Global well-posedness and optimal large-time behavior of strong solutions to the non-isentropic particle-fluid flows
Yanmin Mu, Dehua Wang

TL;DR
This paper establishes the global existence and optimal decay rates of strong solutions for three-dimensional non-isentropic particle-fluid flows, using new analytical techniques for coupled kinetic-fluid systems.
Contribution
It introduces a novel macro-micro decomposition and energy estimates to prove well-posedness and decay rates for the coupled Vlasov-Fokker-Planck and Navier-Stokes system.
Findings
Global well-posedness near equilibrium for non-isentropic flows
Algebraic decay rate in the whole space
Exponential decay rate in periodic domain
Abstract
In this paper, we study the three-dimensional non-isentropic compressible fluid-particle flows. The system involves coupling between the Vlasov-Fokker-Planck equation and the non-isentropic compressible Navier-Stokes equations through momentum and energy exchanges. For the initial data near the given equilibrium we prove the global well-posedness of strong solutions and obtain the optimal algebraic rate of convergence in the three-dimensional whole space. For the periodic domain the same global well-posedness result still holds while the convergence rate is exponential. %The proof is based on the new macro-micro decomposition and energy estimates. New ideas and techniques are developed to establish the well-posedness and large-time behavior. For the global well-posedness our methods are based on the new macro-micro decomposition and fine energy estimates, while the proofs of the optimal…
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Taxonomy
TopicsNavier-Stokes equation solutions · Gas Dynamics and Kinetic Theory · Computational Fluid Dynamics and Aerodynamics
Global well-posedness and optimal large-time behavior of strong solutions to the non-isentropic particle-fluid flows
Yanmin Mu
School of Applied Mathematics, Nanjing University of Finance & Economics, Nanjing 210046, China; and School of Mathematical Sciences and Mathematical Institute, Nanjing Normal University, Nanjing 210023, China
and
Dehua Wang
Department of Mathematics, University of Pittsburgh, Pittsburgh, PA 15260, USA.
Abstract.
In this paper, we study the three-dimensional non-isentropic compressible fluid-particle flows. The system involves coupling between the Vlasov-Fokker-Planck equation and the non-isentropic compressible Navier-Stokes equations through momentum and energy exchanges. For the initial data near the given equilibrium we prove the global well-posedness of strong solutions and obtain the optimal algebraic rate of convergence in the three-dimensional whole space. For the periodic domain the same global well-posedness result still holds while the convergence rate is exponential. New ideas and techniques are developed to establish the well-posedness and large-time behavior. For the global well-posedness our methods are based on the new macro-micro decomposition and fine energy estimates, while the proofs of the optimal large-time behavior rely on the Fourier analysis of the linearized Cauchy problem and the energy-spectrum method.
Key words and phrases:
Fluid-particle flows, non-isentropic Navier-Stokes equations, Vlasov-Fokker-Planck equation, global well-posedness, rate of convergence
2010 Mathematics Subject Classification:
35Q30, 76D03, 76D05, 76D07
1. Introduction
In this paper we study the global well-posedness and large time behavior of strong solutions for the three-dimensional fluid-particle flows, governed by the following Navier-Stokes equations of compressible non-isentropic fluids coupled with the Vlasov-Fokker-Planck equation of particles [3, 13, 33]:
[TABLE]
where, for denote the density, velocity, pressure, total energy, and temperature of the fluids, respectively; for denotes the density distribution function of particles in the phase space; the spatial domain is or (a periodic domain in ); and are the viscosity and heat conductivity constants. The total energy , internal energy , pressure , and temperature satisfy the following relations: where is the adiabatic constant and is constant. The Fokker-Planck operator is defined by
[TABLE]
which accounts for the friction force exerting on the particles by the surrounding fluids and the Brownian motion of the particles, that is, the friction force is assumed proportional to the relative velocity , and the Brownian motion depending on the temperature of the fluid induces diffusion with respect to the velocity variable. The two-phase flows have a disperse phase from a statistical viewpoint for particles, and a dense phase from continuum mechanics for fluids. The coupling terms depict the interaction between the disperse phase and the dense phase, and read
[TABLE]
indicating the momentum exchanges and the energy exchanges, respectively. For smooth solutions of the compressible non-isentropic Navier-Stokes-Vlasov-Fokker-Planck system (1.1)-(1.4), the temperature satisfies the following equation
[TABLE]
The fluid-particle flows have a wide range of applications from dynamics of sprays, combustion, pollution processes, waste water treatment, to biomedical flows; see [2, 3, 4, 7, 10, 13, 19, 33, 39, 40, 44, 43] and the references therein for the discussions of applications and modeling issues. We remark that in the momentum equation (1.2), we only keep the shear viscosity and skip the bulk viscosity term for the sake of simplicity of presentations, since the bulk viscosity will not add significant difficulty and we shall focus on the complexity caused by the heat conductivity and the Fokker-Planck operator.
The purpose of this paper is to establish the well-posedness of the system (1.1)-(1.4) near a global Maxwellian. Without loss of generality, we normalize the global Maxwellian as
[TABLE]
For the Cauchy problem with the initial data
[TABLE]
we shall prove the global existence and uniqueness as well as the large-time behavior of the strong solution for the unknowns near the global equilibrium state .
There exist many different systems describing the kinetic-fluid for the physical regimes under consideration, such as the compressible or incompressible fluids, viscous or inviscid fluids, with or without thermal diffusion acting on the particles and so on. The mathematical analysis of such mathematical models is very difficult due to the nonlinear coupling of partial differential equations of different types.
We now give a brief review of works in literature on some kinetic-fluid models related to our system (1.1)-(1.4). The global existence of classical and weak solutions for the incompressible fluid-particle flows have been studied in many papers, see [28, 9, 45, 20, 14, 15, 6, 21, 22, 30, 31, 32, 42] and their references. For the compressible fluid, when the drag force exerted by the surrounding fluid is proportional to the relative velocity , the global weak solution and the asymptotic analysis were obtained in Mellet and Vasseur [36, 37], the global classical solutions near an equilibrium and exponential decay were obtained in Chae, Kang, and Lee [16], and the dissipative quantities, equilibria and their stability were studied in Carrillo and Goudon [12]. When the drag force depends on both the relative velocity and the density of the fluid, the local existence of classical solutions to the Euler-Vlasov system was obtained in Baranger and Desvillettes [5], and global strong solution near an equilibrium and large-time behavior to the isentropic compressible Navier-Stokes-Vlasov-Fokker-Planck system were established in Li, Mu and Wang [29].
To the best of our knowledge, there is few rigorous mathematical results concerning the case of non-isentropic kinetic-fluid equations. In[8, 23], some numerical analysis on the kinetic-fluid models with energy exchange involved was presented. In this paper, we shall address two problems for the non-isentropic system (1.1)-(1.4): (1) the global existence of strong solution in the framework of small perturbation of an equilibrium, (2) the asymptotic behavior to the given Maxwellian equilibrium. As far as we know, this is the first rigorous mathematical work which deals with the energy exchange between the disperse phase and the dense phase.
The perturbation of solutions to the Navier-Stokes-Vlasov-Fokker-Planck system (1.1)-(1.5) near the global equilibrium state satisfies the system (2.1)-(2.5). To prove the global existence of strong solution to the problem (2.1)-(2.5), we mainly use the fine energy estimates together with the local existence of strong solutions and continuum argument. It is well known that under the condition of a smallness condition on the perturbation, using fine energy estimates will lead to the global existence of strong solutions. This approach is in the spirit of the papers [26, 27, 34, 35] for the Boltzmann, Landau and Navier-Stokes equations.
The fact that the unknowns of the Navier-Stokes-Vlasov-Fokker-Planck system do not depend on the same set of variables yields many technical difficulties, and the proof requires sharp estimates to the kinetic equation and the fluid equations. We shall adopt the techniques in the works of Guo [24, 25, 26, 27] where the full coercivity of the linearized collision operator of the Boltzmann equation are crucial to obtain the global classical solution of the nonlinear kinetic equations near an equilibrium. In brief, its solution to the Boltzmann equation is decomposed into macro and micro components, the dissipative effect through the microscopic H-theorem can be obtained for the microscopic component, which is important in order to use the energy method. The macro-micro decomposition is gained with the help of spectral structure of the linearized collision operator of the Boltzmann equation. Here, the linear Fokker-Planck operator and the collision operator of the Boltzmann equation have certain features in common, thus we can use the idea of the macro-micro decomposition of depending on the spectral structure of the operator. However, our Navier-Stokes-Vlasov-Fokker-Planck system is quite different from the pure Boltzmann equation or the coupled Boltzmann equations, therefore several new difficulties arise as described below.
For the Boltzmann equation, as mentioned in [30], the collision particles have the same mass and momentum as well as kinetic energy. As we mentioned earlier, there exists momentum and energy exchange between particles and the surrounding fluids. As a result, some linear terms appear in the kinetic equation and some coupling terms appear in the fluid equations, which leads to some new difficulties. Because we want to establish the global well-posesdness in the case of small perturbation near an equilibrium, naturally these terms may be very small, but throughout our analysis, the main difficulties arise from these linear terms which are worse than the nonlinear terms. In order to handle these linear terms, we need certain dissipation effect and expect it from the linear Fokker-Planck operator. Unfortunately, as in Section 2.4 from the macro-micro decomposition only by the null space of , we know that the dissipation induced by the linear Focker-Planck operator is only partial, which is not enough to control new linear terms, we eventually find a new macro-micro decomposition, and achieve the desired dissipative effect under the new decomposition. Achieving such control is one of the main new contributions of the present paper.
Due to the interaction between the particles and the fluids, no existing results on the Vlasov-Fokker-Planck system yields the regularity of . Therefore, the new mixed estimates involving the derivatives of the particle velocity variable are necessary.
To obtain the uniform estimates, the macroscopic equations of the particles, i.e., (3.16)-(3.20), are important to achieve that the macroscopic part is bounded by its microscopic part due to (2.8). The macroscopic equations behave like elliptic so that it is straightforward to estimate norms of their derivatives for . In periodic domain, norms of can be estimated by the Poincaré inequality. This leads to different decay rates in the whole space and the periodic domain as time tends to infinity.
In order to achieve the optimal decay rate in the whole space, the main ideas are based on the Fourier analysis to the linearized Cauchy problem of (2.1)-(2.4) and the energy-spectrum method as in [14, 16, 18]. Our main difficulties arise from the strong coupling terms in the system (2.1)-(2.4), namely the nonlinear terms, that is because the Fourier transform of the product of functions is a convolution, which is difficult in our global time-decay analysis. Selecting subtly the functions in (4.2) as the nonhomogeneous source plays an important role to overcome this difficulty.
With the above new ideas and techniques, we shall be able to establish the global existence of strong solutions and optimal decay rates for the compressible non-isentropic Navier-Stokes-Vlasov-Fokker-Planck both in the whole space and in periodic domains. We remark that the methods introduced in the present work may be applied for other related non-sentropic kinetic-fluid models such as the drag force exerted by the fluid depending on the density of the fluid.
We organize the rest of the paper as follows. In Section 2, we reformulate the system (1.1)-(1.5) near the global equilibrium state, present the coercivity estimate of the linear part and the macro-micro decomposition, and state our main results. In Section 3, we first derive the uniform-in-time a priori estimates and then establish the existence of global strong solution. In Section 4, we prove the rate of convergence of solutions. In Section 5, we adapt our proof to the periodic domain case.
2. Preliminaries and main results
In this section, we reformulate the system (1.1)-(1.5) near the global equilibrium state, present the coercivity estimate of the linear part and the macro-micro decomposition, and state our main results.
2.1. Reformulation
We consider the solution of the system (1.1)-(1.5) near the global equilibrium , i.e.,
[TABLE]
We shall take the constants to be one in this paper since their values do not play a role in the analysis. From the sysem (1.1)-(1.5), the perturbations satisfy the following equations:
[TABLE]
Correspondingly, the initial data becomes
[TABLE]
where is a small perturbation near the above equilibrium.
In (2.1)-(2.4), we denote the linearized Fokker-Planck operator by
[TABLE]
and are defined by
[TABLE]
2.2. Notations
For , is the norm defined by
[TABLE]
is the inner product of the space , namely,
[TABLE]
In case of no confusion, we denote by the norm of or for simplicity. Define
[TABLE]
For , we also denote
[TABLE]
The norm is defined by
[TABLE]
for f=f(x,v),\big{(}\rho,u,\theta\big{)}=\big{(}\rho(x),u(x),\theta(x)\big{)} and .
For an integrable function , its Fourier transform is defined by
[TABLE]
for
For multi-indices and , we denote by
[TABLE]
the partial derivatives with respect to and . The length of and are defined as and . We shall use the following norms:
[TABLE]
We shall use the letter to denote a generic positive (generally large) constant, a generic positive (generally small) constant; and use the symbol to denote the relation for some constant .
2.3. Coercivity estimate of the linear part in (2.1)
In this subsection, we first apply the similar coercivity estimate of the linear collision operator of Boltzmann equation to the linearized Fokker-Planck operator by spectrum analysis, that is, (2.6) holds. Then, we find that the dissipative effect of is partial and new difficulties have arisen.
In (2.1), we denote the important linear part by
[TABLE]
It is well-known from [1] that the classical linearized Fokker-Planck operator enjoys the following dissipative properties:
- (1)
The null space of is the one dimensional space
[TABLE]
- (2)
Define the projection in to the null space by
[TABLE]
Using the integration by parts, we have
[TABLE]
- (3)
There exists a constant , such that the following coercivity estimate holds:
[TABLE]
We hope that the linear part also has a similar coercivity estimate. However, we notice that it is straightforward to make estimates on as
[TABLE]
and from (2.6), one gets
[TABLE]
It is difficult to decide which of the two terms on the right hand side of the above inequalities is bigger. To this end, we decompose into the macroscopic component and the microscopic component, however, the dissipative effect for , i.e., (2.6), is not enough to deal with the linear part . It is nontrivial to get a coercivity estimate on the linear part . In order to control , we must extract part of dissipation of corresponding to the momentum component and the energy component respectively.
2.4. New Macro-micro decomposition
In this subsection, we are concerned with the macro-micro decomposition of the solution into its macroscopic (fluid dynamic) and microscopic (kinetic) components. In view of the difficulties mentioned above, we want to extract a better dissipative effect, which is hard and achieved based on the inspiration from the idea of spectrum analysis of the linear operator. In short, since the coupling terms in our system involve the momentum exchange and the energy exchange, we expand the original null space to the new space below. Then, by the macroscopic and microscopic projection on the new space, we can get the new macro-micro decomposition of the solution, as described below.
Denote the linear space by
[TABLE]
and it has the following set of orthogonal basis
[TABLE]
Define the projector operator by
[TABLE]
We also introduce the projector respectively by
[TABLE]
so the projector can be also written as
[TABLE]
As usual, for fixed can be uniquely decomposed as
[TABLE]
where is called the macroscopic component of , while is called the corresponding microscopic component. Interestingly, our new decomposition is formally the same as that of the linearized collision operator of the Boltzmann equation [41], but our decomposition here comes not only from the spectral analysis of the linearized Fokker-Planck operator , but also from the coupling term involving momentum and energy exchanges. Therefore, we further reveal the internal relations and differences between the particle-fluid system and the Boltzmann equation or coupled Boltzmann equation.
According to new decomposition (2.7), the linearized Fokker-Planck operator satisfies the following additional properties besides the above properties (1)-(3):
- (4)
can be written as
[TABLE]
- (5)
There exists a constant , such that
[TABLE]
2.5. Main results
We now state our main results. The first result is the global existence of classical solutions with small initial data and optimal algebraic rate of decay in the whole space.
Theorem 2.1**.**
Let and be the initial data such that and there exists , . Then the Cauchy problem (2.1)-(2.5) admits a unique global solution satisfying and
[TABLE]
for some constant . Moreover, if we further assume that
[TABLE]
then
[TABLE]
for some constant and all
Remark 2.1**.**
Here the algebraic rate of decay in (2.10) is optimal in sense that this rate coincides with that of the corresponding linear system.
The second result is concerned with the periodic spatial domain. Compared with the case of the whole space, here we know that the Poincaré inequality holds, the exponential convergence rate is obtained.
Theorem 2.2**.**
Let and be the initial data such that there exists , , and
[TABLE]
where
[TABLE]
Then, the Cauchy problem (2.1)-(2.5) admits a unique global solution satisfying and
[TABLE]
with some constant, for all
In the rest of this paper, we shall omit the integral domain or in the integrals for simplicity.
3. Global existence of classical solutions in the whole space
In this section, we shall establish the global existence of classical solutions to the problem (2.1)-(2.5) in the whole space . We first obtain the uniform a priori estimates. Then we construct the unique local solution by an iteration process, and obtain the global solution by the continuum argument.
3.1. A priori estimates
In this subsection, we will show the uniform-in-time a priori estimates in the space or . We assume that is a classical solution to the Cauchy problem (2.1)-(2.5) for with a fixed , and
[TABLE]
with sufficiently small constant.
The following lemma in [14] is useful for the forthcoming estimates.
Lemma 3.1** (see [14]).**
There exists a constant such that for any and any multi-index with ,
[TABLE]
The a priori estimates will be proved in the next two subsections, one for the pure -variable part, and one for the mixed derivative part.
3.1.1. Energy estimates in the -variable
Proposition 3.1**.**
For classical solution of the system (2.1)-(2.5), we have
[TABLE]
for all with any
Proof.
Multiplying (2.1)-(2.4) by respectively, then taking integration and summation, we finally get
[TABLE]
By (2.8), we have
[TABLE]
Next, we make estimates of the terms on the right hand side of the equality (3.6).
(1) The estimates for are obtained as follows.
We first notice that
[TABLE]
According to the macro-micro decomposition (2.7), we get
[TABLE]
and meanwhile by Hölder and Sobolev inequalities, one gets
[TABLE]
Thus, we eventually have
[TABLE]
(2) The estimates for are obtained as follows.
First, the term can be rewritten as
[TABLE]
Thus, the following estimates hold
[TABLE]
(3) For the estimates of all the remaining terms, using Hölder and Sobolev inequalities as well as Lemma 3.1, we easily get
[TABLE]
Substituting all the above estimates (3.7), (3.8), (3.9) into (3.6) and using (3.1), we obtain (3.5). ∎
Proposition 3.2**.**
For smooth solutions of the problem (2.1)-(2.5), we have
[TABLE]
for all with any
Proof.
Here, we follow the similar argument [29, Proposition 4.2]. Applying differentiation to (2.1)-(2.4) yields
[TABLE]
where denotes the commutator for two operators and Now, multiplying (3.11)-(3.14) by , respectively, then taking integration and summation, we obtain
[TABLE]
where is constant depending only on and .
We need to estimate each term on the right hand side of (3.15). Firstly
[TABLE]
where we have used the following fact
[TABLE]
and the similar estimate holds for .
Using Hölder, Sobolev and Young inequalities, we get the following bounds
[TABLE]
[TABLE]
[TABLE]
with a small constant, and
[TABLE]
[TABLE]
Substituting all the above estimates on into (3.15) and taking summation over , we complete (3.10). ∎
To estimate the energy dissipation of , namely, , we need to deduce the equations satisfied by . We first introduce the moment functional and the energy functional as
[TABLE]
for any . It is easy to verify that the equations of is as follows
[TABLE]
where are defined by
[TABLE]
In fact, multiplying (2.1) by respectively and then integrating with respect to velocity over , we deduce that (3.16)-(3.18) hold .
In order to get(3.19)-(3.20), we can rewrite (2.1) as
[TABLE]
Applying to (3.21) and combining (3.16), (3.18), we get the equation (3.19). Similarly, applying to (3.21) and combing (3.17), we can obtain the equation (3.20).
Define a temporal functional
[TABLE]
We have the following estimate.
Proposition 3.3**.**
For classical solution of the system (2.1)-(2.5), we have
[TABLE]
for all with any
Proof.
We divide this proof into three steps.
Step 1: It follows from (3.19) that
[TABLE]
Using (3.17), Lemma 3.1 and Young inequality, we get
[TABLE]
with sufficiently small.
The estimate of the final term on the right hand side of (3.24) is as follows,
[TABLE]
Here, we have used the following estimates
[TABLE]
Notice that
[TABLE]
By the above equality, we substitute the above estimates into (3.24), and then the sum over is obtained as
[TABLE]
with sufficiently small.
Step 2: According to (3.20), through direct calculation, we obtain
[TABLE]
By means of (3.18) and direct calculation, one gets
[TABLE]
For the remaining terms on the right hand side of (3.26), we have
[TABLE]
Thus, substituting the above estimates into (3.26), and then taking summation over , we obtain
[TABLE]
with sufficiently small.
Step 3: Making full use of the equations (3.17) and (3.20), by direct calculations, we obtain the following equality
[TABLE]
Using (3.16), one has
[TABLE]
For other terms, the following estimate is obtained:
[TABLE]
Thus, substituting the above estimates into (3.28), and then taking summation over , we have
[TABLE]
Integrating the estimates of the above three parts (3.25), (3.27) and (3.29), and applying the definition of , we conclude that (3.23) holds. ∎
Proposition 3.4**.**
For classical solution of the system (2.1)-(2.5), we have
[TABLE]
for all with any
Proof.
Applying to (2.3), and carrying a direct calculation, we achieve
[TABLE]
For , using (2.2), Hölder, Sobolev and Young inequalities yields
[TABLE]
With the help of (3.1), substituting the above estimates into (3.31), we obtain (3.30). ∎
Now let us define and by
[TABLE]
where denote the temporal energy functional and the corresponding dissipation rate respectively, and are sufficiently small constants and will be determined later. Reorganizing the above estimates in Propositions 3.1-3.4, we obtain
[TABLE]
3.1.2. Energy estimates for mixed space-velocity derivatives
In this subsection, we shall deal with the energy estimates for the mixed space-velocity derivatives of , i.e., . Since for any and , thus, it is enough to estimate below.
First,we have the following facts
[TABLE]
then, using to the equality (2.1), one gets
[TABLE]
Proposition 3.5**.**
Let . Let is a smooth solution of the system(2.1)-(2.5), we have
[TABLE]
for all with any Here is the characteristic function on the set .
Proof.
This proof is based on some ideas of [17, Lemma 4.3].
Fix . let and satisfy and , For (3.33), by standard energy estimate, we get
[TABLE]
with
[TABLE]
Here the fact has been used.
Now we make estimates for each term in (3.35) as the following
[TABLE]
We estimate the term as
[TABLE]
Substituting all the above estimates into (3.35) and selecting small enough, we deduce that (3.34) holds. ∎
Remark 3.1**.**
Choosing some suitable constants together with the above lemma, we have
[TABLE]
Now, let us define and as follows
[TABLE]
Then the total energy functional and the dissipation rate can be defined by
[TABLE]
where is very small and will be determined later.
According to the inequalities (3.32), (3.36) and (3.1), we have
[TABLE]
Thus, as long as is sufficiently small, the integration of (3.37) with respect to time gives
[TABLE]
for all . In addition, (3.1) can be proved by choosing sufficiently small.
3.2. Global Existence
In this subsection, we will show that there exists a unique global-in-time solution to the problem (2.1)-(2.5). The proof is based on the uniform energy estimates for the iteration sequence of approximate solutions. The sequence satisfies the following system:
[TABLE]
[TABLE]
[TABLE]
[TABLE]
where , and is the starting value of iteration.
We try to find solutions in the following function space
[TABLE]
We now state the local existence theorem.
Theorem 3.1**.**
There exist and such that if with and , then for each , is well-defined with
[TABLE]
Further, we obtain:
- (1)
* is a Cauchy sequence in the Banach space ,* 2. (2)
let be the limit function, and then , 3. (3)
* satisfies the system (2.1)-(2.5),* 4. (4)
* is the unique solution of (2.1)-(2.5) in .*
Proof.
Let be a constant which will be fixed later. For simplicity, without loss of generality are assumed to be smooth enough, if not, we can consider the regularized iterative system as
[TABLE]
[TABLE]
[TABLE]
[TABLE]
[TABLE]
for any with a smooth approximation of and pass to the limit by letting
Applying with to the equation (3.39), multiplying the result by and then taking integration over , one has
[TABLE]
Notice that
[TABLE]
By adding to the inequality (3.52), we get the sum on ,
[TABLE]
Similar argument gives, for any ,
[TABLE]
Next, from [34], the system (3.40)-(3.41) has a unique solution such that , and
[TABLE]
[TABLE]
Now we estimate . Applying to the system (3.40)- (3.42), multiplying the results by , respectively, and then taking integration and summation, we get
[TABLE]
Adding up (3.53) and (3.54) gives
[TABLE]
Using induction, we may assume and for some with
[TABLE]
Integrating (3.55) over yields
[TABLE]
It is easy to obtain that for ,
[TABLE]
Choosing satisfying , and small enough, one gains
[TABLE]
By the equation (3.39), satisfies the following equation,
[TABLE]
on the basis of the maximum principle, one achieves
[TABLE]
Now we show that is continuous over .
Actually, similar to the proof of (3.53), the following inequality holds
[TABLE]
Moreover, is integrable over . Thus, (3.51) is true for , namely it follows that (3.51) holds for any .
By straightforward calculation, satisfies the following system:
[TABLE]
Similarly to (3.55), we obtain
[TABLE]
where is a constant that depends on , , , and . Due to , and small enough, according to (3.56), we know that
[TABLE]
is also small enough. Therefore, there exists such that
[TABLE]
According to (3.58), we conclude that is a Cauchy sequence in the Banach space C\big{(}[0,T^{*}],H^{3}(\mathbb{R}^{3}\times\mathbb{R}^{3})\big{)}\times\Big{(}C\big{(}[0,T^{*}],H^{3}(\mathbb{R}^{3})\big{)}\Big{)}^{3}, so we denote the limit function of this sequence by and then satisfies the system (2.1)-(2.5) by letting . The fact that and the Sobolev embedding theorem yields that
[TABLE]
Similar argument to (3.57) yields that f\in C\big{(}[0,T^{*}],H^{3}(\mathbb{R}^{3}\times\mathbb{R}^{3})\big{)}. Namely, we obtain that .
Finally, let be another solution to the Cauchy problem (2.1)-(2.5). Using similar process to (3.58),it follows that
[TABLE]
for . So it is easy to conclude that ,i.e uniqueness holds. ∎
Proof of Theorem 2.1.
By , there exists , such that if , one gets . Next, due to Theorem 3.1, the uniform priori estimate (3.38) holds for the local solution. Finally, the standard bootstrap arguments, as in [17, 24, 34] eventually conclude that the global existence and uniqueness part in Theorem 2.1 hold. ∎
4. Large time behavior
In this section, our main concern is the optimal time-decay rates of global solutions to the problem (2.1)-(2.5). First, we shall study the time-decay of the solution to the linearized Cauchy equations with a nonhomogeneous source, with the help of the Fourier analysis, we can obtain the algebraic decay when time tends to infinity, that is Theorem 4.1 holds. Then, decomposing the nonlinear terms subtly and choosing the appropriate functions as the nonhomogeneous source, together with Theorem 4.1 and the energy-spectrum method developed in [18], we finally conclude the time-decay rate (2.10). To this end, we assume that all conditions in Theorem 2.1 hold, and let be the solution to the system (2.1)-(2.5).
We first consider the linearized Cauchy equations with a nonhomogeneous source, namely,
[TABLE]
Here, has the following form
[TABLE]
with and , meanwhile we suppose that
[TABLE]
for all .
For the linearized problem (4.1), we easily conclude that it is well-posed in , i.e., the following lemma is true.
Lemma 4.1**.**
There is a well-defined linear semigroup such that for any given , is the unique distributional solution to (4.1) with . Further, for any , then there is a unique distributional solution to (4.1) such that
[TABLE]
Proof.
Similar argument as the local existence theorem can give the well-posedness part, thus we do not repeat here, and the variation of constants formula (4.3) is again true by a direct computation. ∎
We first quote two lemmas of [14] for later proofs.
Lemma 4.2** ([14]).**
Given any and
[TABLE]
for all
Lemma 4.3** ([14]).**
Let and with For , define . Then, there exists a constant such that for any ,
[TABLE]
Theorem 4.1**.**
Let and . For any with and ,
[TABLE]
and
[TABLE]
hold for , where C is a positive constant depending only on and
[TABLE]
Proof.
Applying the Fourier transform to (4.1) in , we obtain
[TABLE]
By taking the inner product of the equations in (4.6) with the conjugate of and integrating in , its real part gives
[TABLE]
here, on the basis of the assumptions (4.2), we can calculate
[TABLE]
Similarly, from the last three equations in (4.1) we have
[TABLE]
Then, combining these estimates, using the coercivity of and the Cauchy-Schwarz inequality, we show
[TABLE]
Next, we consider the estimates on . Similar to (3.16)-(3.20), for the system (4.1), one has
[TABLE]
where is still expressed as
[TABLE]
In the same way, taking the Fourier transform in , we obtain
[TABLE]
By adopting the similar calculation method as in Proposition 3.3, we can conclude the following inequalities:
[TABLE]
Choosing small sufficiently, and setting as
[TABLE]
one has
[TABLE]
Similarly, choosing small sufficiently, and setting as
[TABLE]
then we have
[TABLE]
Now, we define the functional by
[TABLE]
where a small constant is chosen such that
[TABLE]
Finally, the linear combination gives
[TABLE]
which further implies
[TABLE]
With the help of Gronwall’s inequality, we have
[TABLE]
In order to obtain the desired time-decay estimates (4.4) and (4.5), the same proof can be adopted as in [17, Theorem 3.1], and we omit the details. ∎
Proof of the large time behavior in Theorem 2.1.
By the definitions of in the previous section, it follows that
[TABLE]
From (3.37), one obtains
[TABLE]
which, together with (4.9), yields
[TABLE]
According to Gronwall inequality, it follows that
[TABLE]
Next, the system (2.1)-(2.4) can be written as
[TABLE]
with
[TABLE]
where can be decomposed as
[TABLE]
with
[TABLE]
Therefore, \big{(}f(t),\rho(t),u(t),\theta(t)\big{)} can be rewritten as the sum of six terms
[TABLE]
Applying directly (4.4) to , one has
[TABLE]
With the help of Hölder and Sobolev inequalities, using (4.5) to , we deduce
[TABLE]
Similarly, for , by means of Hölder and Sobolev inequalities, we can apply (4.4) to them to compute
[TABLE]
Therefore, it follows that
[TABLE]
Define
[TABLE]
Using (4.11) and that are non-increasing in time, with the aid of Lemma 4.2, we obtain
[TABLE]
with . From this, can be further estimated as
[TABLE]
Substituting this inequality into the right hand side of (4.10), and multiplying the resulting inequality by , we obtain
[TABLE]
Thus, by the definition (4.12), we further obtain
[TABLE]
Since and are small enough, and , one has
[TABLE]
for all with , due to Lemma 4.3, which implies
[TABLE]
namely,
[TABLE]
The proof of Theorem 2.1 is completed.
∎
5. The periodic case
In this section we deal with the spatial periodic domain . A straightforward calculation can deduce the conservation laws as follows
[TABLE]
and by the assumption of Theorem 2.2, we obtain
[TABLE]
for all
Now, we give a brief proof of Theorem 2.2.
Proof of Theorem 2.2.
Here, we only give the proof of the global a priori estimates. It follows from Poincaré inequality and the conservation laws (5.1),
[TABLE]
Let the energy functionals and the corresponding dissipation rate functional be defined in the same way as in the case . Similarly, we conclude that
[TABLE]
Define
[TABLE]
where are sufficiently small. Notice
[TABLE]
Combining (5.2), (5.3) and (5.5) together, we conclude that
[TABLE]
Define the functionals as
[TABLE]
where is sufficiently small. (5.6) together with (5.8) yields that
[TABLE]
Based on small enough and uniformly in time, and , it follows that
[TABLE]
for all By Gronwall’s inequality, it is easy to obtain the exponential decay, and we finish the proof of Theorem 2.2. ∎
Acknowledgments
Y. Mu was partially supported by NSFC (Grant No.11701268), Natural Science Foundation of Jiangsu Province of China (BK20171040) and Chinese Postdoctoral Science Foundation (2018M642277). D. Wang’s research was supported in part by the NSF grants DMS-1312800 and DMS-1613213.
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