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Estimation of the residues and technical lemmas

No documento DE L’UNIVERSITÉ PIERRE ET MARIE CURIE (páginas 106-110)

Contrôle de Navier-Stokes avec des conditions au bord

4.5 Estimation of the residues and technical lemmas

The energy contained at high frequencies decays very fast. For low frequencies, we need to use assump- tion (4.51). We introduceρ >0 and we split the energy integral at a cutting threshold whereeζ2ttρ, ie. where|ζ| ≥

ρlnt t

1/2

. Note that the right-hand side tends to zero as t→+∞, enabling us to isolate only asymptotically small frequencies. Let us estimate the high frequencies energy :

W#(t) :=

Z

|ζ|≥|ρlntt |12 1 +ζ22 e−22

Vˆ0(ζ)

2

dζ

t−2ρ Z

R

1 +ζ22

Vˆ0(ζ)

2

dζ

M0t−2ρ.

(4.56)

We move on to low frequencies energy : W[(t) :=

Z

|ζ|≤|ρlntt|12

1 +ζ22 e−22

Vˆ0(ζ)

2

dζ

.

ρlnt t

1 2

· sup

|ζ|≤|ρlntt|12

Vˆ0(ζ)

2

.

(4.57)

Thanks to assumption (4.51), a Taylor expansion atζ= 0 of ˆV0yields :

Vˆ0(ζ) ≤ 1

n!|ζ|n nζVˆ0

.|ζ|n Z

R

zn|V0(z)|dz.|ζ|n Z

R

(1 +z2)n+1|V0(z)|2dz 12

. (4.58)

Combining (4.57) with (4.58) gives :

W[(t).Mn+2

ρlnt t

1 2+n

. (4.59)

Hence, choosingρ=12+nin equation (4.56) and summing with equation (4.59) proves (4.54).Extensions

fork >0 are straightforward with Fourier computations.

Impermeability boundary condition

On O, we have the impermability boundary conditionuε·n= 0. By identification for each power ofεin the expansion, this condition translates to the following conditions for our expansion :

u0·n= 0, (4.62)

v·n= 0, (4.63)

u1+∇xθ˜1+w+Rε

·n= 0, (4.64)

(ρε+ ˜wn= 0. (4.65)

By construction of the Euler trajectory u0, equation (4.62) is true. Since the boundary profile v is tangential, equation (4.63) is also satisfied. By construction, we also already haveu1·n= 0. In order to be able to carry out integrations by part for the estimates of the remainder, we also would like to impose Rε·n= 0. Thus, (4.64) yields :

nθ˜1=−w|z=0·n. (4.66)

Moreover, we see (4.65) as a definition ofu2 once ˜wis known :

ρε·n=−w˜|z=0·n. (4.67)

Incompressibility condition

Similarly, the divergence-free condition on uε translates to :

divu0+n·zv= 0, (4.68) div

slowv+n·zw= 0, (4.69) divu1+ div∇xθ˜1+ div

sloww+ divRε+n·zw˜= 0, (4.70) divρε+ div

sloww˜= 0. (4.71)

Here again, by construction divu0= divu1=n·zv= 0 and we would like to work with divRε= 0. We also build ˜θ1such that ∆˜θ1= 0. Thus, we read equations (4.69), (4.70) and (4.71) as :

n·zw=−div

slowv, (4.72)

n·zw˜=−div

sloww, (4.73)

divρε=−div

sloww.˜ (4.74)

The profilesw·n, ˜w·nand ˜u2are meant to catch up the unwanted divergences of previous profiles.

Slip-with-friction boundary condition

Now, we look at the slip-with-friction boundary condition onO: [D(uε)n+Auε]tan= 0. To lighten the notations, let us introduce an operatorN defined as :

N(f) := [D(f)n+Af]tan. (4.75)

Note that, for functions also depending on the fast variable,D also denotes the derivatives with respect to the slow variables in definition (4.75). Identifying the first orders of the expansion yields :

N(u0)−1

2zv= 0, (4.76)

N(v)−1

2[zw]tan= 0. (4.77)

The remaining terms are left with the remainder : N(u1) +N(∇xθ˜1) +N(w) +N(Rε)−1

2[zwtan+√

ε(N(ρε) +N( ˜w)) = 0. (4.78)

The main boundary profilevwas built to liftN(u0). We choose a basic lifting forN(v) by the profilew.

Other terms are seen as a source term in the equation for the remainder :

N(Rε) =gε:=N(u1) +N(∇xθ˜1) +N(w) +√

εN(ρε) +√

εN( ˜w). (4.79) Note that ˜wis normal and has no tangential component so we can drop it.

4.5.2 Definitions of technical profiles

Let us recall that, at this stage, the three main termsu0,vandu1are defined. In this paragraph, we explain step by step how we build the following terms of the expansion.

Boundary layer pressure

Equation (4.33) only involves the tangential part of the symmetrical convective product between u0 andv. Hence, to compensate its normal part, we introduce as in [108] the pressureqas the unique solution vanishing asz→+∞to :

(u0· ∇)v+ (v· ∇)u0

·n=−zq. (4.80)

Note that the support ofqis included in the support of v. Now, we can write :

tv+ (u0· ∇)v+ (v· ∇)u0+u0[z∂zvzzv+n∂zq= 0. (4.81) Note that this pressure profile vanishes fortT (i.e., onceu0vanishes).

Second boundary correction

The first boundary conditionv generates a non vanishing slow divergence and a non vanishing normal boundary flux. The role of the profilew is to lift to unwanted terms that would be too hard to handle directly in the equation of the remainder. In order to satisfy (4.72) and (4.77), we definewby :

w(t, x, zn:=

Z +∞

z

div

slowv(t, x, z0)dz0, (4.82)

[w(t, x, z)]tan:=−2 [Dx(v(t, x,0))n+Av(t, x,0)]ez. (4.83) Sincevis compactly supported near the boundary, so isw. Moreover,wdepends smoothly on v.

Boundary flux correction

The shape ofw·nis imposed by equation (4.72). The bad consequence is thatw·n6= 0 onO. Thus, we must introduce a dedicated correction∇xθ˜1to ensure (4.66). Therefore, fort≥0, we define ˜θ1as the solution to :

( ∆˜θ1= 0, inO,

nθ˜1=−w(t,·,0)·n, inO. (4.84) It can be check that the compatibility condition is indeed satisfied. This instantaneous defintion is im- portant because it guarantees that ˜u1 := ∇xθ˜1 will inherit decay properties proven for w. This profile solves :









tu˜1+ u0· ∇

˜

u1+ ˜u1· ∇

u0+∇p˜1= 0, inO fort≥0, div ˜u1= 0 inO fort≥0,

˜

u1·n=−w|z=0·n inO fort≥0, u˜1(0,·) = 0 inO att= 0,

(4.85)

where ˜p1:=tθ˜1u0· ∇xθ˜1.

Last instantaneous corrections Eventually, we define :

˜

w(t, x, zn:=

Z +∞

z

div

sloww(t, x, z0)dz0, (4.86)

which is only normal. Here again, we need to lift its normal trace. Fort≥0, we defineρεas the solution to :

( ∆ρε=−div

sloww(t),˜ in O,

nρε=−w(t,˜ ·,0)·n, in O.

(4.87) It can be check that the compatibility condition is indeed satisfied. Thus, the profile solves the evolution equation









txρε+ u0· ∇

xρε+ (∇xρε· ∇)u0+∇µε= 0, in O fort≥0, div∇xρε=−div

sloww˜ in O fort≥0,

xρε·n=−w˜|z=0·n in O fort≥0,

xρε(0,·) = 0 in O att= 0,

(4.88)

whereµε:=tρεu0· ∇xρε.

4.5.3 Equation for the remainder

The equation for the remainder reads :













tRεεRε+ (uε· ∇)Rε+AεRε+∇πε=FεGεHεIε, in Ω fort≥0,

divRε= 0 in Ω fort≥0,

[D(Rε)n+ARε]tan=gε in Ω\Γ fort≥0,

Rε·n= 0 in Ω\Γ fort≥0,

Rε(0,·) = 0 in Ω at t= 0.

(4.89)

Before introducing the source terms, we define the following shortened notations : Wε(t, x, z) :=w(t, x, z) +√

εw(t, x, z),˜ (4.90)

Uε(t, x) :=u1(t, x) + ˜u1(t, x) +√

εu2. (4.91)

Now we can introduce :

AεRε:= (Rε· ∇) u0+εUε

+ (Rε· ∇x) √

εv+εWε

+ (Rε·n) zv+√

ε∂zWε

, (4.92)

Fε:= [∆ϕ∂zv+ 2nzv+zzWε] +√

ε[∆xv+ ∆ϕ∂zWε+ 2nzWε] +ε[∆xWε+ ∆Uε], (4.93) Gε:=u0·n

ϕ z∂zw+ (Wε+Uεn∂z v+√ εWε

+∇x

u0·Wε+v2 2

+√

εx[v·(Wε+Uε)] + ε 2∇x

(Wε+Uε)2

(4.94)

Hε:=∇xq. (4.95)

Iε:=tWε. (4.96)

Functions depending onz are evaluated atz=ϕ(x)/

ε. Moreover, all the source terms are small when εis small. Indeed, the naturalL2 scaling on the fast variable yieldsε1/4 factors.

4.5.4 Size of the remainder

We want to prove that the remainder is sufficiently small at the final time. Since our expansion of uε involvesεRε, we need to prove here thatRε(T /ε,·) =o(1). As usual, we multiply equation (4.89) by Rε and integrate by parts. Since we are controlling the equation on Γ, we can assume that our controls simulate the presence of a Navier slip-with-friction boundary condition on Γ as well (thus, on the whole of Ω). We use [108, Lemma 3, page 150] to win a ε14 factor when evaluating L2 norms of functions involving the fast variable. We can also perform the estimates onOin the same way.

We proceed as we have done in the case of the shape operator. This basic energy method works because with have built enough technical profiles and the following estimates hold :

kAεkL1(L)=O(1), (4.97)

kFεkL1(L2)=O(ε14), (4.98)

kGεkL1(L2)=O(ε14), (4.99)

kHεkL1(L2)=O(ε14), (4.100)

kIεkL1(L2)=O(ε14). (4.101)

Hence, we obtain :

Rε T

ε,·

L2

1/4. (4.102)

No documento DE L’UNIVERSITÉ PIERRE ET MARIE CURIE (páginas 106-110)