On Riemann solutions under different initial periodic perturbations at two infinities for 1-d scalar convex conservation laws
Qian Yuan, Yuan Yuan

TL;DR
This paper studies the long-term behavior of entropy solutions to 1D scalar convex conservation laws with different periodic initial conditions at infinities, revealing algebraic convergence to Riemann solutions and a novel shift effect caused by differing perturbations.
Contribution
It demonstrates that differing periodic perturbations at infinities can cause a constant shift in the background shock, extending previous results where perturbations were identical.
Findings
Solutions approach Riemann solutions algebraically over time.
Different periodic perturbations can induce a constant shift in the shock.
The shift effect is a new discovery contrasting previous work.
Abstract
This paper is concerned with the large time behaviors of the entropy solutions to one-dimensional scalar convex conservation laws, of which the initial data are assumed to approach two arbitrary periodic functions as and respectively. We show that the solutions approach the Riemann solutions at algebraic rates as time increases. Moreover, a new discovery in this paper is that the difference between the two periodic perturbations at two infinities may generate a constant shift on the background shock wave, which is different from the result in [11], where the two periodic perturbations are the same.
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Taxonomy
TopicsNavier-Stokes equation solutions · Geometric Analysis and Curvature Flows · Advanced Mathematical Physics Problems
On Riemann solutions under different initial periodic perturbations at two infinities for 1-d scalar convex conservation laws
Qian YUAN
The Institute of Mathematical Sciences & Department of Mathematics, The Chinese University of Hong Kong, Shatin, N.T., Hong Kong
and
Yuan YUAN
South China Research Center for Applied Mathematics and Interdisciplinary Studies, South China Normal University, Guangzhou, Guangdong, China
Abstract.
This paper is concerned with the large time behaviors of the entropy solutions to one-dimensional scalar convex conservation laws, of which the initial data are assumed to approach two arbitrary periodic functions as and respectively. We show that the solutions approach the Riemann solutions at algebraic rates as time increases. Moreover, a new discovery in this paper is that the difference between the two periodic perturbations at two infinities may generate a constant shift on the background shock wave, which is different from the result in [11], where the two periodic perturbations are the same.
Key words and phrases:
conservation laws, shock waves, rarefaction waves, periodic perturbations
2010 Mathematics Subject Classification:
35L03, 35L65, 35L67
The research of Yuan YUAN is supported by the Start-up Research Grant of South China Normal University, 8S0328.
1. Introduction
In this paper, we consider the Cauchy problem for a convex scalar conservation law in one-dimensional spatial space:
[TABLE]
where the flux is strictly convex, i.e. .
It is well-known that for any data the Cauchy problem Equation 1.1,Equation 1.2 admits a unique entropy solution satisfying the following entropy condition (see [9]),
[TABLE]
where is a constant, depending only on and When the initial data are the Riemann data:
[TABLE]
where and are two constants, the unique entropy solution to Equation 1.1,Equation 1.2 is the well-known Riemann solutions:
- (1)
a shock wave if where
[TABLE]
where is the shock speed;
- (2)
a centered rarefaction wave if where
[TABLE]
which is Lipschitz continuous when
- (3)
a constant if
Riemann solutions are of great importance in the theories of conservation laws. They are the simplest entropy weak solutions, and can be applied as the building blocks to construct global solutions to conservation laws with more general initial data (see [3]). Moreover, they also govern the large time behaviors of entropy solutions to conservation laws with the initial data approaching constant states as In fact, there have been numerous articles showing that the Riemann solutions are asymptotically stable under localized (for instance, compactly supported) perturbations; see Hopf [5], Lax [7], Ilin-Oleinik [6] and Liu [8] for instance.
For the initial data oscillating at infinity, such as the periodic data, Lax [7], Glimm-Lax [4] and Dafermos [1] proved that the entropy solution tends to the constant average in the norm at rates And for the initial data which is a periodic perturbation around a shock wave or a rarefaction wave:
[TABLE]
where and is an arbitrary bounded periodic function with zero average, Xin-Yuan-Yuan [11] showed that the entropy solution to Equation 1.1, Equation 1.7 tends to the background wave in the norm at rates We also refer readers to [10] for the stability of viscous shock profiles and rarefaction waves under periodic perturbations for the viscous conservation laws.
In this paper, we are concerned about more complicated initial data than that in [11], i.e., coincides two different periodic functions, especially maybe with two different periods, on the two sides of -axis:
[TABLE]
where is a constant, and and are two arbitrary bounded periodic functions with periods and , respectively. By adding the averages of and on and respectively, we can assume without loss of generality that both averages are zero, i.e., and satisfy
[TABLE]
It fails to apply the analysis in [11], which is concerned with the initial data Equation 1.7, directly to the case for two different periodic perturbations Equation 1.8. For instance, when a key lemma (Lemma 3.9) in [11] shows that the entropy solution to Equation 1.1, Equation 1.7 coincides the two periodic solutions induced by the initial values and on the two sides of a generalized forward characteristic, respectively, where these two periodic solutions have very nice properties — owning divides and decaying fast to the constant averages as time increases. However, for the problem Equation 1.1,Equation 1.8, [11, Lemma 3.9] shows that the entropy solution coincides with the two solutions induced by the initial data and respectively, which are not periodic any more. Fortunately, by making use of a comparison theorem [2, Theorem 11.4.1], it is found that there are two “well controlled” Lipschitz continuous curves and such that coincides with the periodic solutions induced by the initial data and as and respectively; see 3.5. Although and may not be generalized characteristics of they can be well controlled in the sense that for the shock wave (), they coincide after a finite time; for the rarefaction wave and the constant (), both the distances and can be bounded by with the aid of two time-invariant variables; see Lemmas 4.1 and 5.2 for details. The proof relies on a similar, but more complicated analysis as in [8].
In this paper, we prove that if the entropy solution to Equation 1.1, Equation 1.8 tends to the background Riemann solution in the norm. While if the asymptotic behavior of the solution is the background shock wave with a constant shift, which is due to the non-zero mass of the compact part of the perturbation and the difference between the periodic perturbations and at two infinities; see Equation 2.7. It is noted that the result in this paper is compatible with the previous results in Liu [8] with only compact perturbations and Xin-Yuan-Yuan [11] with the initial data Equation 1.7.
This paper is organized as follows. In Section 2 we first present some notations and the theorems. In Section 3, the decay properties of periodic solutions, the properties of the generalized characteristics and some comparison results are shown. Then the stabilities of shock waves, rarefaction waves and the constants are proved in the subsequent sections.
2. Main results
Let and denote two periodic entropy solutions to Equation 1.1 with the following initial data
[TABLE]
For any let
[TABLE]
Therefore, is the shock speed of the shock and if it holds that
[TABLE]
[TABLE]
The main theorems of this paper are presented as follows:
Theorem 2.1**.**
Suppose that in (1.8). Then for any periodic perturbations and satisfying (1.9), there exist a finite time and a unique Lipschitz continuous curve such that the entropy solution to (1.1), (1.8) satisfies that for all
[TABLE]
Moreover, there exists a constant independent of time such that
[TABLE]
with the constant shift given by
[TABLE]
Theorem 2.2**.**
Suppose that in Equation 1.8. Then for any periodic perturbations and satisfying (1.9), the entropy solution to Equation 1.1,Equation 1.8 satisfies that
[TABLE]
where is a constant independent of time
Theorem 2.3**.**
Suppose that in Equation 1.8. Then for any periodic perturbations and satisfying (1.9), the entropy solution to Equation 1.1,Equation 1.8 satisfies that
[TABLE]
where is a constant independent of time
Compared with the previous result [11], which is concerned with the same periodic perturbation on the two sides of axis, the shift is new in this paper, which is essentially due to the difference between these two masses. Thus, even if two periodic perturbations have same periods, the shift may be non-zero in general.
3. Preliminaries
Before proving the theorem, in this section we present some preliminary lemmas, and also important propositions derived from the comparison principles of conservation laws.
It is well-known in the theory of generalized characteristics that for one-dimensional scalar convex conservation laws, through every point pass two forward and two backward extreme generalized characteristics. Moreover, when the forward generalized characteristic is unique and the two backward extreme generalized characteristics are straight lines. We refer to [2, Chapters 10 & 11] for details, or [11, Definition 3.1 & Lemma 3.2] for a short summary.
Lemma 3.1**.**
Assume that the initial data in Equation 1.2 is periodic with period and average Then the entropy solution to Equation 1.1, Equation 1.2 is also periodic with period and average for each and satisfies that
[TABLE]
where is a constant, independent of time
Lemma 3.2**.**
[1, Proposition 3.2]** Assume that the initial data in Equation 1.2. Then the entropy solution to Equation 1.1, Equation 1.2 takes a constant value along the straight line if and only if
[TABLE]
Such a straight line is a characteristic and it is called a divide ([2, Definition 10.3.3]).
Lemma 3.3**.**
[2, Theorem 11.8.1]** Let and be entropy solutions to (1.1) with the respective initial data and satisfying
[TABLE]
Let be a forward characteristic, associated with the solution , issuing from the point , and be a forward characteristic, associated with the solution , issuing from the point . Then for any with ,
[TABLE]
Now we first show a comparison principle for the problem Equation 1.1,Equation 1.2; see 3.4. And two important propositions Propositions 3.5 and 5.1 can be proved by using the properties in 3.4.
For the initial data Equation 1.8, one can choose and such that
[TABLE]
Hence, for all
[TABLE]
Then for each integer we define
[TABLE]
It follows from 3.2 that and are classical characteristics of and respectively, and there hold that
[TABLE]
Now, let be a fixed large number, such that
[TABLE]
and then denote
[TABLE]
Lemma 3.4**.**
With the notations introduced above, there hold that
- (1)
* if ; if ;* 2. (2)
* if ; if .*
Proof.
We prove only (1), since the proof of (2) is similar. For any fixed satisfying , since is bounded, by the finite propagating speed, one can choose small enough, such that a forward characteristic of , issuing from satisfies see Figure 1.
It is noted that on and , then 3.3 implies that . And if it is similar to prove that ∎
Now, for any we define two Lipschitz continuous curves:
[TABLE]
Then the following proposition follows from 3.4.
Proposition 3.5**.**
The unique entropy solution to Equation 1.1,Equation 1.8 satisfies
[TABLE]
Remark 3.6**.**
Note that and may not be the generalized characteristics of . And we will show in the subsequent sections that these carefully chosen curves and can be “well-controlled” at large time. It is the large time behaviors of and , together with 3.5, that reveal the main results in this paper.
4. Stability of shock waves
In this section, the large time behaviors of and are studied in the case for , and then stability of shock waves under two different perturbations at infinities are proved.
Lemma 4.1**.**
There exists a finite time such that for all
Proof.
It will be established in the following cases.
- i)
and and coincide after some positive time, due to 2. ii)
and Define , then
[TABLE]
Now we claim that there exists a finite time and independent of time such that
[TABLE]
In fact, define a function
[TABLE]
For any denote a compact domain
[TABLE]
where Then for each the strict convexity of implies that there exists a unique such that It follows from the implicit theorem and finite covering theorem that there exist two constants such that for each
Now denote and then the entropy condition yields If then one has that
[TABLE]
And if which means then where is a constant, independent of Then one has that
[TABLE]
Similarly, for and with one has that if
[TABLE]
and if i.e. then
[TABLE]
To conclude, one has that
[TABLE]
where (resp. ) is the intersection of the maximal (resp. minimal) backward characteristic of emanating from (resp. ) with -axis. It is noted that then there exist a large and a small such that Equation 4.1 holds true.
Hence, it follows from Equation 4.1 that
[TABLE]
Thus, for all
[TABLE]
Since Equation 4.7 implies that after some positive time 3. iii)
and Define . Similar to the case ii), there exist and such that for all
[TABLE]
Therefore, by similar arguments to that in ii), one can obtain that and coincide after some positive time. 4. iv)
and The proof is same as above.
∎
Proof of Theorem 2.1.
Denote for Then due to 3.5 and 3.1, to finish the proof of 2.1, it remains to prove the convergence of as
For any fixed one can first choose large enough, such that and for all see Figure 2.
Then integrating the equation Equation 1.1 over the trapezium bounded by -axis, the line and yields that
[TABLE]
where the second equality follows from 3.5 and Equation 3.6. Also, 3.5 implies that
[TABLE]
where the bound in depends only on And Equation 1.9 yields that
[TABLE]
where Equation 3.3 is used and is defined in Equation 2.7. Then it follows from Equations 4.8, 4.9 and 4.10 that
[TABLE]
which finishes the proof of 2.1.
∎
5. Stabilities of rarefaction waves and constants
In this section, we consider the initial data Equation 1.8 where To study the large time behaviors of and , two time-invariant variables are introduced.
For any fixed we first let denote a large integer, such that and for all see Figure 3.
Then 3.5 implies that
[TABLE]
Moreover, when (or ), 3.5 and Equation 3.4 yield that the integral
[TABLE]
is bounded and periodic with respect to Hence, for each we can well define
[TABLE]
It is found that these two functions are actually time-invariant:
Proposition 5.1**.**
There exist two points such that for all
[TABLE]
Proof.
We prove only Equation 5.2, since the other one is similar.
By Equation 1.9, one has that
[TABLE]
Then it follows from Equation 3.4 and that
[TABLE]
Thus one can find a point such that
[TABLE]
which implies that
[TABLE]
This, with 3.2 yields that
[TABLE]
Then by applying 3.2 once more, Equation 5.5 implies that for all
[TABLE]
which means that for all
[TABLE]
Thus, for each fixed by integrating the equation Equation 1.1 over the parallelogram and applying 3.5, Equation 3.6 and Equation 5.5, one can finish the proof. ∎
Now, with the two time-invariant variables and we will estimate the distances and
Lemma 5.2**.**
There exists a constant independent of time such that for all
[TABLE]
Proof.
We prove only Equation 5.8, since the other one is similar.
- i)
If By the definition Equation 3.9, Equation 5.8 holds true obviously.
- ii)
If Denote It is noted that both and the straight line (see Equation 5.5) are forward characteristics of then for
[TABLE]
where and
Thus
[TABLE]
where and Hence, if Equation 5.8 holds true. And if then
[TABLE]
This, with yields that The proof of the lemma is finished.
∎
Once obtained the large time behaviors of and , the stabilities of rarefaction waves and constants under two different periodic perturbations are easily proved.
Proof of 2.2.
Assume that in Equation 1.8. Then for each fixed we prove Equation 2.8 in the following cases.
- i)
If Equation 2.8 follows from 3.5 and 3.1 immediately.
- ii)
If then
[TABLE]
and it follows from 5.2 that
[TABLE]
Hence, one can get that
[TABLE]
which implies Equation 2.8.
- iii)
If Equation 5.13 still holds true, and then Equation 2.8 follows immediately.
- iv)
The proof of remaining cases are similar to i) and ii).
∎
Proof of 2.3.
Assume that in Equation 1.8. Then the proof is similar to that of 2.2, regardless of the case iii).
∎
Acknowledgments: The authors would like to thank Zhouping Xin for his great suggestions on this topic, and Peng Qu for many helpful discussions.
The reference list from the paper itself. Each links out to its DOI / PubMed record.
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- 2[2] by same author, Hyperbolic conservation laws in continuum physics , vol. 325, Springer-Verlag, Berlin, 2000.
- 3[3] J. Glimm, Solutions in the large for nonlinear hyperbolic systems of equations , Comm. Pure Appl. Math. 18 (1965), 697–715.
- 4[4] J. Glimm and P. D. Lax, Decay of solutions of systems of nonlinear hyperbolic conservation laws , American Mathematical Society, Providence, R.I., 1970.
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- 8[8] T.-P. Liu, Invariants and asymptotic behavior of solutions of a conservation law , Proc. Amer. Math. Soc. 71 (1978), no. 2, 227–231. MR 500495
