It is proved that partially dissipative hyperbolic systems converge globally-in-time to parabolic systems in a slow time scaling, when initial data are smooth and sufficiently close to constant equilibrium states. Based on this result, we establish the global-in-time error estimates between the smooth solutions to the partially dissipative hyperbolic systems and those to the isotropic parabolic limiting systems in a three dimensional torus, rather than in the one dimensional whole space (Appl. Anal.100(5) (2021) 1079–1095). This avoids the condition raised for the strong connection between the flux and the source term and make the result obtained more generalized. In the proof, we provide a similar stream function technique which is valid for the three dimensional periodic case. Similar method is provided for the one-dimensional periodic case. As applications of the results, we give several examples arising from physical models at the end of the paper.
We consider the periodic problem in a d-dimensional torus of the following first-order quasilinear hyperbolic system with stiff source terms, which is of the form
with the initial condition
Here is a torus in , is the unknown variable, is a small parameter standing often for the relaxation time in physical models (see Section 5), is the usual time and is the space variable. The source term and the matrices () are all smooth functions. The set S is called the state space. We assume (1.1) is symmetrizable hyperbolic, i.e., there exists a symmetric positive definite matrix , called symmetrizer, such that is symmetric for all and .
Usually, the source term is of the form
where is a smooth function, . With the same partition, we denote
as well as the initial data
More generally, under the same partition, a vector and an matrix M will be denoted by and , respectively. Here and are matrices of order and respectively and and are defined accordingly.
A large number of physical models of the form (1.1) can be found in [20,29]. The local existence of smooth solutions to (1.1)-(1.2) is well-known due to Lax [12] and Kato [10], see also [17]. Generally speaking, smooth solutions of the Cauchy problem (1.1)–(1.2) exist only locally in time and singularities may appear in finite time. However, the dissipative structure of the system may prevent the formation of the singularities and lead to global smooth solutions in a neighborhood of an equilibrium state for (1.1), i.e., . The global existence for (1.1)-(1.2) was proved by Hanouzet–Natalini [5] in one space dimension and was extended by Yong [31] to the case of several space dimensions. In the proof of these results, they need essentially two main conditions. The first one is a partially dissipative condition and the second one is the Shizuta–Kawashima condition (SK) (see [25]) at an equilibrium state.
Now we consider a partially conserved model of (1.1) in the sense that only u satisfies the equations of conservation laws. A partially conserved model for u means that there exist smooth vectors , such that (1.1)–(1.2) can be rewritten into the following
with the initial condition
System (1.3) can be regarded as a special case included in (1.1) if we denote
When the slow time is introduced and the following change of variables is made
(1.3)–(1.4) becomes
with initial conditions
In physics, the limit is often called the zero relaxation limit. This is because when , the system formally converges to the equilibrium state. For this kind of convergence problems, there are rich literatures. Under sub-characteristic conditions [16], system (1.1) converges formally to a hyperbolic system. We refer the readers to [1,2,8,16,24] and references therein for mathematical results. In particular, under stability conditions, the uniform local smooth solutions with respect to ε and their convergence as were investigated in [30]. Under reasonable conditions on and q, system (1.1) converges formally to parabolic-type equations (see [19]). The justification of the local-in-time convergence was proved in [21]. See also [11] for a study close to semilinear case. Moreover, in a neighborhood of an equilibrium state, the uniform existence of global smooth solutions with respect to ε and their global-in-time convergence as were obtained in [22].
Another interesting topic is the convergence rate problem. In the local-in-time convergence result, the convergence rate was clearly shown and it depends on the local existence time [21]. For the global convergence rate problems, few results have been obtained. See Junca–Rascle [9] for the isothermal Euler system with damping, Goudon–Lin [4] for the so-called M1-model in the radiative transfer theory and Li–Peng–Zhao [13] for the general hyperbolic systems of balance laws in the whole space. All of these results are studied in the one-dimensional space. For multi-dimensional cases, to the authors’ best knowledge, no results have been obtained for the general first order quasilinear systems.
The aim of the present paper is to study the global-in-time convergence rate problem of (1.7)–(1.8) as in a multi-dimensional torus. The global convergence rate is hard to obtain mainly due to the difficulty in obtaining the global-in-time -estimate. In detail, when constructing the error system, which are established by subtracting the limiting equations from the original system, the structure of the equations changes. To be clear, it leads to the loss of symmetrizable hyperbolicity and the existence of a strictly convex entropy. That is the reason why we can not obtain the highest order estimates nor the -estimate. However, a stream function technique can overcome this difficulty and provide a error estimate [4,9,13].
The stream function acts as a percise interconnection between the unknowns and the singular source term. Thus it provides an alternative way to estimate the singular terms. However, the previous studies show that this technique is only efficient for the one-dimensional system of conservation laws in the whole space, but not for multi-dimensional cases. In fact, considering the following one-dimensional conservation law,
with sufficiently smooth. We call ϕ a stream function of the above if ϕ satisfies
This can be formally achieved by letting
and be uniquely determined if we pose an initial condition as
However, when we consider the periodic problem in a multi-dimensional space, the construction of the stream function becomes more complicated. For example, for the first equation in (1.3), the usual stream function ϕ satisfies the following
where , such that the j-th column vector of F, . However, these are not sufficient. Compared to the case of one-dimensional whole space, many mixed partial derivative terms will appear. One direct illustration is that for a certain , can not be controlled by , so that we can not use (1.9) to continue the proof. Here denotes the norm of the classical Sobolev space . Consequently, we need to pose additional conditions on the stream function obtained, which makes it less possible for the existence of a proper ϕ. For example, in order to make controlled by , in the paper, we require that the stream function satisfies the following conditions
As a result, by using the Poincaré inequality, we have the following estimate for and ϕ,
Unfortunately, (1.9)–(1.10) are overdetermined. To overcome it, we introduce a new method for constructing the stream function which is valid for our problem. As a sacrifice, additional terms will appear on some of the right hand sides of (1.9). Due to the percise structure of the stream function, these additional terms will bring difficulties in the proof.
Moreover, even in one-dimensional space, additional conditions are needed in the previous studies. In detail, in the one-dimensional whole space, (1.7) becomes
In order to obtain the global convergence rate, the authors in [13] need a strong connection condition between the flux term and the source term,
(H)
There exists a constant matrixsuch thatwhereis a neighbourhood of the equilibrium state.
This condition eliminates all the terms that do not contain derivatives of the stream function, which are hard to handle without the Poincaré inequality. However in a torus, we can avoid using this condition. It is worth mentioning that in order to be able to use the Poincaré inequality, we have to let the average of the stream function ϕ over the torus be zero. That is the main reason why the condition (1.10) is needed.
Another difficulty is the singularity of in in the slow time scaling, in other words, we have for all (see (2.2) in the next section). Especially, it is difficult to obtain the estimates for nonlinear terms containing , among which, terms containing are the most difficult since they can be very singular up to order . One can observe formally through the second equation in (1.7) together with the estimate (2.2) in the next section. To overcome this difficulty, we introduce a decomposition method (see (3.20) in Section 3), in which according to the degree of singularity, we divide the singular terms into two categories. One contains terms that are very singular but with better regularity when ε is fixed while the other is just opposite. The method requires complicated calculations in which a correct division of the singular terms and a careful choice on the power of ε is needed.
The aim of the present paper is to establish the global-in-time error estimates between the solutions to (1.7) and those to the limiting system, which is parabolic and isotropic (see condition (H1) in Section 2). We study these problems in a three-dimensional torus or in a one-dimensional one. Our results are not applicable for or mainly due to the fact that we can not find a suitable rotation operator (see (3.3) in Section 3). In the paper, we introduce a method for constructing the generalized stream function which is valid for multi-dimensional periodic cases and we do not need any additional conditions on the matrix D defined in condition (H), which is necessary in the previous studies. For initial data sufficiently close to the constant equilibrium state in , our error estimates are showed in for u and in for v. The estimates are uniform for all , contrarily to the local convergence case where ε should be small [21].
The paper is organized as follows. In the next section, we give some preliminaries and state the main results of this paper. Sections 3 and 4 are devoted to the proof of the main results in a three-dimensional torus or in a one-dimensional one, respectively. In the last section, we give several examples of systems which include those studied in [4,9,13,21].
Preliminaries and main results
In this paper, we study (1.7)–(1.8) in a three dimensional torus or a one-dimensional one based on the results in [13,22]. In the following, let be an integer and be a generic constant independent of ε and any time. We denote by , and the usual norm of , , and , respectively with integers . In the proof, we use the fact that the embedding from to is continuous for all integer . We denote the inner product in .
We first recall results on the uniform global existence and the global-in-time convergence of the system established in [22]. We assume in the following and be open sets satisfying and . For the periodic problem (1.7)–(1.8), the assumptions needed in [22] are as follows.
(A1)
For all ,
(A2)
The matrix is invertible.
(A3)
For all and , .
(A4)
For all , .
(A5)
There exists a constant such that
where denotes the usual Euclidean norm and ⊤ denotes the transpose of a vector or a matrix.
(SK)
The kernel of the Jacobian , , contains no eigenvector of the matrix , for any (the unit sphere in ), where the matrices are defined in (1.5).
(A1) means that the equilibrium state is of the form , i.e., .
(A2)–(A3) are necessary to derive the limiting system as second-order parabolic partial differential equations (see [19,22]).
(A4) is a technical assumption, which is satisfied when the system is semilinear or . The latter is the case for gas dynamics equations.
(SK) is a dissipative condition, which implies a time dissipative estimate of .
(A5) is the partially dissipative condition, which implies a time dissipative estimate of v. Under this condition, it is proved in [30] (see also Proposition 2.1 in [22]) that there is a neighbourhood of , such that
It follows that, for all ,
Thus (A5) shows that is a positive definite matrix in and
Under these assumptions, in a neighbourhood of the equilibrium state, the uniform global existence of smooth solutions to (1.7)–(1.8) was proved.
Letand integer. Let conditions (A1)–(A5) and (SK) hold. Then in a neighbourhood of the constant equilibrium state, there exists a unique global solutionto (
1.7
)–(
1.8
). Moreover, the following estimate holdswhereis a generic constant independent of ε and any time.
We point out that the above result is also valid for system (1.1)–(1.2).
We now recall the results on the global-in-time convergence as . From (A3), we see that is constant. It follows that
Hence, we may suppose (otherwise, we replace by ). Together with (A1), there are smooth matrix functions of order and of order such that
with
By (2.3), (1.7)–(1.8) can be written as
If we denote the limit of as , then formally satisfies
By (A2), is invertible when is sufficiently small. Then we obtain the following proposition.
Let the conditions in Proposition
2.1
hold. Let. Ifthenwhereis the unique solution to the periodic problem for a system of second-order partial differential equationsandIn addition, the system (
2.6
) is parabolic (see [
22
]and Lemma
2.1
below). Consequently, the following estimate holds for,provided thatis sufficiently small. This together with (
2.7
) yields
Estimates (2.2) and (2.8)–(2.9) are useful in Sections 3 and 4 for the proof of the convergence rate. We point out that in general, from (2.7) and the initial condition of in (1.8), there are initial layers on variable v in the limiting process from (1.7)–(1.8) to (2.6)–(2.7).
The following lemma ensures that system (2.6) is parabolic, which is proved in Lemma 2.2 in [22].
Let (A1)–(A3) and (SK) hold. There is a neighbourhoodof, such that (
2.6
) is parabolic in the sense thatis a positive definite matrix for alland all, in which
For simplicity, we denote from now on for all and ,
and
In the proof, when , we need to pose the following condition on such that the limiting equation is isotropic. This condition automatically holds when .
(H1)
For all, there exists a positive definite matrix, such that the matricessatisfywhereis the Kronecker symbol.
Under condition (H1), the limiting system (2.6) becomes the following isotropic diffusive second order parabolic equations
The main result of this paper is stated as follows.
Let (A1)–(A5), (SK) and (H1) hold. Letand integer. Letbe the unique solution to (
1.7
)–(
1.8
),be the unique solution to (
2.6
) with initial databeing the weak limit ofinandbe given by (
2.7
). There exist positive constants δ,and, independent of ε, such that ifandthen for all, we have the following estimatewhereis introduced in (
1.10
),is a constant independent of ε and. In particular, when, we do not need the condition (H1).
Convergence rate in three-dimensional torus
In this section, we let . In what follows, we assume that the conditions in Theorem 2.1 hold. For convenience, for a given scalar or vector function , we denote its mean value over the torus with respect to x as
Then it follows for integers ,
in which we have used the continuous embedding for integers .
Construction of the stream function
We first construct a generalized stream function, which we will use frequently in later proof. For simplicity, for a matrix , we denote its i-th row as and its k-th column as with , .
(Existence of the stream function).
Letbe an integer. Letbe a matrix of orderwith its i-th column defined asThen there exist stream functionsand functions, such thatwhereandare the k-th component ofand, respectively. Additionally, stream functionssatisfyMoreover, we have the following estimatesandwhereis defined in Theorem
2.1
.
Subtracting (2.6) from the first equation in (2.4), we have
Noticing the definition of in (3.2), we can rewrite (3.6) into
The proof of the existence of the stream function is constructive. First, let be the unique periodic solution to the following Poisson equation
To be clear, we denote . Thus, let
Then it is obvious that , and
Applying the ‘div’ operator to both sides of (3.9), we have
where and are the k-th component of and , respectively. Besides, noticing (3.7), we obtain
Taking the time derivative to both sides of (3.10) and noticing (3.6) yield
which implies that there are functions , satisfying
We now establish the estimates for . Noticing (3.1) and that are rotation free, by using the Poincaré inequality, we have for ,
which implies (3.4). It remains to prove (3.5). Applying to both sides of the first equation in (3.8) and using (3.7) and (3.11), we have
Energy estimates and the explicit expression of in (3.9) imply that
in which we have used the Moser-type inequalities. Let . Noticing the energy estimates (2.2) and (2.8), we have
which implies (3.5) since is arbitrary. □
(Compatibility conditions).
We now define the initial data of . From (3.8), the classical elliptic estimates together with the Poincaré inequality implies
Hence, by the Aubin–Lions lemma, we have
Hence, we may define the initial data of , i.e., , as the unique solution to the following
Similarly, we denote as the k-th component of . Now, we can define the initial data of . By similar methods, we obtain
As a result, , as the initial data of , can be defined by
Consequently, by (2.13), we have
Lemma 3.1 will be frequently used in the later proof. To make the notations easy to follow, for a multi-index , we denote
and for all ,
Convergence rate for
The goal of this subsection is to establish the following estimate.
(Convergence rate for ).
Let the conditions in Theorem
2.1
hold. Thenwhereis defined in Theorem
2.1
.
The proof of Lemma 3.2 follows from a series of lemmas given as follows. Since is sufficiently small, (2.2) together with (2.12) implies that and is uniformly small with respect to ε in . In addition, the weak convergence of to in implies that . By (2.8), we have and is sufficiently small. In the proof, we let i, k be integers with and .
To start, let and be a multi-index with , multiplying , which is defined in (2.10)–(2.11), to the second equation in (2.4) and applying to the resulting equation, we have for ,
For convenience, we introduce the matrices with their i-th columns defined as follows.
Then, (3.14) becomes
which implies
Taking the inner product of this equality with in and integrating the resulting equation over , we get
We will treat the right hand side of the above term by term. In the following, we denote for simplicity that the j-th component of a vector W as . First, we have
For alland a certain, it holdswhereandare defined in Theorem
2.1
, andis defined by
Noticing that
Taking the integration by parts to the first term on the right hand side of (3.15), we have
with matrices and defined as
For all , we use (2.2), (2.8), (2.13), (3.3), (3.4) and (3.12) to obtain
and using (3.5) and the Moser-type inequalities,
For the last term on the right hand side of (3.17), we need a little more calculations. Noticing for ,
Besides, by using (2.4), we have
in which
Using the Moser-type inequalities and the estimate (2.2), we have for ,
Substituting (3.20) into the last term on the right hand side of (3.17), using (2.2), (3.4), the Young’s inequality, the Cauchy–Schwarz inequality, the Poincaré inequality and the Moser-type inequalities, we have when ,
When , we let a multi-index with . Then, after taking the integration by parts, noticing that is rotation free, we have
Combining these estimates and (3.18)–(3.19) yields (3.16). □
We keep the term containing for the moment. For the term containing , we have the following estimate.
For alland a certain, it holdswhereis defined in Theorem
2.1
.
Recall that
When , using (2.2), (3.4), the Cauchy–Schwarz inequality and the Young’s inequality, we have
When , we let a multi-index with , such that after taking the integration by parts,
The above two estimates imply (3.21). □
We now treat the term containing . In view of the expression for and noticing (3.2) and (3.3), we have
For convenience, we denote the matrix in the way that
Then (3.22) implies
Hence, noticing that is rotation free, we have,
Integrating the above over implies
Combining the above, Lemmas 3.3–3.4 and (3.15), we have for all ,
We now estimate the second term on the left hand side of the above inequality. In view of the expression for and , we have
For simplicity, we denote and the matrices of order , with
Then
For alland a certain, it holdswhereandare defined in Theorem
2.1
.
Recall that
Using the Taylor’s formula, we have
in which
From (2.2) and (2.8), it is clear that is sufficiently small in , uniformly with respect to and . Besides, noticing (3.11), we obtain that is independent of t. As a result, using (2.13),
Hence,
Then, using (2.2), (3.4), the Poincaré inequality and the Young’s inequality, we have when ,
When , by taking the integration by parts, we have
which ends the proof. □
Substituting (3.25) into (3.24) and summing up for all , we have
It remains to estimate the second term on the left hand side of the above inequality. We have
There exists a constant, such that for all, it holdswhereis defined in Theorem
2.1
.
We first take the inner product of two matrices in a different way. If we denote a matrix such that
Consequently, it is easy to see that
Further noticing the expression of , we can rewrite the above into a much simplier form, which is as follows
where the partitioned matrix is defined as
Under the condition (H1), there exists a matrix K such that , where is the unit matrix. By taking the integration by parts, we have
We will estimate the right hand side of the above equality term by term. First, since is positive definite, which means there exists a constant such that
For the rest of the terms, we have the following estimates. First, by the Moser-type inequalities,
and
Substituting these estimates into (3.30) and combining (3.29) yield (3.28). □
Substituting (3.28) into (3.27), we have for all ,
Summing up the above for all , we have
provided that δ is sufficiently small. Taking the superior limit with respect to T yields
provided that δ is sufficiently small. Finally, using (3.1), (3.3) and the Moser-type inequalities, we obtain
and as a result, for ,
which imply (3.13). □
Convergence rate for
In this section, we obtain the convergence rate of . For convenience, we introduce
From (2.4) and (2.5), satisfies
where, by noting ,
with
Recall that is a symmetric positive definite matrix and . Hence, is also a symmetric positive definite matrix. It follows that there is a constant such that
Similarly, (2.1) implies that
The solutionto (
3.32
) satisfieswhereis defined in Theorem
2.1
.
Let . For a multi-index with , applying to both sides of (3.32), taking the inner product of the resulting equation with in and integrating this equality over , since is symmetric, we have
with the natural correspondence of , and , which are treated term by term as follows. First,
where using (3.35),
and using the Moser-type inequalities and the Cauchy–Schwarz inequality, we have
Hence,
For , we need to establish the estimates for . In view of the expression of in (3.33), similar to the treatment to in (3.26), we have for ,
As a result, by (2.8) and (2.9),
Consequently, using (2.2), (2.9) and (3.13) obtained in the last section, we have
Moreover,
Hence, by the Young’s inequality,
For , from (2.8), the limiting equation (2.6) and the weak convergence of to in , we have
It follows that, for all ,
Combining (3.37) and the estimates (3.38)–(3.40), we have
Summing up for all , we have
provided that δ is sufficiently small. We notice that (3.34) implies are equivalent to . Consequently, noticing (2.12), we have
which implies (3.36) since is arbitrary. □
Convergence rate in one-dimensional torus
In this section, we consider the problem over one-dimensional torus. We let and integer . When , (2.4) becomes
with its limiting system
and
For convenience, in accordance with the notations in previous sections, we denote
We first construct a stream function over a one-dimensional torus.
(Existence of stream function over one-dimensional torus).
There exists a stream functionsuch that
Subtacting (4.2) from the first equation in (4.1), we have
Let be the unique solution to the following
By (4.4), it is clear that
Besides, taking the time derivative to both sides of the first equation in (4.5), we have
which implies that there exists a function , such that
Noticing that , taking the average of the above equation over the torus gives
which implies (4.3).
We can define the initial data of similarly to that in Remark 3.1.
We now turn to the global convergence rate of . Noticing when , the condition (H1) automatically holds. Let be integers. Multiplying D and then applying to the second equation in (4.1), we have
Taking the inner product of this equality with in and integrating over , we get
with the natural correspondence of , , and , which are treated term by term in the way similar to that in the previous section. First, taking the integration by parts with respect to time for , we have
Similar to (3.17), denoting , we have
Using (2.2), (2.8) and (3.1), we have
then by the Moser-type inequalities,
These estimates imply
Similar to (3.21), we have
For , using (3.23) and the explicit expression of in (4.3), we have
Combining (4.7) and these estimates, we have
Similar to (3.25) and (3.28), we have
which implies
Following the same procedure as we did in (3.31), we have
The convergence rate of is similar based on the above estimate. Hence, we have
which ends the proof. □
Examples
In this section, we give several examples of systems which fulfill all conditions (A1)–(A5), (SK) and (H1). Then Theorem 2.1 can be applied to the periodic problems of all the examples in the section. In these examples, is the slow time and the systems are expressed after scaling (1.6). We denote from now on and be the canonical basis of . Example 5.2 in the isothermal case and Example 5.4 were studied in [9] and [4], respectively.
Examples in multi-dimensional spaces
(Wave equation of heat conduction).
This concerns a linear equation which is written as (see [6,21] and references therein)
Let us introduce
then the equation becomes
which is of the form (1.7) with
Its corresponding parabolic limiting equation is
which is the classical heat equation. It is easily checked that conditions (A1)–(A5), (SK) and (H1) are satisfied. Then Theorem 2.1 can be applied.
(Euler equations with nonlinear damping).
The model is written as (see [3,13,14,18,22,26])
where is the relaxation time, is the density and w is the velocity. The pressure function is supposed to be smooth and strictly increasing. The damping coefficient is a smooth function and there exists positive constants and , such that
When , system (5.1) is equivalent to the following
where h is the enthalpy function satisfying
System (5.3) is of the form (1.7) with
and
and its corresponding limiting equation is
which is in general a nonlinear parabolic equation under condition (5.2). It is easily checked that conditions (A1)–(A5), (SK) and (H1) are satisfied. Then Theorem 2.1 can be applied. For weak solutions, an error estimate for ρ in was obtained in [9] in the isothermal case with linear damping, i.e., and , which implies that (5.4) is a linear heat equation.
Examples in one-dimensional space
(The Euler equations with linear damping in Lagrangian coordinates).
In this example (see [7,13,22]), let and . Then the Lagrangian coordinates are well defined for and the Euler equations in (5.1) are equivalent to (see [28])
where
System (5.5) is still of the form (4.1) with
The corresponding limiting equation is
which is a nonlinear parabolic equation. It is easily checked that conditions (A1)–(A5) and (SK) are satisfied. Then Theorem 2.1 can be applied. We remark that (5.6) is a nonlinear equation even if p is a linear function.
(The M1 model).
This model in one space variable is written as
where is the density, w is the velocity and is defined by
This system is of the form (4.1) with
and
Noticing when , we obtain its corresponding limiting equation is
which is a linear heat equation. It is easily checked that conditions (A1)–(A5) and (SK) are satisfied. Then Theorem 2.1 can be applied. Remark that for smooth solutions an error estimate for ρ in was obtained in [4].
(A generalized discrete two-velocity model).
The model is written as (see for instance [13,15,22,23,27]):
where ν is a real number and . If we introduce
then the equivalent system is
which is of the form (4.1) with
Its corresponding limiting equation is
which is a nonlinear parabolic equation for . It is easily checked that conditions (A1)–(A5) and (SK) are satisfied. Then Theorem 2.1 can be applied.
Footnotes
Acknowledgements
The authors want to express their sincerely thanks to the referees for their valuable remarks and suggestions, which made this paper more readable. The Second author was supported by the Cultivation Project of Young and Innovative Talents in Universities of Shandong Province.
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