Local well-posedness and blow-up criteria of solutions for a rod equation
Transcript of Local well-posedness and blow-up criteria of solutions for a rod equation
Math. Nachr. 278, No. 14, 1726 – 1739 (2005) / DOI 10.1002/mana.200310337
Local well-posedness and blow-up criteria of solutions for a rod equation
Yong Zhou∗ 1
1 Department of Mathematics, East China Normal University, Shanghai 200062
Received 14 April 2003, revised 29 December 2003, accepted 17 January 2004Published online 6 October 2005
Key words Well-posedness, blow-upMSC (2000) 49K40, 37L05
In this paper we consider a new rod equation derived recently by Dai [Acta Mech. 127 No. 1–4, 193–207(1998)] for a compressible hyperelastic material. We establish local well-posedness for regular initial dataand explore various sufficient conditions of the initial data which guarantee the blow-up in finite time bothfor periodic and non-periodic case. Moreover, the blow-up time and blow-up rate are given explicitly. Someinteresting examples are given also.
c© 2005 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim
1 Introduction
Although a rod is always three-dimensional, if its diameter is much less than the axial length scale, one-dimensionalequations can give a good description of the motion of the rod. Recently Dai [7] derived a new (one-dimensional)nonlinear dispersive equation including extra nonlinear terms involving second-order and third-order derivativesfor a compressible hyperelastic material. The equation reads
vτ + σ1vvξ + σ2vξξτ + σ3(2vξvξξ + vvξξξ) = 0
where u(ξ, τ) represents the radial stretch relative to a pre-stressed state, and σ1 �= 0, σ2 < 0 and σ3 ≤ 0 areconstants determined by the pre-stress and the material parameters. If one introduces the following transforma-tions
τ =3√−σ2
σ1t , ξ =
√−σ2 x ,
then the above equation turns into
ut − utxx + 3uux = γ(2uxuxx + uuxxx) (1.1)
where γ = 3σ3/(σ1σ2). In [8], the authors derived that value range of γ is from −29.4760 to 3.4174 for somespecial compressible materials. In this paper, from the mathematical view point, we regard γ as a real number.
When γ = 1 in Eq. (1.1), we recover the shallow water (Camassa–Holm) equation derived physically byCamassa and Holm in [2] by approximating directly the Hamiltonian for Euler’s equations in the shallow waterregime, where u(x, t) represents the free surface above a flat bottom. Some satisfactory results have been obtainedfor this shallow water equation recently. Local well-posedness for the initial datum u0(x) ∈ Hs with s > 3/2was proved by several authors, see [14, 16, 18]. On the other hand, Himonas and Misiole [10] showed thatthe Camassa–Holm equation is not well-posed for initial data in Hs for s < 3/2. These results suggest thats = 3/2 is the critical index for well-posedness. Moreover, wave breaking for a large class of initial data hasbeen established in [3, 4, 5, 14, 15, 21, 22]. However, in [19, 20], Xin and Zhang showed global existence anduniqueness for weak solutions with u0(x) ∈ H1. The solitary waves of Camassa–Holm equation are peakedsolitons [2] and are orbitally stable [6].
∗ e-mail: [email protected], Phone: +21 6223 3050 (O), +21 6245 7134 (H), Fax: +21 6223 8105
c© 2005 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim
Math. Nachr. 278, No. 14 (2005) / www.mn-journal.com 1727
If γ = 0, Eq. (1.1) is the BBM equation, a well-known model for surface waves in a canal [1], and its solutionsare global.
We now conclude this introduction by outlining the rest of the paper. In Section 2, we establish local well-posedness for Eq. (1.1) with initial datum u0 ∈ Hs, s > 3/2, and that the lifespan of the corresponding solutionis finite if and only if its first-order derivative blows up. In Section 3, we investigate various sufficient conditions(which are different for different γ) of the initial datum to guarantee the finite time blow-up for periodic case andsome examples are given at the end of that section. Blow-up criteria are established for the non-periodic case inSection 4. Finally we compare the rod equation with Camassa–Holm equation and some questions are proposedin Section 5.
2 Local well-posedness
In this section, we consider both periodic and nonperiodic case for γ �= 0. Let S := R/Z be the unit circle andT = R or S.
Set Qs =(1 − ∂2
x
)s/2, then the operator Q−2 can be expressed by
Q−2f = G ∗ f =∫
T
G(x − y)f(y) dy
for any f ∈ L2(T ) with
G(x) =
⎧⎪⎪⎨⎪⎪⎩
12
e−|x| , if T = R ,
cosh(x − [x] − 1/2)2 sinh(1/2)
, if T = S ,
where [x] denotes the integer part of x. Then Eq. (1.1) can be written as
ut + γuux + ∂xQ−2„
3 − γ
2u2 +
γ
2u2
x
«= 0 . (2.1)
The local well-posedness theorem for Eq. (1.1) reads
Theorem 2.1 Let u0(x) ∈ Hs(T), s > 3/2, be the initial datum. Then there exists T = T (‖u0‖Hs) > 0 anda unique solution u, which depends continuously on the initial datum u0, to Eq. (1.1) (or Eq. (2.1)) such that
u ∈ C([0, T ); Hs(T)
) ∩ C1([0, T ); Hs−1(T)
).
Moreover, the following two quantities E and F , defined by⎧⎪⎪⎨⎪⎪⎩
E(u)(t) =∫
T
(u2(x, t) + u2
x(x, t))dx ,
F (u)(t) =∫
T
(u3(x, t) + γu(x, t)u2
x(x, t))dx ,
are invariants with respect to time t for Eq. (1.1).
This result can be showed by applying Kato’s theorem [11, 13], just as what was done for the Camassa–Holmequation (γ = 1 in Eq. (2.1)) [4, 16]. So we would like to skip the detailed proof here, for concise.
The maximum value of T in Theorem 2.1 is called the lifespan of the solution, in general. If T < ∞, that islim supt↑T ‖u(., t)‖Hs = ∞, we say that the solution blows up in finite time. The following theorem tells us thatthe solution blows up if and only if the first-order derivative blows up. This phenomenon coincides physicallywith the rod breaking.
Theorem 2.2 Let u0(x) ∈ Hs(T), s ≥ 2, and u be the corresponding solution to problem (1.1) with lifespanT . Then
supx∈T, 0≤t<T
|u(x, t)| ≤ C (‖u0‖H1) . (2.2)
c© 2005 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim
1728 Zhou: Well-posedness and blow-up for a rod equation
T is bounded if and only if
lim inft↑T
infx∈T
{γux(x, t)} = −∞ . (2.3)
P r o o f. First, we have the following Sobolev embedding inequality
‖f‖2L∞ ≤ C ‖f‖2
H1 ,
where C is an absolute constant. More precisely,
C =
⎧⎪⎪⎨⎪⎪⎩
e1/2 + e−1/2
2(e1/2 − e−1/2), if T = S ,
12
, if T = R ,
see Theorem 3.1 and Eq. (4.1) below, respectively. Then Eq. (2.2) follows from the conservation of H1-norm ofthe solution.
Taking y = u − uxx, then from Eq. (1.1) one can get the equation for y
yt + γyxu + 2γyux + 3(1 − γ)uux = 0 . (2.4)
Applying y on Eq. (2.4) and integration by parts, we obtain
d
dt
∫T
y2 dx = − 3γ
∫T
y2ux dx + 6(γ − 1)∫
T
yuux dx
≤ − 3γ
∫T
y2ux dx + 6C |γ − 1|∫
T
yux dx
≤ − 3γ
∫T
y2ux dx + 3C |γ − 1|∫
T
(y2 + u2
x
)dx
≤ − 3γ
∫T
y2ux dx + 6C |γ − 1|∫
T
y2 dx ,
(2.5)
where we use the bounds of u and that ‖y‖L2 is equivalent to ‖u‖H2 .Due to Gronwall’s inequality, it is clear that, from Eq. (2.5), γux is bounded from below on [0, T ), then the
H2-norm of the solution is also bounded on [0, T ).On the other hand,
u = Q−2y =∫
T
G(x − ξ)y(ξ) dξ ,
therefore
‖ux‖L∞ ≤ ‖Gx‖L2‖y‖L2 . (2.6)
Eq. (2.6) tells us if the H2-norm of the solution is bounded then the L∞-norm of the first derivative is bounded.This finishes the proof.
For γ �= 0, we set
m(t) := infx∈T
ux(x, t)sign{γ} , t ≥ 0 , (2.7)
where sign{a} is the sign function of a ∈ R and we set m0 := m(0). Then for every t ∈ [0, T ) there existsat least one point ξ(t) ∈ T with m(t) = ux(ξ(t), t). Just as the proof given in [5], one can show the followingproperty of m(t).
Lemma 2.3 Let u(t) be the solution to Eq. (1.1) on [0, T ) with initial data u0 ∈ H2(T), as given by Theorem2.1. Then the function m(t) is almost everywhere differentiable on [0, T ), with
dm(t)dt
= utx(ξ(t), t) a.e. on (0, T ) .
To consider the quantity m(t) for wave breaking comes from an idea of Seliger [17] originally, the rigorousregularity proof is given in [5] for Camassa–Holm equation.
c© 2005 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim
Math. Nachr. 278, No. 14 (2005) / www.mn-journal.com 1729
3 Blow-up criteria for periodic case
Before give the main theorems of this section, we would like to prove the following theorem concerning optimalconstant for Sobolev embedding.
Theorem 3.1 For all f ∈ H1(S), the following inequality
maxx∈[0,1]
f2(x) ≤ C0‖f‖2H1(S)
holds, where C0 = e1/2+e−1/2
2(e1/2−e−1/2).
Moreover, C0 is the minimum value, so in this sense, C0 is the optimal constant which is obtained by the
associated Green function G = cosh(x−[x]− 12 )
2 sinh( 12 )
.
P r o o f. The aim of the proof is to find the optimal constant c such that
‖u‖2L∞(S) ≤ c ‖u‖2
H1(S) for all u ∈ H1(S) .
Let
A ={u ∈ H1(S)
∣∣ ‖u‖L∞(S) = 1}
and
I[u] = ‖u‖2H1(S) =
∫S
(u2 + u2
x
)dx , u ∈ A .
Step 1. We need to find the minimizer of the functional I[u] in the space A.Let {uk}∞k=1 ⊂ A be a minimizing sequence, i.e., I[uk] → infu∈A I[u] as k → ∞.
Since I[1] = 1, then 0 < infu∈A I[u] ≤ 1. Therefore {uk}∞k=1 is bounded in H1(S), so there exists asubsequence {ukj}∞k=1 ⊂ {uk}∞k=1, which we also denote by {uk}∞k=1, and a u0 ∈ H1(S) with
uk ⇀ u0 in H1(S) .
On the other hand,
I[u] = ‖u‖2H1(S) and I[u0] ≤ lim inf
k→∞I[uk] ,
so I[u0] = infu∈A I[u] and we can get uk → u0 in H1(S). By the Sobolev embedding, we know that
‖uk − u0‖2L∞(S) ≤ c ‖uk − u0‖2
H1(S) ,
so ‖u0‖L∞(S) = 1. Hence we have u0 ∈ A and uk → u0 in A.
Step 2. By step 1, we know that I[u] has a minimizer in A, say g. In the following steps, the property of g willbe explored. Let
f(x) =4π2 + 1 + 2 cos(2πx)
4π2 + 3.
By direct computation, it is easy to obtain that f ∈ A and
I[f ] =4π2 + 14π2 + 3
.
Therefore, the steady state 1 is not a minimizer and consequently, for g, there exists some point, say x0, such thatg(x0) < 1.
Now let ϕ be any C∞ function with compact support in a small neighborhood U(x0, δ) = {x ∈ S ||x − x0| < δ}. Since g is continuous
(H1(S) ⊂ C(S)
), one can choose δ and ε sufficiently small such that
(εϕ + g)(x) < 1 for all x ∈ U(x0, δ) .
Then ‖g + εϕ‖L∞(S) = 1, since εϕ ≡ 0 outside U(x0, δ).
c© 2005 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim
1730 Zhou: Well-posedness and blow-up for a rod equation
Set
i(t) = I[g + tεϕ] =∫
S
((g + tεϕ)2 + (gx + tεϕx)2
)dx ,
where t ∈ R satisfies ‖g + tεϕ‖L∞(S) = 1.By g being a minimizer,
0 = i′(0) = 2ε
∫S
(gϕ + gxϕx) dx = 2ε
∫U(x0,δ)
g(ϕ − ϕxx) dx .
So in the sense of distribution, g is a weak (smooth) solution to the following equation
u − uxx = 0 in {x ∈ S | g(x) < 1} .
Step 3. We will show that g must have only one maximum point.Since g is continuous on S, ‖g‖L∞(S) = maxx∈S |g(x)|.Claim 1 The maximum points cannot be dense in any interval contained in S.
Suppose otherwise, then by the continuity of g, we get g ≡ 1 on some interval, say [a, b] ⊂ [0, 1].Let
g(x) =
⎧⎪⎨⎪⎩
4π2 + 1 + 2 cos(
2π(x−a)b−a
)4π2 + 3
, if x ∈ [a, b] ,
g(x), otherwise .
It is easy to check that g(x) ∈ A. But
I[g] =∫
S
(g2 + g2
x
)dx =
∫[a,b]
(g2 + g2
x
)dx +
∫S\[a,b]
(g2 + g2
x
)dx
= (b − a)4π2 + 14π2 + 3
+∫
S\[a,b]
(g2 + g2
x
)dx
< I[g] .
This is a contradiction, since g is a minimizer.
Claim 2 The number of maximal points cannot exceed 1.
Suppose that the number of maximal points is larger than or equal to 2. By Claim 1, we can suppose that x0
is a maximal point and there exist 0 < ε0 < 1 and 0 < δ < 1/2 such that
1 − ε0 < |g(x)| < 1 for all x ∈ {U(x0, δ) \ x0} .
Let M0 = max{|g(x0 − δ)|, |g(x0 + δ)|} and U(x0) be a neighborhood of x0 defined as follows
U(x0) = {x ∈ U(x0, δ) | M0 ≤ |g(x)| } .
Then set
g1(x) =
{M0 sign{g(x0)} , if x ∈ U(x0) ,
g(x) , otherwise .
It is not difficult to check that g1 ∈ A, and
I[g1] =∫
S
(g21 + g2
1x
)dx =
∫U(x0)
M20 dx +
∫S\U(x0)
(g2 + g2
x
)dx
<
∫U(x0)
g2 + g2x dx +
∫S\U(x0)
(g2 + g2
x
)dx
= I[g] .
c© 2005 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim
Math. Nachr. 278, No. 14 (2005) / www.mn-journal.com 1731
This contradicts the fact that g is the minimizer. Hence Claim 2 is true.
Step 4. By step 3 we know that g has only one maximal point. After choosing a suitable coordinate, we canassume that
g < 1 in (0, 1) and g(0) = g(1) = 1 .
It follows from step 2 that g is a weak solution of the following equation in (0, 1):
g − gxx = 0 , x ∈ (0, 1) , g(0) = g(1) = 1 . (3.1)
For the above equation, we know the nontrivial classical solution has the form aex + ce−x. Thus by the boundarycondition, after calculation we get
a =1 − e−1
e − e−1and c =
e − 1e − e−1
.
Then, by the uniqueness of solutions to Eq. (3.1), one obtains
g =cosh
(x − 1
2
)cosh
(12
) , 0 ≤ x ≤ 1 .
Finally, we can get the constant C0 = e1/2+e−1/2
2(e1/2−e−1/2).
Let m(t) be defined by Eq. (2.7), we have the following blow-up criterion first.
Theorem 3.2 Let γ ∈ R, γ �= 0, 3. Assume that u0 ∈ H2(S) satisfies m0 < 0 and
m20 >
⎧⎪⎪⎪⎪⎪⎪⎪⎪⎨⎪⎪⎪⎪⎪⎪⎪⎪⎩
(3 − γ)C0
−γ‖u0‖2
H1(S) , if γ < 0 ,
(6 − γ −
√12γ − 3γ2
)C0
2γ‖u0‖2
H1(S) , if 0 < γ < 3 ,
(γ − 3)C0
γ‖u0‖2
H1(S) , if γ > 3 ,
where m0 = infx∈S u0x(x), and C0 is given in Theorem 3.1. Then the life span T > 0 of the correspondingsolution to Eq. (1.1) is finite, i.e., rod breaking occurs. If γ = 3, all solutions with non-constant initial datau0 ∈ H2(S) blow up in finite time.
P r o o f. Differentiating Eq. (2.1) with respect to x, one obtains
uxt + γuuxx +γ
2u2
x =3 − γ
2u2 − G ∗
(3 − γ
2u2 +
γ
2u2
x
). (3.2)
Then by Lemma 2.5 and the definition of m(t) (see Eq. (2.7)), we have the equation for m(t), from Eq. (3.2)
sign{γ} dm
dt= −γ
2m2 +
3 − γ
2u2(ξ(t), t) −
[G ∗
(3 − γ
2u2 +
γ
2u2
x
)](ξ(t), t) (3.3)
a.e. on (0, T ).If γ < 0, from Eq. (3.3), we get
dm
dt=
γ
2m2 − 3 − γ
2u2(ξ(t), t) +
[G ∗
(3 − γ
2u2 +
γ
2u2
x
)](ξ(t), t)
≤ γ
2m2 +
[G ∗ (3 − γ)u2
2
](ξ(t), t)
≤ γ
2m2 +
3 − γ
2‖G‖L∞‖u2‖L1
≤ γ
2m2 +
(3 − γ)C0
2‖u0‖2
H1 .
(3.4)
c© 2005 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim
1732 Zhou: Well-posedness and blow-up for a rod equation
It is easy to prove that if
m0 < 0 and m20 >
(3 − γ)C0
−γ‖u0‖2
H1 ,
then the solution m(t) of the Riccati type equation (3.4) goes to −∞ in finite time. More precisely, if we set aconstant δ ∈ (0, 1) satisfying
δm20 =
(3 − γ)C0
−γ‖u0‖2
H1 ,
then the lifespan of the solution to Eq. (1.1) is less than 2/(m0(1 − δ)γ).Now we go to the case 0 < γ < 3. By the representation of G, it follows[
G ∗(
3 − γ
2u2 +
γ
2u2
x
)](x, t)
=1
2 sinh(
12
) ∫ x
0
ex−η− 12 + e
12+η−x
2
(3 − γ
2u2(η, t) +
γ
2u2
x(η, t))
dη
+1
2 sinh(
12
) ∫ 1
x
ex−η+ 12 + eη−x− 1
2
2
(3 − γ
2u2(η, t) +
γ
2u2
x(η, t))
dη .
(3.5)
Since ∫ x
0
e−η(γ
2α2u2(η, t) +
γ
2u2
x(η, t))
dη ≥ −∫ x
0
e−ηγαu(η, t)ux(η, t) dη
= − e−η γα
2u2(η, t)
∣∣x0−∫ x
0
e−η γα
2u2(η, t) dη
holds for any α > 0, we have∫ x
0
e−η((
α2 + α) γ
2u2(η, t) +
γ
2u2
x(η, t))
dη ≥ −αγ
2e−ηu2(η, t)
∣∣x0
.
Now we let
α2 + α =3 − γ
γ. (3.6)
Eq. (3.6) has one positive root α0 with
α0 = −12
+12
√12 − 3γ
γ.
Therefore ∫ x
0
e−η
(3 − γ
2u2(η, t) +
γ
2u2
x(η, t))
dη ≥ −α0γ
2e−ηu2(η, t)
∣∣x0.
Moreover, from Eq. (3.5), just use the above trick for each term, then one obtains[G ∗(
3 − γ
2u2 +
γ
2u2
x
)](ξ(t), t) ≥ α0γ
2u2(ξ(t), t) . (3.7)
Now combining Eqs. (3.3) and (3.7), we have
dm
dt≤ − γ
2m2 +
6 − γ −√
12γ − 3γ2
4u2(ξ(t), t)
≤ − γ
2m2 +
6 − γ −√
12γ − 3γ2
4C0 ‖u0‖2
H1 .
(3.8)
c© 2005 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim
Math. Nachr. 278, No. 14 (2005) / www.mn-journal.com 1733
Just as the case γ < 0, we can get that if
m0 < 0 and m20 ≥ 6 − γ −
√12γ − 3γ2
2γC0 ‖u0‖2
H1 ,
then the solution to Eq. (1.1) (or Eq. (3.8)) blows up in finite time. And we can give an explicit estimate for thelifespan of the corresponding solution. Note that
6 − γ −√12γ − 3γ2
4<
3 − γ
2for 0 < γ < 3 .
If γ > 3, it follows from Eq. (3.3) that m(t) satisfies
dm
dt≤ − γ
2m2 +
[G ∗ (γ − 3)u2
2
](ξ(t), t)
≤ − γ
2m2 +
γ − 32
‖G‖L∞‖u2‖L1
≤ − γ
2m2 +
(γ − 3)C0
2‖u0‖2
H1 .
(3.9)
Eq. (3.9) is similar to Eq. (3.4) and a corresponding condition for blow-up is easy to be obtained.If γ = 3, Eq. (3.3) reduces to
dm
dt= −3
2m2 −
[G ∗ 3
2u2
x
](ξ(t), t) ≤ −3
2m2. (3.10)
For any non-constant initial datum u0, we have m0 < 0. Hence the solution to Eq. (3.10) (also Eq. (1.1)) blowsup in finite time.
Theorem 3.3 Suppose u0 ∈ H2(S) satisfies m0 < 0 and
m20 >
(6 − γ −
√12γ − 3γ2
)2γ
(‖u0‖2
H1(S) +(∫
S
u0 dx
)2)
,
for 0 < γ < 3. Then the life span of the corresponding solution to Eq. (1.1) is finite.
P r o o f. First we prove the following inequality for any function f ∈ H2(S):
‖f‖2L∞ ≤ ‖f‖2
H1 +(∫
S
f dx
)2
. (3.11)
Indeed, since f is continuous on S, there exists a point x0 ∈ S such that∫
Sf dx = f(x0). For any x ∈ S, we
have
f2(x) −(∫
S
f dx
)2
= f2(x) − f2(x0) =∫ x
x0
2ffx dx ≤∫ x
x0
(f2 + f2
x
)dx ≤ ‖f‖2
H1(S) ,
which yields Eq. (3.11).On the other hand, it is obvious that∫
S
u(x, t) dx
is unchanged for solutions u(x, t) with respect to time for initial data u0 ∈ H2(S).Therefore Theorem 3.3 can be proved if one uses
‖u(., t)‖2L∞(S) ≤ ‖u0‖2
H1(S) +(∫
S
u0 dx
)2
, for all t ≥ 0 ,
in Eq. (3.8) instead of ‖u(., t)‖2L∞(S) ≤ C0‖u0‖2
H1(S).
c© 2005 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim
1734 Zhou: Well-posedness and blow-up for a rod equation
Remark 3.4 Even for γ = 1 (Camassa–Holm equation), Theorem 3.2 is a significant improvement of theprevious result (see [3]). Theorem 3.3 is similar to the criterion established by the author in [21] for Camassa–Holm equation.
When we study the blow-up problems for differential equations, according to [9], the basic questions includeswhen, where, and how. Theorems 3.2 and 3.3 give answer to the first two questions. The following theoremanswers one aspect of the third question, the rate of blow-up.
Theorem 3.5 Suppose u0(x) ∈ H2(S), and that u(x, t) is the corresponding solution. If the lifespan of thesolution u(x, t) is finite, then
limt→T
{(T − t)m(t)} = − 2|γ| .
P r o o f. The conclusion follows from the theory of ordinary differential equation corresponding to Eq. (3.3).Indeed, for any γ �= 0, we have
0 ≤ dm
dt+
|γ|2
m2 ≤ C , (3.12)
where C > 0 is a constant depending on γ, C0 and ‖u0‖H1 . Since m(t) → −∞ as t → T , from Eq. (3.3) itfollows that for any 0 < ε < |γ|/2 there exists a t0 such that m(t) < −C/ε for all t ∈ (t0, T ). Then we obtain
−|γ|2
≤ 1m2
dm
dt≤ −|γ|
2+ ε . (3.13)
For t ∈ (t0, T ), integrating Eq. (3.13) on (t, T ) gives( |γ|2
− ε
)(T − t) ≤ − 1
m(t)≤ |γ|
2(T − t) .
The proof is complete from the arbitrariness of ε.
At the end of this section, some examples are given to illustrate the applications of Theorem 3.2 and The-orem 3.3, respectively. We just take γ = 1, for simplicity. Of course, we can give examples for any fixed0 < γ < 3.
Example 3.6 u0(x) = sin(2πx) + 4, x ∈ [0, 1].Direct computation yields
‖u0‖2H1(S) = 2π2 +
12
+ 16
and
minx∈S
u0x(x) = −2π > −(‖u0‖2
H1(S) +(∫ 1
0
u0 dx
)2)1/2
(≈ −7.22767) .
So the classical solution u(x, t) to Eq. (1.1) corresponding to u0(x) = sin(2πx) + 4 only exists for finite timedue to Theorem 3.2 (γ = 1). But Theorem 3.3 does not work. Note that also none of theorems in [3, 4] can beapplied in this case.
Example 3.7 We would like to give an example, which illustrates the applicability of Theorem 3.3 as follows.Let
u0(x) =
⎧⎪⎨⎪⎩
x − a , 0 ≤ x ≤ a ,
0 , a ≤ x ≤ 1 − a ,
1 − a − x , 1 − a ≤ x ≤ 1 ,
where 0 < a < 12 is to be determined later. By simple computations, we get
‖u0‖2H1(S) =
2a3
3+ 2a and
(∫ 1
0
u0(x) dx
)2
= a4 .
c© 2005 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim
Math. Nachr. 278, No. 14 (2005) / www.mn-journal.com 1735
Since minx∈S u0(x) = −1, we want a to satisfy
1 < C0
(2a3
3+ 2a
)and 1 >
2a3
3+ 2a + a4 .
By Mathematica, one obtains that when a = 0.44,
−1 > −√
C0
(2a3
3+ 2a
)(≈ −1.01358) (3.14)
and
−1 < −√
2a3
3+ 2a + a4 (≈ −0.97427) . (3.15)
It is easy to show that by standard mollification at the points 0, a and 1−a (a = 0.44), we can get a new functionu0 ∈ H2(S) that also satisfies Eqs. (3.14) and (3.15).
Let u0 be the initial data to Eq. (1.1). By the above analysis, we can see in this case, only Theorem 3.3 works.
4 Blow-up criteria for non-periodic case
Theorem 4.1 Assume that the initial profile u0 ∈ H2(R) satisfies m0 < 0 and
m20 >
⎧⎪⎪⎪⎪⎪⎪⎪⎨⎪⎪⎪⎪⎪⎪⎪⎩
3 − γ
−2γ‖u0‖2
H1(R) , if γ < 0 ,
6 − γ −√
12γ − 3γ2
4γ‖u0‖2
H1(R) , if 0 < γ < 3 ,
γ − 32γ
‖u0‖2H1(R) , if γ > 3 .
Then the life span T > 0 of the corresponding solution to Eq. (1.1) is finite, i.e., rod breaking occurs. If γ = 3,all solutions with nonzero initial data u0 ∈ H2(R) blow up in finite time.
P r o o f. First, we have the following inequality
‖f‖L∞(R) ≤ 1√2‖f‖H1(R) for all f ∈ H1(R) . (4.1)
Indeed, for any x ∈ R, we have
2f2(x) = 2(∫ x
−∞ffx dx −
∫ ∞
x
ffx dx
)≤∫
R
(f2 + f2
x
)dx = ‖f‖H1(R) ,
which yields Eq. (4.1).For the rod equation, since the H1-norm is conserved, one has
supx∈R,t∈[0,T )
|u(x, t)| ≤ 1√2‖u0‖H1 .
Just as the proof for Theorem 3.2, we have Eq. (3.3) for m(t) and the remaining proof is similar. For example, inEq. (3.4) we use ‖G‖L∞(R) ≤ 1/2 instead. So for γ < 0, we have
dm
dt≤ γ
2m2 +
3 − γ
4‖u0‖2
H1 ,
and the case γ > 3 is similar to this case.
c© 2005 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim
1736 Zhou: Well-posedness and blow-up for a rod equation
For 0 < γ < 3, we obtain by the representation of G, that
G ∗(
3 − γ
2u2 +
γ
2u2
x
)(x) =
12
∫ x
−∞e−x+y
(3 − γ
2u2 +
γ
2u2
x
)(y) dy
+12
∫ ∞
x
ex−y
(3 − γ
2u2 +
γ
2u2
x
)(y) dy .
(4.2)
The following inequality∫ x
−∞ey(α2
0
γ
2u2 +
γ
2u2
x
)(y) dy ≥
∫ x
−∞eyαγ(uux)(y) dy
=αγ
2exu2(x) +
∫ x
−∞
αγ
2eyu2(y) dy
implies ∫ x
−∞e−x+y
((α2 + α)
γ
2u2 +
γ
2u2
x
)(y) dy ≥ αγ
2u2(x) . (4.3)
Then we take α2 + α = 3−γγ , that is
α = −12
+12
√12 − 3γ
γ.
Similarly we get the estimate of the second term in Eq. (4.2) as∫ ∞
x
ex−y
(3 − γ
2u2 +
γ
2u2
x
)(y) dy ≥ αγ
2u2(x) . (4.4)
Combining Eqs. (4.2), (4.3) and (4.4), one has[G ∗(
3 − γ
2u2 +
γ
2u2
x
)](ξ(t), t) ≥ αγ
2u2(ξ(t), t) =
−γ +√
12γ − 3γ2
4u2(ξ(t), t) . (4.5)
Hence Eq. (3.3) reduces to
dm
dt≤ −γ
2m2 +
6 − γ −√12γ − 3γ2
8‖u0‖2
H1 .
For γ = 3, we have the following equation for m(t)
dm
dt= −3
2m2 − G ∗
(32
u2x
)≤ −3
2m2 .
For any nonzero u0 ∈ H2(R), it is clearly that m(0) is negative, hence the lifespan of the solution is finite.The proof is complete.
Theorem 4.2 Assume that u0 ∈ H2(R) and that u(x, t) is the corresponding solution. Set
q(t) := sign{γ}∫
R
u3x(x, t) dx and q0 := q(0) .
If q0 < 0 the following conditions are satisfied:
q20 >
⎧⎪⎪⎪⎪⎪⎪⎪⎨⎪⎪⎪⎪⎪⎪⎪⎩
3(3 − γ)−2γ
‖u0‖6H1(R) , if γ < 0 ,
3(6 − γ −
√12γ − 3γ2
)4γ
‖u0‖6H1(R) , if 0 < γ < 3 ,
3(γ − 3)2γ
‖u0‖6H1(R) , if γ > 3 .
Then the u(x, t) to Eq. (1.1) blows up in finite time.
c© 2005 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim
Math. Nachr. 278, No. 14 (2005) / www.mn-journal.com 1737
P r o o f. First, for any f ∈ H2(R), since∣∣∣∣∫
R
f3x dx
∣∣∣∣ ≤(∫
R
f4x dx
)1/2(∫R
f2x dx
)1/2
,
it follows that∫R
f4x dx ≥ 1
‖f‖2H1
(∫R
f3x dx
)2
. (4.6)
Multiplying Eq. (3.2) by u2x, after integration by parts, one has
sign{γ}dq
dt= −γ
2
∫R
u4x dx +
3(3 − γ)2
∫R
u2xu2 dx − 3
∫R
u2xG ∗
(3 − γ
2u2 +
γ
2u2
x
)dx . (4.7)
If γ < 0, by Eqs. (4.1), (4.6) and (4.7), one obtains
dq
dt≤ γ
2‖u0‖2H1
q2 +3(3 − γ)
2
∫R
u2x
(G ∗ u2
)dx
≤ γ
2 ‖u0‖2H1
q2 +3(3 − γ)
2‖u0‖2
H1 ‖G ∗ u2‖L∞ (4.8)
≤ γ
2 ‖u0‖2H1
q2 +3(3 − γ)
4‖u0‖4
H1 .
It is easy to see that under the corresponding condition of Theorem 4.2, the solution of Eq. (4.8) blows up in finitetime.
If 0 < γ < 3, from Eqs. (4.5) and (4.7), we obtain,
dq
dt≤ − γ
2‖u0‖2H1
q2 +3(3 − γ)
2
∫R
u2u2x dx − 3α0γ
2
∫R
u2u2x dx
≤ − γ
2‖u0‖2H1
q2 +3(6 − γ −
√12γ − 3γ2
)4
‖u‖2L∞
∫R
u2x dx (4.9)
≤ − γ
2 ‖u0‖2H1
q2 +3(6 − γ −
√12γ − 3γ2
)8
‖u0‖4H1 .
Similarly for γ > 3, one has
dq
dt≤ − γ
2 ‖u0‖2H1
q2 +3(γ − 3)
2
∫R
u2x
(G ∗ u2
)dx
≤ − γ
2 ‖u0‖2H1
q2 +3(γ − 3)
4‖u0‖4
H1 .
(4.10)
From standard argument for Riccati type equations, it is clear that under the condition of Theorem 4.2 the solutionof Eqs. (4.9) and (4.10) blow up in finite time. Therefore, for any γ ∈ R, γ �= 0, we have
limt→T
[sign{γ}
∫R
u3x(x, t) dx
]= −∞ for some T > 0 . (4.11)
Eq. (4.11) and the estimate∣∣∣∣∫
R
u3x dx
∣∣∣∣ ≤ C(s) ‖u‖2H1‖u‖Hs = C(s) ‖u0‖2
H1‖u‖Hs , for any s ∈ (3/2, 2] ,
show that limt→T ‖u‖H2 = ∞. Moreover,
sign{γ}∫
R
u3x(x, t) dx ≥ 1
|γ| infx∈R
{γux} ‖u0‖2H1
yields that limt→T infx∈R{γux(x, t)} = −∞.
c© 2005 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim
1738 Zhou: Well-posedness and blow-up for a rod equation
From the above argument, we show that if γ = 3 then any solution with nonzero initial datum blows up infinite time again.
Remark 4.3 Theorem 4.1 is a similar result as that in [5], where γ = 1 for Camassa–Holm equation, whileTheorem 4.2 is a improvement of that in [14], even for γ = 1.
Just as the periodic case, we have the blow-up rate for non-periodic case
limt→T
{(T − t)m(t)} = − 2|γ| and lim
t→T
{(T − t)
∫R
u3(x, t) dx
}= −2 ‖u0‖2
H1
|γ| .
5 Comparison with Camassa–Holm equation
In [15], McKean gave a sufficient and necessary criterion on y0 = Q2u0 (initial potential) for the finite timeformation of singularities in a smooth solution to Camassa–Holm equation
ut − utxx + 3uux = 2uxuxx + uuxxx . (5.1)
He showed that the solution to Eq. (5.1) with u0 ∈ H3(T) blows up in finite time if and only if there exist pointsξ < ζ such that y0(ξ) > 0 and y0(ζ) < 0. In other words, the smooth solution exists globally if and only if
i) y0 does not change sign for periodic case,ii) y0 does not change sign or the set {x | m0(x) > 0} locates right to the set {x | m0(x) < 0} for
non-periodic case.Let u(x, t) solve Eq. (5.1) and let q(x, t) be the particle line along u(x, t), i.e., q(x, t) satisfies the following
equation {qt = u(q, t) , 0 < t < T , x ∈ R ,
q(x, 0) = x , x ∈ R ,(5.2)
where T is the life span of the solution, then q is a diffeomorphism of the line.Set the potential y := u − uxx, then
yt = −yxu − 2yux . (5.3)
From Eqs. (5.2) and (5.3), one obtains⎧⎪⎪⎪⎪⎪⎪⎪⎪⎪⎪⎪⎨⎪⎪⎪⎪⎪⎪⎪⎪⎪⎪⎪⎩
qx(x, t) = eR t0 ux(q,s) ds , y(q)q2
x = y0(x) ,
d
dt[eq(ux − u)] (q) = −1
2eq(ux − u)2(q) − 1
2
∫ q
−∞es(ux − u)2(s) ds ,
d
dt
[e−q(ux + u)
](q) = −1
2e−q(ux + u)2(q) − 1
2
∫ ∞
q
e−s(ux + u)2(s) ds ,
d
dtux(q) =
12
u2(q) − 12
u2x(q) − 1
4
∫ ∞
−∞e−|q−s|(ux ± u)2(s) ds .
The above identities are the most important ingredients of the whole paper [15].But for the rod equation Eq. (1.1), y := u − uxx satisfies
yt = −γyxu − 2γyux + 3(γ − 1)uux ,
which destroys all the above important and beautiful identities, if γ �= 1.So far, the sufficient conditions to guarantee the global existence of smooth solution to Eq. (1.1) are not clear
for general γ ∈ R, γ �= 1. We hope to report it later.Dai and Hou investigated the solitary waves for the rod equation in [8] for γ ∈ R. They showed that only for
γ < 1, there are smooth solitary waves such that
u(x, t) = u(ζ) ∈ H1(R) , ζ = x − V t with V a speed parameter ,
c© 2005 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim
Math. Nachr. 278, No. 14 (2005) / www.mn-journal.com 1739
and only for γ = 1, the solitary waves u(x, t) = u(ζ) ∈ H1(R) are peaked solitons (see also [2]). For γ = 1,Constantin and Strauss [6] proved the orbital stability in H1-norm of peakons by a method which depends on thespecial structure of Camassa–Holm equation. We hope to discuss the stability of the smooth solitary waves forγ < 1 in a forthcoming paper, since it is very interesting and useful both mathematically and for applications.
On the other hand, one can establish like in [19, 20] the well-posedness of weak solutions for the problem(1.1).
Acknowledgements The author would like to express sincere gratitude to his supervisor Professor Zhouping Xin for en-thusiastic guidance and constant encouragement. Thanks also to Professor Shing-Tung Yau and Professor Zhouping Xin forproviding an excellent study and research environment in The Institute of Mathematical Sciences. This work is partiallysupported by NSFC and Shanghai Rising-Star Program 05QMX1417.
References
[1] T. B. Benjamin, J. L. Bona, and J. J. Mahony, Model equations for long waves in nonlinear dispersive systems, Philos.Trans. Roy. Soc. London Ser. A 272, No. 1220, 47–78 (1972).
[2] R. Camassa and D. Holm, An integrable shallow water equation with peaked solitons, Phys. Rev. Lett. 71, 1661–1664(1993).
[3] A. Constantin and J. Escher, On the blow-up rate and the blow-up set of breaking waves for a shallow water equation,Math. Z. 233, 75–91 (2000).
[4] A. Constantin and J. Escher, Well-posedness, global existence and blow-up phenomena for a periodic quasi-linear hy-perbolic equation, Comm. Pure Appl. Math. 51, 475–504 (1998).
[5] A. Constantin and J. Escher, Wave breaking for nonlinear nonlocal shallow water equations, Acta Math. 181, 229–243(1998).
[6] A. Constantin and W. Strauss, Stability of peakons, Comm. Pure Appl. Math. 53, 603–610 (2000).[7] H. H. Dai, Model equations for nonlinear dispersive waves in a compressible Mooney-Rivlin rod, Acta Mech. 127, No.
1–4, 193–207 (1998).[8] H. H. Dai and Y. Huo, Solitary shock waves and other travelling waves in a general compressible hyperelastic rod,
R. Soc. Lond. Proc. Ser. A Math. Phys. Eng. Sci. 456, No. 1994, 331–363 (2000).[9] V. A. Galaktionov and J. L. Vazquez, The problem of blow-up in nonlinear parabolic equations, in: Proceeding of the
Conference on Current Developments in Partial Differential Equations, Temuco 1999, Discrete Contin. Dyn. Syst. 8,No. 2, 399–433 (2002).
[10] A. Himonas and G. Misiołek, The Cauchy problem for an integrable shallow-water equation, Differential Integral Equa-tions 14, No. 7, 821–831 (2001).
[11] T. Kato, Quasi-linear equations of evolution, with applications to partial differential equations, in: Proceedings of theSymposium on Spectral Theory and Differential Equations, Dundee 1974, dedicated to Konrad Jorgens, Lecture Notesin Mathematics Vol. 448 (Springer, Berlin, 1975), pp. 25–70.
[12] T. Kato, On the Korteweg-de Vries equation, Manuscripta Math. 28, No. 1–3, 89–99 (1979).[13] T. Kato, Abstract evolution equations, linear and quasilinear, revisited, in: Proceedings of the Conference on Functional
Analysis and Related Topics, Kyoto 1991, Lecture Notes in Mathematics Vol. 1540 (Springer, Berlin, 1993), pp. 103–125.
[14] Y. Li and P. Olver, Well-posedness and blow-up solutions for an integrable nonlinear dispersive model wave equation,J. Differential Equations 162, 27–63 (2000).
[15] H. P. McKean, Breakdown of a shallow water equation, Asian J. Math. 2, No. 4, 867–874 (1998).[16] G. Rodriguez-Blanco, On the Cauchy problem for the Camassa–Holm equation, Nonlinear Anal. 46, 309–327 (2001).[17] R. Seliger, A note on the breaking of waves, Proc. Roy. Soc. Lond Ser. A. 303, 493–496 (1968).[18] S. Shkoller, Geometry and curvature of diffeomorphism groups with H1 metric and mean hydrodynamics, J. Funct.
Anal. 160, No. 1, 337–365 (1998).[19] Z. Xin and P. Zhang, On the weak solution to a shallow water equation, Comm. Pure Appl. Math. 53, 1411–1433 (2000).[20] Z. Xin and P. Zhang, On the uniqueness and large time behavior of the weak solutions to a shallow water equation,
Comm. Partial Differential Equations 27, No. 9–10, 1815–1844 (2002).[21] Y. Zhou, Wave breaking for a periodic shallow water equation, J. Math. Anal. Appl. 290, 591–604 (2004).[22] Y. Zhou, Wave breaking for a shallow water equation, preprint (2002).
c© 2005 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim