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Blow-up in damped abstract nonlinear equations

  • As a typical example of our analysis we consider a generalized Boussinesq equation, linearly damped and with a nonlinear source term. For any positive value of the initial energy, in particular for high energies, we give sufficient conditions on the initial data to conclude nonexistence of global solutions. We do our analysis in an abstract framework. We compare our results with those in the literature and we give more examples to illustrate the applicability of the abstract formulation.

    Citation: Jorge A. Esquivel-Avila. Blow-up in damped abstract nonlinear equations[J]. Electronic Research Archive, 2020, 28(1): 347-367. doi: 10.3934/era.2020020

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  • As a typical example of our analysis we consider a generalized Boussinesq equation, linearly damped and with a nonlinear source term. For any positive value of the initial energy, in particular for high energies, we give sufficient conditions on the initial data to conclude nonexistence of global solutions. We do our analysis in an abstract framework. We compare our results with those in the literature and we give more examples to illustrate the applicability of the abstract formulation.



    We first consider the following generalized Boussinesq equation with linear damping and a nonlinear source term

    (GB){uttα1Δuα2Δutt+α3Δ2u+m2u+δutδα2Δut+Δf(u)=0,u(0,x)=u0(x),ut(0,x)=u1(x),

    on R+×RN, R+[0,), where m2>0,δ0,αi>0,i=1,2,3, and f is a nonlinear function of the unknown u.

    In [2], Boussinesq obtained an approximate equation from the Euler equation to describe bidirectional solitary waves propagating on the free surface of a constant depth in irrotational motion. This a particular case without dissipation of the one-dimensional version of (GB) and it is called the classical Boussinesq equation, Since then, several modifications have been proposed. See [23,3] for historical remarks and the physical foundations of several generalizations of the original Boussinesq equation to model nonlinear wave propagation in elasticity and fluid mechanics.

    For an evolution equation, like the Cauchy problem (GB), we have the following questions. With respect to a functional framework and in terms on the initial data, study:

    ● Local existence and uniqueness of solutions.

    ● Non-global existence: maximal time of existence TMAX<.

    ● Global existence: TMAX=.

    ● In the latter case, the behavior of the solution as time approaches infinity.

    Here, we shall study the second point. In fact, we will give conditions on the initial data, u0,u1, for which the corresponding solution, in some sense given later, exists only up to a finite time. In order to do that, we are going to consider an abstract formulation of problem (GB), so that can be applied to other equations.

    We consider the following abstract differential equation.

    For every initial data u0,u1, find tu(t),t0, such that

    (P){Putt+Au+δPut=f(u),u(0)=u0,ut(0)=u1.

    Here, utddtu, and we assume that the operators

    P:WPWP,A:VAVA,

    are linear, continuous, positive and symmetric, and

    VAWPH

    are linear subspaces of the Hilbert space H with inner product (,) and norm . Here, H,WP,VA, are the corresponding dual spaces and we identify H=H. Then,

    HWPVA.

    By means of the operators P and A, we define the following bilinear forms

    P(u,w)(Pu,w)WP×WP,u,wWP,A(u,w)(Au,w)VA×VA,u,wVA,

    and corresponding norms

    u2WPP(u,u),uWP,u2VAA(u,u),uVA.

    The following problem (GB) has the abstract form (P). Indeed, we remember that (Δ)su=F1(|ω|2s(Fu)(ω)), for s>0, where F,F1 are the Fourier transform and the inverse Fourier transform, respectively. Applying (Δ)1, to (GB), we get

    (GB){((Δ)1+α2Id)utt+(α3Δ+m2(Δ)1+α1Id)u+δ((Δ)1+α2Id)ut=f(u),u(0,x)=u0(x),ut(0,x)=u1(x),

    on R+×RN.

    Then, as usual u(t)u(t,), and we define H=L2(RN), with inner product (,)2 and norm 2. Also,

    Put=((Δ)1+α2Id)ut,Au=(α3Δ+m2(Δ)1+α1Id)u,

    are defined, respectively, on the subspaces of H

    WP={uL2(RN):(Δ)12uL2(RN)},VA={uH1(RN):(Δ)12uL2(RN)}.

    Moreover, if

    u2=(u,u)((Δ)12u,(Δ)12u)2,

    then

    u2WP=u2+α2u22,u2VA=α3u22+m2u2+α1u22.

    The analysis of problem (P) is in the framework of weak solutions in the sense of the following Definition 2.1. To this end, we consider the phase space

    HVA×WP,

    with norm

    (u,v)2Hv2WP+u2VA,

    and we assume that the following hypotheses hold.

    There exists c>0, such that

    (H0)u2VAcu2WP,uVA.

    The nonlinear source term f:VAH, is such that f(0)=0, and it is a potential operator with potential F:VAR, that is, f(u)=DuF(u). Moreover, they satisfy

    (H1)(f(u),u)rF(u)0,uVA,

    and some constant r>2+δ/c.

    Definition 2.1. For every initial data (u0,u1)H, the map (u0,u1))(u(t),˙u(t))H, where ˙u(t)ddtu(t), is a weak local solution of problem (P), if there exists some T>0, such that (u,˙u)C([0,T);H), with u(0)=u0,˙u(0)=u1, and

    ddtP(˙u(t),w)+A(u(t),w)+δP(˙u(t),w)=(f(u(t)),w),

    a. e. in (0,T) and for every wVA. We shall consider that the solution in this sense is unique and satisfies the following energy equation for T>tt00,

    E(u(t0),˙u(t0))=E(u(t),˙u(t))+δtt0˙u(τ)2WPdτ,E(t)E(u(t),˙u(t))12˙u(t)2WP+J(u(t)),J(u(t))12u(t)2VAF(u(t))E(t)=12(u(t),˙u(t))2HF(u(t)).

    Furthermore, if the maximal time of existence TMAX< then

    limtTMAX(u(t),˙u(t))H=,

    equivalently, by the energy equation,

    limtTMAXF(u(t))=.

    For the Boussinesq equation, hypothesis (H0) holds with c=min{m2,α1α2}. We assume that the source terms f and the corresponding potential operator F do not have any particular form but they satisfy (H1). The existence and uniqueness of weak solutions of (GB), in the sense of Definition 2.1 holds, see [29,25,33].

    An important set of solutions are the equilibria, that is solutions independent of time, that is, ˙u=0. In this case, u satisfies

    A(u,w)=(f(u),w),

    for every wVA. In particular, for w=u,

    u2VA=(f(u),u),

    and then

    I(u)u2VA(f(u),u)=0.

    By (H0), (u,0)(0,0) is an equilibrium. The set of nonzero equilibria, denoted by E, with minimal energy is called ground state, and the corresponding value of the energy is the mountain pass level denoted by d, see [32]. Indeed,

    dinfuNJ(u)=12infuN((f(u),u)2F(u)), (1)

    where

    N{u0:I(u)=0},

    is the Nehari manifold. By means of this number, the potential well method has been used to characterize the qualitative behavior for solutions of some equations of the type (P). For dissipative equations, δ>0, the behavior is completely different from the conservative case δ=0. Indeed, consider the initial and homogeneous Dirichlet boundary value problem of the nonlinear wave equation, which is a particular case of problem (P).

    (NLW){uttαΔu+g(ut)=f(u),xΩu(0,x)=u0(x),ut(0,x)=u1(x),xΩu(x,t)=0,xΩ

    where ΩRN is a bounded domain with smooth boundary Ω, tR+, and α>0,g(ut)=δut,δ>0,f(u)=μ|u|r2u,r>2. Here,

    P=Id,H=WP=L2(Ω),Au=αΔu,VA=H10(Ω).

    Hypothesis (H0) holds because of the Sobolev-Poincaré inequality,

    αu22cu22,

    and (H1) holds if r>2+δ/c, with rF(u)=μurr, where r is the norm in Lr(Ω). The following result about the dynamics of (NLW) holds.

    Theorem 2.2. ([7,14]). For every solution (u,˙u) of (NLW), in the sense of Definition 2.1, with initial data (u0,u1)H=VA×WPH10(Ω)×L2(Ω), only one of the following holds.

    ● There exists some t00 such that E(t0)<d, then either

    u(t0)V{u:I(u)<0,J(u)<d}

    and the solution blows up in a finite time or

    u(t0)W{u:I(u)>0oru=0,J(u)<d}

    and the solution is global, uniformly bounded in time in the norm of H, and

    limt(u(t),˙u(t))H=0,

    exponentially in time.

    E(t)d, for all t0, then the solution is global, uniformly bounded in time in the norm of H, and

    (u(t),˙u(t))East,

    strongly in H, where

    E{(u,0)E:J(u)=limtE(t)}.

    We notice that the only way to get blow up of in finite time is that, along the solution and since the energy is a non-increasing function, there exists some t00 such that E(t0)<d and u(t0)V. If the damping term is nonlinear of the form g(ut)δ|ut|λut,λ>2, although the dynamics is more complicated, a similar result holds, see [8]. Indeed, the solution blows up in a a finite time if and only if r>λ and there exists some t00 such that E(t0)<d and u(t0)V. An open problem is to characterize the set of initial data such that E(t0)<d and u(t0)V, for some t0>0, especially when E0E(0)d and u0V. Another open problem is to find conditions on the initial data in order to get E(t)d, for all t0. Then, according with Theorem 2.2 those solutions are global and they approach to the set of nonzero equilibria. See also [9], where Theorem 2.2 is proved for the Timoshenko equation. In the conservative case, δ=0, we know the following result for E0d.

    Theorem 2.3 ([24,10]). Consider any solution (u,˙u) of (NLW), in the sense of Definition 2.1, with initial data (u0,u1)H=VA×WPH10(Ω)×L2(Ω) and δ=0.

    If E0<d, then

    ● the solution blows up in a finite time if and only if u0V.

    ● the solution is global if and only if u0W, and in this case the solution is uniformly bounded in time in the norm of H.

    If E0=d, and

    ● there exists some t00 such that I(u(t0))>0, then the solution is global and uniformly bounded in time in the norm of H.

    ● there exists some t00 such that I(u(t0))<0 and (u(t0),v(t0))20, then the solution blows up in finite time.

    The asymptotic behavior of the global solutions with E0d is unknown, as well as the characterization of the qualitative behavior for E0>d in terms of the initial data. We have to mention two remarkable papers, [18,27] where the blow up of solutions for the Cauchy problem associated to (NLW) is studied, that is with Ω=RN. In those works a nonlinear damping term of the form g(ut)δ|ut|λut is considered and it is proved that for any (η,ξ)(0,)×[0,), there are infinitely many compactly supported initial data (u0,u1) such that if u02=η and E0=ξ, the corresponding solution blows up in finite time. We notice that this result is not true for the initial boundary value problem (NLW) with that nonlinearity g(ut). Indeed, for ξ<d and η2<2rdα(r2) the solution is globally defined, see [8], because u0W if and only if αu022<2rr2d. However, the result in [18,27] exhibits a complex dynamics because it is known that there are global solutions for the Cauchy problem associated to (NLW) with initial data such that η and ξ are small, see [27] and references therein.

    For the (GB) problem, characterizations of blow-up and global solutions with E0<d by means of the potential well method were proved in [21,22,16] and in [34], for the one-dimensional and the multidimensional problems, respectively. For E0d, there are only partial results on the dynamics of particular equations of the type (GB). Most of them are results for blow up of solutions, see [29,25,16]. Similar analysis, for E0d, have been performed to prove the same qualitative properties for other equations, see [14,28] to cite just some of the most influential papers on the subject, and see [4,19,20,26,30,31,35,36,37] and references therein for some recent works. In [6] a numerical study for the Cauchy problem of the focusing cubic nonlinear Klein-Gordon equation in three dimensions for radial initial data shows that for high energies, the qualitative behavior seems to be much more complicated than for E<d, and more research is required to find a threshold between globality and blow up of solutions. In [17] some numerical experiments were performed for the one-dimensional case of (GB), with δ=0, to calculate the mountain pass level and confirm the range of validity of the potential well method. In particular, for E0>d, it was observed that the sign of I(u0) is irrelevant to get the blow up of solutions in finite time, but instead, the sign of the inner product P(u0,u1) is important to obtain nonexistence of global solution. In [11,12] we have proved that this is true for the undamped nonlinear Klein-Gordon equation and for the problem (P) with δ=0. Here, we are going to prove that, for any δ>0 and any positive E0, the sign of P(u0,u1) is the main ingredient to prove the nonexistence of global solutions for problem (P) and in particular for (GB). However, we shall consider δ0, in order to see the influence of the damping in the qualitative behavior.

    We define

    Ψ(u)u2WP,Φ(u,˙u)(rδ/cr)(|P(u,˙u)|2Ψ(u)+cΨ(u)),

    where c>0 is the constant in (H0), δ0 is the damping coefficient, we have assumed that r>2+δ/c, see (H1), and from the orthogonal decomposition

    ˙u=P(˙u,u)u2WPu+h,P(u,h)=0,

    we have that

    ˙u2WP=h2WP+|P(˙u,u)|2u2WP|P(˙u,u)|2u2WP=|P(˙u,u)|2Ψ(u).

    We also define the following functions

    ηq,δ(u,˙u)12Φ(u,˙u)crΨ(u)((rδ/cr)cΨ(u)Φ(u,˙u))q,q0,μλ,δ(u,˙u)12Φ(u,˙u)crΨ(u)((rδ/cr)λcΨ(u)Φ(u,˙u))r2δ/c2,λ(0,1),σν(u,˙u)12Φ(u,˙u)cνrΨ(u),ν>1.

    If P(u,˙u)>0 and for fixed δ, we notice that qηq,δ is strictly increasing, λμλ,δ is strictly decreasing and νσν is strictly decreasing. They have the following relations

    limλ1μλ,δ(u,˙u)=ηq,δ(u,˙u)|q=r2δ/c2,limν1σν(u,˙u)=ηq,δ(u,˙u)|q=0,

    and, σν(u,˙u)<ηq,δ(u,˙u)|q=0<ηq,δ(u,˙u)|q=r2δ/c2<μλ,δ(u,˙u).

    Now, we are able to present the main result of this work.

    Theorem 3.1. Consider any solution of problem (P) in the sense of Definition 2.1. Assume that hypotheses (H0) and (H1) hold, and that

    u02WP>0,P(u0,u1)>0, (2)

    are satisfied. Then, there exists a nonempty interval

    Iδ(αδ,βδ)(0,12Φ(u0,u1)),

    where, by means of the functions σν,δ(u0,u1) and μλ,δ(u0,u1), we can obtain the size of such interval

    αδ=σν,δ(u0,u1)=(r2δ/c2r)(cΨ(u0)ν(2r2δ/c)),βδ=μλ,δ(u0,u1)=(r2δ/crδ/c)(Φ(u0,u1)2λ),

    for some r2δ/crδ/c<λ<1 and ν>1, with the following consequences:

    (i) If the initial energy is such that E0Iδ, then the maximal time of existence of the solution is finite.

    (ii) For fixed Ψ(u0) and δ,

    P(u0,u1)|Iδ|=βδαδ,

    is strictly increasing, and we have the limit values

    limP(u0,u1)αδ=0=limP(u0,u1)|βδ12Φ(u0,u1)|,limP(u0,u1)ν=,limP(u0,u1)λ=r2δ/crδ/c.

    Corollary 1. Assume that hypotheses of Theorem 3.1 are met. For every number K>0, we can choose initial data with P(u0,u1) large enough, so that KIδ, and then the corresponding solution with E0=K exists only up to a finite time.

    Proof. (of Theorem 3.1.) We assume that Ψ(u(t))u2WP exists for any t0. If such a thing does not happen, then the solution cannot be global. We observe that

    ddtΨ(u(t))=2(P(u(t),˙u(t)),

    and then we get the following estimate

    2(P(u(t),˙u(t))cu2WP+1c˙u(t)2WPcu2WP+1c|P(˙u,u)|2u2WP.

    Hence,

    ddtΨ(u(t))cΨ(u(t))+14c(ddtΨ(u(t)))2Ψ(u(t)) (3)

    By energy equation and hypotheses (H0) and (H1), we get the following chain of estimates

    d2dt2Ψ(u(t))+δddtΨ(u(t))=2(˙u(t)2WPI(u(t)))=2(˙u(t)2WPI(u(t)))+2rE(t)2rE(t)=(r+2)˙u(t)2WP+(r2)u(t)2VA2rE(t)(r+2)|P(˙u,u)|2u2WP+c(r2)u(t)2WP2rE0=r+24((ddtΨ(u(t)))2Ψ(u(t)))+c(r2)Ψ(u(t))2rE0.

    Hence, by (3),

    d2dt2Ψ(u(t))(r+2δ/c4)(ddtΨ(u(t)))2Ψ(u(t)+(c(r2)δc)Ψ(u(t))2rE0. (4)

    We define

    F(t)Ψ(r2δ/c4)(u(t)).

    Consequently, from (4),

    d2dt2F(t)=(r2δ/c4)Ψ(r+2δ/c4)(u(t))×((r+2δ/c4)(ddtΨ(u(t)))2Ψ(u(t))d2dt2Ψ(u(t)))(r2δ/c4)Ψ(r+2δ/c4)(u(t)){(c(r2)δc)Ψ(u(t))+2rE0}.

    That is,

    d2dt2F(t)c(r2δ/c)24F(t)+E0r(r2δ/c)2F(t)(r+2δ/cr2δ/c). (5)

    Due to (2) and since r>2+δ/c, see (H1), we have that the following inequality is true

    ddtF(t)=(r2δ/c4)Ψ(r+2δ/c4)(u(t))ddtΨ(u(t))=(r2δ/c2)Ψ(r+2δ/c4)(u(t))P(u(t),˙u(t))<0,

    for any t0 sufficiently close to zero. That is,

    ddtF(t)=(r2δ/c4)F(r+2δ/cr+2δ/c)(u(t))ddtΨ(u(t))<0.

    Now, we multiply (5) by ddtF(t)<0. Then, after an easy integration, we get

    (ddtF(t))2(r2δ/c2)2×((2rrδ/c)E0F(2(rδ/c)r2δ/c)(t)cF2(t))+C0, (6)

    where

    C0(ddtF(0))2(r2δ/c2)2((2rrδ/c)E0F(2(rδ/c)r2δ/c)(0)cF2(0)).

    We shall prove that there exists a constant κ0>0 such that

    (ddtF(t))2κ20>0, (7)

    and then

    ddtF(t)κ0<0.

    Hence,

    0F(t)κ0t+F(0).

    Which is impossible for any t>F(0)κ0. Then, the solution only exits up to a finite time.

    Next, we prove that (7) holds. To this end, we consider the right hand side of (6) and define, for s0,

    G(s)(r2δ/c2)2((2rrδ/c)E0s(rδ/cr2δ/c)cs)+C0,

    and we notice that G attains an absolute minimum, that is

    G(s)G(s0),s0,

    with s0(c(r2)δc2rE0)(r2δ/c2)>0, since c(r2)δc>0, and

    G(s0)=(r2δ/c2)2((2rrδ/c)E0s(rδ/cr2δ/c)0cs0)+C0,=rE0(r2δ/crδ/c)(c(r2)δc2rE0)(rδ/c2)+C0,

    On the other hand,

    C0=(r2δ/c2)2Ψ(u0)(r+2δ/c2)(P(u0,u1))2(r2δ/c2)2Ψ(u0)(r2δ/c2)(2rE0rδ/cΨ(u0)1c).

    Notice that (7) is satisfied for κ20=G(s0), and G(s0)>0 holds if and only if

    c(c(r2)δc2rE0)(r2δ/c2)+E0Ψ(u0)(rδ/c2)<(rδ/c2r)(Ψ(u0)(r+2δ/c2)(P(u0,u1))2+cΨ(u0)(r2δ/c2)),

    which is equivalent to

    E0+((c(r2)δc2rE0)Ψ(u0))(r2δ/c2)crΨ(u0)<12Φ(u0,u1), (8)

    where, we remember that

    Φ(u0,u1)(rδ/cr)((P(u0,u1))2Ψ(u0)+cΨ(u0)).

    We consider the left hand side of (8) to define, for s0,

    J(s)s+((c(r2)δc2rs)Ψ(u0))(r2δ/c2)crΨ(u0).

    We observe that (8) is satisfied if and only if

    J(E0)<12Φ(u0,u1), (9)

    We notice that J(s) as, either s0 or s, and J attains an absolute minimum, that is

    J(s)J(s1)=c(rδ/c2r)Ψ(u0),s0,

    for s1(c(r2)δc2r)Ψ(u0). Moreover, by (2), there exist exactly two different roots of J(s)=12Φ(u0,u1), denoted by αδ and βδ, such that

    0<αδ<s1<βδ<12Φ(u0,u1),

    and

    c(rδ/c2r)Ψ(u0)<J(s)<12Φ(u0,u1),sIδ(αδ,βδ),ss1.

    And since J is strictly monotone for s<s1 and s>s1, it follows that, for fixed Ψ(u0), the interval Iδ grows as P(u0,u1) grows. Precisely,

    limP(u0,u1)|12Φ(u0,u1)βδ|=0=limP(u0,u1)αδ.

    Then, (8) holds if and only if the initial energy satisfies (9). That is, if and only if E0Iδ. This proves that the maximum time of existence must be finite if the initial energy is within this interval.

    We shall use the functions σν and μλ,δ to find the values of αδ and βδ, respectively. Remember that these are the roots of J(s)=12Φ(u0,u1). To find αδ, we consider the equation

    J(σν(u0,u1))=12Φ(u0,u1), (10)

    where

    σν(u0,u1)12Φ(u0,u1)cνrΨ(u0),

    is defined for ν>1. Notice that (10) holds if and only if

    1ν(2r2δ/c)=2rc(r2)δc(σν(u0,u1)Ψ(u0)).

    Which is equivalent to

    2rν+(r2δ/cr)1ν(2r2δ/c)=Φ(u0,u1)cΨ(u0). (11)

    We consider the function, defined for s>0,

    f(s)2rs+(r2δ/cr)1s(2r2δ/c),

    and notice that

    f(ν),

    as ν0 and ν. Furthermore, f has an absolute minimum, that is

    f(s)f(1)=rδ/cr,s>0.

    Moreover, from (2) and the definition of Φ(u0,u1),

    Φ(u0,u1)cΨ(u0)>rδ/cr.

    Then, equation (11) equivalently (10), has two roots and only one bigger than one, that is, ν>1. Furthermore, at this root,

    αδ=σν(u0,u1)=(r2δ/c2r)(cΨ(u0)ν(2r2δc)),

    and

    limP(u0,u1)ν=.

    Next, we consider the equation

    J(μλ,δ(u0,u1))=12Φ(u0,u1), (12)

    where

    μλ,δ(u0,u1)12Φ(u0,u1)crΨ(u0)((rδ/c)rλcΨ(u0)Φ(u0,u1))(r2δ/c2),

    is defined for 0<λ<1. We observe that (12) holds if and only if

    (c(r2δ/c)2rΨ(u0)μλ,δ(u0,u1))(r2δ/c2)=((rδ/cr)λcΨ(u0)Φ(u0,u1))(r2δ/c2)

    And this is characterized by

    r2δ/c2(rδ/c)=λμλ,δ(u0,u1)Φ(u0,u1).

    Which is equivalent to

    2rδ/c(λ(rδ/cr)cΨ(u0)Φ(u0,u1))(rδ/c2)=λr2δ/crδ/c. (13)

    We consider the functions, defined for s[s2,1], with s2=r2δ/crδ/c,

    g(s)2rδ/c(s(rδ/cr)cΨ(u0)Φ(u0,u1))(rδ/c2),

    and

    h(s)sr2δ/crδ/c,

    are strictly monotone increasing, and

    g(s2)>h(s2)=0,g(1)<h(1)=2rδ/c,

    since, from (2) and definition of Φ(u0,u1),

    (rδ/cr)cΨ(u0)Φ(u0,u1)<1.

    Then, there exists one and only one λ(r2δ/crδ/c,1) where g(λ)=h(λ). That is, only one root λ of equation (13), equivalently (12). Moreover,

    βδ=μλ,δ(u0,u1)=(r2δ/crδ/c)(Φ(u0,u1)2λ),

    and

    limP(u0,u1)λ=r2δ/crδ/c.

    Proof. (of Corollary 1.) Since

    P(u0,u1)αδ0andβδ

    then, for every K>0 there exists L>0, such that

    P(u0,u1)>LKIδ=(αδ,βδ).

    Hence, the corresponding solution with initial energy E0=K satisfying (2) exists only up to a finite time.

    Remark 1. It is well known that when the potential well method is applied, for E0<d, the qualitative behavior is determinated by the sign of I(u0). In particular, the blow-up of a solution is characterized if the initial data are such that I(u0)<0. For any positive value of the initial energy, this is not the case. Indeed, under the assumptions of Theorem 3.1, we get from energy equation, if E0<βδ, and since r2δ/crδ/c<λδ<1, the following consequences

    I(u0)=2E0u12WP+2F(u0)(f(u0),u0)2E0|P(u0,u1)|2u02WP+2F(u0)(f(u0),u0)<2βδ|P(u0,u1)|2Ψ(u0)+2F(u0)(f(u0),u0)=(r2δ/crδ/c)Φ(u0,u1)λδ|P(u0,u1)|2Ψ(u0,v0)+2F(u0)(f(u0),u0)=((r2δ/crδ/c)1λδrrδ/c)Φ(u0,u1)((f(u0),u0)2F(u0)cΨ(u0))<(1rrδ/c)Φ(u0,u1)((f(u0),u0)2F(u0)cΨ(u0)).

    Hence,

    I(u0)<(δ/crδ/c)Φ(u0,u1)((f(u0),u0)2F(u0)cΨ(u0)) (14)

    Let us assume that the source term is large enough, that is,

    (f(u0),u0)2F(u0)cΨ(u0), (15)

    then, by (14),

    I(u0)<(δ/crδ/c)Φ(u0,u1)0.

    From (H1), (15) holds if the source term is such that

    F(u0)1r2cΨ(u0).

    Then, in this case the inequality I(u0)<0 is a necessary condition for nonexistence of global solutions. However, it seems that the condition I(u0)<0, alone, does not imply nonexistence of global solutions for high energies, see [14,28]. Moreover, the sign of I(u0) is not required in the proof of Theorem 3.1.

    By (H1) and the energy equation

    {2E0I(u0)(f(u0),u0)+2F(u0)}Ψ(u0){2(E0+F(u0))u02VA}Ψ(u0)|P(u0,u1)|2.

    If E0<d, the mountain pass level defined in (1), and f(u)|u|r2u, then rF(u)=urr, and

    {2dI(u0)r2ru0rr}Ψ(u0)>|P(u0,u1)|2.

    From Corollary 1, global nonexistence is obtained if P(u0,u1)>0. Hence, in order to conclude global nonexistence for E0<d, it is necessary that

    I(u0)<2dr2ru0rr.

    We remember that for E0<d, see [7], we have that I(u0)<0 if and only if 2rd<(r2)u0rr. Apparently, only for energies E0<d, the condition I(u0)<0 characterizes the nonexistence of global solutions of problem (P).

    Remark 2. We shall prove the following lower bound for βδ

    βδ>12Φ(u0,u1)1rcΨ(u0),

    which is equivalent to

    βδ>(rδ/c2r)|P(u0,u1)|2Ψ(u0)+(r2δ/c2r)cΨ(u0).

    To this end, consider first the following inequality

    βδ>(rδ/c2r)|P(u0,u1)|2Ψ(u0).

    Notice that it is equivalent to

    (λ(rδ/cr2δ/c)1)|P(u0,u1)|2<cΨ2(u0),

    where r2c/crc/c<λ<1.

    In order to prove last inequality, let us define for any s>0, the positive function

    l(s)(λ(rδ/cr2δ/c)1)s>0,

    and, from the proof of Theorem 3.1, we remember that λ is a function of s|P(u0,u1)|2, defined implicitly by

    2rδ/c(λ(rδ/cr)cΨ0Φ0)(rδ/c2)=λr2δ/crδ/c,

    where

    Ψ0Ψ(u0),Φ0Φ(u0,u1)=(rδ/cr)(cΨ0+sΨ0).

    Also, from the proof of Theorem 3.1 we know that

    limsλ=r2δ/crδ/c,lims0λ=1.

    Then, from the definition of λ and Φ0,

    limsl(s)=(2r2δ/c)limss(λ(rδ/cr)cΨ0Φ0)rδ/c2=2r2limss(λcΨ20cΨ20+s)(rδ/c2)=0.

    Also,

    lims0l(s)=0.

    Consequently, there is some s(0,), such that l(s)=maxs(0,)l(s). After some calculations, we find that

    s=cΨ20((r2δ/c)(1λ)(rδ/c)λ(r2δ/c)(1λ)),l(s)=cΨ20(((rδ/c)λ(r2δ/c))(1λ)(rδ/c)λ(r2δ/c)(1λ)),

    and consequently

    l(s)l(s)foranys>0.

    Hence,

    (λ(rδ/cr2δ/c)1)|P(u0,u1)|2<cΨ20η(λ), (16)

    where

    η(λ)(((rδ/c)λ(r2δ/c))(1λ)(rδ/c)λ(r2δ/c)(1λ))<1.

    Notice that (16) is equivalent to

    βδ>(rδ/c2r)|P(u0,u1)|2Ψ(u0)+ζ(λ)cΨ(u0),

    where

    ζ(λ)12r((rδ/c)(r2δ/c)λ(rδ/c)λ(r2δ/c)(1λ))>r2δ/c2r,

    since λ<1.

    Consequently,

    βδ>(rδ/c2r)|P(u0,u1)|2Ψ(u0)+(r2δ/c2r)cΨ(u0)=12Φ(u0,u1)1rcΨ(u0),

    Remark 3. We shall prove the following upper bound for αδ

    αδ<(r2δ/c2r)cΨ(u0).

    To this end, notice that this inequality is equivalent to

    ν(rδ/c2c)|P(u0,u1)|2Ψ2(u0)>1,

    where ν>1.

    In order to prove last inequality, we define for any s>0, the function

    l(s)ν(rδ/c2c)sΨ2(u0),

    where we remember from the proof of Theorem 3.1 that ν depends of s|P(u0,u1)|2, defined implicitly by

    2rν+(r2δ/cr)1ν(2r2δ/c)=Φ0cΨ0,

    where like in Remark 2

    Ψ0Ψ(u0),Φ0Φ(u0,u1)=(rδ/cr)(cΨ0+sΨ0).

    Furthermore, from the proof of Theorem 3.1 we know that

    limsν=,lims0ν=1

    Now, from the definition of ν and Φ0,

    limsl(s)=rδ/c2lims(r2δ/c2)1ν(2r2δ/c)=rδ/c2.

    Also,

    lims0l(s)=1.

    After some calculations, it follows that,

    ddsl(s)=(rδ/c2cΨ20)(111ν(rδ/cr2δ/c)1)>0.

    Moreover,

    limsddsl(s)=0,lims0ddsl(s)=.

    Then, l(s) is strictly increasing and bounded by

    1<l(s)<rδ/c2.

    And this is equivalent to

    0<αδ<(r2δ/c2r)cΨ(u0).

    Remark 4. The length of Iδ depends on the size of the damping coefficient δ0 and decreases as δ grows. Therefore, as the damping coefficient increases, the set of initial energies where we can have global non existence becomes smaller. In fact, from Remarks 2 and 3, we have that

    (rδ/c2r)|P(u0,u1)|2Ψ(u0)<|Iδ|<(rδ/c2r)(|P(u0,u1)|2Ψ(u0)+cΨ(u0)).

    In [1], the abstract problem (P) is studied with a more general linear damping term. In that paper, the nonexistence of global solutions is analyzed for any positive value of the initial energy. In fact, it is proved that the following functional, written in terms of our problem (P),

    P(u(t),u(t))+δt0P(u(s),u(s))ds,

    blows up in finite time if (H0),(H1) and

    0E0<P(u0,u1)u0WPδ4(r+2r1)u0WP,

    hold. We notice that the last condition implies u0WP>0,P(u0,u1)>0, and that for large values of E0, necessarily correspond large values of P(u0,u1), conclusion that agrees with our results.

    We consider the equation (GB). We remember that hypothesis (H0) holds with c=min{m,α1α2}. Also, we assumed that the source terms f and the corresponding potential operator F do not have any particular form but they satisfy (H1). The solution in the sense of Definition 2.1 holds, see [29,25,33], then nonexistence of global solutions is due to blow-up. By Theorem 3.1, if the initial data are such that

    u02+α2u022>0,(u0,u1)+α2(u0,u1)2>0,

    and the initial energy

    E0=12(u12+α2u122+α3u022+m2u02+α1u022)F(u0),

    is such that E0Iδ=(αδ,βδ), given in Theorem 3.1, then the corresponding solution is not global and blows up in finite time. Moreover, by Corollary 1, for every positive initial energy E0, there exists initial data such that imply the nonexistence of global solutions in the norm of H.

    There are several results in the literature showing blow up for large positive values of the initial energy for equations of the type (GB). They consider either δ=0, see [16,4,36], or a linear damping term, which can be either weak or strong, see [25,26,29,30,31]. In most of them, the blow up is proved under the assumption (2) and if the initial energy satisfies an inequality of the type

    E0<C1Ψ(u0)+C2|P(u0,u1)|2Ψ(u0), (17)

    with Cj0,j=1,2,C1+C2>0, are numbers depending on the damping constant δ and on the numbers c,r in (H0),(H1). See Remark 2 to compare this condition with a lower bound of βδ.

    In [16], the one dimensional equation (GB) with a source term of polynomial type, δ=0 and m2=1=αj,j=1,2,3, and consequently with c=1, is considered. There, blow up is proved if E0 satisfies, implicitly, the condition given in (8).

    Very recently, characterizations for blow up and globality where given in [5] for a one dimensional sixth order nonlinear double dispersive equation with a linear restoring force and with δ=0. This equation is of the type (P), with

    Put=(Δ+Id+(Δ)1)ut,Au=Pu,

    defined on the subspace of H=L2(RN),

    WP=VA={uH1(RN):(Δ)12uL2(RN)},

    with norms

    u2WP=u2VA=u22+u22+u2,

    where

    u2=(u,u)((Δ)12u,(Δ)12u)2.

    Hence c=1 in (H0) and the source term is of polynomial type and (H1) is satisfied. The characterizations are as follows.

    Theorem 6.1 ([5]). For this particular example, the following characterizations hold.

    ● The solution blows up in a finite time, TMAX<, if and only if

    lim suptTMAXI(u(t))<0.

    ● The solution is global, TMAX=, if and only if

    lim inftTMAXI(u(t))0.

    Those conditions are not easy to verify. Hence, sufficient conditions in terms of the initial data are needed. In [5], blow up in finite time is guaranteed if

    0<E0<r2rP(u0,u1)+r22rΨ(u0). (18)

    We observe that this inequality is not of the type (17), like the upper bound of βδ in Remark 2. However for P(u0,u1) large enough, βδ is larger than (18).

    Now, we consider the following problem with a linear damping term

    (KG){uttΔu+m2u+δut=f(u),u(0,x)=u0(x),ut(0,x)=u1(x),

    on R+×RN, where δ0,m2>0.

    This equation was studied in [28] with δ=0. Here,

    P=Id,H=WP=L2(RN),Au=Δu+m2u,VA=H1(RN).

    Hypothesis (H0) holds with c=min{1,m2}, and (H1) holds since f is assumed of a polynomial type.

    The solution in the sense of Definition 2.1 holds and nonexistence of global solutions is due to blow-up, see [28] for the details in the undamped case. Consequently, by Theorem 3.1, if the initial data satisfy

    u022>0,(u0,u1)2>0,

    and the initial energy is such that E0Iδ, the corresponding solution blows up in finite time in the norm of H. And by Corollary 1 for every positive initial energy E0, there exist initial data satisfying last inequality such that the solution blows up.

    In [28], blow up was proved under the assumption (2), and if the following inequalities hold

    0<E0<r22ru022,I(u0)<0.

    We observe that in Theorem 3.1 we did not assume any sign of I(u0) and βδ is larger than the upper bound on E0 given in [28], see Remark 2.

    The one dimensional case of (KG), with δ=0 and m2=1, was studied in [4] and blow up is showed under the assumption (2), and if the initial energy satisfies the implicit inequality given in (8).

    In [37] the following initial and homogeneous Dirichlet boundary value problem of a nonlinear wave equation of the type (KG), with a strong linear damping term, a source f of a polynomial type and m2=0, is studied.

    (KG){uttΔuωΔut+δut=f(u),xΩ,t>0,u(0,x)=u0(x),ut(0,x)=u1(x),xΩ,u(x,t)=0,xΩ,t>0,

    where ΩRN, is a bounded domain with smooth boundary

    The blow up is proved under the assumption (2), and if the initial energy satisfies the inequality

    0<E0<C(u0,u1)2, (19)

    where C>0, depends on ω,δ and c,r in (H0),(H1), and in the case that ω=0, the constant is equal to C=c(r2)r(1+δ). This inequality is not of the type of the upper bound of βδ in Remark 2, but for (u0,u1)2 large enough, βδ is larger than the bound in (19).

    Many works have been published about the Kirchhoff equation. In particular, in [15] blow up of solutions of the following problem was studied.

    (KE){uttϕ(u22)Δu+δut=g(u),xΩ,t>0,u(0,x)=u0(x),ut(0,x)=u1(x),xΩ,u(x,t)=0,xΩ,t>0,

    where ΩRN, is a bounded domain with smooth boundary

    In [15], existence and uniqueness is proved in the phase space

    H=(H10(Ω)H2(Ω))×H(Ω)

    for a set of functions g and ϕ, satisfying several conditions. In particular, g satisfies (H1), that is,

    (g(u),u)θG(u)0,uH10(Ω)H2(Ω),θ>2,

    where G is the potential of g, and a typical form of ϕ is

    ϕ(u22)=c1u22+c2u2q2

    with cj>0,j=1,2 and q1. In this case, if c1=c2=1 for simplicity,

    f(u)=g(u)+u22qΔu,

    has the potential

    F(u)=G(u)12(q+1)u2q2,

    and satisfies (H1) with

    θr2(q+1)4,

    that is, the nonlinearity of the source term g is stronger than the one of ϕ. In contrast, for a Timoshenko equation where these two nonlinearities appear, if θ<2(q+1) holds then all the solutions are global and uniformly bounded in the phase space H defined above. Furthermore, all the solutions are attracted by the set of equilibria as times goes to infinity, see [13].

    The blow up result showed in [15] holds if the initial data are such that

    0<E0<12u022((u0,u1)22δr2u022)2,(u0,u1)2>0.

    Note that this upper bound of E0 is smaller than

    12|(u0,u1)2|2u022+2(δr2)2u022,

    which is of the type (17). And also, it is smaller than βδ in Theorem 3.1.

    I thank Professor Howard Levine for calling our attention to his work with Professor Todorova, [18]. We also thank to Professor Varga Kalantarov for sharing his articles, especially [1]. Finally, we thank to the anonymous referees for their valuable comments that improved the final form of this article. This work was supported by the Universidad Autónoma Metropolitana, Unidad Azcapotzalco.



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