Antoine Remond-Tiedrez - Department of Mathematicsremondtiedre/talks/usc-summer... · 2020. 9....

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Setup Goal Difficulties Key “tool” Variants Viscous surface waves and their stability Antoine Remond-Tiedrez Carnegie Mellon University USC Summer School on Mathematical Fluids, May 2017 Antoine Remond-Tiedrez (CMU) Viscous surface waves and their stability May 2017

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Page 1: Antoine Remond-Tiedrez - Department of Mathematicsremondtiedre/talks/usc-summer... · 2020. 9. 14. · Antoine Remond-Tiedrez Carnegie Mellon University USC Summer School on Mathematical

Setup Goal Difficulties Key “tool” Variants

Viscous surface waves and their stability

Antoine Remond-Tiedrez

Carnegie Mellon University

USC Summer School on Mathematical Fluids, May 2017

Antoine Remond-Tiedrez (CMU) Viscous surface waves and their stability May 2017

Page 2: Antoine Remond-Tiedrez - Department of Mathematicsremondtiedre/talks/usc-summer... · 2020. 9. 14. · Antoine Remond-Tiedrez Carnegie Mellon University USC Summer School on Mathematical

Setup Goal Difficulties Key “tool” Variants

Setup

η(t)

d

Σ(t)

Σb

Ω(t) ⊆ R3

ρ(∂tu + (u · ∇) u

)+∇ · S = 0 in Ω(t)

∇ · u = 0 in Ω(t)

Sν = −σHν + ρgην on Σ(t)

∂tη = (u · ν)

√1 + |∇η|2 on Σ(t)

u = 0 on Σb

• S = pI − µDu is the stress tensor

• H is the mean curvature of the free surface

• ρ, σ, µ > 0 are constants

Antoine Remond-Tiedrez (CMU) Viscous surface waves and their stability May 2017

Page 3: Antoine Remond-Tiedrez - Department of Mathematicsremondtiedre/talks/usc-summer... · 2020. 9. 14. · Antoine Remond-Tiedrez Carnegie Mellon University USC Summer School on Mathematical

Setup Goal Difficulties Key “tool” Variants

GoalAsymptotic stability of equilibrium (i.e. global well-posedness forsmall data, and decay to equilibrium).

Antoine Remond-Tiedrez (CMU) Viscous surface waves and their stability May 2017

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Setup Goal Difficulties Key “tool” Variants

Difficulties

• Semilinear problem in a time-dependent domain←→ Quasilinear problem in a fixed domain

• System of PDEs of mixed type

ρ(∂At u + (u · ∇A) u

)− µ∆Au +∇Ap = 0 in Ω ∼ parabolic in u

∇A · u = 0 in Ω

(pI − µDAu) ν = −σ ∇ ·

∇η√1 + |∇η|2

ν + ρgην on Ω ∼ elliptic in h

∂tη + (u1, u2) · ∇η = u3 on Σ ∼ hyperbolic in h

u = 0 on Σb

Antoine Remond-Tiedrez (CMU) Viscous surface waves and their stability May 2017

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Setup Goal Difficulties Key “tool” Variants

Fixing the domain

Σ(t)

Σb

Ω(t)Φ−1

Σ

Σb

Ω

Φ = I + χηe3, where χ =

1 on Σ

0 on Σb

→ ∇Φ ∼ ∇η

∇A is the manifestation of ∇ in the new coordinates, i.e. ∇A is“Φ-conjugate” to ∇ (and similarly for ∂At )

∇Au := ∇(u Φ−1

) Φ ∼ (∇u) (∇η)−1

Antoine Remond-Tiedrez (CMU) Viscous surface waves and their stability May 2017

Page 6: Antoine Remond-Tiedrez - Department of Mathematicsremondtiedre/talks/usc-summer... · 2020. 9. 14. · Antoine Remond-Tiedrez Carnegie Mellon University USC Summer School on Mathematical

Setup Goal Difficulties Key “tool” Variants

Key “tool”: energy-dissipation relation

d

dt

(∫Ω(t)

ρ

2|u|2 +

∫R2

σ

√1 + |∇η|2 +

∫R2

g

2|η|

2)

︸ ︷︷ ︸Energy

+

∫Ω(t)

µ

2|Du|2︸ ︷︷ ︸

Dissipation

= 0

If moreover D is coercive over E , thenE +D = 0

CE ≤ D

→ E + CE ≤ 0

→ E(t) ≤ E(0)e−Ct

i.e. exponential decay to equilibrium (of small data) [Guo & Tice 2013]

Antoine Remond-Tiedrez (CMU) Viscous surface waves and their stability May 2017

Page 7: Antoine Remond-Tiedrez - Department of Mathematicsremondtiedre/talks/usc-summer... · 2020. 9. 14. · Antoine Remond-Tiedrez Carnegie Mellon University USC Summer School on Mathematical

Setup Goal Difficulties Key “tool” Variants

Variants

• Surfactants

• Elastic sheets

Incorporating various additional physics effects boils down totinkering with the surface energy.Recall that the surface energy associated with surface tension is∫

R2

σ

√1 + |∇η|2 =

∫Σ(t)

σ

which appears in the dynamic boundary condition via

Sν = −σHν︸ ︷︷ ︸δ(∫

Σ(t) σ)+ ρgην

Antoine Remond-Tiedrez (CMU) Viscous surface waves and their stability May 2017

Page 8: Antoine Remond-Tiedrez - Department of Mathematicsremondtiedre/talks/usc-summer... · 2020. 9. 14. · Antoine Remond-Tiedrez Carnegie Mellon University USC Summer School on Mathematical

Setup Goal Difficulties Key “tool” Variants

Surfactants

Antoine Remond-Tiedrez (CMU) Viscous surface waves and their stability May 2017

Page 9: Antoine Remond-Tiedrez - Department of Mathematicsremondtiedre/talks/usc-summer... · 2020. 9. 14. · Antoine Remond-Tiedrez Carnegie Mellon University USC Summer School on Mathematical

Setup Goal Difficulties Key “tool” Variants

SurfactantsSurfactants introduce Marangoni forces, due to surface tensiongradients. In other words, the surface energy changes∫

Σ(t)σ 7→

∫Σ(t)

σ(c)

and therefore the dynamic boundary condition changes

i.e. Sν = −σHν +ρgην on Σ(t)

becomes Sν = −σ(c)Hν +∇Σ(t)σ(c) +ρgην on Σ(t)

We must also specify the dynamics of the surfactants

∂tc +∇Σ(t) · (cu) = ∆Σ(t)c

Once again, exponential decay to equilibrium for small data can beshown [Kim & Tice 2016]

Antoine Remond-Tiedrez (CMU) Viscous surface waves and their stability May 2017

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Setup Goal Difficulties Key “tool” Variants

Elastic sheets

Antoine Remond-Tiedrez (CMU) Viscous surface waves and their stability May 2017

Page 11: Antoine Remond-Tiedrez - Department of Mathematicsremondtiedre/talks/usc-summer... · 2020. 9. 14. · Antoine Remond-Tiedrez Carnegie Mellon University USC Summer School on Mathematical

Setup Goal Difficulties Key “tool” Variants

Elastic sheetsThe elastic sheet covering the free surface is accounted for byadding an elastic surface energy term.∫

Σ(t)σ 7→

∫Σ(t)

σ +

∫Σ(t)

1

2H2

and therefore an additional term appears in the dynamic boundarycondition

Sν = −σHν +

[∆Σ(t)H−H

(H2 − 4K

)]ν + ρgην on Σ(t)

Once again, small data decays to equilibrium exponentially fast(coming soon-ish to a journal near you).

Antoine Remond-Tiedrez (CMU) Viscous surface waves and their stability May 2017

Page 12: Antoine Remond-Tiedrez - Department of Mathematicsremondtiedre/talks/usc-summer... · 2020. 9. 14. · Antoine Remond-Tiedrez Carnegie Mellon University USC Summer School on Mathematical

Setup Goal Difficulties Key “tool” Variants

Elastic sheetsRecall that the total surface energy is

σ

∫Σ(t)

1 +

∫Σ(t)

1

2H2

where∫Σ(t)

1 ∼∫R2

1

2|∇η|2 since

(1 + |∇η|2

)1/2∼ 1 +

1

2|∇η|2∫

Σ(t)

1

2H2 ∼

∫R2

1

2|∇2η|2 since |H|2 ∼ |∆η|2

and

∫R2

|∆η|2 =

∫R2

|∇2η|2

Antoine Remond-Tiedrez (CMU) Viscous surface waves and their stability May 2017

Page 13: Antoine Remond-Tiedrez - Department of Mathematicsremondtiedre/talks/usc-summer... · 2020. 9. 14. · Antoine Remond-Tiedrez Carnegie Mellon University USC Summer School on Mathematical

Setup Goal Difficulties Key “tool” Variants

Thank you for your attention!

Antoine Remond-Tiedrez (CMU) Viscous surface waves and their stability May 2017