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Phase field models in fluid dynamics

Eduard Feireisl

Institute of Mathematics, Academy of Sciences of the Czech Republic, Prague

joint work with

H.Abels (Regensburg), H.Petzeltov´a (Praha) E.Rocca (Milano), G.Schimperna (Pavia) Villa Clythia, Fr´ejus, April 7th - 12th, 2013

Eduard Feireisl Phase field models

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Motto

Johann von Neumann [1903-1957]

In mathematics you don’t understand things.

You just get used to them.

Eduard Feireisl Phase field models

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Fluid equations

Mass conservation - equation of continuity

t% + divx(%u) = 0 Momentum balance

t(%u) + divx(%u ⊗ u) = divxT+ %g

% = %(t, x ) . . . mass density u = u(t, x ) . . . velocity field T . . . Cauchy stress g . . . external (volume) force

Eduard Feireisl Phase field models

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Phase field models

Phase field function - concentration difference

−1 ≤ c(t, x) ≤ 1

t(%c) + divx(%cu) = divxxµ

µ = µ(t, x ) . . . chemical potential Cahn-Hillard type equation

%µ = %∂f (%, c)

∂c − ∆c

t(%c) + divx(%cu) = ∆ ∂f (%, c)

∂c −1

%∆c



f = f (%, c) . . . free energy

Eduard Feireisl Phase field models

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Stress relation

Young-Laplace law

[T· n] = σHn on interface Viscous stress

S= ν(c)



xu + ∇txu −2 3divxuI



+ η(c)divxuI

Pressure

p(%, c) = %2∂f (%, c)

∂%

Extra stress

T=S− pI



xc ⊗ ∇xc − 1

2|∇xc|2I



Eduard Feireisl Phase field models

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Anderson, McFadden, and Wheeler [1998]

Equation of continuity

t% + divx(%u) = 0 Momentum balance

t(%u) + divx(%u ⊗ u) + ∇xp(%, c)

= divx

 ν(c)



xu + ∇txu −2 3divxuI



+ η(c)divxuI



−divx



xc ⊗ ∇xc −1

2|∇xc|2I

 + %g

Phase field equation

t(%c) + divx(%cu) = ∆ ∂f (%, c)

∂c −1

%∆c



Eduard Feireisl Phase field models

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Boundary conditions

x ∈ Ω ⊂ R3

Ω . . . regular (bounded) domain No-slip

u|∂Ω= 0 No-flux

xc · n|∂Ω= 0, ∇xµ · n|∂Ω= 0

Eduard Feireisl Phase field models

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A bit of history of global existence for large data

Jean Leray [1906-1998]

Global existence of weak solutions for the

incompressible Navier-Stokes system (3D)

Olga Aleksandrovna Ladyzhenskaya [1922-2004] Global existence of classical solutions for the incompressible 2D Navier-Stokes system

Pierre-Louis Lions[*1956] Global existence of weak solutions for the compressible barotropic Navier-Stokes system (2,3D)

and many, many others...

Eduard Feireisl Phase field models

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Constitutive relations

Free energy

f (%, c) = fe(%) + fmix(%, c), fmix(%, c) = H(c) log(%) + G (c) Pressure

p(%, c) = %2∂f (%, c)

∂% = pe(%) + %H(c), fe(%) = Z %

1

pe(z) z2 dz pe(0) = 0, p1%γ−1− p2 ≤ pe0(%) ≤ p3(1 + %γ−1), γ > 3

2 Mixing

−H1 ≤ H0(c), H(c) ≤ H2, G1c − G2≤ G0(c) ≤ G3(1 + c)

Eduard Feireisl Phase field models

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Energy estimates

Total energy E (t) =

Z

1

2%|u|2 + 1

2|∇xc|2+ %f (%, c) dx Total mass

M = Z

% dx , M(t) = Z

%(t, ·) dx = Z

%0 dx , %(0, ·) = %0

Energy (in)equality d

dtE (t) + Z

S: ∇xu + |∇xµ|2 dx ≤

Z

%g · u dx

Eduard Feireisl Phase field models

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Kinetic energy

t

Z

1

2%|u|2 dx + Z

S: ∇xu dx

= Z

p(%)divxu dx + Z

∆c∇xc · u dx

µ = ∂f (%, c)

∂c − 1

%∆c, p(%, c) = %2∂f (%, c)

∂%

“Phase field” stored energy

t

Z

1

2|∇xc|2 dx + Z

|∇xµ|2 dx

= − Z



%∂f (%, c)

∂c ∂tc + %∂f (%, c)

∂c u · ∇xc

 dx

− Z

∆c∇xc · u dx

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Dissipative bounds and Korn’s inequality

Z

S: ∇xu dx ≥ Z

ν(c) 2

xu + ∇txu −2 3divxuI

2

dx

Korn’s inequality Z

ν(c) 2

xu + ∇txu −2 3divxuI

2

dx ≥ νk∇xuk2L2(Ω)

Transport coefficients

ν ≤ ν(c) ≤ ν

0 ≤ η(c) ≤ η

Eduard Feireisl Phase field models

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Available a priori bounds

ess sup

t∈(0,T )

k%(t, ·)kLγ(Ω) ≤ C (data)

ess sup

t∈(0,T )

k∇xc(t, ·)kL2(Ω;R3) ≤ C (data)

ess sup

t∈(0,T )

k√

%u(t, ·)kL2(Ω;R3)≤ C (data)

Z T 0

h

k∇xu(t, ·)k2L2(Ω;R3×3)+ k∇xµ(t, ·)k2L2(Ω;R3)

i

dt ≤ C (data)

Eduard Feireisl Phase field models

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Div-Curl lemma

Hypotheses

Un→ U weakly in Lp(RN; RN), Vn→ V weakly in Lq(RN; RN) 1

p + 1 q = 1

r < 1

{DIV[Un]}n=1, {CURL[Vn]}n=1 precompact in W−1,s for a certain s ≥ 1

Conclusion

Un· Vn→ U · V weakly in Lr(RN)

Eduard Feireisl Phase field models

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Weak compactness of the convective terms

General principle

tSn+ divxFn= rn∈ precompat set in W−1,s

xHn∈ bounded in Lp Application of DIV-CURL lemma

Un= [Sn, Fn], Vn= [Hn, 0, 0, 0]

Conclusion

SH = S H

Eduard Feireisl Phase field models

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Convective terms

Direct application of DIV-CURL lemma

%u = %u, %u ⊗ u = %u ⊗ u

%c = %c, %c2 = %c2 Strong convergence outside vacuum

cn→ c in L2 on the set {% > 0}

Eduard Feireisl Phase field models

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Strong convergence of ∇

x

c

−∆cn= %n∂f (%n, cn)

∂c − %nµn

−∆c = %∂f (%, c)

∂c − %µ

Application of previous observations

%∂f (%, c)

∂c c = %∂f (%, c)

∂c c

%µc = %µc Conclusion

xcn→ ∇xc (strongly) in L2((0, T ) × Ω; R3)

Eduard Feireisl Phase field models

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Renormalized equation of continuity

b ∈ C1[0, ∞), b0(z) = 0 for all z ≥ z0

Renormalized equation

tb(%) + divx(b(%)u) +



b0(%)% − b(%)



divxu = 0

t(% log(%)) + divx



% log(%)u



+ %divxu = 0

Eduard Feireisl Phase field models

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Density oscillations - first approximation

Limit of renormalized equations

t% log(%) + divx

% log(%)u

+ %divxu = 0

Renormalized limit equation

t

% log(%)

+ divx

% log(%)u

+ %divxu = 0

Density oscillations d dt

Z



% log(%) − % log(%)

 dx

+ Z



%divxu − %divxu



dx = 0

Eduard Feireisl Phase field models

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DiPerna-Lions’ regularization method

vδ= κδ∗ v Regularized equation

t%δ+ divx(%δu) = divx



%δu



− [divx(%u)]δ ≡ rδ

xu ∈ Lp, % ∈ Lp0 1 p + 1

p0 = 1

⇒ rδ → 0 as δ → 0

Eduard Feireisl Phase field models

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Effective viscous flux identity

“Weak continuity” of the effective viscous flux p(%)% − 4

3ν(c) + η(c)



%divxu

= p(%)% − 4

3ν(c) + η(c)



%divxu

%divxu − %divxu ≥ 0

% log(%) = % log(%)

%ε→ % a.a. in (0, T ) × Ω

Eduard Feireisl Phase field models

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Effective viscous flux - Step I

“Approximate equation”

p(%n)

= divx−1divxSn− ∂t−1divx[%nun] − divx−1divx[%nun⊗ un] +“compact terms”

Limit equation

p(%) = divx−1divxS− ∂t−1divx[%u] − divx−1divx[%u ⊗ u]

+“compact terms”

Eduard Feireisl Phase field models

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Effective viscous flux - Step II

ν > 0, η = 0 constant

“Approximate equation”

p(%n)%n−4ν

3 %ndivxun

= −∆−1divx[%nun]divx(%nun) − divx−1divx[%nun⊗ un]%n

+“compact terms”

Limit equation

p(%)% − 4ν

3 %divxu

= −∆−1divx[%u]divx(%u) − divx−1divx[%u ⊗ u]%

+“compact terms”

Eduard Feireisl Phase field models

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Effective viscous flux - Step III

Effective viscous flux identity revisited p(%)% −4ν

3 %divxu ≈ p(%)% − 4ν 3 %divxu +weak − limn→∞un·h

%ndivx−1divx[%nun] − %nundivx−1divx[%n]i

−u · h

%divx−1divx[%u] − %udivx−1divx[%]i

Eduard Feireisl Phase field models

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Div-Curl lemma revisited

Hypotheses

Un→ U weakly in Lp(RN; RN), Vn→ V weakly in Lq(RN; RN) 1

p + 1 q = 1

r < 1 Ri ,j = ∂xi−1xj

Conclusion

X

i ,j

UniRi ,j[Vnj] − VniRi ,j[Unj] →X

i ,j

UiRi ,j[Vj] − ViRi ,j[Uj]

weakly in Lr(RN)

Eduard Feireisl Phase field models

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Conclusion

un→ u weakly in L2(0, T ; W01,2(Ω; R3))

%n→ % in Cweak([0, T ]; Lγ(Ω))

%nun→ %u inCweak([0, T ]; L2γ/γ+1(Ω; R3)) Conclusion

un·h

%ndivx−1divx[%nun] − %nundivx−1divx[%n] i

→ u ·h

%divx−1divx[%u] − %udivx−1divx[%]i

Eduard Feireisl Phase field models

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Non-constant viscosity coefficients

Commutator Ri ,j

 ν(cn)



xun+ ∇xutn−2

3divxun∈ I



= Ri ,j

 ν(cn)



xun+ ∇xutn−2

3divxun∈ I



−4

3ν(cn)divxun +4

3ν(cn)divxun

Eduard Feireisl Phase field models

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Commutator lemma [Coifman and Meyer]

Lemma

Let w ∈ W1,r(RN), V ∈ Lp(RN; RN) be given, where 1 < r < N, 1 < p < ∞, 1

r + 1 p − 1

N < 1.

The for any s satisfying 1 r + 1

p − 1 N < 1

s < 1 there exists β > 0 such that

N

X

j =1

Ri ,j[wVj] −

N

X

j =1

w Ri ,j[Vj]

Wβ,s(RN,RN)

≤ ckw kW1,rkVkLp,

i = 1, . . . , n

Eduard Feireisl Phase field models

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General constitutive relations

Oscillations defect measure

ωq[%n→ %](Q) = sup

k>0

 lim sup

n→∞

Z

Q

|Tk(%n) − Tk(%)|q dx dt



Tk(r ) = min{r , k}

Claim

ωq[%n→ %]((0, T ) × Ω) < ∞, q = γ + 1 > 2

Eduard Feireisl Phase field models

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Renormalized equation revisited

Lemma

ωq[%n→ %]((0, T ) × Ω) < ∞, q > 2

%, u satisfy the renormalized equation

Eduard Feireisl Phase field models

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Conclusion - possible extensions

Sir Winston Churchill, [1874–1965]

However beautiful the strategy, you should occasionally look at the results

Eduard Feireisl Phase field models

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Allen-Cahn model

Allen-Cahn equation

t(%c) + divx(%cu) = −µ

µ = µ(t, x ) . . . chemical potential

%µ = %∂f (%, c)

∂c − ∆c

Singular elastic pressure

pe(%) ≈ (% − %)−3 as % → %−

Eduard Feireisl Phase field models

References

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