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Blow-up phenomena for porous medium equation driven by the fractional p-sub-Laplacian

  • In this paper, we investigate the global existence and blow-up phenomena of the solution to the fractional nonlinear porous medium equation on stratified groups, employing the concavity method. Specifically, we establish the necessary conditions for the existence of global solutions and blow-up solutions. Our findings not only contribute to the understanding of this equation on stratified groups but also extend the existing knowledge in the classical Euclidean setting to the fractional case.

    Citation: Khumoyun Jabbarkhanov, Amankeldy Toleukhanov. Blow-up phenomena for porous medium equation driven by the fractional p-sub-Laplacian[J]. AIMS Mathematics, 2025, 10(6): 13498-13511. doi: 10.3934/math.2025606

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  • In this paper, we investigate the global existence and blow-up phenomena of the solution to the fractional nonlinear porous medium equation on stratified groups, employing the concavity method. Specifically, we establish the necessary conditions for the existence of global solutions and blow-up solutions. Our findings not only contribute to the understanding of this equation on stratified groups but also extend the existing knowledge in the classical Euclidean setting to the fractional case.



    This paper studies the fractional nonlinear porous medium equation of the form

    ut(x,t)+(Δp,G)s(um(x,t))=f(u(x,t)),m1,(x,t)Ω×(0,), (1.1)

    where Ω denotes an open, bounded subset of a stratified (Lie) group G. The model involves the extension of the p-Laplacian operator by the fractional p-sub-Laplacian (Δp,G)s with p(1,) and s(0,1). Note that case s=1 is understood as the p-sub-Laplacian operator. The source function f satisfies f(0)=0, and f(u)>0 when u>0. We consider the initial condition

    u(x,0)=u0(x)0,xˉΩ,u0C0(Ω), (1.2)

    and the boundary condition

    u(x,t)=0,xΩ,t>0. (1.3)

    The porous medium equation is a well-known nonlinear parabolic equation with numerous applications in fluid flow, diffusion, and various other fields such as lubrication and mathematical biology. For a comprehensive mathematical analysis, see [1], and for more recent references, see [2]. The fractional porous medium equation is discussed by [3,4]. Fractional Sobolev spaces are well described in [5], while the fractional p-sub-Laplacian is covered in [6]. For studies on blow-up phenomena and global existence in Euclidean space, the seminal reference is the book by [7]. Blow-up in the fractional setting is studied in [8,9], and within group settings in [10].

    Fractional Laplacian models have also been used in many applications instead of integer-order Laplacians [11]. For instance, when m=1 in Eq (1.1) on the Euclidean space, it describes stable jump Lévy processes, anomalous diffusion, and population dynamics [12].

    Stan and Vázquez [13] studied the propagation properties of the problem with p=2. Their research suggests that exponential propagation is a common phenomenon, and the presence of traveling wave behavior can be reduced to the classical Fisher-KPP model. They also studied the existence of a unique mild solution to problem (1.1) using the semigroup approach. Grillo, Muratori, and Punzo [14,15] investigated the existence and uniqueness of the solution to the problem with p=2 and f=0.

    Blow-up and global existence phenomena have also been extensively investigated using the perturbed energy method, with notable contributions found in [16,17] and the references therein. For additional related results concerning existence, blow-up behavior, and optimal decay estimates, we refer the reader to [18,19] and the references cited therein.

    In recent years, various researchers have investigated the global and blow-up behavior of solutions to nonlinear equations using different techniques. One approach is the so-called concavity method, which was first introduced by Levine [20,21]. Chung and Choi [22] recently proposed a condition of the form

    αu0f(s)dsuf(u)+βup+αθ,u>0, (1.4)

    for certain parameters β, α, and θ. Utilizing the concavity method, they established blow-up results for parabolic equations. Building on this work, Ruzhansky, Sabitbek, and Torebek [23] extended the analysis to a nonlinear porous medium equation by generalizing condition (1.4) to obtain similar blow-up criteria for positive solutions. We also refer to an earlier related work of Jleli, Kirane, and Samet on the Heisenberg group [24]. Nevertheless, relatively limited research has been conducted on fractional problems for the Heisenberg group and/or more general classes of stratified Lie groups.

    Recently, the fractional version of this problem with m=1 (the linear case) in the Euclidean space has been investigated in our papers [25,26]. Additionally, important results related to global and blow-up solutions, with the nonlinearity function represented as f(u)=u(u1), can be found in [27].

    In this work, we aim to expand on existing ideas by investigating the global and blow-up phenomena of the fractional porous medium problem (1.1) on stratified groups. Our contribution seems new not only for the case of general stratified groups but also for the Heisenberg group case and even for the classical Euclidean case. Specifically, we prove the existence of global and blow-up solutions under certain conditions.

    To structure this paper, we organize our discussion as follows: Section 2 provides preliminaries on stratified groups, fractional Sobolev spaces, and a blow-up property. Section 3 establishes the main results on the global existence and blow-up phenomena of the solution to the fractional nonlinear porous medium equation on stratified groups by using the concavity method. In Section 4, we briefly discuss consequences of our results in the context of the Euclidean setting.

    Extensive research has been conducted in the field of fractional Sobolev spaces on stratified groups, with contributions from recent works such as [28,29]. In this section, we aim to facilitate an understanding of the subsequent sections by introducing essential notations that hold importance.

    Definition 2.1. A Lie group G=(RN,) is said to be a stratified group (or a homogeneous Carnot group) if it satisfies the following conditions:

    ● The space RN can be decomposed as RN=RN1×...×RNr for some natural numbers N1,N2,,Nr such that N=N1+N2++Nr, and the dilation δλ:GG is provided by

    δλ(x)σλ(x(1),x(2),...x(r)):=(λx,λ2x(2),...λrx(r))

    is an automorphism of the group G for every λ>0, where xx(1)RN1 and x(k)RNk for k=1,2,...r.

    ● Let N be defined as above, and let X1,,XN be the left-invariant vector fields on G satisfying Xk(0)=/xk|0 for k=1,,N. Then the iterated commutators of X1,,XN span the Lie algebra of G. That is, we have the Hörmander condition

    rank(Lie{X1,X2,...XN})=N

    for every xRN.

    Note that the left-invariant vector fields X1,X2,...XN are called the Jacobian generators of a stratified group G, and r is called the step of G. Additionally, the left-invariant vector fields Xk can be written in the explicit form

    Xk=xk+rl=2Nlm=1a(l)k,m(x,x2,,xl1)x(l)m,

    where a(l)k,m is a homogeneous polynomial with degree l1.

    The homogeneous dimension of G is given by

    Q=rk=1kNk,N=N1.

    Remark 2.2. The (classical) Euclidean group (RN,+) with the dilation

    δλ(x)=λx,λ>0,

    where Jacobian generators are given by x1,...,xN with step r=1, is obviously a (Abelian) stratified group.

    In this paper, to simplify the notations, u(x,t) can be written simply as u. However, if u is part of an integrand with the differential dτ, then it is understood as u:=u(x,τ). The same idea applies for u(x):=u(x,t), u(y):=u(y,t), and f(u):=f(u(x,t)).

    Definition 2.3. Let ΩG be an open subset. Let u:ΩR be a measurable function. The Gagliardo semi-norm [u]s,p,Ω is defined as follows:

    [u]s,p,Ω:=(ΩΩ|u(x)u(y)|p|y1x|Q+psdxdy)1p.

    Definition 2.4. Let ΩG be an open subset. For p>1, and 0<s<1, the space Ws,p(Ω) is defined as

    Ws,p(Ω)={uLp(Ω):[u]s,p,Ω<}, (2.1)

    and is equipped with the norm

    uWs,p(Ω)=(upLp(Ω)+[u]ps,p,Ω)1p.

    This space is called the fractional Sobolev space on G.

    We define the space Ws,p0(Ω) as the closure of C0(Ω) with respect to the norm uLp(Ω)+[u]s,p,G. It can be represented in the form

    Ws,p0(Ω)={uWs,p(G):u=0 in GΩ},

    where Ω is an open bounded set (with at least a continuous boundary Ω).

    Definition 2.5. Let 1<p< and 0<s<1. The fractional p-sub-Laplacian on G is defined as follows:

    (Δp,G)su(x):=CQ,s,pP.V.G|u(x)u(y)|p2(u(x)u(y))|y1x|Q+psdy,xG, (2.2)

    where P.V. denotes the Cauchy principal value, and CQ,s,p>0 is independent of u.

    We define the following product:

    (Δp,G)su,φ=G×G|u(x)u(y)|p2(u(x)u(y))(φ(x)φ(y))|y1x|Q+psdxdy (2.3)

    for all φWs,p0(Ω).

    The equation on a stratified group G of the form

    {(Δp,G)su=λ|u|p2u, in Ω,u=0 in GΩ (2.4)

    is called the fractional p-sub-Laplacian eigenvalue problem.

    We recall the Poincaré inequality for the Gagliardo seminorm [28]:

    λQ,p,s(Ω)Ω|u(x)|pdxGG|u(x)u(y)|p|y1x|Q+psdxdy. (2.5)

    where p>1, 0<s<1, and λQ,p,s(Ω)=C(Q,p,s)p|Ω|psQ>0.

    Definition 2.6. umL(0,T;Ws,p0(Ω)), with utL(0,T;L2(Ω)), is called a weak (local) solution of (1.1)–(1.3) if it satisfies the following equation:

    Ωut(x,t)φ(x)dx+G×G|um(x)um(y)|p2(um(x)um(y))(φ(x)φ(y))|y1x|Q+psdxdy=Ωf(u)φ(x)dx (2.6)

    for all φWs,p0(Ω) and a.e. time 0tT with

    um(x,0)=um0(x) in W1,p0(Ω).

    Here we provide a definition of the blow-up phenomena and recall an important lemma that is used in our proofs.

    Definition 2.7. Assume that u(x,t) is a weak solution to problem (1.1). We say that u(x,t) blows up in finite time T if it satisfies the estimate

    limtTt0Ωum+1(x,τ)dxdτ=+.

    Lemma 2.8. [21,30,31] Let E(t) be a twice-differentiable function satisfying the following inequalities for some constant ρ>0:

    {E(t)E(t)(1+ρ)E2(t)0,t>0,E(0)>0,andE(0)>0. (2.7)

    Then there exists

    0<TE(0)ρE(0),

    such that limtTE(t)=+.

    Throughout this paper, we refer to the function u as a weak solution in the sense of Definition 2.6. Furthermore, we assume the existence of a local weak solution for the problem under consideration.

    Theorem 3.1. Let Ω be a bounded open set of a stratified group G. Assume that

    αF(u)umf(u)+βupm+αθ,u>0, (3.1)

    where

    F(u)=pmm+1u0sm1f(s)ds,

    for m1, and

    0>β(α(m+1))λQ,p,s(Ω)(m+1),andα0, (3.2)

    where 1<p<, and λQ,p,s(Ω)>0 is the constant given in (2.5). For the initial data u0C0(Ω), if we have a constant θ>0 such that

    [u0]ps,p,G(m+1)Ω(F(u0)θ)dx, (3.3)

    then a non-negative solution u of problem (1.1)–(1.3) is global and satisfies the estimate

    u(x,t)m+1Lm+1(Ω)u0(x)m+1Lm+1(Ω).

    Proof. Assume that u0 is a solution of the fractional porous medium Eq (1.1), and

    E(t):=Ωum+1(x,t)dx.

    Then

    E(t)=(m+1)Ωum(x,t)ut(x,t)dx=(m+1)(GG|um(x)um(y)|p2(um(x)um(y))2|y1x|Q+psdxdy+Ωum(x,t)f(u(x,t))dx).

    Applying the Poincaré inequality and the assumptions (3.1) and (3.2), we have

    E(t)(m+1)(GG|um(x)um(y)|p|y1x|Q+psdxdy+Ω(αF(u)βupmαθ)dx)(m+1)α(1m+1GG|um(x,t)um(y,t)|p|y1x|Q+psdxdy+Ω(F(u)θ)dx)+[(α(m+1))λQ,p,s(Ω)(m+1)β]Ω|u(x,t)|pmdx(m+1)α(1m+1GG|um(x,t)um(y,t)|p|y1x|Q+psdxdy+Ω(F(u)θ)dx)(m+1)αI(t), (3.4)

    where we set

    I(t):=1m+1GG|um(x,t)um(y,t)|p|y1x|Q+psdxdy+Ω(F(u)θ)dx.

    We can further derive that

    I(t)=I(0)+t0ddτI(τ)dτ=I(0)+pmm+1t0Ω[uτ(x,τ)]2um1(x,τ)dxdτ. (3.5)

    To see it, we compute

    t0ddτI(τ)dτ=1m+1t0ddτ(GG|um(x,τ)um(y,τ)|p|y1x|Q+psdxdy)dτ+t0Ωddτ(F(u(x,τ))θ)dxdτ=pm+1t0GG|um(x)um(y)|p2(um(x)um(y))([um(x)]τ[um(y)]τ)|y1x|Q+psdxdydτ+t0Ω(Fu(u(x,τ))uτ(x,τ)dxdτ=pm+1t0GG|um(x)um(y)|p2(um(x)um(y))([um(x)]τ[um(y)]τ)|y1x|Q+psdxdydτ+pmm+1t0Ωum1(x,τ)f(u)uτ(x,τ)dxdτ,

    From the definition of the weak solution, it implies that

    t0ddτI(τ)dτ=pm+1t0Ωuτ(x,τ)umτ(x,τ)dxdτpm+1t0Ωf(u)umτ(x,τ)dxdτ+pmm+1t0Ωum1(x,τ)f(u)uτ(x,τ)dxdτ=pmm+1t0Ω[uτ(x,τ)]2um1(x,τ)dxdτpmm+1t0Ωf(u)uτ(x,τ)um1τ(τ,x)dxdτ+pmm+1t0Ωum1(x,τ)f(u)uτ(x,τ)dxdτ=pmm+1t0Ω[uτ(x,τ)]2um1(x,τ)dxdτ.

    Observe that I(t)>0, due to the assumption I(0)>0 (given in (3.3)) and the positive integrand in (3.5).

    Finally, we conclude

    E(t)(m+1)α(I(0)+pmm+1t0Ω[uτ(x,τ)]2um1(x,τ)dxdτ)0,

    since α0. It yields that

    E(t)E(0)0,

    and

    u(x,t)m+1Lm+1(Ω)u0(x)m+1Lm+1(Ω)

    for all t(0,).

    Theorem 3.2. Assume Ω is a bounded open set of a stratified group G, and let f be a function that satisfies the inequality

    αF(u)umf(u)+βupm+αθ,u>0,

    where 1<p<, θ>0 is a constant, and m1. Here we have

    F(u):=pmm+1u0sm1f(s)ds.

    Furthermore, suppose that α>m+1 and 0<β(α(m+1))λQ,p,s(Ω)(m+1), where λQ,p,s(Ω)>0 is the constant given in (2.5).

    If the initial condition u0C0(Ω) satisfies

    [u0]ps,p,G(m+1)Ω(F(u0)θ)dx, (3.6)

    for a constant θ, then a solution u of (1.1)–(1.3) blows up in finite time T, that is,

    0<TMρΩum+10(x)dx,

    where

    M=pm(Ωum+10(x)dx)2(m+1)2(αpm(m+1))I(0)

    with ρ=ε=αpmm+11>0.

    Proof. Let u0 be a solution of the fractional porous medium Eq (1.1). Assume that

    E(t):=Ωt0um+1(x,τ)dτdx+M,

    where M>0 is a constant that will be defined later.

    According to Lemma 2.8, we need to prove that

    E(t)E(t)(1+ρ)(E(t))2>0. (3.7)

    Applying the fundamental calculus, we have

    E(t)=Ωum+1(x,t)dx=(m+1)Ωt0um(x,τ)uτ(x,τ)dτdx+Ωum+10(x)dx.

    Now we compute

    E(t)=(m+1)Ωum(x,t)ut(x,t)dx(m+1)(GG|um(x)um(y)|p|y1x|Q+psdxdy+Ω(αF(u)βupmαθ)dx)(m+1)α(1m+1GG|um(x,t)um(y,t)|p|y1x|Q+psdxdy+Ω(F(u(x,t))θ)dx)+[(α(m+1))λQ,p,s(Ω)(m+1)β]Ω|u(x,t)|pmdx(m+1)α(1m+1GG|um(x,t)um(y,t)|p|y1x|Q+psdxdy+Ω(F(u(x,t))θ)dx)(m+1)αI(t),

    where

    I(t):=1m+1GG|um(x,t)um(y,t)|p|y1x|Q+psdxdy+Ω(F(u(x,t))θ)dx,

    and 0<β(α(m+1))λQ,p,s(Ω)(m+1) with λQ,p,s(Ω)>0 is the constant given in (2.5). Moreover, we have I(0)>0 from the assumption (3.6), and estimate

    I(t)=I(0)+pmm+1t0Ω[uτ(x,τ)]2um1(x,τ)dxdτ>0

    obtained in the proof of Theorem 3.1. Therefore, it yields

    E(t)(m+1)αI(t)(m+1)αI(0)+αpmt0Ω[uτ(x,τ)]2um1(τ,x)dxdτ,

    where α>m+1. For arbitrary ε>0, we use the Cauchy-Schwarz inequality to obtain

    [E(t)]2=((m+1)Ωt0um(x,τ)uτ(x,τ)dτdx+Ωum+10(x)dx)2(m+1)2(1+ε)(Ωt0um(x,τ)uτ(x,τ)dxdτ)2+(1+1ε)(Ωum+10(x)dx)2.

    Now we apply the Hölder inequality to obtain

    [E(t)]2=(m+1)2(1+ε)(Ωt0u(m+1)/2+(m1)/2(x,τ)uτ(x,τ)dxdτ)2+(1+1ε)(Ωum+10(x)dx)2(m+1)2(1+ε)(Ω(t0um+1dτ)1/2(t0um1[uτ(x,τ)]2dτ)1/2dx)2+(1+1ε)(Ωum+10(x)dx)2(m+1)2(1+ε)(t0Ωum+1dxdτ)(t0Ωum1[uτ(x,τ)]2dxdτ)+(1+1ε)(Ωum+10(x)dx)2.

    Using the computations above, we have

    E(t)E(t)[(m+1)αI(0)+αpmt0Ω[uτ(x,τ)]2um1(τ,x)dxdτ]×(Ωt0um+1(x,τ)dτdx+M)(m+1)αI(0)M+αpmt0Ω[uτ(x,τ)]2um1(x,τ)dxdτΩt0um+1(x,τ)dτdx.

    Finally, using the estimates above, we obtain

    E(t)E(t)(1+ρ)(E(t))2α(m+1)I(0)M+αpm(t0Ω[uτ(x,τ)]2um1(x,τ)dxdτ)(Ωt0um+1(x,τ)dτdx)(1+ρ)(1+ε)(m+1)2(t0Ωum+1(x,τ)dxdτ)(t0Ωum1(x,τ)[uτ(x,τ)]2dxdτ)(1+ρ)(1+1ε)(Ωum+10(x)dx)2.

    We choose ρ=ε=αpmm+11>0, and

    M:=pm(Ωum+10(x)dx)2(m+1)2(αpm(m+1))I(0).

    Thus, we arrive at

    E(t)E(t)(1+ρ)(E(t))2α(m+1)I(0)M(1+ρ)(1+1ε)(Ωum+10(x)dx)20.

    Consequently, the blow-up time is given by

    0<TMρΩum+10(x)dx.

    It completes the proof.

    Remark 3.3. Note that the value of θ in Theorems 3.1–3.2 can be chosen to satisfy the condition F(u)>θ due to the conditions I(t)>0 and the assumption I(0)>0 in the theorems.

    Let us briefly discuss some special cases, that is, the consequences in the Euclidean setting. Specifically, for an open, bounded subset ΩRN, consider the problem

    {ut(x,t)+(Δp)s(um(x,t))=f(u(x,t)),m1,(x,t)Ω×(0,),u(x,0)=u0(x)0,xˉΩ,u(x,t)=0, in RNΩ,t>0, (4.1)

    where the fractional operator is denoted by

    (Δp)su(x):=CN,s,pP.V.RN|u(x)u(y)|p2(u(x)u(y))|xy|N+psdy,xRN, (4.2)

    with p(1,) and s(0,1). A function f satisfies f(0)=0, and f(u)>0 when u>0.

    According to Remark 2.2, (4.1) is a particular case of Eq (1.1) with initial-boundary conditions given by (1.2) and (1.3). Thus, the results presented in Theorems 3.1 and 3.2 imply new insights in the Euclidean case.

    Specifically, in the context of problem (4.1), a global solution exists when

    αF(u)umf(u)+βupm+αθ,u>0,

    with

    F(u)=pmm+1u0zm1f(z)dz,m1,

    and certain conditions on the parameters α, β, and θ given in Theorem 3.1. Additionally, under other conditions on the parameters α, β, and θ provided in Theorem 3.2, blow-up solutions exist when

    αF(u)umf(u)+βupm+αθ,u>0.

    Khumoyun Jabbarkhanov: Conceptualization, investigation, original draft preparation, writing-review and editing; Amankeldy Toleukhanov: Investigation, writing-review and editing. All authors have read and approved the final version of the manuscript for publication.

    The authors declare they have not used Artificial Intelligence (AI) tools in the creation of this article.

    This research is funded by the Committee of Science of the Ministry of Science and Higher Education of Kazakhstan (Grant number BR24993094). This work is also supported by the NU program 20122022CRP1601. The authors express their gratitude to Dr. Durvudkhan Suragan for valuable guidance and discussions on the topic of this paper.

    The authors declare that they have no conflict of interest.



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