This paper considers nonlinear Kirchhoff equation with Kelvin–Voigt damping. This model is used to describe the transversal motion of a stretched string. The existence of smooth stationary solutions of nonlinear Kirchhoff equation has been studied widely. In the present contribution, we prove that a class of stationary solutions is asymptotic stable by overcoming the “loss of derivative” phenomenon causing from the Kirchhoff operator. The key point is to find a suitable weighted function when we carry out the energy estimate for the linearized equation.
G. Kirchhoff [19] proposed a model equation (integro-differential equation) to describe the transversal motion of the elastic string, which now is called Kirchhoff equation
which is a Hamiltonian structure, that is, we define the energy
then it holds
as long as the solution exists.
In this paper, we consider the nonlinear Kirchhoff equation with Kelvin–Voigt damping. Kelvin–Voigt damping originates from the internal friction of the material of the vibrating structures and in thus called “internal damping”. It is one of the most important physical dampings. The damped equation takes the form:
with the initial data
where the dimension , the unknown function , this term is a constructive viscoelastic damping, it models the vibrations of an elastic body which has one part made of viscoelastic material. and are two non-negative parameters. When , equation (1.1) is reduced into the Kelvin–Voigt damped Kirchhoff equation
In 1940, Bernstein [8] proved the existence of global in time analytic solutions for Kirchhoff equation on an interval of real line. Pohozaev [25] extended Bernstein’s result to more general Hilbert spaces. The global existence for real analytic data has been shown by D’Ancona–Spagnolo [10]. Ghisi–Gobbino [14] showed some counterexamples in order to prove that the regularity required in the existence results is sharp. After that, they [15] obtained a uniqueness result for a general Kirchhoff equation with non-Lipschitz nonlinear term. D’Ancona–Spagnolo [11] considered the following nonlinear Kirchhoff equation
with small smooth initial data and smooth function
then they showed that above nonlinear equations admitted a unique solution for the dimension . Autuori–Pucci–Salvatori [7] studied a more general nonlinear equation
where the -Dirichlet energy integral is denoted by , and denotes the vectorial -Laplacian operator. By some assumption on nonlinear term, they showed above nonlinear equation admited the global non-existence of solution. After that, they gave the lifespan estimate of solution in [4]. We refer the reader’s to [3,5,6,13,22,26,35] for more interesting results on this equation.
Clearly, the existence of ground state (or stationary solutions) for the nonlinear Kirchhoff equation (1.1) and (1.2) is related to the non-local elliptic problem
and
respectively, the existence of solution for stationary equations (1.3)–(1.4) depend on the nonlinear term strongly. It has been studied widely by using variational method, we refer the readers to [9,12,13,16,21] for more details. By Giorgi–Moser iteration, one can obtain the existence of smooth solution for above problem. Thus a nature question is
Is the smooth stationary solution stable in functional space?
In the present paper, we will answer this question. Meanwhile, our result gives the global well-posedness for the nonlinear Kirchhoff equations with Kelvin–Voigt damping (1.1) and (1.2). Since we deal with the dissipative case, we can consider the general initial data of the dissipative equation. Assume that the stationary equation (1.3) admits a smooth solution , and satisfies the following conditions:
for a positive small constant ε.
Then we have the following result.
Let constantswith. The smooth stationary solution of nonlinear Kirchhoff equations with Kelvin–Voigt damping (
1.1
) is asymptotic stable in the Sobolev spacefor any integer, that is, for a sufficient small, if the initial datathen the nonlinear Kirchhoff equation (
1.1
) admits a global solutionsuch that
Sketch of the proof. Assume that is a stationary solution of equation (1.1), i.e. it satisfies the stationary Kirchhoff equation
Let
then substituting it into the equation (1.1) to get the following perturbation equation
with the initial data
where the symbol
From the structure of nonlinear equation (1.6), the loss of derivative phenomenon should appear, thus we have to smooth the linearized equation by using the smooth operator (see [2] for more details about this operator), and then a suitable Nash–Morse iteration scheme will be constructed to show a unique approximation solution. This method has been used in [28–34]. We refer the reader to [17,18,23,24] for more details on the classical iteration scheme.
We introduce the iteration scheme. Suppose that we have chosen a smooth initial function . Since it is not a solution of nonlinear equation (1.6), there must be an error term, we denoted it by
Meanwhile, the choice of should make the error term small enough in Sobolev space, i.e.
The first approximation solution takes the following form
where is the solution of linear damped non-local wave equation
where the linearized operator
According to this idea, we get the m-th approximation step by solving the linear equation
where the error term . So the m-th approximation solution has the following form
thus we need to prove
and the error term
where is the solution of (1.6).
Notation. In this paper, we use to represent that there exists a positive constant C such that , and means that a and b are equivalent. The notation is the space of , and u is infinitely differentiable with a compact support. Furthermore, we denote the usual norm of Sobolev space by for convenience.
The paper is organize as follows. In Section 2, we prove the global well-posedness of linear damped wave equation with variable coefficients. In Section 3, we construct an approximate solution of nonlinear approximation perturbation problem. The last section is devoted to show the convergence of approximation scheme.
Well-posedness of the linearized problem
Assume the fixed function . Inspired by (1.6), we now consider the following linear damped non-local wave equation with variable coefficients
with the initial data
Assume that coefficients of (2.1) satisfy the following conditions:
for a positive small constant ε.
We choose two positive, bounded smooth functions and in , and satisfying
with two positive constants and , .
Furthermore, there exists a positive constant C depend on , and σ such that
And it also need to suppose
and
We have the following weighted -estimate of solution for the linear damped wave equation with variable coefficients (2.1).
Let constantswith. Assume that (
2.3
) hold. Then the solution of equation (
2.1
) satisfies
On one hand, we multiply equation (2.1) with , then integrating it over on x, it holds
For some terms, integration by part give that
and
Combining (2.13)–(2.16), we reduce (2.12) into
In addition, we use Cauchy’s inequality and Hölder’s inequality to obtain
and
and
Based on the above inequality, we can deduce (2.17) into
On the other hand, we multiply equation (2.1) with , then integrating it over on x, it holds
Therefore summing up (2.18) with (2.26), it holds
where
Let us now deal with coefficients of inequality (2.27). Using the assumptions given in (2.3) and (2.5)–(2.6), there exists a positive constant C depending on , , σ, and ε such that
Similarly, by (2.3)–(2.9), we can get
and
Based on above estimation, we deduce (2.27) into
Applying Gronwall’s inequality to (2.32) we can get
In particularly, we can take weighted functions
with a positive constant C, then assumptions (2.4)–(2.8) hold. Then (2.11) can be obtained from (2.33). □
In what follows, we derive -estimates for any and . Applying to both side of (2.1), it holds
where
with the symbol
Then we have the following priori estimation:
Let constantswith. Assume that (
2.3
) hold. Then the solution of equation (
2.1
) satisfies
This proof is based on the induction. When , we rewrite the liner equation as
where
We can see that the linear equation (2.37) has the same structure with equation (2.1), so we can multiply both sides of equation (2.37) with and , respectively, using the same method of getting (2.27), we deduce
where
We next estimate the right hand side term of (2.38). We first use Hölder’s inequality and Cauchy’s inequality to get the following inequalities
and
Based on above estimation, summing up (2.38) from to , it holds
where
and
We now analyze the coefficients of inequality (2.39). By (2.3)–(2.8), it holds
and
According to above estimation and (2.28)–(2.30) and (2.31), (2.39) can be reduced into
We notice that the term can be controlled by (2.32), thus by Gronwall’s inequality, it derives
Let . Assume it holds
When , we multiply both sides of (2.35) with and , respectively, using the same process with (2.40), we derive
with
where C is a positive constant depending on , and σ.
Since the term can be controlled by (2.41), we can use Gronwall’s inequality to derive
then according to the special weight function chosen in (2.34), we can get (2.36). □
Based on above results, we are ready to prove the global existence of solution for the linear damped non-local wave equation with variable coefficients (2.1).
Let constantswith. Assume that (
2.3
) hold. The linear problem (
2.1
) with the initial date (
2.2
) admits a unique global solutionMoreover, it satisfies
The proof follows theorem 3.2 given in page 18 of [27] by applying the standard fixed point iteration. We only state the outline here. We set and define and as follows
with
and
The linear equation (2.1) can be written as
with the initial data
We now consider the approximation problem
In fact, it has a Cauchy sequence in that converges to , and it is the solution of linearized system (2.43) in . Furthermore, according to Lemma 2.1–2.2, it holds
thus the constructed local solution can be extended to the global solution in time.
Suppose that and are two solutions of system (2.43) with the same initial data, then admits zero Cauchy data, and
through (2.42) we can launch , so the solution of system (2.43) is unique. This completes the proof. □
Construction of approximation solutions
In this section, we will construction an approximation solution of nonlinear approximation problem. We first introduce a family of smooth operators (see the [1,2]). Let such that in , otherwise, . Following Proposition 1.6 of [2, p.83] or page 72 of [20], we define by
and by
We define
according to the proof given in [1, p.192] or [2], it holds
where .
In our iteration scheme, we assume that
where is a fixed positive constant, we denote it by for convenience, then by (3.1), it holds
The first iteration step
We suppose that the initial approximation function satisfies the following conditions
Then we get the nonhomogeneous linear damped wave equation (3.8) with variable coefficients by linearizing nonlinear equation (1.6) at :
where
We now consider the linear damped non-local wave equation with variable coefficient derive external force as follows
with the initial data
where the external force is related to the error term at the initial approximation function.
Furthermore, It can be inferred that there is a global solution of linear equation (3.9) by means of assumptions (3.5)–(3.7) and proposition 2.1.
Let constantswith. The linear problem (
3.9
) with the initial data (
3.10
) admits a unique global solutionMoreover, it satisfies
The general iteration step
Let , we define
with the integer .
We denote the m-th approximate step of the nonlinear equation (1.6) with , where we set
it holds
We consider the following initial value problem (3.12) by the linearization of nonlinear equation (1.6) around :
where the error term is
and
which is also the nonlinear term in the approximation problem (1.6) at .
By the same process of getting proposition 3.1, we can construct the m-th approximation solution.
Let constantswith. The linearized problem (
3.12
) admits a unique global solutionwhich satisfies
On one hand, we find the m-th approximation solution , which is equivalent to find such that
substituting (3.16) into (1.6), it holds
then we set
which is a linear damping non-local wave equation as in the form of (3.8) by replacing with , and the error term
On the other hand, we denote the s-th derivatives of time or spacial variables in , and apply to both side of (3.16) to get
for a sufficient small positive parameter ε, it holds
thus we can see that
it imply that the initial approximation function is the leading term of the m-th approximation solution. We notice that the linear equation (3.9) and the linear equation of m-th approximation solutions have the same structure. By means of the same argument as in the proof of Proposition 3.1, we can verify that the linear problem (3.12) exists a unique global solution
Meanwhile, (3.15) can be obtained. The proof is completed. □
The nonlinear problem
In this section, the target is to show that is indeed a unique global solution of the nonlinear equations (1.6). This is equivalent to prove that the series is convergent.
We now give the tame estimation of error term in each iteration scheme.
Let. The error term verifies
The error term is
and the highest order for the derivative of x is 4. Since the solution of (3.12) should be constructed in , it holds
Thus we can estimate each term of by applying Cauchy‘s inequality and (4.2)
□
We now prove that the iteration scheme is convergent. For any , let and
which gives that
The nonlinear problem (
1.6
) with the initial data (
1.7
) admits a unique global Sobolev regularity solution
The proof is based on the induction. For convenience, we first consider the case with . After that, we discuss the case and . Note that with . For all , we claim that there is a positive constant ε small enough to hold
For the case of , by (3.15), and by setting , it holds
Moreover, according to (4.1) and the above estimation, we derive
and
which imply that .
Assume that the case of holds
Then we prove that the case of m holds. Combining with (3.15) and the second inequality of (4.5), we derive
which combining with (4.1)–(4.3) gives
We choose a sufficiently small positive constant ε such that
thus by (4.7), we have
and it holds
On the other hand, note that , by (4.5)–(4.6), it holds
This means that . Hence we conclude that (4.4) holds.
Therefore, the nonlinear equation (1.6) with the zero initial data exists a unique global Sobolev solution
and we use (3.6) to get
We now discuss the case of small non-zero initial data. Introduce the auxiliary function
the initial data can be reduced into
and nonlinear equation (1.6) is transformed into equations of .
Thus we can construct a unique global Sobolev solution by above iteration scheme. Furthermore, the global Sobolev solution of nonlinear equation (1.6) with a small non-zero initial data takes the form
and this solution is unique due to the uniqueness of each iteration step . This completes the proof. □
Footnotes
Acknowledgement
The third author is supported by Guangxi Natural Science Foundation No 2021JJG110002 and NSFC No 12161006.
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