Abstract
In this paper, we consider the generalized porous medium equation. For small initial data belonging to the Fourier-Besov-Morrey spaces with variable exponent, we obtain the global well-posedness results of generalized porous medium equation by using the Fourier localization principle and the Littlewood-Paley decomposition technique. Furthermore, we also show Gevrey class regularity of the solution.
1. Introduction
We consider the three dimensional generalized porous medium (GPM) equation:
where denotes the concentration or density. The dissipative coefficient is the inviscid case, while represents the viscous case. P is an abstract operator and the fractional Laplacian term is the Fourier Transform defined by . For simplicity we chose .
The Equation (1) was first introduced by Zhou et al. [1]. Actually, by applying the fractional dissipative term to the continuity equation , Caffarelli et al. [2] obtained the Equation (1), where the velocity V derives from the potential, , and the velocity potential or pressure is associated with u by the abstract operator [3]. There are a number of physical applications of porous medium of equations, mainly to describe processes involving fluid flow, heat transfer or diffusion. May be the best known of them is the description of the flow of an isentropic gas through a porous medium. Other applications have been proposed in mathematical biology, lubrication, boundary layer theory and other fields. For detailed study related to the physical significance of (1), we refer the reader to [4] and the references therein.
The abstract form pressure term gives a good suitability in many cases. The simplest case comes from a model in ground water in filtration [5,6]. For more general case and , , Zhou et al. [7] obtained the strong solution for Equation (1) in Besov spaces and for any initial data in the local solution is obtained. Lin and zhang [8] considered (1) for (critical case), which gives the mean field equation. For more details in this direction we refer the reader to [1,9] and the references therein.
Another similar model appears in the aggregation equation, which explains a aggregation phenomena and collective motion in mechanics of continuous media and biology [10,11]. This equation has many applications in various applied sciences such as chemistry, biology, physics and population dynamics. In the aggregation equation, the operator P can also be written as convolution operator with kernel as . The typical kernels are exponential potential [12] and the Newton Potential [13]. For more results related to the well-posedness and blowup criterion, we refer the reader to [14,15] and the references therein.
Furthermore, using the same initial data, we can write the Equation (1) as:
Then the Equation (2) can be compared to the geostrophic model and the convective velocity for the generalized porous medium equation is not absolutely divergence-free. In addition, if the divergence-free vector function v satisfies the equation , the Equation (2) will hold the quasi-geostrophic (Q-G) equation [16,17].
One of the main problems to the Equation (1) is the singularity of the abstract form pressure term that establish the well-posedness or gives the blow up solution. Zhou et al. [1] established the local well-posedness for large initial data in Besov spaces and the global solution for small inital data. They also given a blowup criterion for the solution. Li and Rodrigo [12] obtained well-posedness and the blownup criterion for the solution of Equation (1) associated with the pressure , where belongs to Sobolev space. Moreover, their work is further extended by Wu and Zhang [18] to the case and . Xiao and Zhou [3] have shown the local well-posedness for large initial data in Fourier-Besov spaces and obtained the global well-posedness for small initial data for . The controllability of convolution and its gradient in Besov spaces leads to these result.
Inspired by the above works, we obtain the global well-posedness and analyticity for Equation (1) and show the Gevery class regularity of the solution in homogenous Fourier-Besov-Morrey spaces with variable exponent by considering The Fourier-Besov spaces goes back to the work of Konieczny and Yoneda [19] in the context of Navier-Stokes equation (NSE) with Coriolis force. Fourier-Besov spaces and Fourier-Besov-Morrey spaces have been extensively considered by many authors in order to deal with the well-posedness, self-similar solution, regularity etc. For more study in this direction, we refer the reader to [20,21,22] and the references therein.
The variable exponent Lebesgue spaces , comes from Orlicz [23] and further developed by Musielak [24] and Nakano [25]. However the recent improvement begins with Kovacik and Rakosnik [26] and further advancement by Cruzuribe [27] and Diening [28]. The main reason of variable exponent function spaces is their applications in fluid dynamics [29], image processing [30] and partial differential equations [31]. For detailed study related to Besov spaces with variable exponent and Besov-Morrey spaces with variable exponent, we refer the reader to [32,33,34,35,36,37] and the references therein.
2. Preliminaries
In this section, we recall some definitions of various functions spaces with variable exponent, basic facts about dyadic decomposition, and some useful propositions. Throughout this paper, denotes that for some constant . We obtained the global well-posedness result and prove Gevrey class regularity in Section 3 and Section 4, respectively. The conclusion is given in Section 5.
Definition 1.
Let denotes the set of all measurable functions such that
The Lebesgue space with variable exponent is defined by
with Luxemburg-Nakano norm
In order to differentiate between constant and variable exponent, we denote constant exponent by p, and variable exponent by . Also is a Banach space.
Since the does not have the same desired properties like . So, to ensure that the Hardy-Littlewood maximal operator M is bounded on , we postulate the following standard conditions:
(1) (locally log-Hölder continuous) There exists a constant such that
(2) (locally log-Hölder continuous) There exists a constant and some constant independent of x such that
denote the set of all functions satisfying (1) and (2).
Definition 2.
Let with , the Morrey space with variable exponent := be the set of measurable functions on with finite quasinorm
By the definition of quasinorm also has the following form
Now we present some essential lemmas from [36].
Lemma 1.
Let with and f be any measurable function. Then
Lemma 2.
. For any measurable function f
Lemma 3.
If , then .
Now we recall dyadic decomposition of . Let and be the two non negative radial functions such that
We denote and to define the frequency localization as follows:
where is a frequency projection to the annulus and is a frequency to the ball . we can easily obtain that
Definition 3.
Let , , , the mixed Lebesgue-sequence space is defined as the set of all sequences of measurable functions in such that
where
Notice that if and , then
Definition 4.
Let and with . We define the homogeneous Besov-Morrey space with variable exponent by
with norm
The space is the dual space of
Definition 5.
Let and with . We define the homogeneous Fourier-Besov-Morrey space with variable exponent by
with norm
Definition 6.
Let and . We define the Chemin-Lerner type homogeneous Fourier-Besov-Morrey space with variable exponent by
with norm
Proposition 1.
The following inclusions are established for the Morrey spaces with variable exponent.
(1) ([37]) let , such that . Then there exists a constant C depending only on and such that
holds for every and .
(2) [37]) Let , and with . If and
are locally log- Hölder continuous, then
(3) ([36]) For and assume is integrable. Then
for all , where and C depends only on n.
Next, we recall the paradifferential calculus which enables us to define a generalized product between distributions. The paraproduct between u and v is defined by
Then we have the formal decomposition:
with
This decomposition is called Bony’s paraproduct decomposition.
Proposition 2.
Let , , , and . Then we have
Proof.
Applying Bony’s paraproduct decomposition for some fixed , we can write
To prove this proposition, we estimate the above three terms separately. According to the Proposition 1, we have
Then we have
Considering , we have
Similarly, for we have
To estimate , using Proposition 1 and obtain
Then we get
Considering , we have
By combining the above estimates yields the result. □
Proposition 3.
Let , , , and . Then we have
Proof.
Replacing in the proof of Proposition 2 by , we can obtain the desired inequality. □
3. The Well-Posedness
In this section, we obtain the global well-posedness of generalized porous equations by using contraction mapping in critical Banach spaces. To insure the global well-posedness for small initial data , the following lemma is very important.
Lemma 4.
(Lemma 5.5, [38]) Let X be a Banach space with norm and be a bounded linear operator satisfying for any and a constant . Then for any such that , the equation has a solution . In particular, the solution is such that and it is the only one such that .
The main tool to to prove the result is to obtain the priori estimates of the Equation (1). First, we prove the linear estimates of (1). To obtain this, we consider the linear homogeneous dissipative equation
for which we show the following lemma.
Lemma 5.
Let , , , for , and . Assume that and . Then the Cauchy problem (3) has a unique solution such that for all
Moreover, if , then .
Proof.
Clearly, solution to the Cauchy problem (3) can be written by the following integral equation:
The Fourier Transform of Equation (5) gives
Multiplying both sides of Equation (6), we have
Applying on both sides of Equation (7), we have
We estimate the above two terms separately. Let , using Proposition 1 and considering , we get
where we have used the following fact in the above estimate
To estimate , using Proposition 1, we have
Using the inequalities (9), (10) in (8) and taking the -norm, we can obtain the desired estimate (4). □
Theorem 1.
Let , , , , and then there exists a constant such that for any satisfies , the Equation (1) has a unique global solution
such that
Proof.
For , we can write the solution of the Equation (1) in the following integral form
Next we define
and consider the mapping below
We have to show that the above mapping is a contraction mapping. First, we can write
To estimate , using Lemma 5 with and considering the hypothesis , we obtain
Hence, we get
To estimate , let , using Propositions 1 and 3, then
Similarly, we have
and
Hence, we obtain
Using the estimates (15) and (19) in (14), we have
Choosing and for any with
we get
Using Lemma 4, we can directly obtain that Equation (1) has a unique global solution with for sufficiently small . □
4. Gevrey Class Regularity
In this section, we show the gevrey class regularity for Equation (1). Many researchers have studied analyticity with respect to Navier-Stokes equations. For more study related to Gevrey class regularity we refer the reader to to [39,40]. In order to prove the spatial analyticity, the following lemma is very helpful.
Lemma 6.
(Lemma 4.1 [41]) Let and . Then the following inequality holds
for all .
Theorem 2.
Let ,, , , then there exist a constant such that for all initial data satisfying . The Equation (1) has a unique analytic solution u in the sense that
Proof.
Assume and using Equation (11), we obtain
It is easy to obtain
Using and Lemma 6, we obtain
The remaining part of the proof is similar to the proof of Theorem 3.3, therefore the details can be omitted. □
5. Conclusions
In this paper, we considered the generalized porous medium equations. Young’s inequality is one of the important tools to obtain the global well-posedness result of such equations. In the previous work of Xiao and Zhou [3], they obtained the local well-posedness for large initial data and the global well-posedness for small initial data in Fourier-Besov spaces. We can’t use Young’s inequality in variable exponent function spaces in order to obtain the global well-posedness result. We overcame with this problem and obtained the global well-posedness results of this equation for small initial data belonging to the homogeneous Fourier-Besov-Morrey spaces with variable exponent. In addition, we also shown the Gevrey class regularity of the solution.
Author Contributions
Methodology, M.Z.A.; Project administration, J.C.; Software, M.Z.A.; Supervision, J.C.; Writing—original draft, M.Z.A.; Writing—review & editing, J.C. All authors have read and agreed to the published version of the manuscript.
Funding
The research was supported by NSF of China (No. 12071437).
Acknowledgments
The authors is highly thankful to the Editor-in-Chief and the anonymous referees for their valuable comments and suggestions for the improvement of our manuscript.
Conflicts of Interest
The authors declare no conflict of interest.
References
- Zhou, X.; Xiao, W.; Zheng, T. Well-posedness and blowup criterion of generalized porous medium equation in Besov spaces. Electron. J. Differ. Equ. 2015, 2015, 1–14. [Google Scholar]
- Caffarelli, L.; Vazquez, J.L. Nonlinear Porous Medium Flow with Fractional Potential Pressure. Arch. Ration. Mech. Anal. 2011, 202, 537–565. [Google Scholar] [CrossRef] [Scilit]
- Xiao, W.; Zhou, X. On the Generalized Porous Medium Equation in Fourier-Besov Spaces. J. Math. Study 2020, 53, 316–328. [Google Scholar]
- Vázquez, J.L. The Porous Medium Equation: Mathematical Theory; Oxford University Press: New York, NY, USA, 2007. [Google Scholar]
- Bear, J. Dynamics of Fluids in Porous Media; Courier Corporation: Chelmsford, MA, USA, 2013. [Google Scholar]
- Aronson, D.G. The porous medium equation. In Nonlinear Diffusion Problems; Springer: Berlin/Heidelberg, Germany, 1986; pp. 1–46. [Google Scholar]
- Zhou, X.; Xiao, W.; Chen, J. Fractional porous medium and mean field equations in Besov spaces. Electron. J. Differ. Equ. 2014, 2014, 1–14. [Google Scholar]
- Lin, F.; Zhang, P. On the hydrodynamic limit of Ginzburg-Landau wave vortices. Commun. Pure Appl. Math. 2002, 55, 831–856. [Google Scholar] [CrossRef] [Scilit]
- Biler, P.; Imbert, C.; Karch, G. Barenblatt profiles for a nonlocal porous medium equation. Comptes Rendus Math. 2011, 349, 641–645. [Google Scholar] [CrossRef] [Scilit]
- Blanchet, A.; Carrillo, J.A.; Masmoudi, N. Infinite time aggregation for the critical Patlak-Keller-Segel model in R2. Commun. Pure Appl. Math. 2008, 61, 1449–1481. [Google Scholar] [CrossRef]
- Topaz, C.M.; Bertozzi, A.L.; Lewis, M.A. A nonlocal continuum model for biological aggregation. Bull. Math. Biol. 2006, 68, 1601. [Google Scholar] [CrossRef] [Scilit]
- Li, D.; Rodrigo, J.L. Well-posedness and regularity of solutions of an aggregation equation. Rev. Mat. Iberoam. 2010, 26, 261–294. [Google Scholar] [CrossRef] [Scilit]
- Li, D.; Zhang, X. Global wellposedness and blowup of solutions to a nonlocal evolution problem with singular kernels. Commun. Pure Appl. Anal. 2010, 9, 1591. [Google Scholar] [CrossRef] [Scilit]
- Karch, G.; Suzuki, K. Blow-up versus global existence of solutions to aggregation equations. Appl. Math. 2011, 38, 243–258. [Google Scholar] [CrossRef] [Scilit]
- Laurent, T. Local and global existence for an aggregation equation. Commun. Partial. Differ. Equ. 2007, 32, 1941–1964. [Google Scholar] [CrossRef] [Scilit]
- Chen, Q.; Zhang, Z. Global well-posedness of the 2D critical dissipative quasi-geostrophic equation in the Triebel–Lizorkin spaces. Nonlinear Anal. Theory Methods Appl. 2007, 67, 1715–1725. [Google Scholar] [CrossRef] [Scilit]
- Wang, H.; Zhang, Z. A frequency localized maximum principle applied to the 2D quasi-geostrophic equation. Commun. Math. Phys. 2011, 301, 105–129. [Google Scholar] [CrossRef] [Scilit]
- Wu, G.; Zhang, Q. Global well-posedness of the aggregation equation with supercritical dissipation in Besov spaces. ZAMM J. Appl. Math. Mech./Z. Angew. Math. Mech. 2013, 93, 882–894. [Google Scholar] [CrossRef] [Scilit]
- Konieczny, P.; Yoneda, T. On dispersive effect of the Coriolis force for the stationary Navier–Stokes equations. J. Differ. Equ. 2011, 250, 3859–3873. [Google Scholar] [CrossRef] [Scilit]
- Iwabuchi, T.; Takada, R. Global well-posedness and ill-posedness for the Navier–Stokes equations with the Coriolis force in function spaces of Besov type. J. Funct. Anal. 2014, 267, 1321–1337. [Google Scholar] [CrossRef] [Scilit]
- Liu, Q.; Zhao, J. Global well-posedness for the generalized magneto-hydrodynamic equations in the critical Fourier–Herz spaces. J. Math. Anal. Appl. 2014, 420, 1301–1315. [Google Scholar] [CrossRef] [Scilit]
- Toumlilin, M. Global well-posedness and analyticity for generalized porous medium equation in critical Fourier-Besov-Morrey spaces. Open J. Math. Anal. 2019, 3, 71–80. [Google Scholar] [CrossRef] [Scilit]
- Orlicz, W. Über eine gewisse Klasse von Räumen vom Typus B. Bull. Int. Acad. Pol. Ser. A 1932, 8, 207–220. [Google Scholar]
- Musielak, J. Orlicz spaces and modular spaces. Lect. Notes Math. 1983, 1034, 1–216. [Google Scholar]
- Nakano, H. Topology and Linear Topological Spaces; Maruzen Company: Tokyo, Japan, 1951; Volume 3. [Google Scholar]
- Kováčik, O.; Rákosník, J. On spaces Lp(x) and Wk,p(x). Czechoslov. Math. J. 1991, 41, 592–618. [Google Scholar] [CrossRef] [Scilit]
- Cruz-Uribe, D. Operator on variable-LP spaces. In Seminar of Mathematical Analysis: Proceedings; Universidad de Sevilla: Sevilla, Spain, 2003; p. 147. [Google Scholar]
- Diening, L. Maximal Function on Generalized Lebesgue Spaces Lp(x). Math. Inequal. Appl. 2004, 7, 245–253. [Google Scholar]
- Ruzicka, M. Electrorheological Fluids: Modeling and Mathematical Theory; Springer Science & Business Media: Berlin/Heidelberg, Germany, 2000. [Google Scholar]
- Chen, Y.; Levine, S.; Rao, M. Variable exponent, linear growth functionals in image restoration. SIAM J. Appl. Math. 2006, 66, 1383–1406. [Google Scholar] [CrossRef] [Scilit]
- Fan, X. Global C1, α regularity for variable exponent elliptic equations in divergence form. J. Differ. Equ. 2007, 235, 397–417. [Google Scholar] [CrossRef] [Scilit]
- Almeida, A.; Hästö, P. Besov spaces with variable smoothness and integrability. J. Funct. Anal. 2010, 258, 1628–1655. [Google Scholar] [CrossRef] [Scilit]
- Ru, S.; Abidin, M.Z. Global well-posedness of the incompressible fractional Navier–Stokes equations in Fourier–Besov spaces with variable exponents. Comput. Math. Appl. 2019, 77, 1082–1090. [Google Scholar] [CrossRef] [Scilit]
- Abidin, M.Z.; Chen, J. Global well-posedness of the generalized rotating magnetohydrodynamics equations in variable exponent Fourier-Besov spaces. J. Appl. Anal. Comput. 2020. [Google Scholar] [CrossRef] [Scilit]
- Khan, A.A.; Bukhari, S.R.; Marin, M.; Ellahi, R. Effects of chemical reaction on third-grade MHD fluid flow under the influence of heat and mass transfer with variable reactive index. Heat Transf. Res. 2019, 50, 1061–1080. [Google Scholar] [CrossRef] [Scilit]
- Almeida, A.; Caetano, A. Variable exponent Besov—Morrey spaces. J. Fourier Anal. Appl. 2020, 26, 1–42. [Google Scholar] [CrossRef] [Scilit]
- Abidin, M.Z.; Chen, J. Global well-posedness for fractional Navier-Stokes equations in variable exponent Fourier-Besov-Morrey spaces. Acta Math. Sci. 2021, 41, 164–176. [Google Scholar] [CrossRef] [Scilit]
- Bahouri, H.; Chemin, J.Y.; Danchin, R. Fourier Analysis and Nonlinear Partial Differential Equations; Springer Science & Business Media: Berlin/Heidelberg, Germany, 2011; Volume 343. [Google Scholar]
- Bae, H.; Biswas, A.; Tadmor, E. Analyticity and decay estimates of the Navier–Stokes equations in critical Besov spaces. Arch. Ration. Mech. Anal. 2012, 205, 963–991. [Google Scholar] [CrossRef] [Scilit]
- Foias, C.; Temam, R. Gevrey class regularity for the solutions of the Navier-Stokes equations. J. Funct. Anal. 1989, 87, 359–369. [Google Scholar] [CrossRef] [Scilit]
- Ferreira, L.C.; Villamizar-Roa, E.J. Exponentially-stable steady flow and asymptotic behavior for the magnetohydrodynamic equations. Commun. Math. Sci. 2011, 9, 499–516. [Google Scholar] [CrossRef] [Scilit]
Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations. |
© 2021 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (http://creativecommons.org/licenses/by/4.0/).