1 Introduction

Recently, the following generalized periodic Degasperis-Procesi equation (μ DP) was introduced and studied in [13]

μ ( u ) t u t x x +3μ(u) u x =3 u x u x x +u u x x x ,

where u(t,x) is a time-dependent function on the unite circle S=R/Z and μ(u)= S u(t,x)dx denotes its mean. The μ DP equation can be formally described as an evolution equation on the space of tensor densities over the Lie algebra of smooth vector fields on the circle S. In [2], the authors verified that the periodic μ DP equation describes the geodesic flows of a right-invariant affine connection on the Fréchet Lie group Diff (S) of all smooth and orientation-preserving diffeomorphisms of the circle S.

Analogous to the generalized periodic Camassa-Holm (μ CH) equation [46], μ DP equation possesses bi-Hamiltonian form and infinitely many conservation laws. Here we list some of the simplest conserved quantities:

H 0 = 9 2 S ydx, H 1 = 1 2 S u 2 dx, H 2 = S ( 3 2 μ ( u ) ( A 1 x u ) 2 + 1 6 u 3 ) dx,

where y=μ(u) u x x , A=μ x 2 is an isomorphism between H S and H s 1 . Moreover, it is easy to see that S u(t,x)dx is also a conserved quantity for the μ DP equation.

Obviously, under the constraint of μ0, the μ DP equation is reduced to the μ Burgers equation [7].

It is clear that the closest relatives of the μ DP equation are the DP equation [811]

u t u t x x +4u u x =3 u x u x x +u u x x x ,

which was derived by Degasperis and Procesi in [8] as a model for the motion of shallow water waves, and its asymptotic accuracy is the same as for the Camassa-Holm equation.

Generally speaking, energy dissipation is a very common phenomenon in the real world. It is interesting for us to study this kind of equation. Recently, Wu and Yin [12] considered the weakly dissipative Degasperis-Procesi equation. For related studies, we refer to [13] and [14]. Liu and Yin [15] discussed the blow-up, global existence for the weakly dissipative μ-Hunter-Saxton equation.

In this paper, we investigate the Cauchy problem of the following weakly dissipative periodic Degasperis-Procesi equation [16]:

{ μ ( u ) t u t x x + 3 μ ( u ) u x = 3 u x u x x + u u x x x λ ( μ ( u ) u x x ) , t > 0 , x R , u ( 0 , x ) = u 0 ( x ) , x R , u ( t , x + 1 ) = u ( t , x ) , t 0 , x R ,
(1.1)

the constant λ is a nonnegative dissipative parameter and the term λy=λ(μ(u) u x x ) models energy dissipation. Obviously, if λ=0 then the equation reduces to the μ DP equation. we can rewrite the system (1.1) as follows:

{ y t + u y x + 3 u x y + λ y = 0 , t > 0 , x R , y = μ ( u ) u x x , t > 0 , x R , u ( 0 , x ) = u 0 ( x ) , x R , u ( t , x + 1 ) = u ( t , x ) , t 0 , x R .
(1.2)

Let G(x):= 1 2 x 2 1 2 |x|+ 13 12 , xR be the associated Green’s function of the operator A 1 , then the operator can be expressed by its associated Green’s function,

A 1 f(x)=(Gf)(x),f L 2 ,

where ∗ denotes the spatial convolution. Then equation (1.1) takes the equivalent form of a quasi-linear evolution equation of hyperbolic type:

{ u t + u u x + 3 μ ( u ) A 1 x u + λ u = 0 , t > 0 , x R , u ( 0 , x ) = u 0 ( x ) , x R , u ( t , x + 1 ) = u ( t , x ) , t 0 , x R .
(1.3)

It is easy to check that the operator A=μ x 2 has the inverse

( A 1 f ) ( x ) = ( 1 2 x 2 1 2 x + 13 12 ) μ ( f ) + ( x 1 2 ) 0 1 0 y f ( s ) d s d y 0 x 0 y f ( s ) d s d y + 0 1 0 y 0 s f ( r ) d r d s d y .
(1.4)

Since A 1 and x commute, the following identities hold:

( A 1 x f ) (x)= ( x 1 2 ) 0 1 f(x)dx 0 x f(y)dy+ 0 1 0 x f(y)dydx
(1.5)

and

( A 1 x 2 f ) (x)=f(x)+ 0 1 f(x)dx.
(1.6)

The paper is organized as follows. In Section 2, we briefly give some needed results, including the local well-posedness of equation (1.1), and some useful lemmas and results which will be used in subsequent sections. In Section 3, we establish the precise blow-up scenarios and blow-up criteria of strong solutions. In Section 4, we give the blow-up rate of strong solutions. In Section 5, we give two global existence results of strong solutions.

Remark 1.1 Although blow-up criteria and global existence results of strong solutions to equation (1.1) are presented in [16], our blow-up results improve considerably earlier results.

2 Preliminaries

In this section we recall some elementary results which we want to use in this paper. We list them and skip their proofs for conciseness. Local well-posedness for equation (1.1) can be obtained by Kato’s theory [17], in [16] the authors gave a detailed description on well-posedness theorem.

Theorem 2.1 [16]

Let s>3/2 and u 0 H s (S); then there is a maximal time T and a unique solution

uC ( [ 0 , T ) ; H s ( S ) ) C 1 ( [ 0 , T ) ; H s 1 ( S ) )

of the Cauchy problems (1.1) which depends continuously on the initial data, i.e. the mapping

H s (S)C ( [ 0 , T ) ; H s ( S ) ) C 1 ( [ 0 , T ) ; H s 1 ( S ) ) , u 0 u(, u 0 ),

is continuous.

Remark 2.1 The maximal time of existence T>0 in Theorem 2.1 is independent of the Sobolev index s>3/2.

Next we present the Sobolev-type inequalities, which play a key role to obtain blow-up results for the Cauchy problem (1.1) in the sequel.

Lemma 2.2 [18]

If f H 1 (S) is such that S f(x)dx=0, then we have

max x S f 2 (x) 1 12 S f x 2 (x)dx.

Lemma 2.3 [19]

If r>0, let Λ= ( 1 x 2 ) 1 / 2 , then

[ Λ r , f ] g L 2 c ( x f L Λ r 1 g L 2 + Λ r f L 2 g L ) ,

where c is a constant depending only on r.

Lemma 2.4 [20]

Let t 0 >0 and v C 1 ([0, t 0 ); H 2 (R)), then for every t[0, t 0 ) there exists at least one point ξ(t)R with

m(t):= inf x R v x (t,x)= v x ( t , ξ ( t ) ) ,

and the function m is almost everywhere differentiable on (0, t 0 ) with

d d t m(t)= v t x ( t , ξ ( t ) ) a.e. on (0, t 0 ).

We also need to introduce the classical particle trajectory method which is motivated by McKean’s deep observation for the Camassa-Holm equation in [21]. Suppose u(x,t) is the solution of the Camassa-Holm equation and q(x,t) satisfies the following equation:

{ q t = u ( q , t ) , 0 < t < T , x R , q ( x , 0 ) = x , x R , q ( x + 1 , t ) = x , 0 < t < T , x R ,
(2.1)

where T is the maximal existence time of solution, then q(t,) is a diffeomorphism of the line. Taking the derivative with respect to x, we have

d q x d t = q t x = u x (q,t) q x ,t(0,T).

Hence

q x (x,t)=exp ( 0 t u x ( q , s ) d s ) >0, q x (x,0)=1,
(2.2)

which is always positive before the blow-up time.

In addition, integrating both sides of the first equation in equation (1.1) with respect to x on S, we obtain

d d t μ(u)=λμ(u),

it follows that

μ(u)=μ( u 0 ) e λ t := μ 0 e λ t ,
(2.3)

where

μ 0 :=μ( u 0 )= S u 0 (x)dx.
(2.4)

3 Blow-up solutions

In this section, we are able to derive an import estimate for the L -norm of strong solutions. This enables us to establish precise blow-up scenario and several blow-up results for equation (1.1).

Lemma 3.1 Let u 0 H s , s>3/2 be given and assume the T is the maximal existence time of the corresponding solution u to equation (1.1) with the initial data u 0 . Then we have

u ( t , x ) L e λ t ( 3 | μ 0 | ( 1 2 | μ 0 | + 2 μ 2 ) λ + u 0 L ) ,t[0,T).
(3.1)

Proof The first equation of the Cauchy problem (1.1) is

u t +u u x +3μ(u) A 1 x u+λu=0.

In view of equation (1.5), we have

| A 1 x u| 1 2 | μ 0 | e λ t +2 ( S u 2 d x ) 1 2 .

A direct computation implies that

d d t S u 2 d x = 2 S 2 u u t d x = 2 S 2 u ( u u x + 3 μ ( u ) A 1 x u + λ u ) d x = 2 λ S u 2 d x .

It follows that

S u 2 dx= S u 0 2 dx e 2 λ t := μ 2 2 e 2 λ t .
(3.2)

So we have

| A 1 x (u)| ( 1 2 | μ 0 | + 2 μ 2 ) e λ t .

In view of equation (2.1) we have

d u ( t , q ( t , x ) ) d t = u t ( t , q ( t , x ) ) + u x ( t , q ( t , x ) ) d q ( t , x ) d t =( u t +u u x ) ( t , q ( t , x ) ) .

Combing the above relations, we arrive at

| d u ( t , q ( t , x ) ) d t +λu ( t , q ( t , x ) ) |3| μ 0 | ( 1 2 | μ 0 | + 2 μ 2 ) e 2 λ t .

Integrating the above inequality with respect to t<T on [0,t] yields

| e λ t u ( t , q ( t , x ) ) u 0 (x)| 3 | μ 0 | ( 1 2 | μ 0 | + 2 μ 2 ) λ .

Thus

|u ( t , q ( t , x ) ) | u ( t , q ( t , x ) ) L e λ t ( 3 | μ 0 | ( 1 2 | μ 0 | + 2 μ 2 ) λ + u 0 L ) .

In view of the diffeomorphism property of q(t,), we can obtain

|u(t,x)| u ( t , x ) L e λ t ( 3 | μ 0 | ( 1 2 | μ 0 | + 2 μ 2 ) λ + u 0 L ) .

This completes the proof of Lemma 3.1. □

Theorem 3.2 Let u 0 H s , s>3/2 be given and assume that T is the maximal existence time of the corresponding solution u(t,x) to the Cauchy problem (1.1) with the initial data u 0 . If there exists M>0 such that

u x ( t , ) L M,t[0,T),

then the H s -norm of u(t,) does not blow up on [0,T).

Proof We assume that c is a generic positive constant depending only on s. Let Λ= ( 1 x 2 ) 1 / 2 . Applying the operator Λ s to the first one in equation (1.3), multiplying by Λ s u, and integrating over S, we obtain

d d t u H s 2 =2 ( u u x , u ) H s 6 ( u , A 1 x ( μ ( u ) u ) ) H s 2λ ( u , u ) H s .
(3.3)

Let us estimate the first term of the above equation,

| ( u u x , u ) H s | = | ( Λ s ( u u x ) , Λ s u ) L 2 | = | ( [ Λ s , u ] u x , Λ s u ) L 2 + ( u Λ s u x , Λ s u ) L 2 | [ Λ s , u ] u x L 2 Λ s u L 2 + 1 2 | ( u x Λ s u , Λ s u ) L 2 | 2 ( u , v ) H 1 × H 1 2 ( 2 ( u , v ) H 1 × H 1 2 ) c u x L u H s 2 ,
(3.4)

where we used Lemma 2.3 with r=s. Furthermore, we estimate the second term of the right hand side of equation (3.3) in the following way:

| ( u , A 1 x ( μ ( u ) u ) ) H s | = | ( u , A 1 x ( e λ t μ 0 u ) ) H s | e λ t | μ 0 | u H s A 1 x u H s c | μ 0 | u H s 2 .
(3.5)

Combing equations (3.4) and (3.5) with equation (3.3) we arrive at

d d t u H s 2 c ( | μ 0 | + u x L + 2 λ ) | u H s 2 .

An application of Gronwall’s inequality and the assumption of the theorem yield

u H s 2 e c ( | μ 0 | + M + 2 λ ) t u 0 H s 2 .

This completes the proof of the theorem. □

The following result describes the precise blow-up scenario. Although the result which is proved in [16], our method is new, concise, and direct.

Theorem 3.3 Let u 0 H s , s>3/2 be given and assume that T is the maximal existence time of the corresponding solution u(t,x) to the Cauchy problem (1.1) with the initial data u 0 . Then the corresponding solution blows up in finite time if and only if

lim inf t T { inf x S u x ( t , x ) } =.

Proof Since the maximal existence time T is independent of the choice of s by Theorem 2.1, applying a simple density argument, we only need to consider the case s=3. Multiplying the first one in equation (1.2) by y and integrating over S with respect to x yield

d d t S y 2 d x = 2 S y y t d x = 2 S y ( u y x + 3 u x y + λ y ) d x = 2 S u y y x d x 6 S u x y 2 d x 2 λ S y 2 d x = 5 S u x y 2 d x 2 λ S y 2 d x .

If u x is bounded from below on [0,T)×S, then there exists N>λ>0 such that

u x (t,x)N,(t,x)[0,T)×S,

then

d d t S y 2 dx(5N2λ) S y 2 dx.

Applying Gronwall’s inequality then yields for t[0,T)

S y 2 dx e ( 5 N 2 λ ) t S y 2 (0,x)dx.

Note that

S y 2 dx= μ 2 (u)+ S u x x 2 dx u x x L 2 2 .

Since u x H 2 H 1 and S u x =0, Lemma 2.2 implies that

u x L 1 2 3 u x x L 2 e ( 5 N 2 λ ) t 2 y ( 0 , x ) L 2 .

Theorem 3.1 ensures that the solution u does not blow up in finite time. On the other hand, by the Sobolev embedding theorem it is clear that if

lim inf t T { inf x S u x ( t , x ) } =,

then T<. This completes the proof of the theorem. □

We now give first sufficient conditions to guarantee wave breaking.

Theorem 3.4 Let u 0 H s , s>3/2 and T be the maximal time of the solution u(t,x) to equation (1.1) with the initial data u 0 . If

inf x S u 0 (x)< 1 2 λ 1 2 λ 2 + 4 α ,

then the corresponding solution to equation (1.1) blow up in finite time in the following sense: there exists T 0 satisfying

0< T 0 1 λ 2 + 4 α ln ( 2 inf x S u 0 ( x ) + λ λ 2 + 4 α 2 inf x S u 0 ( x ) + λ + λ 2 + 4 α ) ,

where α=3| μ 0 |( 3 | μ 0 | ( 1 2 | μ 0 | + 2 μ 2 ) λ + u 0 L ), such that

lim inf t T 0 { inf x S u x ( t , x ) } =.

Proof As mentioned early, we only need to consider the case s=3. Let

m(t):= inf x S [ u x ( t , x ) ] ,t[0,T)

and let ξ(t)S be a point where this minimum is attained by using Lemma 2.4. It follows that

m(t)= u x ( t , ξ ( t ) ) .

Differentiating the first one in equation (1.3) with respect to x, we have

u t x + u x 2 +u u x x +3μ(u) A 1 x 2 u+λ u x =0.

From equation (1.6) we deduce that

u t x = u x 2 u u x x +3μ(u)(u μ 0 )λ u x .
(3.6)

Obviously u x x (t,ξ(t))=0 and u(t,) H 3 (S) C 2 (S). Substituting (t,ξ(t)) into equation (3.6), we get

d m ( t ) d t = m 2 ( t ) λ m ( t ) + 3 μ ( u ) u ( t , ξ ( t ) ) 3 μ 2 ( u ) = m 2 ( t ) λ m ( t ) + 3 μ 0 e λ t u ( t , ξ ( t ) ) 3 μ 0 2 e 2 λ t m 2 ( t ) λ m ( t ) + 3 | μ 0 | ( 3 | μ 0 | ( 1 2 | μ 0 | + 2 μ 2 ) λ + u 0 L ) .

Set

α=3| μ 0 | ( 3 | μ 0 | ( 1 2 | μ 0 | + 2 μ 2 ) λ + u 0 L ) .

Then we obtain

d m ( t ) d t m 2 ( t ) λ m ( t ) + α 1 4 ( 2 m ( t ) + λ + λ 2 + 4 α ) ( 2 m ( t ) + λ λ 2 + 4 α ) .

Note that if m(0)< 1 2 λ 1 2 λ 2 + 4 α , then m(t)< 1 2 λ 1 2 λ 2 + 4 α for all t[0,T). From the above inequality we obtain

2 m ( 0 ) + λ + λ 2 + 4 α 2 m ( 0 ) + λ λ 2 + 4 α e λ 2 + 4 α t 1 2 λ 2 + 4 α 2 m ( t ) + λ λ 2 + 4 α 0.

Since

0< 2 m ( 0 ) + λ + λ 2 + 4 α 2 m ( 0 ) + λ λ 2 + 4 α <1,

then there exists T 0 ,

0< T 0 1 λ 2 + 4 α ln ( 2 m ( 0 ) + λ λ 2 + 4 α 2 m ( 0 ) + λ + λ 2 + 4 α )

such that lim t T 0 m(t)=. Theorem 3.3 implies that the solution u blows up in finite time. □

We give another blow-up result for the solutions of equation (1.1).

Theorem 3.5 Let u 0 H s , s>3/2 and T be the maximal time of the solution u(t,x) to equation (1.1) with the initial data u 0 . If u 0 is odd satisfies u 0 <λ, then the corresponding solution to equation (1.1) blows up in finite time.

Proof By μ(u(t,x))= μ 0 (t,x) e λ t = μ 0 (t,x) e λ t =μ(u(t,x)), we can check the function

v(t,x):=u(t,x),t[0,T),xR,

is also a solution of equation (1.1), therefore u(x,t) is odd for any t[0,T). By continuity with respect to x of u and u x x , we get

u(t,0)= u x x (t,0)=0,t[0,T).

Define h(t):= u x (t,0) for t[0,T). From equation (3.6), we obtain

d h ( t ) d t = h 2 ( t ) λ h ( t ) 3 μ 2 ( u ) h 2 ( t ) λ h ( t ) = h ( t ) ( h ( t ) + λ ) .

Note that if h(0)<λ, then h(t)<λ for all t[0,T). From the above inequality we obtain

( 1 + λ h ( 0 ) ) e λ t 1 λ h ( t ) 0.

Since

0< h ( 0 ) + λ h ( 0 ) <1,

there exists T 0 ,

0< T 0 1 λ ln h ( 0 ) h ( 0 ) + λ

such that lim t T 0 m(t)=. Theorem 3.3 implies that the solution u blows up in finite time. □

4 Blow-up rate

In this section, we consider the blow-up profile; the blow-up rate of equation (1.1) with respect to time can be shown as follows.

Theorem 4.1 Let u 0 H s , s>3/2 and T be the maximal time of the solution u(t,x) to equation (1.1) with the initial data u 0 . If T is finite, then

lim t T { ( T t ) min x S u x ( x , t ) } =1.

Proof It is inferred from Lemma 2.4 that the function

m(t):= min x S u x (x,t)= u x ( t , ξ ( t ) )

is locally Lipschitz with m(t)<0, t[0,T). Note that u x x =0, a.e. t[0,T). Then we deduce that

| m ( t ) + m 2 ( t ) + λ m ( t ) | = | 3 μ ( u ) u ( t , ξ ( t ) ) 3 μ 2 ( u ) | = | 3 μ 0 e λ t u ( t , ξ ( t ) ) 3 μ 0 2 e 2 λ t | 3 | μ 0 | ( 3 | μ 0 | ( 1 2 | μ 0 | + 2 μ 2 ) λ + u 0 L + | μ 0 | ) : = K .

It follows that

K m (t)+ m 2 (t)+λm(t)Ka.e. on (0,T).
(4.1)

Thus,

K 1 4 λ 2 m (t)+ ( m ( t ) + 1 2 λ ) 2 K+ 1 4 λ 2 a.e. on (0,T).

Now fix any ε(0,1). In view of Theorem 3.1, there exists t 0 (0,T) such that m( t 0 )< ( K + 1 4 λ 2 ) ( 1 + 1 ε ) 1 2 λ. Being locally Lipschitz, the function m(t) is absolutely continuous on [0,T). It then follows from the above inequality that m(t) is decreasing on [ t 0 ,T) and satisfies

m(t)< ( K + 1 4 λ 2 ) ( 1 + 1 ε ) 1 2 λ,t[ t 0 ,T).

Since m(t) is decreasing on [ t 0 ,T), it follows that

lim t T m(t)=.

It is found from equation (4.1) that

1ε d d t ( m ( t ) + 1 2 λ ) 1 = m ( t ) ( m ( t ) + 1 2 λ ) 2 1+ε.
(4.2)

Integrating both sides of equation (4.2) on (t,T), we obtain

(1ε)(Tt) 1 ( m ( t ) + 1 2 λ ) (1+ε)(Tt),t[ t 0 ,T),
(4.3)

that is,

1 ( 1 + ε ) ( m ( t ) + 1 2 λ ) (Tt) 1 ( 1 ε ) ,t[ t 0 ,T).
(4.4)

By the arbitrariness of ε(0, 1 2 ), we have

lim t T (Tt) ( m ( t ) + λ ) =1.
(4.5)

This completes the proof of the theorem. □

5 Global existence

In this section, we will present some global existence results. Let us now prove the following lemma.

Lemma 5.1 Let u 0 H s , s>3/2 be given and assume that T>0 is the maximal existence time of the corresponding solution u(t,x) to the Cauchy problem (1.1). Let q C 1 ([0,T)×R;R) be the unique solution of equation (2.1). Then we have

y ( t , q ( t , x ) ) q x 3 = y 0 (x) e λ t ,

where y=μ(u) u x x .

Proof By the first one in equation (1.2) and equation (2.1) we have

d d t y ( t , q ( t , x ) ) q x 3 = ( y t + y x q t ) q x 3 + 3 y q x q x t = ( y t + y x u ) q x 3 + 3 y q x q x t = ( y t + u y x + 3 y u x y x u ) q x 3 = λ y q x 3 .

Therefore

y ( t , q ( t , x ) ) q x 3 = y 0 (x) e λ t .

 □

Lemma 5.1 and equation (2.2) imply that y and y 0 have the same sign.

Theorem 5.2 Let u 0 H s , s>3/2. If y 0 = μ 0 u 0 , x x H 1 does not change sign, then the corresponding solution u(t,x) to equation (1.1) with the initial data u 0 exists globally in time.

Proof By equation (2.1), we know that q(t,) is diffeomorphism of the line and the periodicity of u with respect to spatial variable x, given t[0,T), there exists a ξ(t)S such that u x (t,ξ(t))=0.

We first consider the case that y 0 0 on S, in which case Lemma 5.1 ensures that y0. For x[ξ(t),ξ(t)+1], we have

u x ( t , x ) = ξ ( t ) x u x x ( t , x ) d x = ξ ( t ) x ( y μ ( u ) ) d x = ξ ( t ) x y d x μ ( u ) ( x ξ ( t ) ) S y d x μ ( u ) ( x ξ ( t ) ) = μ ( u ) ( 1 x + ξ ( t ) ) | μ 0 | .

It follows that u x (t,x)| μ 0 |.

On the other hand, if y 0 0 on S, then Lemma 5.1 ensures that y0. Therefore, for x[ξ(t),ξ(t)+1], we have

u x ( t , x ) = ξ ( t ) x u x x ( t , x ) d x = ξ ( t ) x ( y μ ( u ) ) d x = ξ ( t ) x y d x μ ( u ) ( x ξ ( t ) ) μ ( u ) ( x ξ ( t ) ) | μ 0 | .

It follows that u x (t,x)| μ 0 |. By using Theorem 3.2, we immediately conclude that the solution is global. This completes the proof of the theorem. □

Corollary 5.3 If the initial value u 0 H 3 such that

x 3 u 0 L 2 2 3 | μ 0 |,

then the corresponding solution u of the initial value u 0 exists globally in time.

Proof Since S x 2 u 0 dx=0, by Lemma 2.2, we obtain

x 2 u 0 L 1 2 3 x 3 u 0 L 2 .

If μ 0 0, we have

y 0 = μ 0 x 2 u 0 μ 0 1 2 3 x 3 u 0 L 2 μ 0 | μ 0 |=0.

If μ 0 <0, we have

y 0 = μ 0 x 2 u 0 μ 0 + x 2 u 0 L μ 0 + 1 2 3 x 3 u 0 L 2 μ 0 +| μ 0 |=0.

 □

Thus the theorem is proved by using Theorem 5.2.