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Hindawi Publishing Corporation Abstract and Applied Analysis Volume 2012, Article ID 872187, 15 pages doi:10.1155/2012/872187 Research Article The Well-Posedness of Solutions for a Generalized Shallow Water Wave Equation Shaoyong Lai and Aiyin Wang Department of Applied Mathematics, Southwestern University of Finance and Economics, Chengdu 610074, China Correspondence should be addressed to Shaoyong Lai, [email protected] Received 9 January 2012; Accepted 28 March 2012 Academic Editor: Yonghong Wu Copyright q 2012 S. Lai and A. Wang. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. A nonlinear partial dierential equation containing the famous Camassa-Holm and Degasperis- Procesi equations as special cases is investigated. The Kato theorem for abstract dierential equa- tions is applied to establish the local well-posedness of solutions for the equation in the Sobolev space H s R with s> 3/2. Although the H 1 -norm of the solutions to the nonlinear model does not remain constant, the existence of its weak solutions in the lower-order Sobolev space H s with 1 s 3/2 is proved under the assumptions u 0 H s and u 0x L < . 1. Introduction Constantin and Lannes 1 derived the shallow water equation u t u x 3 2 ρuu x μ ( αu xxx βu txx ) ρμ ( γu x u xx δuu xxx ) , 1.1 where the constants α, β, γ, δ, ρ, and μ satisfy certain conditions. Under several restrictions on the coecients of model 1.1, the large time well-posedness was established on a time scale O|ρ| 1 provided that the initial value u 0 belongs to H s R with s> 5/2, and the wave-break- ing phenomena were also discussed in 1. As stated in 1, using suitable mathematical trans- formations, one can turn 1.1 into the form u t u txx 2ku x muu x au x u xx buu xxx , 1.2

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Page 1: The Well-Posedness of Solutions for a Generalized Shallow Water

Hindawi Publishing CorporationAbstract and Applied AnalysisVolume 2012, Article ID 872187, 15 pagesdoi:10.1155/2012/872187

Research ArticleThe Well-Posedness of Solutions fora Generalized Shallow Water Wave Equation

Shaoyong Lai and Aiyin Wang

Department of Applied Mathematics, Southwestern University of Finance and Economics,Chengdu 610074, China

Correspondence should be addressed to Shaoyong Lai, [email protected]

Received 9 January 2012; Accepted 28 March 2012

Academic Editor: Yonghong Wu

Copyright q 2012 S. Lai and A. Wang. This is an open access article distributed under the CreativeCommons Attribution License, which permits unrestricted use, distribution, and reproduction inany medium, provided the original work is properly cited.

A nonlinear partial differential equation containing the famous Camassa-Holm and Degasperis-Procesi equations as special cases is investigated. The Kato theorem for abstract differential equa-tions is applied to establish the local well-posedness of solutions for the equation in the SobolevspaceHs(R)with s > 3/2. Although theH1-norm of the solutions to the nonlinear model does notremain constant, the existence of its weak solutions in the lower-order Sobolev space Hs with1 ≤ s ≤ 3/2 is proved under the assumptions u0 ∈ Hs and ‖u0x‖L∞ < ∞.

1. Introduction

Constantin and Lannes [1] derived the shallow water equation

ut + ux +32ρuux + μ

(αuxxx + βutxx

)= ρμ

(γuxuxx + δuuxxx

), (1.1)

where the constants α, β, γ, δ, ρ, and μ satisfy certain conditions. Under several restrictions onthe coefficients of model (1.1), the large time well-posedness was established on a time scaleO(|ρ|−1) provided that the initial value u0 belongs toHs(R)with s > 5/2, and the wave-break-ing phenomenawere also discussed in [1]. As stated in [1], using suitablemathematical trans-formations, one can turn (1.1) into the form

ut − utxx + 2kux +muux = auxuxx + buuxxx, (1.2)

Page 2: The Well-Posedness of Solutions for a Generalized Shallow Water

2 Abstract and Applied Analysis

where a, b, k, and m are constants. Obviously, (1.2) is a generalization of both the Camassa-Holm equation [2]

ut − utxx + 2kux + 3uux = 2uxuxx + uuxxx, k is a constant (1.3)

and the Degasperis-Procesi model [3]

ut − uxxt + 2kux + 4uux = 3uxuxx + uuxxx. (1.4)

Equations (1.3) and (1.4) are bi-Hamiltonian and arise in the modeling of shallow waterwaves. These two equations pertain to waves of medium amplitude (cf. the discussionsin [1, 4]) and accommodate wave-breaking phenomena. Moreover, the Camassa-Holm andDegasperis-Procesi models admit peaked (periodic as well as solitary) traveling waves cap-turing the main feature of the exact traveling wave solutions of the greatest height of thegoverning equations for water waves (cf. [5, 6]). For other dynamic properties about (1.3)and (1.4), the reader is referred to [7–20].

Recently, Lai andWu [21] investigate (1.2) in the case where k = 0,m = a+b, a > 0, andb > 0. The well-posedness of global solutions is established in [21] in Sobolev space Hs(R)with s > 3/2 under certain assumptions on the initial value. The local strong and weak solu-tions for (1.2) are discussed in [22] in the case where b > 0, a, k, andm are arbitrary constants.

Motivated by the desire to extend the work in [22], we investigate the following gene-ralized model of (1.2):

ut − utxx + 2kux +muux = auxuxx + buuxxx + βunx, (1.5)

where b > 0, a, k,m, and β are arbitrary constants, and n is a positive integer.The aim of this paper is to investigate (1.5). Since a, b,m, and β are arbitrary constants,

we do not have the result that the H1 norm of the solution of (1.5) remains constant. We willapply the Kato theorem [23] to prove the existence and uniqueness of local solutions for (1.5)in the space C([0, T),Hs(R))

⋂C1([0, T),Hs−1(R))(s > 3/2) provided that the initial value

u0(x) belongs to Hs(R)(s > 3/2). Moreover, it is shown that there exists a weak solution of(1.5) in lower-order Sobolev space Hs(R)with 1 ≤ s ≤ 3/2.

The structure of this paper is as follows. The main results are given in Section 2. Theexistence and uniqueness of the local strong solution for the Cauchy problem (1.5) are provedin Section 3. The existence of weak solutions is established in Section 4.

2. Main Results

Firstly, we give some notations.The space of all infinitely differentiable functions φ(t, x) with compact support in

[0,+∞) × R is denoted by C∞0 . We let Lp = Lp(R)(1 ≤ p < +∞) be the space of all measurable

functions h such that ‖h‖pLp =∫R |h(t, x)|pdx < ∞. We define L∞ = L∞(R) with the standard

norm ‖h‖L∞ = infm(e)=0 supx∈R\e|h(t, x)|. For any real number s, we letHs = Hs(R) denote theSobolev space with the norm defined by

‖h‖Hs =(∫

R

(1 + |ξ|2

)s∣∣∣h(t, ξ)∣∣∣2dξ

)1/2

< ∞, (2.1)

Page 3: The Well-Posedness of Solutions for a Generalized Shallow Water

Abstract and Applied Analysis 3

where h(t, ξ) =∫R e

−ixξh(t, x)dx. Here, we note that the norms ‖ · ‖pLp , ‖ · ‖L∞ , and ‖ · ‖Hs dependon variable t.

For T > 0 and nonnegative number s, letC([0, T);Hs(R)) denote the space of functionsu : [0, T)×R → Rwith the properties that u(t, ·) ∈ Hs(R) for each t ∈ [0, T], and the mappingu : [0, T) → Hs(R) is continuous and bounded.

For simplicity, throughout this paper, we let c denote any positive constant which isindependent of parameter ε and set Λ = (1 − ∂2x)

1/2.In order to study the existence of solutions for (1.5), we consider its Cauchy problem

in the form

ut − utxx = −∂x(2ku +

m

2u2)+ auxuxx + buuxxx + βun

x,

u(0, x) = u0(x),(2.2)

where b > 0, a, k,m, β, and n are arbitrary constants. Now, we give the theorem to describe thelocal well-posedness of solutions for problem (2.2).

Theorem 2.1. Let u0(x) ∈ Hs(R)with s > 3/2, then the Cauchy problem (2.2) has a unique solutionu(t, x) ∈ C([0, T);Hs(R))

⋂C1([0, T);Hs−1(R)) where T > 0 depends on ‖u0‖Hs(R).

For a real number swith s > 0, suppose that the function u0(x) is inHs(R), and let uε0

be the convolution uε0 = φε � u0 of the function φε(x) = ε−1/4φ(ε−1/4x) and u0 such that theFourier transform φ of φ satisfies φ ∈ C∞

0 , φ(ξ) ≥ 0, and φ(ξ) = 1 for any ξ ∈ (−1, 1). Thus onehas uε0(x) ∈ C∞. It follows from Theorem 2.1 that for each ε satisfying 0 < ε < 1/4, theCauchy problem

ut − utxx = −∂x(2ku +

m

2u2)+ auxuxx + buuxxx + βun

x,

u(0, x) = uε0(x), x ∈ R

(2.3)

has a unique solution uε(t, x) ∈ C∞([0, Tε);H∞), in which Tε may depend on ε. However, onewill show that under certain assumptions, there exist two constants c and T > 0, bothindependent of ε, such that the solution of problem (2.3) satisfies ‖uεx‖L∞ ≤ c for any t ∈[0, T), and there exists a weak solution u(t, x) ∈ L2([0, T],Hs) for problem (2.2). These resultsare summarized in the following two theorems.

Theorem 2.2. If u0(x) ∈ Hs(R) with s ∈ [1, 3/2] such that ‖u0x‖L∞ < ∞, let uε0 be defined as insystem (2.3), then there exist two constants c and T > 0, which are independent of ε, such that thesolution uε of problem (2.3) satisfies ‖uεx‖L∞ ≤ c for any t ∈ [0, T).

Theorem 2.3. Suppose that u0(x) ∈ Hs with 1 ≤ s ≤ 3/2 and ‖u0x‖L∞ < ∞, then there exists a T >0 such that problem (2.2) has a weak solution u(t, x) ∈ L2([0, T],Hs(R)) in the sense of distributionand ux ∈ L∞([0, T] × R).

Page 4: The Well-Posedness of Solutions for a Generalized Shallow Water

4 Abstract and Applied Analysis

3. Proof of Theorem 2.1

Consider the abstract quasilinear evolution equation

dv

dt+A(v)v = f(v), t ≥ 0, v(0) = v0. (3.1)

Let X and Y be Hilbert spaces such that Y is continuously and densely embedded in X, andlet Q : Y → X be a topological isomorphism. Let L(Y,X) be the space of all bounded linearoperators from Y to X. If X = Y , we denote this space by L(X). We state the following con-ditions in which ρ1, ρ2, ρ3, and ρ4 are constants depending only on max{‖y‖Y , ‖z‖Y}:

(I) A(y) ∈ L(Y,X) for y ∈ X with

∥∥(A(y) −A(z)

)w∥∥X ≤ ρ1

∥∥y − z

∥∥X‖w‖Y , y, z, w ∈ Y, (3.2)

and A(y) ∈ G(X, 1, β) (i.e., A(y) is quasi-m-accretive), uniformly on bounded setsin Y .

(II) QA(y)Q−1 = A(y) + B(y), where B(y) ∈ L(X) is bounded, uniformly on boundedsets in Y . Moreover,

∥∥(B(y) − B(z)

)w∥∥X ≤ ρ2

∥∥y − z∥∥Y‖w‖X, y, z ∈ Y, w ∈ X. (3.3)

(III) f : Y → Y extends to a map from X into X, is bounded on bounded sets in Y , andsatisfies

∥∥f(y) − f(z)

∥∥Y ≤ ρ3

∥∥y − z∥∥Y , y, z ∈ Y,

∥∥f(y) − f(z)

∥∥X ≤ ρ4

∥∥y − z∥∥X, y, z ∈ Y.

(3.4)

Kato Theorem (see [23])

Assume that (I), (II), and (III) hold. If v0 ∈ Y , there is a maximal T > 0 depending only on‖v0‖Y and a unique solution v to problem (3.1) such that

v = v(·, v0) ∈ C([0, T);Y )⋂

C1([0, T);X). (3.5)

Moreover, the map v0 → v(·, v0) is a continuous map from Y to the space

C([0, T);Y )⋂

C1([0, T);X). (3.6)

In fact, problem (2.2) can be written as

ut − utxx = −[2ku +

m

2u2]

x+b

2∂3x u

2 − 3b − a

2∂x(u2x

)+ βun

x,

u(0, x) = u0(x),(3.7)

Page 5: The Well-Posedness of Solutions for a Generalized Shallow Water

Abstract and Applied Analysis 5

which is equivalent to

ut + buux = −Λ−2[(

2ku +m

2u2)

x+ buux − 3b − a

2∂x(u2x

)+ βun

x

],

u(0, x) = u0(x).(3.8)

We set A(u) = bu∂x with constant b > 0, Y = Hs(R), X = Hs−1(R), Λ = (1 − ∂2x)1/2,

f(u) = −Λ−2(2ku + (m/2)u2)x + bΛ−2(uux) − ((3b − a)/2)Λ−2∂x(u2x) + βΛ−2un

x, and Q = Λs.We know that Q is an isomorphism of Hs onto Hs−1. In order to prove Theorem 2.1, we onlyneed to check that A(u) and f(u) satisfy assumptions (I)–(III).

Lemma 3.1. The operator A(u) = u∂x with u ∈ Hs(R), s > 3/2 belongs to G(Hs−1, 1, β).

Lemma 3.2. Let A(u) = bu∂x with u ∈ Hs and s > 3/2, then A(u) ∈ L(Hs,Hs−1) for all u ∈ Hs.Moreover,

‖(A(u) −A(z))w‖Hs−1 ≤ ρ1‖u − z‖Hs−1‖w‖Hs , u, z,w ∈ Hs(R). (3.9)

Lemma 3.3. For s > 3/2, u, z ∈ Hs, and w ∈ Hs−1, it holds that B(u) = [Λ, u∂x]Λ−1 ∈ L(Hs−1)for u ∈ Hs and

‖(B(u) − B(z))w‖Hs−1 ≤ ρ2‖u − z‖Hs‖w‖Hs−1 . (3.10)

Proofs of the above Lemmas 3.1–3.3 can be found in [24] or [25].

Lemma 3.4 (see [23]). Let r and q be real numbers such that −r < q ≤ r, then

‖uv‖Hq ≤ c‖u‖Hr‖v‖Hq , if r >12,

‖uv‖Hr+q−1/2 ≤ c‖u‖Hr‖v‖Hq , if r <12.

(3.11)

Lemma 3.5. Let u, z ∈ Hs with s > 3/2 and f(u) = −Λ−2(2ku+(m/2)u2)x + bΛ−2(uux) − ((3b −a)/2)Λ−2∂x(u2

x) + βΛ−2(unx), then f is bounded inHs and satisfies

∥∥f(u) − f(z)∥∥Hs ≤ ρ3‖u − z‖Hs,

∥∥f(u) − f(z)∥∥Hs−1 ≤ ρ4‖u − z‖Hs−1 .

(3.12)

Page 6: The Well-Posedness of Solutions for a Generalized Shallow Water

6 Abstract and Applied Analysis

Proof. Using the algebra property of the space Hs0 with s0 > 1/2 and s − 1 > 1/2, we have

∥∥f(u) − f(z)

∥∥Hs

≤∥∥∥∥Λ

−2((

2ku +m

2u2)

x−(2kz +

m

2z2)

x

)∥∥∥∥Hs

+∥∥∥bΛ−2(uux − zzx)

∥∥∥Hs

+∥∥∥∥3b − a

2Λ−2∂x

(u2x − z2x

)∥∥∥∥Hs

+∥∥∥βΛ−2(un

x − znx)∥∥∥Hs

≤ c

⎝‖u − z‖Hs−1(1 + ‖u‖Hs−1 + ‖z‖Hs−1) +∥∥∥Λ−2

(u2 − z2

)

x

∥∥∥Hs

+∥∥∥u2

x − z2x

∥∥∥Hs−1

+ ‖ux − zx‖Hs−1

n−1∑

j=0‖ux‖n−jHs−1‖zx‖jHs−1

≤ c

⎝‖u − z‖Hs(1 + ‖u‖Hs + ‖z‖Hs) + ‖(u − z)(u + z)‖Hs−1

+∥∥∥u2

x − z2x

∥∥∥Hs−1

+ ‖ux − zx‖Hs−1

n−1∑

j=0‖u‖n−jHs ‖z‖jHs

≤ c‖u − z‖Hs

⎝1 + ‖u‖Hs + ‖z‖Hs +n−1∑

j=0‖u‖n−jHs ‖z‖jHs

≤ cρ3‖u − z‖Hs,

(3.13)

from which we obtain (3.12).Applying Lemma 3.4, uux = 1/2(u2)x, s > 3/2, we get

∥∥f(u) − f(z)∥∥Hs−1

≤ c

(∥∥∥2ku +

m

2u2 −

(2kz +

m

2z2)∥∥∥

Hs−2+∥∥∥u2 − z2

∥∥∥Hs−2

+‖(ux − zx)(ux + zx)‖Hs−2 + ‖unx − znx‖Hs−1

)

≤ c‖u − z‖Hs−2(1 + ‖u‖Hs−1 + ‖z‖Hs−1)

+ c‖ux − zx‖Hs−2(‖ux‖Hs−1 + ‖zx‖Hs−1)

+ c‖ux − zx‖Hs−2

n−1∑

j=0‖ux‖n−jHs−1‖zx‖jHs−1

≤ c‖u − z‖Hs−1

⎝1 + ‖u‖Hs + ‖z‖Hs +n−1∑

j=0‖u‖n−jHs ‖z‖jHs

⎠,

(3.14)

which completes the proof of (3.12).

Page 7: The Well-Posedness of Solutions for a Generalized Shallow Water

Abstract and Applied Analysis 7

Proof of Theorem 2.1. Using the Kato theorem, Lemmas 3.1, 3.2, 3.3, and 3.5, we know that sys-tem (3.11) or problem (2.2) has a unique solution

u(t, x) ∈ C([0, T);Hs(R))⋂

C1([0, T);Hs−1

). (3.15)

4. Proofs of Theorems 2.2 and 2.3

Before establishing the proofs of Theorems 2.2 and 2.3, we give several lemmas.

Lemma 4.1 (Kato and Ponce [26]). If r ≥ 0, thenHr⋂L∞ is an algebra. Moreover,

‖uv‖Hr ≤ c(‖u‖L∞‖v‖Hr + ‖u‖Hr‖v‖L∞), (4.1)

where c is a constant depending only on r.

Lemma 4.2 (Kato and Ponce [26]). Let r > 0. If u ∈ Hr⋂W1,∞ and v ∈ Hr−1⋂L∞, then

‖[Λr , u]v‖L2 ≤ c(‖∂xu‖L∞

∥∥∥Λr−1v∥∥∥L2

+ ‖Λru‖L2‖v‖L∞

), (4.2)

where [Λr , u]v = Λr(uv) − uΛrv.Using the first equation of problem (2.2) gives rise to

d

dt

[∫

R

(u2 + u2

x

)dx

]+ (a − 2b)

R

(ux)3dx = 2β∫

R

uunx dx, (4.3)

from which one has

R

(u2 + u2

x

)dx +

∫ t

0

[∫

R

((a − 2b)u3

x − 2βuunx

)dx

]dτ =

R

(u20 + u2

0x

)dx. (4.4)

Lemma 4.3. Let s ≥ 3/2, and the function u(t, x) is a solution of the problem (2.2) and the initial datau0(x) ∈ Hs, then it holds that

‖u‖L∞ ≤ c‖u‖H1 ≤ c‖u0‖H1ec0∫ t0(‖ux‖L∞+‖ux‖n−1L∞ )dτ , (4.5)

where c0 = 1/2max(|a − 2b|, |β|).For q ∈ (0, s − 1], there is a constant c depending only on q such that

R

(Λq+1u

)2dx ≤

R

(Λq+1u0

)2dx + c

∫ t

0

(‖ux‖L∞ + ‖ux‖n−1L∞

)‖u‖2Hq+1 dτ. (4.6)

If q ∈ [0, s − 1], there is a constant c depending only on q such that

‖ut‖Hq ≤ c‖u‖Hq+1

(1 + ‖u‖H1 + ‖ux‖n−1L∞

). (4.7)

Page 8: The Well-Posedness of Solutions for a Generalized Shallow Water

8 Abstract and Applied Analysis

Proof. Using ‖u‖2H1 ≤ c

∫R(u

2 + u2x)dx and (4.4) derives (4.5).

We write (1.5) in the equivalent form

ut − utxx = −[2ku +

m

2u2]

x+b

2∂3xu

2 − 3b − a

2∂x(u2x

)+ βun

x. (4.8)

Applying ∂2x = −Λ2 + 1 and the Parseval’s equality gives rise to

R

ΛquΛq∂3x

(u2)dx = −2

R

(Λq+1u

)Λq+1(uux)dx + 2

R

(Λqu)Λq(uux)dx. (4.9)

For q ∈ (0, s − 1], applying (Λqu)Λq on both sides of (4.8), noting the above equality,and integrating the new equation with respect to x by parts, we obtain the equation

12d

dt

[∫

R

((Λqu)2 + (Λqux)

2)dx

]

= −∫

R

(Λqu)Λq[2ku +

m

2u2]

xdx − b

R

(Λq+1u

)Λq+1(uux)dx

+3b − a

2

R

(Λqux)Λq(u2x

)dx + b

R

(Λqu)Λq(uux)dx + β

R

ΛquΛqunx dx.

(4.10)

Wewill estimate each of the terms on the right-hand side of (4.10). For the first and thefourth terms, using integration by parts, the Cauchy-Schwartz inequality, and Lemmas 4.1-4.2, we have

∫R(Λ

qu)Λq(uux)dx =∫

R

(Λqu)[Λq(uux) − uΛqux]dx +∫

R

(Λqu)uΛqux dx

≤ c‖u‖Hq(‖ux‖L∞‖u‖Hq + ‖ux‖L∞‖u‖Hq)

+12‖ux‖L∞‖Λqu‖2L2

≤ c‖u‖2Hq‖ux‖L∞ ,

(4.11)

where c only depends on q. Using the above estimate to the second term yields

R

(Λq+1u

)Λq+1(uux)dx ≤ c‖u‖2Hq+1‖ux‖L∞ . (4.12)

Page 9: The Well-Posedness of Solutions for a Generalized Shallow Water

Abstract and Applied Analysis 9

For the third term, using Lemma 4.1 gives rise to

R

(Λqux)Λq(u2x

)dx ≤ ‖Λqux‖L2

∥∥∥Λqu2

x

∥∥∥L2

≤ c‖u‖Hq+1‖ux‖L∞‖ux‖Hq

≤ c‖u‖2Hq+1‖ux‖L∞ .

(4.13)

For the last term, using Lemma 4.1 repeatedly, we get

∣∣∣∣

R

(Λqu)Λq(ux)ndx∣∣∣∣ ≤ ‖u‖Hq‖un

x‖Hq ≤ c‖u‖2Hq+1‖ux‖n−1L∞ . (4.14)

It follows from (4.10)–(4.14) that

12

R

[(Λqu)2 + (Λqux)

2]dx − 1

2

R

[(Λqu0)

2 + (Λqu0x)2]dx

≤ c

∫ t

0

(‖ux‖L∞ + ‖ux‖n−1L∞

)‖u‖2Hq+1dτ,

(4.15)

which results in (4.6). Applying the operator (1 − ∂2x)−1 on both sides of (4.8) yields the equa-

tion

ut =(1 − ∂2x

)−1[−[2ku +

m

2u2]

x+b

2∂3xu

2 − 3b − a

2∂x(u2x

)+ βun

x

].

(4.16)

Multiplying both sides of (4.16) by (Λqut)Λq for q ∈ [0, s − 1] and integrating the resultantequation by parts give rise to

R

(Λqut)2dx

=∫

R

(Λqut)(1 − ∂2x

)−1Λq

[−[2ku +

m

2u2]

x+b

2∂3xu

2 − 3b − a

2∂x(u2x

)+ βun

x

]dx.

(4.17)

On the right-hand side of (4.17), we have

∣∣∣∣

R

(Λqut)(1 − ∂2x

)−1Λq(−2kux)dx

∣∣∣∣ ≤ |2k|‖ut‖Hq‖u‖Hq , (4.18)

Page 10: The Well-Posedness of Solutions for a Generalized Shallow Water

10 Abstract and Applied Analysis∣∣∣∣

R

(Λqut)(1 − ∂2x

)−1Λq∂x

(−m2u2 − 3b − a

2u2x

)dx

∣∣∣∣

≤‖ut‖Hq ×(∫

R

(1 + ξ2

)q−1dξ

(∫

R

[m

2u(ξ − η

)u(η)+3b − a

2ux

(ξ − η

)ux

(η)]dη

)2)1/2

≤ c‖ut‖Hq

(∫

R

c(‖u‖Hq‖u‖L2 + ‖ux‖L2‖ux‖Hq)1 + ξ2

)1/2

≤ c‖ut‖Hq‖u‖H1‖u‖Hq+1 ,

(4.19)

in which we have used Lemma 4.1. As

R

(Λqut)(1 − ∂2x

)−1Λq∂2x(uux)dx = −

R

(Λqut)Λq(uux)dx

+∫

R

(Λqut)(1 − ∂2x

)−1Λq(uux)dx,

(4.20)

by using ‖uux‖Hq ≤ c‖u2‖Hq+1 ≤ c‖u‖L∞‖u‖Hq+1 ≤ c‖u‖H1‖u‖Hq+1 , we have

∣∣∣∣

R

(Λqut)Λq(uux)dx∣∣∣∣ ≤ c‖ut‖Hq‖uux‖Hq ≤ c‖ut‖Hq‖u‖H1‖u‖Hq+1 , (4.21)

∣∣∣∣

R

(Λqut)(1 − ∂2x

)−1Λq(uux)dx

∣∣∣∣ ≤ c‖ut‖Hq‖u‖H1‖u‖Hq+1 . (4.22)

Using the Cauchy-Schwartz inequality and Lemma 4.1 yields

∣∣∣∣

R

(Λqut)(1 − ∂2x

)−1Λq(un

x)dx∣∣∣∣ ≤ c‖ut‖Hq‖ux‖n−1L∞ ‖u‖Hq+1 . (4.23)

Applying (4.18)–(4.23) to (4.17) yields the inequality

‖ut‖Hq ≤ c‖u‖Hq+1

(1 + ‖u‖H1 + ‖ux‖n−1

), (4.24)

for a constant c > 0.

Page 11: The Well-Posedness of Solutions for a Generalized Shallow Water

Abstract and Applied Analysis 11

Lemma 4.4. For s > 0, u0 ∈ Hs(R), and uε0 = φε � u0, the following estimates hold for any ε withε ∈ (0, 1/4) :

‖uε0x‖L∞ ≤ c‖u0x‖L∞ , ‖uε0‖Hq ≤ c if q ≤ s,

‖uε0‖Hq ≤ cε(s−q)/4 if q > s,

‖uε0 − u0‖Hq ≤ cε(s−q)/4 if q ≤ s,

‖uε0 − u0‖Hs = o(1),

(4.25)

where c is a constant independent of ε.

The proof of this lemma can be found in [21].Applying Lemmas 4.3 and 4.4, we can now state the following lemma, which plays an

important role in proving existence of weak solutions.

Lemma 4.5. For s ≥ 1 and u0 ∈ Hs(R), there exists a constant c independent of ε, such that thesolution uε of problem (2.3) satisfies

‖uε‖H1 ≤ cec0∫ t0(‖uεx‖L∞+‖uεx‖n−1L∞ )dτ for t ∈ [0, Tε), (4.26)

where c0 = 1/2max(|a − 2b|, |β|).

Proof. The proof can be directly obtained from Lemma 4.4 and inequality (4.5).

Proof of Theorem 2.2. Using notation u = uε and differentiating (4.16) with respect to x giverise to

uxt + buuxx +a − b

2u2x = 2ku +

m − b

2u2

−Λ−2[2ku +

m − b

2u2 +

3b − a

2u2x − β(un

x)x

].

(4.27)

Using

R

uuxx(ux)2p+1dx =∫

R

u(ux)2p+1dux

= −∫

R

ux

[(ux)2p+2 +

(2p + 1

)u(ux)2puxx

]dx,

(4.28)

we get

R

uuxx(ux)2p+1dx = − 12p + 2

R

(ux)2p+3dx. (4.29)

Page 12: The Well-Posedness of Solutions for a Generalized Shallow Water

12 Abstract and Applied Analysis

Letting p > 0 be an integer and multiplying (4.27) by (ux)2p+1 and then integrating the

resulting equation with respect to x yield the equality

12p + 2

d

dt

R

(ux)2p+2dx +(a − b)p + a − 2b

2p + 2

R

(ux)2p+3dx

=∫

R

(ux)2p+1(2ku +

m − b

2u2)dx

−∫

R

(ux)2p+1Λ−2[2ku +

m − b

2u2 +

3b − a

2u2x − β(un

x)x

]dx.

(4.30)

Applying the Holder’s inequality, we get

12p + 2

d

dt

R

(ux)2p+2dx ≤⎧⎨

(∫

R

∣∣∣∣2ku +m − b

2u2∣∣∣∣

2p+2

dx

)1/(2p+2)

+(∫

R

|G|2p+2dx)1/(2p+2)

}(∫

R

|ux|2p+2dx) (2p+1)/(2p+2)

+∣∣∣∣(a − b)p + a − 2b

2p + 2

∣∣∣∣‖ux‖L∞

R

|ux|2p+2dx,

(4.31)

or

d

dt

(∫

R

(ux)2p+2dx) 1/(2p+2)

≤⎧⎨

(∫

R

∣∣∣∣2ku +m − b

2u2∣∣∣∣

2p+2

dx

) 1/(2p+2)

+(∫

R

|G|2p+2dx)1/(2p+2)

⎫⎬

+∣∣∣∣(a − b)p + a − 2b

2p + 2

∣∣∣∣‖ux‖L∞

(∫

R

|ux|2p+2dx)1/(2p+2)

,

(4.32)

where

G = Λ−2[2ku +

m − b

2u2 +

3b − a

2u2x − β(un

x)x

]. (4.33)

Since ‖f‖Lp → ‖f‖L∞ as p → ∞ for any f ∈ L∞⋂L2, integrating (4.32) with respect to t andtaking the limit as p → ∞ result in the estimate

‖ux‖L∞ ≤ ‖u0x‖L∞ +∫ t

0

[c

(∥∥∥∥2ku +m − b

2u2∥∥∥∥L∞

+ ‖G‖L∞

)+a − b

2‖ux‖2L∞

]dτ. (4.34)

Page 13: The Well-Posedness of Solutions for a Generalized Shallow Water

Abstract and Applied Analysis 13

Using the algebraic property of Hs0(R)with s0 > 1/2 and Lemma 4.5 leads to

∥∥∥∥2ku +

m − b

2u2∥∥∥∥L∞

≤ c

∥∥∥∥2ku +

m − b

2u2∥∥∥∥H1/2+

≤ c(‖u‖H1 + ‖u‖2H1

)

≤ ce2c0∫ t0(‖ux‖L∞+‖ux‖n−1L∞ )dτ ,

(4.35)

‖G‖L∞ =∥∥∥∥Λ

−2[2ku +

m − b

2u2 +

3b − a

2u2x − β(un

x)x

]∥∥∥∥L∞

≤ c

(∥∥∥∥Λ

−2(2ku +

m − b

2u2)∥∥∥∥H1/2+

+∥∥∥Λ−2u2

x

∥∥∥H1/2+

+∥∥∥Λ−2(un

x)x∥∥∥H1/2+

)

≤ c

(∥∥∥∥2ku +m − b

2u2∥∥∥∥H1/2+

+ ‖u‖H1‖ux‖L∞ + ‖unx‖H0

)

≤ c(‖u‖H1 + ‖u‖2H1 + ‖u‖H1‖ux‖L∞ + ‖u‖H1‖ux‖n−1L∞

)

≤ c(1 + ‖ux‖L∞ + ‖ux‖n−1L∞

)e2c0

∫ t0(‖ux‖L∞+‖ux‖n−1L∞ )dτ ,

(4.36)

where c is independent of ε, c0 = 1/2max(|a − 2b|, |β|) and H1/2+ means that there exists asufficiently small δ > 0 such that ‖uε‖H1/2+ = ‖uε‖H1/2+δ . From Lemma 4.5, we have

∫ t

0‖G‖L∞dτ ≤ c

∫ t

0

(1 + ‖ux‖L∞ + ‖ux‖n−1L∞

)× e2c0

∫τ0 (‖ux‖L∞+‖ux‖n−1L∞ )dξ dτ. (4.37)

Applying (4.25), (4.34), (4.35), and (4.37) and writing out the subscript ε of u, weobtain

‖uεx‖L∞ ≤ c‖u0x‖L∞

+ c

∫ t

0

[(1 + ‖uεx‖L∞ + ‖uεx‖n−1L∞

)× e2c0

∫τ0 (‖uεx‖L∞+‖uεx‖n−1L∞ )dξ + ‖uεx‖2L∞

]dτ.

(4.38)

It follows from the contraction mapping principle that there is a T > 0 such that theequation

‖W‖L∞ = c‖u0x‖L∞

+ c

∫ t

0

[(1 + ‖W‖L∞ + ‖W‖n−1L∞

)× e2c0

∫τ0 (‖W‖L∞+‖W‖n−1L∞ )dξ + ‖W‖2L∞

]dτ

(4.39)

has a unique solution W ∈ C[0, T]. From (4.39), we know that the variable T only dependson c and ‖u0x‖L∞ . Using the theorem presented on page 51 in [16] or Theorem 2 in Section 1.1

Page 14: The Well-Posedness of Solutions for a Generalized Shallow Water

14 Abstract and Applied Analysis

in [27] derives that there are constants T > 0 and c > 0 independent of ε such that ‖uεx‖L∞ ≤W(t) for arbitrary t ∈ [0, T], which leads to the conclusion of Theorem 2.

Remark 4.6. Under the assumptions of Theorem 2.2, there exist two constants T and c, bothindependent of ε, such that the solution uε of problem (2.3) satisfies ‖uεx‖L∞ ≤ c for any t ∈[0, T]. This states that in Lemma 4.5, there exists a T independent of ε such that (4.26) holds.

Using Theorem 2.2, Lemma 4.5, (4.6), (4.7), notation uε = u, and Gronwall’s inequalityresults in the inequalities

‖uε‖Hq ≤ c exp

[

c

∫ t

0

(‖uεx‖L∞ + ‖uεx‖n−1L∞

)dτ

]

≤ c,

‖uεt‖Hr ≤ ‖uε‖Hr+1

(1 + ‖uε‖H1 + ‖uεx‖n−1L∞

)≤ c,

(4.40)

where q ∈ (0, s], r ∈ (0, s − 1], and t ∈ [0, T). It follows from Aubin’s compactness theo-remthat there is a subsequence of {uε}, denoted by {uεn1

}, such that {uεn1} and their temporal

derivatives {uεn1 t} are weakly convergent to a function u(t, x) and its derivative ut in L2([0, T],

Hs) and L2([0, T],Hs−1), respectively. Moreover, for any real number R1 > 0, {uεn1} is con-

vergent to the function u strongly in the space L2([0, T],Hq(−R1, R1)) for q ∈ (0, s], and {uεn1 t}

converges to ut strongly in the space L2([0, T],Hr(−R1, R1)) for r ∈ [0, s − 1].

Proof of Theorem 2.3. From Theorem 2.2, we know that {uεn1x}(εn1 → 0) is bounded in the

space L∞. Thus, the sequences{uεn1}, {uεn1x

}, {u2εn1x

}, and {unεn1x

} are weakly convergent to u,ux, u2

x, and unx in L2([0, T],Hr(−R1, R1)) for any r ∈ [0, s−1), separately. Hence, u satisfies the

equation

−∫T

0

R

u(gt − gxxt

)dx dt =

∫T

0

R

[(2ku +

m

2u2 +

3b − a

2u2x

)gx − b

2u2gxxx − βun

xg

]dxdt,

(4.41)

with u(0, x) = u0(x) and g ∈ C∞0 . Since X = L1([0, T] × R) is a separable Banach space and

{uεn1x} is a bounded sequence in the dual space X∗ = L∞([0, T] × R) of X, there exists a

subsequence of {uεn1x}, still denoted by {uεn1x

}, weakly star convergent to a function v inL∞([0, T]×R). As {uεn1x

}weakly converges to ux in L2([0, T]×R), it results that ux = v almosteverywhere. Thus, we obtain ux ∈ L∞([0, T] × R).

Acknowledgment

This work is supported by the Applied and Basic Project of Sichuan Province (2012JY0020).

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