Quantitative error estimates for the large friction limit of Vlasov equation with nonlocal forces
Jos\'e A. Carrillo, Young-Pil Choi

TL;DR
This paper provides a rigorous quantitative analysis of the large friction limit of a Vlasov equation with nonlocal forces, connecting kinetic models to continuum aggregation equations using Wasserstein distances.
Contribution
It introduces an intermediate pressureless Euler system to accurately estimate the error between kinetic and continuum models in the large friction regime.
Findings
Quantitative error bounds between kinetic and continuum models.
Use of Wasserstein distance for error estimation.
Extension of previous results to nonlocal interaction forces.
Abstract
We study an asymptotic limit of Vlasov type equation with nonlocal interaction forces where the friction terms are dominant. We provide a quantitative estimate of this large friction limit from the kinetic equation to a continuity type equation with a nonlocal velocity field, the so-called aggregation equation, by employing -Wasserstein distance. By introducing an intermediate system, given by the pressureless Euler equations with nonlocal forces, we can quantify the error between the spatial densities of the kinetic equation and the pressureless Euler system by means of relative entropy type arguments combined with the -Wasserstein distance. This together with the quantitative error estimate between the pressureless Euler system and the aggregation equation in -Wasserstein distance in [Commun. Math. Phys, 365, (2019), 329--361] establishes the quantitative bounds on the error…
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Quantitative error estimates for the large friction limit of Vlasov equation with nonlocal forces
José A. Carrillo
Department of Mathematics
Imperial College London, London SW7 2AZ, United Kingdom
and
Young-Pil Choi
Department of Mathematics
Yonsei University, Seoul 03722, Republic of Korea
Abstract.
We study an asymptotic limit of Vlasov type equation with nonlocal interaction forces where the friction terms are dominant. We provide a quantitative estimate of this large friction limit from the kinetic equation to a continuity type equation with a nonlocal velocity field, the so-called aggregation equation, by employing -Wasserstein distance. By introducing an intermediate system, given by the pressureless Euler equations with nonlocal forces, we can quantify the error between the spatial densities of the kinetic equation and the pressureless Euler system by means of relative entropy type arguments combined with the -Wasserstein distance. This together with the quantitative error estimate between the pressureless Euler system and the aggregation equation in -Wasserstein distance in [Commun. Math. Phys, 365, (2019), 329–361] establishes the quantitative bounds on the error between the kinetic equation and the aggregation equation.
Key words and phrases:
hydrodynamic limit, large friction limit, relative entropy, pressureless Euler system, Wasserstein distance, aggregation equation, kinetic swarming models.
2010 Mathematics Subject Classification:
primary 35Q70, 35Q83; secondary 35B25, 35Q35, 35Q92.
1. Introduction
Let be the particle distribution function at and at time for the following kinetic equation:
[TABLE]
subject to the initial data
[TABLE]
where is the local particle velocity, i.e.,
[TABLE]
and are the confinement and the interaction potentials, respectively. In (1.1), the first two terms take into account the free transport of the particles, and the third term consists of linear damping with a strength and the particle confinement and interaction forces in position due to the potentials with strength . The right hand side of (1.1) is the local alignment force for particles as introduced in [22] for swarming models. In fact, it can also be understood as the localized version of the nonlinear damping term introduced in [28] as a suitable normalization of the Cucker-Smale model [16]. Notice that this alignment term is also a nonlinear damping relaxation towards the local velocity used in classical kinetic theory [10, 32]. Throughout this paper, we assume that is a probability density, i.e., for , since the total mass is preserved in time.
In the current work, we are interested in the asymptotic analysis of (1.1) when considering singular parameters. More specifically, we deal with the large friction limit to a continuity type equation from the kinetic equation (1.1) when the parameters , and get large enough. Computing the moments on the kinetic equation (1.1), we find that the local density and local velocity satisfy
[TABLE]
As usual, the moment system is not closed. By letting the friction of the equation (1.1) very strong, i.e., , for instance, with as , then at the formal level, we find
[TABLE]
and thus,
[TABLE]
is the element in its kernel with the initial monokinetic distribution .
Those relations provide that the density satisfies the following continuity type equation with a nonlocal velocity field, the so-called aggregation equation, see for instance [3, 4, 6] and the references therein,
[TABLE]
The large friction limit has been considered in [21], where the macroscopic limit of a Vlasov type equation with friction is studied by using a PDE approach, and later the restrictions on the functional spaces for the solutions and the conditions for interaction potentials are relaxed in [17] by employing PDE analysis and the method of characteristics. More recently, these results have been extended in [18] for more general Vlasov type equations; Vlasov type equations with nonlocal interaction and nonlocal velocity alignment forces. However, all of these results in [17, 18, 21] are based on compactness arguments, and to our best knowledge, quantitative estimates for the large friction limit have not yet been obtained. The large friction limit has received a lot of attention at the hydrodynamic level by the conservation laws community, see for instance [15, 27, 26, 20, 25], but due to their inherent difficulties, it has been elusive at the kinetic level.
The main purpose of this work is to render the above formal limit to the nonlocal aggregation equation completely rigorous with quantitative bounds. Our strategy of the proof uses an intermediate system to divide the error estimates as depicted in Figure 1.
We first fix and with and take . We denote by the solution to the associated kinetic equation (1.1). We then introduce an intermediate system, given by the pressureless Euler equations with nonlocal interactions, between the kinetic equation (1.1) and the limiting equation (1.2):
[TABLE]
In order to estimate the error between two solutions and to (1.1) and (1.3), respectively, where
[TABLE]
we use the Wasserstein distance which is defined by
[TABLE]
for and , where is the set of all probability measures on with first and second marginals and and bounded -moments, respectively. We refer to [1, 31] for discussions of various topics related to the Wasserstein distance.
Employing the -Wasserstein distance, we first obtain the quantitative estimate for with the aid of the relative entropy argument. It is worth mentioning that the entropy for the system (1.3) is not strictly convex with respect to due to the absence of pressure in the system, see Section 2.1 for more details. Thus the relative entropy estimate is not enough to provide the error estimates between the spatial density and the density . We also want to emphasize that the relative entropy estimate is even not closed due to the nonlinearity and nonlocality of the interaction term . We provide a new inequality which gives a remarkable relation between the -Wasserstein distance and the relative entropy, see Lemma 2.2. Using that new observation together with combining the relative entropy estimate and the -Wasserstein distance between the solutions in a hypocoercivity type argument, we have the quantitative error estimate for the vertical part of the diagram in Figure 1. Let us point out that in order to make this step rigorous, we need to work with strong solutions to the pressureless Euler system (1.3) for two reasons. On one hand, strong solutions are needed for making sense of the integration by parts required for the relative entropy argument. On the other hand, some regularity on the velocity field, the boundedness of the spatial derivatives of the velocity field uniformly in , is needed in order to control terms appearing due to the time derivatives of and the relative entropy.
We finally remark that the closest result in the literature to ours is due to Figalli and Kang in [19]. It concerns with the vertical part of the diagram in Figure 1 for a related system without interaction forces but Cucker-Smale alignment terms. Even if they already combined the -Wasserstein distance and the relative entropy between and , they did not take full advantage of the -Wasserstein distance, see Remark 2.3 for more details. This is our main contribution in this step.
The final step, corresponding to the bottom part of the diagram in Figure 1, is inspired on a recent work of part of the authors [7]. Actually, we can estimate the error between the solutions and to (1.3) and (1.2), respectively, in the -Wasserstein distance again. Here, it is again crucial to use the boundedness of the spatial derivatives of the velocity field uniformly in . Combining the above arguments, we finally conclude the main result of our work: the quantitative error estimate between two solutions and to the equations (1.1) and (1.2), respectively, in the -Wasserstein distance.
Before writing our main result, we remind the reader of a well known estimate for the total energy of the kinetic equation (1.1). For this, we define the total energy and the associated dissipations and as follows:
[TABLE]
[TABLE]
respectively. Suppose that is a solution of (1.1) with sufficient integrability, then it is straightforward to check that
[TABLE]
Notice that weak solutions may only satisfy an inequality in the above relation that is enough for our purposes.
In order to control the velocity field for the intermediate pressureless Euler equations (1.3), we assume that the confinement potential and the interaction potential satisfy:
- (H)
The confinement potential , and the interaction potential satisfies , , and with
[TABLE]
We are now in position to state the main result of this work.
Theorem 1.1**.**
Assume that initial data satisfy
[TABLE]
for all . Let be a solution to the equation (1.1) with , with up to time , such that satisfying the energy inequality (1.5) with initial data . Let be a solution of (1.2) up to the time , such that with initial data satisfying
[TABLE]
Suppose that holds. Then, for small enough, we have the following quantitative bound:
[TABLE]
where and is independent of .
Remark 1.1**.**
As mentioned above, our strategy consists in using (1.3) as intermediate system and compare the errors from the kinetic equation (1.1) to the pressureless Euler equations (1.3) and from (1.3) to the aggregation equation (1.2). These estimates hold as long as there exist strong solutions to the system (1.3) up to the given time . Strong solutions can be obtained locally in time by only assuming , see Theorem 4.3. However, in order to ensure existence on any arbitrarily large time interval , the additional regularity for is required, see Theorem 4.4. Moreover, our error estimates in Section 2 and Section 3 only need the regularity too.
The rest of paper is organized as follows. In Section 2, we provide a quantitative error estimate the kinetic equation (1.1) and the intermediate pressureless Euler system with nonlocal forces (1.3) by means of the relative entropy argument together with -Wasserstein distance. Section 3 is devoted to give the details of the proof for our main result on the large friction limit, and the required global-in-time existence theories for the equations (1.1), (1.2), and (1.3) are presented in Section 4.
2. Quantitative error estimate between (1.1) and (1.3)
In this section, we provide the quantitative error estimate between weak solutions to the kinetic equation (1.1) and a unique strong solution to the system (1.3) by employing the relative entropy estimate together with -Wasserstein distance. As mentioned in Introduction, we estimate the -Wasserstein distance between the spatial density of (1.1) and the density of (1.3). This together with the standard relative entropy estimate gives our desired quantitative estimate. Note that in this section the result allows more general potentials and ; the particular choice is not required, and the condition appeared in (H) is not needed. The assumption (H) implies that the sum of the last two terms in (1.4) related to the macroscopic density involving and in the total energy is displacement convex with respect to -Wasserstein distance. This fact will be used for the estimate of the large friction limit from (1.3) to (1.2) in Section 3.
For notational simplicity, we drop the -dependence in solutions and denote by throughout this section. In the following two subsections, we prove the proposition below on the quantitative estimate of -Wasserstein distance between solutions to (1.1) and (1.3).
Proposition 2.1**.**
Let be the solution to the equation (1.1) and be the strong solution to the system (1.3) on the time interval . Suppose that is large enough such that , where . Furthermore, we assume that the confinement potential is bounded from below and the interaction potential is symmetric and . Then we have
[TABLE]
where is given by
[TABLE]
and is independent of and , but depends on .
Remark 2.1**.**
Without loss of generality, we assume that in the rest of this section.
2.1. Relative entropy estimate
We rewrite the equations (1.3) in conservative form:
[TABLE]
and
[TABLE]
Then the above system has the following macro entropy form . Note that the entropy defined above is not strictly convex with respect to . We now define the relative entropy functional as follows.
[TABLE]
where denotes the derivation of with respect to , i.e.,
[TABLE]
This yields
[TABLE]
We next derive an evolution equation for the integrand relative entropy in the lemma below.
Lemma 2.1**.**
The relative entropy defined in (2.1) satisfies the following equality:
[TABLE]
where is the relative flux functional.
Proof.
It follows from (2.1) that
[TABLE]
Integrating by parts, the following identity holds
[TABLE]
see [24, Lemma 4.1] for details of proof. Moreover, we also find from [24] that
[TABLE]
Thus we obtain
[TABLE]
For the estimate , we notice that
[TABLE]
Then, by a direct calculation, we find
[TABLE]
and
[TABLE]
Thus we obtain
[TABLE]
Combining the above estimates concludes the desired result. ∎
In the light of the previous lemma, we provide the following proposition.
Proposition 2.2**.**
Let be the solution to the equation (1.1) and be the strong solution to the system (1.3) on the time interval . Then we have
[TABLE]
Proof.
It follows from Lemma 2.1 that
[TABLE]
Here can be estimated as follows.
Estimate of : Note that
[TABLE]
This gives
[TABLE]
Thus, by adding and subtracting the functional , we find
[TABLE]
Estimate of : It follows from [24, Lemma 4.3] that
[TABLE]
This together with the fact yields
[TABLE]
Estimate of : A direct computation asserts
[TABLE]
On the other hand, we get
[TABLE]
This together with (1.5) gives
[TABLE]
where .
Estimate of : Integrating by parts gives
[TABLE]
Thus we get
[TABLE]
Estimate of : Note that
[TABLE]
This yields
[TABLE]
We now combine the estimates to get
[TABLE]
We then use (1.5) and (2.3) to find
[TABLE]
We finally combine all the above estimates to conclude the proof. ∎
Remark 2.2**.**
Note that we proved , if is a fixed constant, in contrast with [24, Lemma 4.4], where they only proved due to the pressure term in the Euler equations.
2.2. Relative entropy combined with -Wasserstein distance
In this part, we show that the -Wasserstein distance can be bounded by the relative entropy.
Note that the local densities and satisfy
[TABLE]
respectively. Let us define forward characteristics and , which solve the following ODEs:
[TABLE]
with , respectively. Since we assumed that is bounded and Lipschitz continuous on the time interval , there exists a unique solution , which is determined as the push-forward of the its initial densities through the flow maps , i.e., . Here stands for the push-forward of a probability measure by a measurable map, more precisely, for probability measure and measurable map implies
[TABLE]
for all . Note that the solution is Lipschitz in with the Lipschitz constant . Indeed, we estimate
[TABLE]
Apply Grönwall’s lemma to the above gives
[TABLE]
On the other hand, the regularity of is not enough to have the existence of solutions to the second differential equation in (2.4). Thus, inspired by the following proposition from [1, Theorem 8.2.1], see also [19, Proposition 3.3], we overcome this difficulty.
Proposition 2.3**.**
Let and be a narrowly continuous solution of (2.4), that is, is continuous in the duality with continuous bounded functions, for a Borel vector field satisfying
[TABLE]
for some . Let denote the space of continuous curves. Then there exists a probability measure on satisfying the following properties:
- (i)
* is concentrated on the set of pairs such that is an absolutely continuous curve satisfying*
[TABLE]
for almost everywhere with .
- (ii)
* satisfies*
[TABLE]
for all , .
Note that it follows from (1.5), see also (2.3), that
[TABLE]
i.e., (2.6) holds for , and thus by Proposition 2.3, we have the existence of a probability measure in , which is concentrated on the set of pairs such that is a solution of
[TABLE]
with . Moreover, we have
[TABLE]
for all , .
Lemma 2.2**.**
Let be the solution to the equation (1.1) and be the strong solution to the system (1.3) on the time interval . Then we have
[TABLE]
for , where and depends only on .
Proof.
Let us introduce a density which is determined by the push-forward of through the flow map , i.e., . For the proof, we estimate and to have the error estimate between and in -Wasserstein distance. Let us first show the estimate of . We choose an optimal transport map between and such that . Then since and , we find
[TABLE]
Then this together with the Lipschitz estimate of appeared in (2.5) yields
[TABLE]
that is,
[TABLE]
For the estimate of , we use the disintegration theorem of measures (see [1]) to write
[TABLE]
where is a family of probability measures on concentrated on solutions of (2.7). We then introduce a measure on defined by
[TABLE]
We also introduce an evaluation map defined as . Then we readily show that measure on has marginals and for , see (2.8). This yields
[TABLE]
In order to estimate the right hand side of (2.9), we use (2.4) and (2.7) to have
[TABLE]
subsequently, this yields
[TABLE]
where is independent of . Combining this with (2.9), we have
[TABLE]
where is independent of , and we used the relation (2.8). Combining all of the above estimates asserts
[TABLE]
where is independent of . This completes the proof. ∎
Proposition 2.4**.**
Let be the solution to the equation (1.1) and be the strong solution to the system (1.3) on the time interval . Then we obtain
[TABLE]
Here and is independent of and , but depends on .
Proof.
Since , we get
[TABLE]
This enables us to estimate the last term on the right hand side of (2.2) as
[TABLE]
where we used . This together with Proposition 2.2 gives
[TABLE]
We then combine the above inequality and Lemma 2.2 to have
[TABLE]
where . This completes the proof. ∎
Remark 2.3**.**
If we study the hydrodynamic limit with fixed , then assuming
[TABLE]
yields the relative entropy and the -Wasserstein distance between solutions decays to zero as :
[TABLE]
In this case, the limit of is also determined by
[TABLE]
for a.e. . Indeed, for , we have
[TABLE]
where can be estimated as
[TABLE]
as , due to (1.5). For the estimate of , we obtain
[TABLE]
as . We finally note that in [19], -Wasserstein distance is also used to handle the nonlocal velocity alignment force, however, they need a slightly stronger assumption like rather than . We also want to emphasize that our estimate is more consistent in the sense that we need to assume the condition for to have the estimate for . Moreover, it is not clear that the strategy used in [19] works for the whole space case since they make use of the periodicidity and the boundedness of the domain. In a recent work [14], it is observed that the -Wasserstein distance can be also bounded by the relative entropy.
Remark 2.4**.**
Suppose that is large enough such that . Then it follows from Proposition 2.4 that
[TABLE]
where
[TABLE]
We now provide the details of Proof of Proposition 2.1.
Proof of Proposition 2.1.
Combining Lemma 2.2 and Remark 2.4 yields
[TABLE]
This concludes the desired result. ∎
3. Proof of Theorem 1.1: Large friction limit
In this section, we provide the details of proof of Theorem 1.1 on the large friction limit from the kinetic equation (1.1) to the aggregation equation (1.2). Our main strategy is to combine the -Wasserstein distance estimate in Proposition 2.1 and the recent work [7] where the overdamped limit to the aggregation equation from damped Euler system with interaction forces is established by optimal transport techniques. We notice that the intermediate system (1.3) depends on the parameters and and the estimates in Section 2 also depend on the . Thus we need to check how it depends on the parameters and . Throughout this section, we set .
3.1. -estimate on the velocity field.
Let us denote by the strong solution to the system (1.3). Our goal in this part is to provide the -estimate of .
Define the characteristic flow associated to the fluid velocity by
[TABLE]
Lemma 3.1**.**
Let and be the strong solution to the system (1.3) on the time interval . Then there exist and such that
[TABLE]
for and .
Proof.
It follows from the momentum equations in (1.3) that
[TABLE]
Then, along the characteristic flow defined in (3.1), we find
[TABLE]
and this yields
[TABLE]
due to . Set and
[TABLE]
Since , we can define , and if , then the following holds:
[TABLE]
On the other hand, for , we get
[TABLE]
We now choose sufficiently large and small enough so that for and . Thus we obtain
[TABLE]
and this is a contradiction. Hence we have , and this completes the proof. ∎
3.2. Overdamped limit: from Euler to aggregation equations
Let us consider the pressureless Euler equations (1.3):
[TABLE]
Then, an easy generalization of [7, Theorem 5] implies the following error estimate between and , which is a solution to (1.2) in -Wasserstein distance.
Proposition 3.1**.**
Let and be the strong solution of (3.2) for sufficiently large , and let be the unique strong solution to the following equation on the time interval :
[TABLE]
We further assume that the initial data satisfy
[TABLE]
and
[TABLE]
where
[TABLE]
Then we have
[TABLE]
where is given by
[TABLE]
Remark 3.1**.**
The improvement of Proposition 3.1 with respect to [7, Theorem 5] is on the initial data assumptions to allow the initial data depending on .
Then we are now in a position to give the details of proof of Theorem 1.1.
Proof of Theorem 1.1.
For a given satisfying the assumptions in Theorem 1.1, we consider its approximation with satisfying
[TABLE]
Set . Then it is clear to get
[TABLE]
and
[TABLE]
We now take into account the pressureless Euler system (1.3) with above the initial data and the singular parameter , i.e., . This, together with Lemma 3.1, Proposition 2.1, and choosing small enough, yields
[TABLE]
where is independent of and
[TABLE]
Note that
[TABLE]
where is independent of . Then this implies
[TABLE]
where is independent of . Furthermore, since , we have
[TABLE]
For the error estimate of solutions to (1.2) and (1.3), we use Proposition 3.1 with to obtain
[TABLE]
We finally combine all the above estimates to conclude
[TABLE]
This completes the proof. ∎
4. Well-posedness of equations (1.1), (1.2), and (1.3)
In this section, we show the global-in-time existence of solutions to the equations (1.1), (1.2), and (1.3) under suitable assumptions on the initial data, making our main result completely rigorous.
4.1. Global-in-time existence of weak solutions to the equation (1.1)
We first present a notion of weak solutions of the equation (1.1) and our result on the global-in-time existence of weak solutions.
Definition 4.1**.**
For a given , we say that is a weak solution to the equation (1.1) if the following conditions are satisfied:
- (i)
,
- (ii)
for any ,
[TABLE]
We also recall the velocity averaging lemma whose proof can be found in [22, Lemma 2.7].
Lemma 4.1**.**
For , let be bounded in . Suppose that
- (i)
* is bounded in ,*
- (ii)
* is bounded in .*
If and satisfy the following equation: then, for any satisfying as , the sequence is relatively compact in .
We can now show the existence results for this type of solutions.
Theorem 4.1**.**
Let . Suppose that satisfies
[TABLE]
Furthermore, we assume
[TABLE]
Then there exists a weak solution of the equation (1.1) in the sense of Definition 4.1 satisfying Furthermore, the total energy inequality (1.5) holds.
For notational simplicity, in the rest of this section, we set .
Remark 4.1**.**
Our strategy can be directly applied to the case, where the confinement potential satisfies as , and for . Without loss of generality, we may assume that in the rest of this subsection.
The global-in-time existence of weak solutions for the Vlasov equation with local alignment forces was studied in [22]. In the presence of diffusion, the global-in-time existence classical solutions around the global Maxwellian was obtained in [12]. We basically take a similar strategy as in [22] and develop it to handle the additional terms, confinement and interaction potentials, in order to provide the details of proof of Theorem 4.1.
4.1.1. Regularized equation
In this part, we deal with a regularized equation of (1.1). Inspired by [22], we regularize the local velocity and apply the high-velocity cut-off to the regularized local velocity. More precisely, we consider
[TABLE]
with the initial data where
[TABLE]
with and .
Then our goal of this part is to prove the global well-posedness of the regularized equation (4.1).
Proposition 4.1**.**
Let satisfy the condition of Theorem 4.1. Then, for any , there exists a solution with of (4.1) satisfying
[TABLE]
and
[TABLE]
where is independent of and .
Proof.
Since the proof is similar to [22, Proposition 3.1], we briefly give the idea of that.
Step 1 (Setup for fixed point argument): We first fix . For a given , we let be the solution of
[TABLE]
with the initial data
[TABLE]
We then define a map by
[TABLE]
Step 2 (Existence): We first show that the operator is well-defined. In fact, the global-in-time existence and uniqueness of solution to (4.3) is standard at this point since . Furthermore, we can also obtain the uniform estimate (4.2). Indeed, it can be easily found by using the fact that
[TABLE]
For the energy estimate, we obtain
[TABLE]
and this gives
[TABLE]
The continuity of the operator just follows from [22, Lemma 3.3]. We next provide that the operator is compact. More precisely, let be a bounded sequence in , then we show that converges strongly in up to a subsequence. This proof relies on the velocity averaging lemma, Lemma 4.1, and for the proof it is enough to estimate the uniform bound of force fields given in (4.3) with , see [22, Section 3.2]. Let us denote by . Then we find from the above estimate of and (4.5) that
[TABLE]
where we used
[TABLE]
for . Then using this, Lemma 4.1, the argument in [22, Section 3.2], we can apply Schauder fixed point theorem to conclude the existence of solutions to the regularized equation (4.1).
Step 3 (Uniform energy estimate): Similarly to (4.4), we find
[TABLE]
We then use the following facts
[TABLE]
to get
[TABLE]
Hence we have
[TABLE]
This completes the proof. ∎
4.1.2. Proof of Theorem 4.1
In order to conclude the proof of Theorem 4.1, we need to pass to the limits and . Note that we obtain the uniform estimate and the energy estimate in Proposition 4.1, and the uniform-in- bound estimate of in with can be obtained by using the similar argument as before. Those observations together with the argument in [22, Section 4] conclude the proof of Theorem 4.1.
4.2. Global-in-time existence of weak solutions to the equation (1.2)
In this subsection, we discuss the global-in-time existence and uniqueness of weak solutions to the continuity type equation (1.2). We just refer to [4, 9, 2, 6, 29, 30] for related results. We adapt some of these ideas for our particular purposes. We first introduce a definition of weak solutions to the equation (1.2) and state the our main theorem in this part.
Definition 4.2**.**
For a given , we say that is a weak solution to the equation (1.2) if the following conditions are satisfied:
- (i)
,
- (ii)
* satisfies the system (1.2) in the sense of distributions.*
Theorem 4.2**.**
Let . Suppose that the confinement potential is given by and the interaction potential is symmetric and . If , then there exists a unique global solution to the equation (1.2) on the time interval in the sense of Definition 4.2. In particular, we have .
Proof.
We first introduce the flow , generated by the velocity field :
[TABLE]
for all . Note that the above flow is well-defined globally in time due to the regularity of and . Concerning the integrability , we first find
[TABLE]
This yields
[TABLE]
On the other hand, it follows from [5, 6, 2] that
[TABLE]
Hence we have
[TABLE]
This completes the proof. ∎
4.3. Global-in-time existence of strong solutions to the system (1.3)
In this part, we study the global-in-time existence of strong solutions to the following system:
[TABLE]
with the initial data
[TABLE]
We now introduce a notion of strong solution to the system (4.6).
Definition 4.3**.**
Let . For given , the pair is a strong solution of (4.6) on the time interval if and only if the following conditions are satisfied:
- (i)
, , and ,
- (ii)
* satisfy the system (4.6) in the sense of distributions.*
We first present the local-in-time existence and uniqueness results for the systems (4.6).
Theorem 4.3**.**
Let and . Suppose that the confinement potential is given by and the interaction potential is symmetric and . For any , there is a positive constant depending only on , , and such that if
[TABLE]
then the Cauchy problem (4.6) has a unique strong solution , in the sense of Definition 4.3, satisfying
[TABLE]
where denotes a ball of radius centered at the origin.
Proof.
Since the proof of local-in-time existence theory is by now classical, we sketch the proof here, see [13, Section 2.1] for detailed discussions. For simplicity, we set .
Step 1 (Linearized system): We first consider the associate linear system:
[TABLE]
with the initial data satisfying the assumptions in Theorem 4.3. Here satisfies
[TABLE]
We notice that the existence of the above linear system can be proved by a standard linear theory [23]. Since is globally Lipschitz, by using the method of characteristics, we can show the positivity of the density . By a straightforward computation, we first find from the continuity equation in (4.7) that
[TABLE]
For , we obtain
[TABLE]
where denotes any partial derivative with multi-index , , and we estimate
[TABLE]
Here, in order to bound and , we used Moser-type inequality [11, Lemma 2.1] as
[TABLE]
for and . This, together with (4.8), yields
[TABLE]
due to . For the estimate of , we use the positivity of to divide the momentum equation in (4.7) by and use the similar argument as in Lemma 3.1 to get
[TABLE]
Applying Gronwall’s inequality to the above, we obtain
[TABLE]
For , similarly as above, we next estimate
[TABLE]
Summing the above inequality over gives
[TABLE]
Then we combine the above, (4.10), and (4.11) to have
[TABLE]
Thus we obtain
[TABLE]
On the other hand, we get
[TABLE]
due to (4.11). By using Gronwall’s inequality, we find
[TABLE]
Combining all of the above observations yields
[TABLE]
We finally choose small enough such that the right hand side of the above inequality is less than . Hence we have
[TABLE]
Notice that , , and do not depend on .
Step 2 (Existence): We now construct the approximated solutions for the system (4.6) by solving the following linear system:
[TABLE]
with the initial data and first iteration step defined by
[TABLE]
and
[TABLE]
Then it follows from Step 1 that for any , there exists such that if , then we have
[TABLE]
Note that and satisfy
[TABLE]
and
[TABLE]
respectively. Then a straightforward computation gives
[TABLE]
where depends on , , , and . We also find
[TABLE]
where depends on , , and . This provides that is a Cauchy sequence in . Interpolating this strong convergences with the above uniform-in- bound estimates gives
[TABLE]
[TABLE]
due to . In order to show the limiting functions and satisfy the regularity in Theorem 4.3 we can use a standard functional analytic arguments. For more details, we refer to [13, Section 2.1] and [8, Appendix A]. We also notice that it is easy to show the limiting functions and are solutions to (4.6) in the sense of Definition 4.3.
Step 3 (Uniqueness): Let and be the strong solutions obtained in the previous step with the same initial data . Then it directly follows from the Cauchy estimate in Step 2 that
[TABLE]
Thus we obtain
[TABLE]
for all . Hence we have the uniqueness of strong solutions. ∎
We next show global-in-time existence of strong solutions to the system (4.6) under additional assumptions on parameters , , see below, and the interaction potential . We remark that the assumption on and is used in Lemma 3.1 for the uniform bound estimate of . The strong regularity of is needed for the global-in-time existence of solutions. Note that we do not require any small assumptions on the initial data.
Theorem 4.4**.**
Let , , and . Suppose that the confinement potential is given by and the interaction potential is symmetric and . Suppose that initial data satisfy
[TABLE]
Then there exist and such that
[TABLE]
for and , where depends on the initial data , , , , and . Here and are appeared in Lemma 3.1.
Proof.
Similarly as (4.9), we estimate
[TABLE]
and
[TABLE]
This yields
[TABLE]
i.e.,
[TABLE]
On the other hand, it follows from Lemma 3.1 that there exist and such that
[TABLE]
for and . Then this, together with using the method of characteristics, gives
[TABLE]
Combining all of the above observations, we obtain
[TABLE]
for and . We also easily estimate
[TABLE]
For , we find
[TABLE]
and
[TABLE]
Then we have from (4.14)
[TABLE]
This together with (4.12) implies
[TABLE]
where depends on the initial data , , and . We back to (4.13) to obtain
[TABLE]
where we used (4.15) and (4.12). It also follows from (4.14) that
[TABLE]
Combining the above two differential inequalities yields
[TABLE]
and subsequently we find
[TABLE]
where depends on the initial data , , , , and . We next estimate (4.13) and (4.14) as
[TABLE]
where we used
[TABLE]
By summing it over and applying Gronwall’s inequality to the resulting differential inequality, we finally have
[TABLE]
where depends on the initial data , , , , and . Combining all of the above discussion concludes the desired result. ∎
Acknowledgements
JAC was partially supported by the EPSRC grant number EP/P031587/1. YPC was supported by NRF grant(No. 2017R1C1B2012918 and 2017R1A4A1014735) and POSCO Science Fellowship of POSCO TJ Park Foundation.
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