 1 1 η , u η 0 κ η u 0 , u η 1 κ η u 1 for η 2 is a positive integer. Now, we consider the following problem:

(4.8) u n t t Δ u n Δ u n t + ρ n ( x ) u n t = k ( t ) u n p 2 u n , ( x , t ) Ω × ( 0 , + ) ,

(4.9) u ( x , t ) = 0 , ( x , t ) Ω × ( 0 , + ) ,

(4.10) u ( x , 0 ) = u η 0 ( x ) , u t ( x , 0 ) = u η 1 ( x ) , x Ω .

First, we claim that I ( u n 0 ; 0 ) > 0 and E ( u n 0 , u n 1 ) < d ( ) .

Indeed, using I ( u 0 ; 0 ) > 0 and Lemma 2.2, we observe that λ > 1 , combining with 0 < κ n < 1 , we have

(4.11) I ( u n 0 ; 0 ) = I ( κ n u 0 ; 0 ) > 0 .

In addition, by direct calculation, we can obtain

d d κ n J ( κ n u 0 ; 0 ) = 1 κ n ( κ n 2 u 0 2 2 κ n p k ( 0 ) u 0 p p ) = 1 κ n I ( κ n u 0 ; 0 ) > 0 .

Then J ( κ n u 0 ; 0 ) strictly increases with respect to κ n and

(4.12) E ( u n 0 , u n 1 ) = 1 2 u n 1 2 2 + J ( u n 0 ; 0 ) = 1 2 κ n u 1 2 2 + J ( κ n u 0 ; 0 ) < 1 2 u 1 2 2 + J ( u 0 ; 0 ) = E ( 0 ) = d ( ) .

Thus, we can deduce I ( u n 0 ; 0 ) > 0 , E ( u n 0 , u n 1 ) < d ( ) and u n ( x , t ) W ( t ) . Similar to Step 1, we derive that problems (4.8)–(4.10) admit a global weak solution, and for any n 2 , ζ H 0 1 ( Ω ) and for t ( 0 , + ) ,

( u n t t , ζ ) + ( u n , ζ ) + ( u n t , ζ ) + ( ρ n ( x ) u n t , ζ ) = k ( t ) ( u n p 2 u n , ζ ) .

We can obtain a weak global solution of (1.1)–(1.3) by passing to the limit n + and using u ( x , 0 ) = u 0 ( x ) in H 0 1 ( Ω ) and u t ( x , 0 ) = u 1 ( x ) in L 2 ( Ω ) .

Step 3: Polynomial decay estimate of energy.

Multiplying (1.1) by u and integrating in Ω × ( 0 , t ) , combining with Lemma 2.1, (4.7), Young’s inequality, and Hölder’s inequality, we obatin

(4.13) 0 t I ( u ; t ) d τ = 0 t ( u τ τ , u ) d τ 0 t Ω u τ u d x d τ 0 t Ω u τ u x s d x d τ 1 2 u t 2 2 + 1 2 C 1 u 2 2 + 1 2 u 1 2 2 + 1 2 C 1 u 0 2 2 + 0 t u τ 2 2 d τ + ( H + 1 ) u 2 2 C 3 , 0 t + .

From I ( u ; t ) 0 and Lemma 2.2, we know that there exists a constant λ 1 such that I ( λ u ; t ) = 0 . Hence, from the definition of d ( t ) and (4.5), we obtain

(4.14) d ( t ) J ( λ u ; t ) = 1 2 1 p λ 2 u 2 2 + I ( λ u ; t ) λ p 1 2 1 p u 2 2 λ p 1 2 1 p u 2 2 + I ( u ; t ) = λ p J ( u ; t ) .

By the definitions of E ( t ) , I ( u ; t ) 0 and (4.5), we obtain

(4.15) 1 2 1 p u 2 2 J ( u ; t ) < E ( t ) E ( 0 ) d ( t ) .

It follows from (4.14) and (4.15) that

(4.16) λ d ( t ) J ( u ; t ) 1 p > d ( t ) E ( 0 ) 1 p 1 .

On the other hand, we obtain

(4.17) 0 = I ( λ u ; t ) = λ 2 u 2 2 λ p k ( t ) u p p = λ p I ( u ; t ) [ λ p λ 2 ] u 2 2 ,

which implies that

(4.18) I ( u ; t ) = 1 1 λ p 2 u 2 2 .

The combination of (4.17), λ > 1 , the assumption of k ( t ) , and (4.18), there exists a θ > 1 such that

(4.19) 0 t u 2 2 d τ λ p 2 λ p 2 1 0 t I ( u ; τ ) d τ 1 + 1 θ p 2 1 0 t I ( u ; τ ) d τ C .

Meanwhile, (4.8) yields that

(4.20) 0 t u τ 2 2 d τ 1 Λ 1 0 t u τ 2 2 d τ < d ( ) Λ 1 ,

where Λ 1 is the first eigenvalue of the problem:

ω + Λ 1 ω = 0 , in Ω , ω = 0 , on Ω .

Then we will show polynomial decay estimate of energy. Due to monotonicity of E ( t ) , we conclude

d d t [ ( 1 + t ) E ( t ) ] = ( 1 + t ) E ( t ) + E ( t ) E ( t ) .

Integrating the aforementioned inequality from 0 to t , and from embedding inequality, we infer

( 1 + t ) E ( t ) 1 p 0 t I ( u ( τ ) ; τ ) d τ + p 2 2 p 0 t u 2 2 d τ + 1 2 0 t u τ 2 2 d τ + E ( 0 ) .

Hence, from E ( 0 ) d ( ) , (4.7), (4.13), (4.19), and (4.20), we obtain

E ( t ) C 4 1 + t , 0 t < + .

Consequently, the proof of Theorem 4.1 is completed.□

Next, we present finite time blow-up phenomena of the solution to problems (1.1)–(1.3) by virtue of the convex method with E ( 0 ) d ( ) . To state our results, we first recall Levine’s convexity lemma, which plays a key role in the proof.

Lemma 4.1

(cf. [11]) Let L ( t ) be a positive C 2 function, which satisfies, inequality

L ( t ) L ( t ) ( 1 + ρ ) ( L ( t ) ) 2 0 , t t 0 > 0 ,

with some ρ > 0 . If L ( t 0 ) > 0 and L ( t 0 ) > 0 , then there exists a time T t 0 + L ( t 0 ) ρ L ( t 0 ) such that lim t T L ( t ) = + .

Lemma 4.2

Let u 0 ( x ) V ( 0 ) , E ( 0 ) d ( ) , then we have u ( x , t ) V ( t ) for t [ 0 , T max ) .

Proof

We discuss the following two cases:

Case 1: E ( 0 ) < d ( ) . Making use of (4.2) and (4.3), we can obtain

(4.21) J ( u ; t ) E ( t ) E ( 0 ) < d ( ) d ( t ) , 0 t < T max .

Since u 0 ( x ) V ( 0 ) implies I ( u 0 ; 0 ) < 0 , combined with the continuity of u yields that there exists a t 2 > 0 small enough such that I ( u ( t ) ; t ) < 0 for t [ 0 , t 2 ) . By contradiction, we assume that I ( u ( t ) ; t ) < 0 in [ t 2 , T max ) does not hold, i.e., there exists a t 2 ( t 2 t 2 < T max ) such that I ( u ( t 2 ) ; t 2 ) = 0 and I ( u ( t ) ; t ) < 0 in t 2 t < t 2 . Then by the definition of d ( t ) and Lemma 2.2, we have

J ( u ( t 2 ) ; t 2 ) d ( t 2 ) ,

which contradicts (4.21).

Case 2: E ( 0 ) = d ( ) . Similarly as case 1, there exists a t 3 > 0 small enough such that I ( u ( t ) ; t ) < 0 for t [ 0 , t 3 ) . Arguing by contradiction, we suppose that I ( u ( t ) ; t ) < 0 in [ t 3 , T max ) does not hold, i.e., there exists a t 3 ( t 3 t 3 < T max ) such that I ( u ( t 3 ) ; t 3 ) = 0 and d ( t 3 ) J ( u ( t 3 ) ; t 3 ) . Then from

1 2 u t ( t 3 ) 2 2 + J ( u ( t 3 ) ; t 3 ) + 0 t 3 u τ 2 2 d τ + 0 t 3 u τ x s 2 2 2 d τ + 1 p 0 t 3 k ( τ ) u p p d τ = E ( 0 ) = d ( ) d ( t 3 ) ,

and the monotonicity of k ( t ) , it holds that 0 t 3 u τ x s 2 2 2 d τ = 0 t 3 u τ 2 2 d τ = 0 , which implies d u ( x , t ) d t = 0 and u ( x , t ) = u 0 ( x ) for 0 t t 3 . Thus, we can conclude I ( u ( t 3 ) ; t 3 ) = I ( u 0 ; 0 ) < 0 , which contradicts I ( u ( t 3 ) ; t 3 ) = 0 .□

Now, we describe the result of finite time blow-up as follows:

Theorem 4.2

Let ( ( u 0 ( x ) , u 1 ( x ) ) ) , u 0 ( x ) V ( 0 ) , and E ( 0 ) d ( ) , then we have u ( x , t ) V ( t ) and the solution blows up in finite time. Furthermore, if E ( 0 ) < d ( ) , we have

T max A ( 0 ) p + 2 ( 2 p E ( 0 ) + 2 p d ( ) ) σ ˜ 0 2 ( p 2 ) ( B ( 0 ) p + ( 2 p E ( 0 ) + 2 p d ( ) ) σ ˜ 0 ) 2 C ( 0 ) p ,

where

A ( 0 ) = 2 u 0 2 2 , B ( 0 ) = Ω u 0 u 1 d x , C ( 0 ) = u 0 x s 2 2 2 + u 0 2 2 ,

and σ ˜ 0 is given by (4.33).

Proof

We show that T max < + . We choose t 0 and T [ 0 , T max ) such that 0 t 0 < T < T max and define the function:

L ( t ) u ( t ) 2 2 + t 0 t u 2 2 d τ + t 0 t u x s 2 2 2 d τ + ( T t ) u ( t 0 ) 2 2 + u ( t 0 ) x s 2 2 2 + η ( t + σ ) 2 , t [ t 0 , T ] .

where η > 0 , σ > t 0 , and it is clear that L ( t ) is a positive continuous on t [ t 0 , T ] . By differentiating directly, we obtain

(4.22) L ( t ) = 2 Ω u u t d x + t 0 t d d τ u 2 2 d τ + t 0 t d d τ u x s 2 2 2 d x d τ + 2 η ( t + σ ) = 2 Ω u u t d x + 2 t 0 t Ω u u τ d x d τ + 2 t 0 t Ω u u τ x s d x d τ + 2 η ( t + σ ) ,

(4.23) L ( t ) = 2 u t 2 2 + 2 Ω u u t t d x + 2 Ω u u t d x + 2 Ω 1 x s u u t d x + 2 η .

By multiplying (1.1) u and integrating the result over Ω , we obtain

Ω u u t t d x = k ( t ) u p p u 2 2 Ω Ω u u t d x Ω 1 x s u u t d x .

Applying (1.1) and the definition of E ( t ) and (4.23) can be rewritten by

(4.24) L ( t ) = 2 p E ( t ) + ( p + 2 ) u t 2 2 + ( p 2 ) u 2 2 + 2 η .

For any constant χ > 0 , we directly compute

(4.25) L ( t ) L ( t ) χ ( L ( t ) ) 2 = L ( t ) L ( t ) + 4 χ ξ ( t ) L ( t ) ( T t ) u ( t 0 ) 2 2 + u ( t 0 ) x s 2 2 2 × u t 2 2 + t 0 t u τ 2 2 d τ + t 0 t u τ x s 2 2 2 d τ + η ,

where

ξ ( t ) u ( t ) 2 2 + t 0 t u 2 2 d τ + t 0 t u x s 2 2 2 d τ + η ( t + σ ) 2 u t 2 2 + t 0 t u τ 2 2 d τ + t 0 t u τ x s 2 2 2 d τ + η Ω u u t d x + t 0 t Ω u u τ d x d τ + t 0 t Ω 1 x s u u t d x d τ + η ( t + σ ) 2 .

Now, let us estimate ξ ( t ) . It follows from Hölder’s inequality, we obtain

(4.26) ξ ( t ) u 2 2 + t 0 t u 2 2 d τ + t 0 t u x s 2 2 2 d τ + η ( t + σ ) 2 u t 2 2 + t 0 t u τ 2 2 d τ + t 0 t u τ x s 2 2 2 d τ + η u 2 u t 2 + t 0 t u 2 2 d τ 1 2 t 0 t u τ 2 2 d τ 1 2 + t 0 t u x s 2 2 2 d τ 1 2 t 0 t u τ x s 2 2 2 d τ 1 2 + η ( t + σ ) 2 .

A combination of Cauchy-Schwarz inequality, we can obtain ξ ( t ) 0 , and by (4.26), one can see that

(4.27) L ( t ) L ( t ) χ ( L ( t ) ) 2 L ( t ) L ( t ) 4 χ L ( t ) ( T t ) u ( t 0 ) 2 2 + u ( t 0 ) x s 2 2 2 × u t 2 2 + t 0 t u τ 2 2 d τ + t 0 t u τ x s 2 2 2 d τ + η L ( t ) 2 p E ( t 0 ) + ( 2 p 4 χ ) t 0 t u τ 2 2 d τ + t 0 t u τ x s 2 2 2 d τ + ( p + 2 4 χ ) u t 2 2 + ( p 2 ) u 2 2 + ( 2 4 χ ) η ] .

On choosing χ = p + 2 4 , then 2 p 4 χ = p 2 > 0 , and (4.27) becomes

(4.28) L ( t ) L ( t ) p + 2 4 ( L ( t ) ) 2 L ( t ) 2 p E ( t 0 ) + ( p 2 ) u 2 2 p η + ( p 2 ) t 0 t u τ 2 2 d τ + t 0 t u τ x s 2 2 2 d τ L ( t ) [ 2 p E ( t 0 ) + ( p 2 ) u 2 2 p η ] .

On the other hand, Lemma 4.2 implies that u ( x , t ) V ( t ) for t [ t 0 , T ] and I ( u ; t ) < 0 , and combining Lemma 2.2 that there exists a λ ( t ) ( 0 , 1 ) such that I ( λ ( t ) u ; t ) = 0 . Then using the definitions of d ( t ) , I ( λ u ; t ) and J ( λ u ; t ) , we have

(4.29) p 2 2 p u 2 2 > p 2 2 p λ 2 u 2 2 = p 2 2 p λ 2 u 2 2 + I ( λ u ; t ) = J ( λ u ; t ) d ( t ) d ( ) .

From (4.28) and (4.29), it follows that

L ( t ) L ( t ) p + 2 4 ( L ( t ) ) 2 L ( t ) [ 2 p E ( t 0 ) + 2 p d ( ) p η ] .

Recalling (2.7) and Lemma 2.2, we arrive at

E ( t ) E ( t 0 ) E ( 0 ) t 0 t u τ 2 2 d τ t 0 t u τ x s 2 2 2 d τ < E ( 0 ) d ( ) .

Then we obtain, for any

t [ t 0 , T ] and η 0 , 2 p E ( t 0 ) + 2 p d ( ) p ,

that

L ( t ) L ( t ) p + 2 4 ( L ( t ) ) 2 0 .

According to the definitions of A ( t ) , B ( t ) , C ( t ) , and Lemma 4.1, it holds that

0 < T t 0 4 L ( t 0 ) ( p 2 ) L ( t 0 ) = 2 A ( t 0 ) + 4 ( T t 0 ) C ( t 0 ) + 4 η ( t 0 + σ ) 2 2 ( p 2 ) ( B ( t 0 ) + η ( t 0 + σ ) ) = A ( t 0 ) + 2 η ( t 0 + σ ) 2 ( p 2 ) ( B ( t 0 ) + η ( t 0 + σ ) ) + ( T t 0 ) 2 C ( t 0 ) ( p 2 ) ( B ( t 0 ) + η ( t 0 + σ ) )

or

(4.30) ( T t 0 ) 1 2 C ( t 0 ) ( p 2 ) ( B ( t 0 ) + η ( t 0 + σ ) ) A ( t 0 ) + 2 η ( t 0 + σ ) 2 ( p 2 ) ( B ( t 0 ) + η ( t 0 + σ ) ) .

Fix a

η 0 0 , 2 p E ( t 0 ) + 2 p d ( ) p .

Then for any

σ 2 C ( t 0 ) η 0 ( p 2 ) 1 η 0 B ( t 0 ) t 0 , + ,

we have

0 < 2 C ( t 0 ) ( p 2 ) ( B ( t 0 ) + η 0 ( t 0 + σ ) ) < 1 .

which, together with (4.30), implies that

(4.31) T t 0 + A ( t 0 ) + 2 η 0 ( t 0 + σ ) 2 ( p 2 ) ( B ( t 0 ) + η 0 ( t 0 + σ ) ) 1 2 C ( t 0 ) ( p 2 ) ( B ( t 0 ) + η 0 ( t 0 + σ ) ) 1 = t 0 + A ( t 0 ) + 2 η 0 ( t 0 + σ ) 2 ( p 2 ) ( B ( t 0 ) + η 0 ( t 0 + σ ) ) 2 C ( t 0 ) .

Minimizing the right-hand side in (4.31) for σ 2 C ( t 0 ) η 0 ( p 2 ) 1 η 0 B ( t 0 ) t 0 , + to yield

(4.32) T inf σ 2 C ( t 0 ) η 0 ( p 2 ) 1 η 0 B ( t 0 ) t 0 , + t 0 + A ( t 0 ) + 2 η 0 ( t 0 + σ ) 2 ( p 2 ) ( B ( t 0 ) + η 0 ( t 0 + σ ) ) 2 C ( t 0 ) = t 0 + A ( t 0 ) + 2 η 0 ( t 0 + σ 0 ) 2 ( p 2 ) ( B ( t 0 ) + η 0 ( t 0 + σ 0 ) ) 2 C ( t 0 ) ,

where

σ 0 = ( 2 ( p 2 ) B ( t 0 ) η 0 4 η 0 C ( t 0 ) ) + ( ( 2 ( p 2 ) B ( t 0 ) η 0 4 η 0 C ( t 0 ) ) 2 + 2 η 0 2 ( p 2 ) 2 A ( t 0 ) ) 1 2 × ( 2 η 0 2 ( p 2 ) ) 1 t 0 .

Minimizing the right-hand side of in the aforementioned formula with respect to η 0 0 , 2 p E ( t 0 ) + 2 p d ( ) p , and by the arbitrariness of T T max , we finally obtain

T max t 0 + A ( t 0 ) p + 2 ( 2 p E ( t 0 ) + 2 p d ( ) ) ( t 0 + σ ¯ 0 ) 2 ( p 2 ) ( B ( t 0 ) p + ( 2 p E ( t 0 ) + 2 p d ( ) ) ( t 0 + σ ¯ 0 ) ) 2 C ( t 0 ) p < + ,

where σ ¯ 0 takes σ 0 at η 0 = 2 p E ( t 0 ) + 2 p d ( ) p , which implies that the weak solution u blows up in finite time.

For the case of E ( 0 ) < d ( ) , recalling that t 0 = 0 , we have

T max A ( 0 ) p + 2 ( 2 p E ( 0 ) + 2 p d ( ) ) σ ˜ 0 2 ( p 2 ) ( B ( 0 ) p + ( 2 p E ( 0 ) + 2 p d ( ) ) σ ˜ 0 ) 2 C ( 0 ) p ,

where

(4.33) σ ˜ 0 = ( 2 ( p 2 ) B ( 0 ) η ˜ 0 4 η ˜ 0 C ( 0 ) ) + ( ( 2 ( p 2 ) B ( 0 ) η ˜ 0 4 η ˜ 0 C ( 0 ) ) 2 + 2 η ˜ 0 2 ( p 2 ) 2 A ( 0 ) ) 1 2 ( 2 η ˜ 0 2 ( p 2 ) ) 1 ,

and η ˜ 0 = 2 p E ( 0 ) + 2 p d ( ) p .

This completes the proof.□

Remark 4.1

Assume that the initial energy in the condition of Theorem 4.2 is negative, i.e., the initial data satisfying E ( 0 ) < 0 can directly lead to blow-up, not like that the initial data satisfying E ( 0 ) d ( ) also need I ( u 0 ; 0 ) < 0 to ensure the finite time blow-up. In fact, repeat the proof steps of Theorem 4.2, and we can choose η = 2 E ( 0 ) such that

L ( t ) L ( t ) p + 2 4 ( L ( t ) ) 2 0 ,

then we can take σ appropriately, and the remaining proof is similar to Theorem 4.2. Therefore, we realize that the condition E ( 0 ) < 0 is stricter than E ( 0 ) d ( ) .

5 Blow-up with arbitrary initial energy ( E ( 0 ) > 0 )

The blow-up result studied in Section 4 is closely dependent on the depth of potential well d ( ) . However, the value of d ( ) is small and difficult to calculate exactly. Thus, we establish a blow-up condition independent of d ( t ) in this section.

Theorem 5.1

Suppose that ( ( u 0 ( x ) , u 1 ( x ) ) ) and satisfying

(5.1) Ω u 0 u 1 d x δ 2 E ( 0 ) > 0 ,

(5.2) p 2 C 1 u 0 2 2 > 2 p E ( 0 ) > 0 ,

where δ is a positive constant to be determined later and C 1 satisfies Poincare inequality u 2 2 C 1 u 2 2 , then the solution of problems (1.1)–(1.3) blows up in finite time.

Proof

Arguing by contradiction, we suppose T max = + . Recalling the auxiliary function L ( t ) , similarly as the proof of Theorem 4.2, combining Poincare inequality, we have

(5.3) L ( t ) L ( t ) p + 2 4 ( L ( t ) ) 2 L ( t ) [ 2 p E ( 0 ) + ( p 2 ) u 2 2 p η ] L ( t ) 2 p E ( 0 ) + ( p 2 ) C 1 u 2 2 p η .

First, we claim that

(5.4) Ω u u t d x e 2 p t δ Ω u 0 u 1 d x δ 2 E ( 0 ) + δ 2 E ( t ) , t [ 0 , T max ) .

Indeed, we may consider K ( t ) Ω u u t d x and differentiating directly to obtain

(5.5) K ( t ) = 1 + p 2 u t 2 2 + p 2 1 u 2 2 Ω u t u d x Ω 1 x s u t u d x p E ( t ) .

Applying Cauchy-Schwarz inequality and basic inequality to the last two terms in the right-hand side of (5.5), we have

(5.6) Ω u t u d x + Ω 1 x s u t u d x ( δ u t 2 2 ) 1 2 ( δ 1 u 2 2 ) 1 2 + δ u t x s 2 2 2 1 2 δ 1 u x s 2 2 2 1 2 δ 2 u t 2 2 + u t x s 2 2 2 + 1 2 δ u 2 2 d x + u x s 2 2 2 ,

where δ > 0 . Next, adding (5.5) to (5.6) and using Lemma 2.1 and Poincare inequality, we can derive

d d t K ( t ) δ 2 E ( t ) = 1 + p 2 u t 2 2 + p 2 1 u 2 2 Ω u t u d x Ω 1 x s u t u d x δ 2 E ( t ) p E ( t ) 1 + p 2 u t 2 2 + p 2 1 u 2 2 δ 2 u t 2 2 + u t x s 2 2 2 + E ( t ) 1 2 δ u 2 2 + u x s 2 2 2 p E ( t ) = 1 + p 2 u t 2 2 + p 2 1 u 2 2 1 2 δ u 2 2 + u x s 2 2 2 p E ( t ) 1 + p 2 u t 2 2 + ( p 2 ) δ ( H + 1 ) 2 δ C 1 u 2 2 p E ( t ) = 2 p δ 1 p + 1 2 δ 2 u t 2 2 + ( p 2 ) δ ( H + 1 ) 4 δ C 1 u 2 2 δ 2 E ( t ) ,

where H is the Hardy-Sobolev constant. Then there exists a sufficiently large δ such that δ max 4 p p + 2 , 4 p C 1 + H + 1 p 2 , combining Hölder’s inequality, we have

d d t K ( t ) δ 2 E ( t ) 2 p δ u t 2 2 + u 2 2 δ 2 E ( t ) 2 p δ K ( t ) δ 2 E ( t ) .

Integrating from 0 to t , we obtain

K ( t ) e 2 p t δ Ω u 0 u 1 d x δ 2 E ( 0 ) + δ 2 E ( t ) , t 0 .

So the claim about (5.4) is proved.

Now, we consider the following two cases:

Case 1: For all t 0 , we first assume that E ( t ) 0 . Making use of (5.1) and (5.4), we can obtain

Ω u u t d x e 2 p t δ Ω u 0 u 1 d x ε 2 E ( 0 ) + δ 2 E ( t ) e 2 p t δ Ω u 0 u 1 d x ε 2 E ( 0 ) 0 ,

which implies that the term u 2 2 is nondecreasing with respect to the time variable, and using (5.3), we have

L ( t ) L ( t ) p + 2 4 ( L ( t ) ) 2 L ( t ) 2 p E ( 0 ) + ( p 2 ) C 1 u 2 2 p η L ( t ) 2 p E ( 0 ) + ( p 2 ) C 1 u 0 2 2 p η .

(5.2) means that we can choose such η satisfying η = ( p 2 ) C 1 p u 0 2 2 2 E ( 0 ) , such that

L ( t ) L ( t ) p + 2 4 ( L ( t ) ) 2 0 .

We can choose σ such that L ( 0 ) > 0 . Therefore, our result can be derived by the same processes as the proof of Theorem 4.2, and the conclusion follows from Lemma 4.1.

Case 2: There exists t 4 > 0 such that E ( t 4 ) < 0 , and it follows from E ( 0 ) > 0 and the continuity of E ( t ) that there exists a t 4 ( 0 , t 4 ) such that E ( t 4 ) = 0 and

E ( t ) 0 , 0 < t t 4 ,

and this proof is also similar to the argument of the Case 1. We omit it here.

Therefore, T max < + and u blows up in finite time.□

6 Lower bound for blow-up time

In this section, we shall derive a lower bound for the blow-up time by modified differential inequalities when blow-up occurs.

Theorem 6.1

Assume that ( ( u 0 ( x ) , u 1 ( x ) ) ) , let

(6.1) M ( t ) u t 2 2 + u 2 2 + u x s 2 2 2 .

u ( t ) be a weak solution to problems (1.1)–(1.3) that blows up at T in the sense of M ( t ) measure. Then

T M 2 p ( 0 ) C T ( p 2 ) ,

where

M ( 0 ) = u 1 2 2 + u 0 2 2 + u 0 x s 2 2 2 ,

and C T a is positive constant that will be determined in (6.4).

Proof

Differentiating M ( t ) and making use of (1.1), we have

(6.2) M ( t ) = 2 ( u t , u t t ) + 2 ( u , u t ) + 2 Ω 1 x s u t u d x = 2 Ω u t u t t Δ u + 1 x s u d x = 2 u t 2 2 + 2 k ( t ) Ω u t u p 2 u d x .

We follow a similar way in (3.5) and (3.6) to estimate the second term in the right-hand side to obtain

(6.3) k ( t ) Ω u t u p 2 u d x k ( T ) Ω u t u p 1 d x k ( T ) B 2 ( p 1 ) 1 4 ε u 2 2 ( p 1 ) + k ( T ) B 2 ε 2 u t 2 2 ,

where T is any finite upper bound for T .

Substituting the aforementioned differential inequality into (6.2) and for sufficiently small parameter ε such that k ( T ) B 2 ε 2 2 , one obtains

(6.4) M ( t ) 2 k ( t ) Ω u t u p 2 u d x k ( T ) B 2 ( p 1 ) 1 4 ε u 2 2 ( p 1 ) k ( T ) B 2 ( p 1 ) 1 4 ε M ( t ) p 1 C T M ( t ) p 1 .

Letting t T in the aforementioned inequality and recalling that lim t T M ( t ) = + , integrating (6.4) over [ 0 , T ] , we have

T M 2 p ( 0 ) C T ( p 2 ) ,

The proof is complete.□

Acknowledgments

The authors would like to deeply thank all the reviewers for their insightful and constructive comments.

  1. Funding information: The work is supported by the Natural Science Foundation of Shandong Province of China (No. ZR2019MA072).

  2. Conflict of interest: The authors declare that there is no conflict of interests regarding the publication of this article.

  3. Data availability statement: Data sharing is not applicable to this article as no data sets were generated or analyzed during the current study.

References

[1] C. O. Alves, G. Ercole, M. Daniel, and H. Bolaños, Ground state solutions for a semilinear elliptic problem with critical-subcritical growth, Adv. Nonlinear Anal. 9 (2020), 108–123. 10.1515/anona-2017-0170Suche in Google Scholar

[2] M. Badiale and G. Tarantello. A Sobolev-Hardy inequality with applications to a nonlinear elliptic equation arising in astrophysics, Arch. Ration. Mech. Anal. 163 (2002), 259–293. 10.1007/s002050200201Suche in Google Scholar

[3] H. F. Di, Y. D. Shang, and Z. F. Song, Initial boundary value problem for a class of strongly damped semilinear wave equations with logarithmic nonlinearity, Nonlinear Anal. Real World Appl. 51 (2020), 22, https://doi.org/10.1016/j.nonrwa.2019.102968. Suche in Google Scholar

[4] Z. B. Fang and Y. X. Wang, Blow-up analysis for a semilinear parabolic equation with time-dependent coefficients under nonlinear boundary flux, Z. Angew. Math. Phys. 66 (2015), 2525–2541. 10.1007/s00033-015-0537-7Suche in Google Scholar

[5] F. Gazzola and M. Squassina, Global solutions and finite time blow up for damped semilinear wave equations, Ann. Inst. H. Poincaré Anal. Non Linéaire. 23 (2006), no. 2, 185–207. 10.1016/j.anihpc.2005.02.007Suche in Google Scholar

[6] Y. Z. Han, Blow-up phenomena for a reaction diffusion equation with special diffusion process, Appl. Anal. 101 (2022), no. 6, 1971–1983. https://doi.org/10.1080/00036811.2020.1792447. Suche in Google Scholar

[7] R. Ikehata and Y. Inoue, Global existence of weak solutions for two-dimensional semilinear wave equations with strong damping in an exterior domain, Nonlinear Anal. 68 (2008), no. 1, 154–169. 10.1016/j.na.2006.10.038Suche in Google Scholar

[8] M. Ikeda and M. Sobajima, Sharp upper bound for lifespan of solutions to some critical semilinear parabolic, dispersive and hyperbolic equations via a test function method, Nonlinear Anal. 182 (2019), 57–74. 10.1016/j.na.2018.12.009Suche in Google Scholar

[9] R. Ikehata and H. Takeda, Uniform energy decay for wave equations with unbounded damping coefficients, Funkcial. Ekvac. 63 (2020), no. 1, 133–152. 10.1619/fesi.63.133Suche in Google Scholar

[10] N. A. Lai and Z. H. Tu, Strauss exponent for semilinear wave equations with scattering space dependent damping, J. Math. Anal. Appl. 489 (2020), no. 2, 24, https://doi.org/10.1016/j.jmaa.2020.124189. Suche in Google Scholar

[11] H. A. Levine, Instability and nonexistence of global solutions to nonlinear wave equations of the form Putt=−Au+F(u), Trans. Amer. Math. Soc. 192 (1974), 1–21. 10.1090/S0002-9947-1974-0344697-2Suche in Google Scholar

[12] W. Lian, J. Wang, and R. Z. Xu, Global existence and blow up of solutions for pseudo-parabolic equation with singular potential, J. Differ. Equ. 269 (2020), no. 6, 4914–4959. 10.1016/j.jde.2020.03.047Suche in Google Scholar

[13] W. Lian and R. Z. Xu, Global well-posedness of nonlinear wave equation with weak and strong damping terms and logarithmic source term, Adv. Nonlinear Anal. 9 (2020), 613–632. 10.1515/anona-2020-0016Suche in Google Scholar

[14] L. W. Ma and Z. B. Fang, Energy decay estimates and infinite blow-up phenomena for a strongly damped semilinear wave equation with logarithmic nonlinear source, Math. Methods Appl. Sci. 41 (2018), no. 7, 2639–2653. 10.1002/mma.4766Suche in Google Scholar

[15] M. Ohta, Remarks on blow up of solutions for nonlinear evolution equations of second order, Adv. Math. Sci. Appl. 8 (1998), no. 2, 901–910. Suche in Google Scholar

[16] K. Ono, On global existence, asymptotic stability and blowing up of solutions for some degenerate non-linear wave equations of Kirchhoff type with a strong dissipation, Math. Methods Appl. Sci. 20 (1997), no. 2, 151–177. 10.1002/(SICI)1099-1476(19970125)20:2<151::AID-MMA851>3.0.CO;2-0Suche in Google Scholar

[17] V. Pata and S. Zelik, Smooth attractors for strongly damped wave equations, Nonlinearity. 19 (2006), no. 7, 1495–1506. 10.1088/0951-7715/19/7/001Suche in Google Scholar

[18] L. E. Payne and G. A. Philippin, Blow-up phenomena in parabolic problems with time dependent coefficients under Neumann Boundary conditions, Proc. R. Soc. Edinb. A. 142 (2012), no. 3, 625–631. 10.1017/S0308210511000485Suche in Google Scholar

[19] M. Sobajima and Y. Wakasugi, Weighted energy estimates for wave equation with space-dependent damping term for slowly decaying initial data, Commun. Contemp. Math. 21 (2019), no. 5, 30, https://doi.org/10.1142/S0219199718500359. Suche in Google Scholar

[20] F. L. Sun, L. S. Liu, and Y. H. Wu, Finite time blow-up for a class of parabolic or pseudo-parabolic equations, Comput. Math. Appl. 75 (2018), 3685–3701. 10.1016/j.camwa.2018.02.025Suche in Google Scholar

[21] Z. Tan, Reaction-diffusion equations with special diffusion processes, Chinese J. Contemp. Math. 22 (2001), no. 4, 371–382. Suche in Google Scholar

[22] Y. Wakasugl, On diffusion phenomena for the linear wave equation with space-dependent damping, J. Hyperbolic Differ. Equ. 11 (2014), no. 4, 795–819. 10.1142/S0219891614500246Suche in Google Scholar

[23] T. Watanabe, Global existence and decay estimates for nonlinear wave equations with space-time dependent dissipative term, J. Hyperbolic Differ. Equ. 12 (2015), no. 2, 249–276. 10.1142/S0219891615500071Suche in Google Scholar

[24] G. F. Webb, Existence and asymptotic behavior for a strongly damped nonlinear wave equation, Canad. J. Math. 32 (1980), no. 3, 631–643. 10.4153/CJM-1980-049-5Suche in Google Scholar

[25] J. Zhou and A. J. Hao, A new blow-up condition for a parabolic equation with singular potential, J. Math. Anal. Appl. 449 (2017), no. 1, 897–906. 10.1016/j.jmaa.2016.12.040Suche in Google Scholar

Received: 2021-12-11
Revised: 2022-07-09
Accepted: 2022-07-16
Published Online: 2022-11-18

© 2023 Yi Yang and Zhong Bo Fang, published by De Gruyter

This work is licensed under the Creative Commons Attribution 4.0 International License.

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