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Interplay of viscosity and dry friction in rate-independent - - PowerPoint PPT Presentation

Introduction Viscous doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies Riccarda


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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

Riccarda Rossi (Universit` a di Brescia) joint work (in progress) with Alexander Mielke (WIAS & Humboldt-Universit¨ at – Berlin) Giuseppe Savar´ e (Universit` a di Pavia) WIAS, Berlin, 22.04.2009

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Rate-independent evolutions in the applications

  • 1. quasistatic propagation of fracture [Bourdin, Cagnetti, Chambolle, Dal Maso,

Francfort, Giacomini, Knees, Larsen, Lazzaroni, Marigo, Mielke, Negri, Ortner, Ponsiglione, Toader, Zanini ......]

  • 2. quasistatic phase transformations in shape memory alloys (SMA) [Auricchio,

Levitas, Mainik, Mielke, Theil, Roub´ ıˇ cek, Stefanelli....]

  • 3. elastoplasticity: linearized & finite-strain [Dal Maso, DeSimone, Fiaschi,

Francfort, Mora, Morini, Mielke, Mainik, Roub´ ıˇ cek...]

  • 4. damage [Francfort, Garroni, Larsen, Mielke, Roub´

ıˇ cek, Thomas...]

  • 5. delamination [Koˇ

cvara, Mielke, Roub´ ıˇ cek, Scardia, Zanini...]

  • 6. ferromagnetism, ferroelectricity, superconductivity [Mielke, Schmid, Timofte...]
  • 7. shape evolution of debonding membranes [Bucur, Buttazzo..]

In these applications

◮ Typical energies are nonsmooth & nonconvex ◮ Ambient spaces may lack a natural linear structure (e.g. in crack propagation) Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Energetic formulation for rate-independent evolutions

Weak formulations (“derivative-free”)

Based on

◮ energetic balance (energy identity) ◮ stability conditions ◮ possibly enforcing irreversibility Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Energetic formulation for rate-independent evolutions

Abstract approach by Mielke

♣ Ambient space U topological space ♣ Dissipation: D : U× U → [0, +∞] pseudo-distance ♣ Energy: E : (0, T) × U → (−∞, +∞]

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Energetic formulation for rate-independent evolutions

Abstract approach by Mielke

♣ Ambient space U topological space ♣ Dissipation: D : U× U → [0, +∞] pseudo-distance ♣ Energy: E : (0, T) × U → (−∞, +∞]

Energetic formulation [Mielke-Theil’99,’04], [Mielke-Theil-Levitas’02],

[Mainik-Mielke’05]

Global energetic solutions u : [0, T] → U: global stability condition & energy balance E(t, u(t)) − E(t, z) ≤ D(u(t), z) ∀ z ∈ U, E(t, u(t)) + DissD(u, [0, t]) = E(0, u(0)) + Z t ∂tE(r, u(r)) dr . DissD being the global dissipation functional associated with D

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The convex case

In [Mielke-Theil’04]: if

◮ ambient space U is a reflexive Banach space B ◮ E(t, ·) (uniformly) convex & smooth ◮ D induced by Ψ1 : B → [0, +∞) convex & 1-positively homogeneous

(Ψ1 ∼ · )

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The convex case

In [Mielke-Theil’04]: if

◮ ambient space U is a reflexive Banach space B ◮ E(t, ·) (uniformly) convex & smooth ◮ D induced by Ψ1 : B → [0, +∞) convex & 1-positively homogeneous

(Ψ1 ∼ · ) then

◮ u ∈ AC([0, T]; B) (even Lipschitz in time) ◮ the energetic formulation is equivalent to the doubly nonlinear equation

∂Ψ1(u′(t)) + ∂E(t, u(t)) ∋ 0 in B′ t ∈ (0, T) (subdifferential formulation) with ∂E(t, ·) convex subdifferential of E(t, ·) w.r.t. u ξ ∈ ∂E(t, u) ⇔ E(t, w) − E(t, u) ≥ ξ, w − u for all w ∈ B

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The convex case

In [Mielke-Theil’04]: if

◮ ambient space U is a reflexive Banach space B ◮ E(t, ·) (uniformly) convex & smooth ◮ D induced by Ψ1 : B → [0, +∞) convex & 1-positively homogeneous

(Ψ1 ∼ · )

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The convex case

In [Mielke-Theil’04]: if

◮ ambient space U is a reflexive Banach space B ◮ E(t, ·) (uniformly) convex & smooth ◮ D induced by Ψ1 : B → [0, +∞) convex & 1-positively homogeneous

(Ψ1 ∼ · ) then

◮ u ∈ AC([0, T]; B) (even Lipschitz in time) ◮ the energetic formulation is equivalent to the doubly nonlinear equation

∂Ψ1(u′(t)) + ∂E(t, u(t)) ∋ 0 in B′ t ∈ (0, T) (subdifferential formulation) with ∂E(t, ·) convex subdifferential of E(t, ·) w.r.t. u ξ ∈ ∂E(t, u) ⇔ E(t, w) − E(t, u) ≥ ξ, w − u for all w ∈ B

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The nonconvex case: towards local stability

If E(t, ·) is nonconvex

◮ Ψ1, 1-homogeneous, has a linear growth at ∞

∂Ψ1(u′(t)) + ∂E(t, u(t)) ∋ 0 in B′ t ∈ (0, T), we only expect u ∈ BV(0, T; B) ( u may jump!!!)

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The nonconvex case: towards local stability

If E(t, ·) is nonconvex

◮ Ψ1, 1-homogeneous, has a linear growth at ∞

∂Ψ1(u′(t)) + ∂E(t, u(t)) ∋ 0 in B′ t ∈ (0, T), we only expect u ∈ BV(0, T; B) ( u may jump!!!)

Problem with the Global Energetic formulation

Global stability forces global energetic solutions to jump too early and overcome too large energy barriers to avoid energy losses

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Bad Vs. Good jumps

The simplest nonconvex case ( B = R , Ψ1(v) = |v| ∀ v ∈ R E(t, u) = W(u) − ℓ(t)u ∀ (t, u) ∈ [0, T] × R

◮ W double well potential ◮ ℓ ∈ C1([0, T]) ∼ external loading

Sign(u′(t)) + W′(u(t)) ∋ ℓ(t), t ∈ (0, T)

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Bad Vs. Good jumps

The simplest nonconvex case ( B = R , Ψ1(v) = |v| ∀ v ∈ R E(t, u) = W(u) − ℓ(t)u ∀ (t, u) ∈ [0, T] × R

◮ W double well potential ◮ ℓ ∈ C1([0, T]) ∼ external loading

Sign(u′(t)) + W′(u(t)) ∋ ℓ(t), t ∈ (0, T) Convexification W∗∗ of W

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Bad Vs. Good jumps

The simplest nonconvex case ( B = R , Ψ1(v) = |v| ∀ v ∈ R E(t, u) = W(u) − ℓ(t)u ∀ (t, u) ∈ [0, T] × R

◮ W double well potential ◮ ℓ ∈ C1([0, T]) ∼ external loading

Sign(u′(t)) + W′(u(t)) ∋ ℓ(t), t ∈ (0, T) Global solutions are given by u(t) = (DW∗∗)−1 (ℓ(t) − 1): jumping too early!

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Bad Vs. Good jumps

The simplest nonconvex case ( B = R , Ψ1(v) = |v| ∀ v ∈ R E(t, u) = W(u) − ℓ(t)u ∀ (t, u) ∈ [0, T] × R

◮ W double well potential ◮ ℓ ∈ C1([0, T]) ∼ external loading

Sign(u′(t)) + W′(u(t)) ∋ ℓ(t), t ∈ (0, T) We aim to model the “right” hysteresis dynamics

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The vanishing viscosity approach

Aim:

Formulation for rate-independent problems

◮ modelling only “natural” jumps (due to u ∈ BV(0, T; B)), ◮ leading to solutions jumping later than global energetic solutions Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The vanishing viscosity approach

Aim:

Formulation for rate-independent problems

◮ modelling only “natural” jumps (due to u ∈ BV(0, T; B)), ◮ leading to solutions jumping later than global energetic solutions

The vanishing viscosity method:

select rate-independent evolutions arising in the limit of viscous regularizations. In:

◮ plasticity with softening: [Dal Maso-DeSimone-Mora-Morini’08], nonconvex

elastoplasticity: [Fiaschi’09].

◮ crack propagation: [Toader-Zanini’06], [Knees-Mielke-Zanini’07, ’08],

[Cagnetti’07].

◮ general rate-independent evolution with discontinuous inputs: [Krejˇ

c´ ı-Liero’07].

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The vanishing viscosity approach

Aim:

Formulation for rate-independent problems

◮ modelling only “natural” jumps (due to u ∈ BV(0, T; B)), ◮ leading to solutions jumping later than global energetic solutions

The vanishing viscosity method:

select rate-independent evolutions arising in the limit of viscous regularizations. In:

◮ plasticity with softening: [Dal Maso-DeSimone-Mora-Morini’08], nonconvex

elastoplasticity: [Fiaschi’09].

◮ crack propagation: [Toader-Zanini’06], [Knees-Mielke-Zanini’07, ’08],

[Cagnetti’07].

◮ general rate-independent evolution with discontinuous inputs: [Krejˇ

c´ ı-Liero’07]. The vanishing viscosity approach leads to formulations oriented towards local stability [Dal Maso-Toader’02], [Negri-Ortner’07], (crack propagation), [Stefanelli’08]..

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The vanishing viscosity approach

Problem

In the vanishing viscosity limit:

◮ local stability ◮ energy inequality

may not be enough for controlling jumps. ¿ Which further conditions better describe them?

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The vanishing viscosity approach

Problem

In the vanishing viscosity limit:

◮ local stability ◮ energy inequality

may not be enough for controlling jumps. ¿ Which further conditions better describe them?

An abstract approach

Approximation by vanishing viscosity of

◮ doubly nonlinear rate-independent equations (subdifferential formulation) ◮ in an abstract Banach setting, with general nonconvex energy functionals

extending previous analysis by Efendiev-Mielke [Efendiev-Mielke’06]

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The technique by Efendiev-Mielke

A reparametrization technique

◮ We are modelling systems with two time scales: ◮ a scale intrinsic to the system, fast time scale ◮ the slow time scale of the external loading ∼ ∂tE (dominating scale)

viscous dissipation is negligible!

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The technique by Efendiev-Mielke

A reparametrization technique

◮ We are modelling systems with two time scales: ◮ a scale intrinsic to the system, fast time scale ◮ the slow time scale of the external loading ∼ ∂tE (dominating scale)

viscous dissipation is negligible!

◮ Jumps in the vanishing viscosity limit correspond to viscous transitions between

stable states

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The technique by Efendiev-Mielke

A reparametrization technique

◮ We are modelling systems with two time scales: ◮ a scale intrinsic to the system, fast time scale ◮ the slow time scale of the external loading ∼ ∂tE (dominating scale)

viscous dissipation is negligible!

◮ Jumps in the vanishing viscosity limit correspond to viscous transitions between

stable states

◮ To capture the viscous transition path: NOT SHRINK jumps at a point, look at

curves with their arc length parametrization

◮ Asymptotic analysis of (reparametrized) trajectories in an extended phase space Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Nonconvex energies

[Mielke-R.-Savar´ e, in progress] In infinite dimensions:

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Nonconvex energies

[Mielke-R.-Savar´ e, in progress] In infinite dimensions: Approximate ∂Ψ(u′(t)) + ∂E(t, u(t)) ∋ 0 in B′ t ∈ (0, T), (DNE) Ψ 1-positively homogeneous

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Nonconvex energies

[Mielke-R.-Savar´ e, in progress] In infinite dimensions: with, as ε ց 0 ∂Ψε(u′(t)) + ∂E(t, u(t)) ∋ 0 in B′ t ∈ (0, T), (DNE) Ψε with superlinear growth

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Nonconvex energies

[Mielke-R.-Savar´ e, in progress] In infinite dimensions: with, as ε ց 0 ∂Ψε(u′(t)) + ∂E(t, u(t)) ∋ 0 in B′ t ∈ (0, T), (DNE) Ψε with superlinear growth Nonconvexity & nonsmoothness of E(t, ·) affect both the viscous and the rate-independent equation

Two issues

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Nonconvex energies

[Mielke-R.-Savar´ e, in progress] In infinite dimensions: with, as ε ց 0 ∂Ψε(u′(t)) + ∂E(t, u(t)) ∋ 0 in B′ t ∈ (0, T), (DNE) Ψε with superlinear growth Nonconvexity & nonsmoothness of E(t, ·) affect both the viscous and the rate-independent equation

Two issues

◮ u → E(t, u) is nonconvex ⇒ choice of a suitable subdifferential notion ∂E Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Nonconvex energies

[Mielke-R.-Savar´ e, in progress] In infinite dimensions: with, as ε ց 0 ∂Ψε(u′(t)) + ∂E(t, u(t)) ∋ 0 in B′ t ∈ (0, T), (DNE) Ψε with superlinear growth Nonconvexity & nonsmoothness of E(t, ·) affect both the viscous and the rate-independent equation

Two issues

◮ u → E(t, u) is nonconvex ⇒ choice of a suitable subdifferential notion ∂E ◮ jumps in the rate-independent evolution ⇒ to be modelled via vanishing

viscosity

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Outline

♣ existence results for “viscous” doubly nonlinear equations with nonconvex energies ♣ two ideas on the vanishing viscosity analysis

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Outline

♣ existence results for “viscous” doubly nonlinear equations with nonconvex energies ♣ two ideas on the vanishing viscosity analysis ♣ parametrized rate-independent evolutions:

◮ local stability ◮ jumps ↔ viscous transitions between metastable states Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Which subdifferential notion? Heuristics

( ∂Ψε(u′(t)) + ∂E(t, u(t)) ∋ 0 in B′ t ∈ (0, T), u(0) = u0 (DNE) Ψε with superlinear growth

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Which subdifferential notion? Heuristics

( ∂Ψε(u′(t)) + ∂E(t, u(t)) ∋ 0 in B′ t ∈ (0, T), u(0) = u0 (DNE) Ψε with superlinear growth

Step 1: approximation by time discretization

◮ Fix time step τ > 0

partition 0 < t1 < . . . tn = nτ < . . . < tN = T of (0, T)

◮ Discrete solutions: the recursive minimization problem

Find U0

τ , U1 τ , . . . , UN τ ∈ B:

Un

τ ∈ ArgminU∈B{τΨε

U − Un−1

τ

τ ! + E(tn, U)}, U0

τ := u0

has a solution if E(t, ·) is coercive (e.g., E(t, ·) + · 2

B has compact sublevels)

◮ Discrete Euler-Lagrange equation: ∂F E(t, ·) the Fr´

echet subdifferential of E(t, ·) ∂Ψε Un

τ − Un−1 τ

τ ! + ∂F E(tn, Un

τ) ∋ 0,

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The Fr´ echet subdifferential

Idea: “localize” the convex subdifferential

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The Fr´ echet subdifferential

Idea: “localize” the convex subdifferential

The convex subdifferential

Given u ∈ D(E(t, ·)), ξ ∈ ∂E(t, u) ⇔ E(t, w) − E(t, u) ≥ ξ, w − u for all w ∈ B

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The Fr´ echet subdifferential

Idea: “localize” the convex subdifferential

The Fr´ echet subdifferential

Given u ∈ D(E(t, ·)), ξ ∈ ∂F E(t, u) ⇔ lim inf

w→u

E(t, w) − E(t, u) ≥ ξ, w − u w − uB ≥ 0

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The Fr´ echet subdifferential

Idea: “localize” the convex subdifferential

The Fr´ echet subdifferential

Given u ∈ D(E(t, ·)), ξ ∈ ∂F E(t, u) ⇔ lim inf

w→u

E(t, w) − E(t, u) ≥ ξ, w − u w − uB ≥ 0

◮ ∂F E(t, u) ≡ ∂E(t, u) if E(t, ·) is convex ◮ ∂F E(t, u) is convex for all u ∈ D(E(t, ·)) ◮ The map u ⇒ ∂F E(t, u) is not strongly-weakly closed in the sense of graphs!!! Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Heuristics

Step 2: estimates on the approximate solutions

◮ Approximate solutions:

interpolants on (0, T) of the discrete solutions {Uk

τ }n k=1:

◮ {Uτ } piecewise constant; ◮ {b

U

τ } piecewise linear. ◮ from the discrete Euler-Lagrange equation Approximate equation:

∂Ψε “ b U′

τ(t)

” + ∂F E(t, Uτ(t)) ∋ 0 t ∈ (0, T)

◮ A priori estimates + compactness (strong for b

U

τ, weak for b

U′

τ)

◮ convergence to some limit curve u ∈ W 1,1(0, T; B)

BUT: you can’t pass to the limit in −∂Ψε “ b U′

τ(t)

” ∋ ∂F E(t, Uτ(t)) ∋ 0 t ∈ (0, T) because u ⇒ ∂F E(t, u) in general is NOT strongly-weakly closed!!

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The limiting subdifferential

First idea:

Consider (a version of) the strong-weak closure of ∂F E(t, u): the limiting subdifferential ∂E(t, ·) [Mordukhovich’84] given u ∈ D(en(t, ·)), ξ ∈ ∂E(t, u) ⇔ ∃ {un}, {ξn} ⊂ B : 8 > > > < > > > : ξn ∈ ∂F E(t, un) ∀ n ∈ N, un → u, ξn ⇀ ξ, supn E(t, un) < +∞ The limiting subdifferential is our notion of subdifferential!

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Heuristics

Second idea:

◮ Instead of passing to the limit in the pointwise equation

−∂Ψε “ b U′

τ(t)

” ∋ ∂F E(t, Uτ(t)) ∋ 0 t ∈ (0, T) pass to the limit in the approximate energy inequality (technical point!) Z t Ψε “ b U′

τ(s)

” ds + Z t Ψ∗

ε

“ −∂F E(s, Uτ(s)) ” ds + E(t, Uτ(t)) ≤ E(0, u0) + Z t ∂tE(s, Uτ(s)) ds with Ψ∗

ε the Fenchel-Moreau conjugate of Ψε

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Heuristics

Second idea:

◮ Instead of passing to the limit in the pointwise equation

−∂Ψε “ b U′

τ(t)

” ∋ ∂F E(t, Uτ(t)) ∋ 0 t ∈ (0, T) pass to the limit in the approximate energy inequality (technical point!) Z t Ψε “ b U′

τ(s)

” ds + Z t Ψ∗

ε

“ −∂F E(s, Uτ(s)) ” ds + E(t, Uτ(t)) ≤ E(0, u0) + Z t ∂tE(s, Uτ(s)) ds with Ψ∗

ε the Fenchel-Moreau conjugate of Ψε

◮ By LOWER-SEMICONTINUITY obtain the limit energy inequality

Z t Ψε(u′(s)) ds + Z t Ψ∗

ε (−∂E(s, u(s))) ds + E(t, u(t))

≤ E(0, u0) + Z t ∂tE(s, u(s)) ds

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Heuristics

Third idea:

If ∂E(t, ·) fulfils the chain rule u ∈ W 1,1(0, T; B) ⇒ d dt E(t, u(t)) = ∂E(t, u(t)), u′(t)+∂tE(t, u(t)) a.e. in (0, T)

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Heuristics

Third idea:

If ∂E(t, ·) fulfils the chain rule u ∈ W 1,1(0, T; B) ⇒ d dt E(t, u(t)) = ∂E(t, u(t)), u′(t)+∂tE(t, u(t)) a.e. in (0, T) then Z t Ψε(u′(s)) ds + Z t Ψ∗

ε (−∂E(s, u(s))) ds + E(t, u(t)) ≤ E(0, u0) +

Z t ∂tE(s, u(s)) ds

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Heuristics

Third idea:

If ∂E(t, ·) fulfils the chain rule u ∈ W 1,1(0, T; B) ⇒ d dt E(t, u(t)) = ∂E(t, u(t)), u′(t)+∂tE(t, u(t)) a.e. in (0, T) then Z t Ψε(u′(s)) ds + Z t Ψ∗

ε (−∂E(s, u(s))) ds + E(t, u(t)) ≤ E(0, u0) +

Z t ∂tE(s, u(s)) ds = E(t, u(t)) − Z t ∂E(s, u(s)), u′(s) ds

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Heuristics

Third idea:

If ∂E(t, ·) fulfils the chain rule u ∈ W 1,1(0, T; B) ⇒ d dt E(t, u(t)) = ∂E(t, u(t)), u′(t)+∂tE(t, u(t)) a.e. in (0, T) then Z t Ψε(u′(s)) ds + Z t Ψ∗

ε (−∂E(s, u(s))) ds + E(t, u(t)) ≤ E(0, u0) +

Z t ∂tE(s, u(s)) ds = E(t, u(t)) − Z t ∂E(s, u(s)), u′(s) ds Z t “ Ψε(u′(s)) + Ψ∗

ε (−∂E(s, u(s))) + ∂E(s, u(s)), u′(s)

” ds = 0

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Heuristics

Third idea:

If ∂E(t, ·) fulfils the chain rule u ∈ W 1,1(0, T; B) ⇒ d dt E(t, u(t)) = ∂E(t, u(t)), u′(t)+∂tE(t, u(t)) a.e. in (0, T) then Z t Ψε(u′(s)) ds + Z t Ψ∗

ε (−∂E(s, u(s))) ds + E(t, u(t)) ≤ E(0, u0) +

Z t ∂tE(s, u(s)) ds = E(t, u(t)) − Z t ∂E(s, u(s)), u′(s) ds Ψε(u′(t)) + Ψ∗

ε (−∂E(t, u(t))) + ∂E(t, u(t)), u′(t) = 0 a.e. in (0, T)

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Heuristics

Third idea:

If ∂E(t, ·) fulfils the chain rule u ∈ W 1,1(0, T; B) ⇒ d dt E(t, u(t)) = ∂E(t, u(t)), u′(t)+∂tE(t, u(t)) a.e. in (0, T) then Z t Ψε(u′(s)) ds + Z t Ψ∗

ε (−∂E(s, u(s))) ds + E(t, u(t)) ≤ E(0, u0) +

Z t ∂tE(s, u(s)) ds = E(t, u(t)) − Z t ∂E(s, u(s)), u′(s) ds whence ∂Ψε(u′(t)) + ∂E(t, u(t)) ∋ 0 for a.a. t ∈ (0, T). and the energy identity Z t Ψε(u′(s)) ds+ Z t Ψ∗

ε (−∂E(s, u(s))) ds+E(t, u(t)) = E(0, u0)+

Z t ∂tE(s, u(s)) ds

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

An existence result

To sum it up

◮ Fr´

echet subdifferential ∂F E(t, ·) naturally pops out from time-incremental minimization

◮ use with its strong-weak closure ∂E(t, ·) Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

An existence result

Existence theorem

Assume

◮ u → E(t, u) is coercive ◮ t → E(t, u) is smooth enough ◮ ∂E(t, ·) complies with the chain rule: for example if

E(t, ·) = Econvex(t, ·) + Econcave(t, ·) & the convex part dominates concave part

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

An existence result

Existence theorem

Assume

◮ u → E(t, u) is coercive ◮ t → E(t, u) is smooth enough ◮ ∂E(t, ·) complies with the chain rule: for example if

E(t, ·) = Econvex(t, ·) + Econcave(t, ·) & the convex part dominates concave part Then, the approximate solutions converge to a curve u ∈ W 1,1(0, T; B) which solves the Cauchy problem for ∂Ψε(u′(t)) + ∂E(t, u(t)) ∋ 0 for a.a. t ∈ (0, T).

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

An existence result

Existence theorem

Assume

◮ u → E(t, u) is coercive ◮ t → E(t, u) is smooth enough ◮ ∂E(t, ·) complies with the chain rule: for example if

E(t, ·) = Econvex(t, ·) + Econcave(t, ·) & the convex part dominates concave part Then, the approximate solutions converge to a curve u ∈ W 1,1(0, T; B) which solves the Cauchy problem for ∂Ψε(u′(t)) + ∂E(t, u(t)) ∋ 0 for a.a. t ∈ (0, T). Moreover, u fulfils the energy identity (due to the chain rule) for all 0 ≤ s ≤ t ≤ T Z t

s

Ψε(u′(r)) dr+ Z t

s

Ψ∗

ε (−∂E(r, u(r))) dr+E(t, u(t)) = E(0, u0)+

Z t

s

∂tE(r, u(r)) dr .

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Setting

Specialize to dissipation Ψε on B Ψε(·) =

rate-independent

z }| { Ψ1(·) + ε

viscous

z }| { Ψ2(·)

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Setting

Specialize to dissipation Ψε on B Ψε(·) =

rate-independent

z }| { Ψ1(·) + ε

viscous

z }| { Ψ2(·) Further specialize to dissipation given by norms!

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Setting

Specialize to dissipation Ψε on B Ψε(·) =

rate-independent

z }| { Ψ1(·) + ε

viscous

z }| { Ψ2(·) Further specialize to dissipation given by norms!

Abstract rate-independent evolutions

◮ Dissipation: ◮ B2 reflexive ◮ B2 ⊂ B1 ≡ B ◮ rate-independent dissipation: Ψ1(·) = | · |1 ◮ Energy: E : (0, T) × B2 → (−∞, +∞], E(t, ·) with compact sublevels in B2,

E(t, ·) nonconvex, smooth with respect to t

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Setting

Specialize to dissipation Ψε on B Ψε(·) =

rate-independent

z }| { Ψ1(·) + ε

viscous

z }| { Ψ2(·) Further specialize to dissipation given by norms!

Abstract rate-independent evolutions

◮ Dissipation: ◮ B2 reflexive ◮ B2 ⊂ B1 ≡ B ◮ rate-independent dissipation: Ψ1(·) = | · |1 ◮ Energy: E : (0, T) × B2 → (−∞, +∞], E(t, ·) with compact sublevels in B2,

E(t, ·) nonconvex, smooth with respect to t ∂Ψ1(u′(t)) + ∂E(t, u(t)) ∋ 0 in B′

2, t ∈ (0, T)

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Setting

Specialize to dissipation Ψε on B Ψε(·) =

rate-independent

z }| { Ψ1(·) + ε

viscous

z }| { Ψ2(·) Further specialize to dissipation given by norms!

Interaction of L1 & L2 norms

◮ Dissipation: ◮ B2 ∼ L2(Ω) ◮ B1 ∼ L1(Ω) ◮ rate-independent dissipation: Ψ1(·) = | · |1 ◮ Energy:

E(t, u) = 1 2 Z

|∇u|2 +

double-well potential

z }| { Z

W(u) − ℓ(t), u

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Setting

Specialize to dissipation Ψε on B Ψε(·) =

rate-independent

z }| { Ψ1(·) + ε

viscous

z }| { Ψ2(·) Further specialize to dissipation given by norms!

Interaction of L1 & L2 norms

◮ Dissipation: ◮ B2 ∼ L2(Ω) ◮ B1 ∼ L1(Ω) ◮ rate-independent dissipation: Ψ1(·) = | · |1 ◮ Energy:

E(t, u) = 1 2 Z

|∇u|2 +

double-well potential

z }| { Z

W(u) − ℓ(t), u ∂Ψ1(u′(t)) + ∂E(t, u(t)) ∋ 0 in B′

2, t ∈ (0, T)

Sign(ut) − ∆u + W′(u) = ℓ(t) in Ω × (0, T)

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Setting

Specialize to dissipation Ψε on B Ψε(·) =

rate-independent

z }| { Ψ1(·) + ε

viscous

z }| { Ψ2(·) Further specialize to dissipation given by norms!

Interaction of L1 & L2 norms

◮ Dissipation: ◮ B2 ∼ L2(Ω) ◮ B1 ∼ L1(Ω) ◮ rate-independent dissipation: Ψ1(·) = | · |1 ◮ viscous approximation Ψε(·) = | · |1 + ε

2 · 2

2 ◮ Energy:

E(t, u) = 1 2 Z

|∇u|2 + Z

W(u) − ℓ(t), u ε∂Ψ2(u′(t)) + ∂Ψ1(u′(t)) + ∂E(t, u(t)) ∋ 0 in B′

2, t ∈ (0, T)

εut + Sign(ut) − ∆u + W′(u) = ℓ(t) in Ω × (0, T)

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Step 1: energy identity

Chain rule for ∂E + convex analysis: every solution of

∂Ψε(u′(t))

z }| { ε∂Ψ2(u′(t)) + ∂Ψ1(u′(t)) + ∂E(t, u(t)) ∋ 0 in B′

2, t ∈ (0, T)

fulfils energy identity ∀ 0 ≤ t1 ≤ t2 ≤ T Z t2

t1

Ψε (˙ u(r)) dr + Z t2

t1

Ψε∗ (−∂E(r, u(r))) dr + E(t2, u(t2)) = E(t1, u(t1)) + Z t2

t1

∂tE(t, u(r)) dr

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Step 1: energy identity

Chain rule for ∂E + convex analysis: every solution of

∂Ψε(u′(t))

z }| { ε∂Ψ2(u′(t)) + ∂Ψ1(u′(t)) + ∂E(t, u(t)) ∋ 0 in B′

2, t ∈ (0, T)

fulfils energy identity ∀ 0 ≤ t1 ≤ t2 ≤ T Z t2

t1

Ψε (˙ u(r)) dr + Z t2

t1

Ψε∗ (−∂E(r, u(r))) dr + E(t2, u(t2)) = E(t1, u(t1)) + Z t2

t1

∂tE(t, u(r)) dr where the conjugate Ψε∗ is: Ψε∗ (−∂E) = 1 2ε min

|z|1,∗≤1 − ∂E− z2 2,∗ = 1

2εd2 (−∂E, K∗)2 and K ∗ unitary ball in B∗

1 .

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Competition between viscous effects & rate-independent behaviour

Z t2

t1

|u′(r)|1 dr + Z t2

t1

ε 2 u′(r)2

2 + 1

2εd2 (−∂E(r, u(r)), K ∗)2 dr + E(t2, u(t2)) = E(t1, u(t1)) + Z t2

t1

∂tE(t, u(r)) dr

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Competition between viscous effects & rate-independent behaviour

Z t2

t1

|u′(r)|1 dr + Z t2

t1

ε 2 u′(r)2

2 + 1

2εd2 (−∂E(r, u(r)), K ∗)2 dr + E(t2, u(t2)) = E(t1, u(t1)) + Z t2

t1

∂tE(t, u(r)) dr ♣ Note that d2 (−∂E(r, u(r)), K ∗) = 0 ⇔ | − ∂E(r, u(r))|1,∗ ≤ 1 LOCAL version of the stability condition: | − ∂E(r, u(r))|1,∗ ≤ 1 vs. E(t, u(t)) − E(t, z) D(u(t), z) ≤ 1 ∀ z

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Competition between viscous effects & rate-independent behaviour

Z t2

t1

|u′(r)|1 dr + Z t2

t1

ε 2 u′(r)2

2 + 1

2εd2 (−∂E(r, u(r)), K ∗)2 dr + E(t2, u(t2)) = E(t1, u(t1)) + Z t2

t1

∂tE(t, u(r)) dr ♣ Note that d2 (−∂E(r, u(r)), K ∗) = 0 ⇔ | − ∂E(r, u(r))|1,∗ ≤ 1 LOCAL version of the stability condition: | − ∂E(r, u(r))|1,∗ ≤ 1 vs. E(t, u(t)) − E(t, z) D(u(t), z) ≤ 1 ∀ z ♣ Energy identity highlights the competition between viscosity & rate-independence

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Step 2: rescaling

The technique by Efendiev-Mielke

◮ Jumps in the vanishing viscosity limit correspond to viscous transitions between

stable states

◮ To capture the viscous transition path: NOT SHRINK jumps at a point, look at

curves with their arclength parametrization

◮ Asymptotic analysis of (reparametrized) trajectories in an extended phase space Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Step 2: rescaling

The technique by Efendiev-Mielke

◮ Jumps in the vanishing viscosity limit correspond to viscous transitions between

stable states

◮ To capture the viscous transition path: NOT SHRINK jumps at a point, look at

curves with their arclength parametrization

◮ Asymptotic analysis of (reparametrized) trajectories in an extended phase space

We reparametrize Z t2

t1

|u′(r)|1 dr + Z t2

t1

ε 2 u′(r)2

2 + 1

2εd2 (−∂E(r, u(r)), K ∗)2 dr + E(t2, u(t2)) = E(t1, u(t1)) + Z t2

t1

∂tE(t, u(r)) dr by the rescaling function: sε(t) = t + Z t ` |u′(r)|1 + u′(r)2 · d2 (−∂E(r, u(r)), K ∗) ´ dr “energy arclength”

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Step 2: rescaling

( sε(t) := t + R t

0 (|u′(r)|1 + u′(r)2 · d2 (−∂E(r, u(r)), K ∗)) dr

ˆ tε = s−1

ε

, ˆ uε = u ◦ ˆ tε Hence we perform the asymptotic analysis for the “extended” trajectory {(ˆ tε, ˆ uε)}

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Step 2: rescaling

( sε(t) := t + R t

0 (|u′(r)|1 + u′(r)2 · d2 (−∂E(r, u(r)), K ∗)) dr

ˆ tε = s−1

ε

, ˆ uε = u ◦ ˆ tε Hence we perform the asymptotic analysis for the “extended” trajectory {(ˆ tε, ˆ uε)} Rescaled energy identity Z s2

s1

|ˆ u′

ε|1 +

Z s2

s1

ε 2ˆ t′

ε

ˆ u′

ε2 2 +

ˆ t′

ε

2εd2 ` −∂E(ˆ tε, ˆ uε), K ∗´2 + E(ˆ tε(s2), ˆ uε(s2)) = E(ˆ tε(s1), ˆ uε(s1)) + Z s2

s1

∂tE(ˆ tε, ˆ uε)ˆ t′

ε

+ “normalization” condition ˆ t′

ε + |ˆ

u′

ε|1 + ˆ

u′

ε2 · d2

` −∂E(ˆ tε, ˆ uε), K ∗´ ≡ 1

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Step 2: rescaling

( sε(t) := t + R t

0 (|u′(r)|1 + u′(r)2 · d2 (−∂E(r, u(r)), K ∗)) dr

ˆ tε = s−1

ε

, ˆ uε = u ◦ ˆ tε Hence we perform the asymptotic analysis for the “extended” trajectory {(ˆ tε, ˆ uε)} Rescaled energy identity Z s2

s1

|ˆ u′

ε|1 +

Z s2

s1

ε 2ˆ t′

ε

ˆ u′

ε2 2 +

ˆ t′

ε

2εd2 ` −∂E(ˆ tε, ˆ uε), K ∗´2 + E(ˆ tε(s2), ˆ uε(s2)) = E(ˆ tε(s1), ˆ uε(s1)) + Z s2

s1

∂tE(ˆ tε, ˆ uε)ˆ t′

ε

+ “normalization” condition ˆ t′

ε + |ˆ

u′

ε|1 + ˆ

u′

ε2 · d2

` −∂E(ˆ tε, ˆ uε), K ∗´ ≡ 1 ⇒ A priori estimates, compactness for {(ˆ tε, ˆ uε)}

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The asymptotic analysis as ε ↓ 0

Theorem [Mielke, R., Savar´ e’09]

◮ B2 reflexive, B2 ⊂ B1 ◮ Energy: E : (0, T) × B2 → (−∞, +∞], with compact sublevels in B2, ◮ E complies with chain rule Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The asymptotic analysis as ε ↓ 0

Theorem [Mielke, R., Savar´ e’09] Up to a subsequence, as ε ց 0 the trajectory {(ˆ tε, ˆ uε)} Z s2

s1

|ˆ u′

ε|1 +

Z s2

s1

ε 2ˆ t′

ε

ˆ u′

ε2 2 +

ˆ t′

ε

2εd2 ` −∂E(ˆ tε, ˆ uε), K ∗´2 + E(ˆ tε(s2), ˆ uε(s2)) = E(ˆ tε(s1), ˆ uε(s1)) + Z s2

s1

∂tE(ˆ tε, ˆ uε)ˆ t′

ε

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The asymptotic analysis as ε ↓ 0

Theorem [Mielke, R., Savar´ e’09] Up to a subsequence, as ε ց 0 the trajectory {(ˆ tε, ˆ uε)} Z s2

s1

|ˆ u′

ε|1 +

Z s2

s1

ε 2ˆ t′

ε

ˆ u′

ε2 2 +

ˆ t′

ε

2εd2 ` −∂E(ˆ tε, ˆ uε), K ∗´2 + E(ˆ tε(s2), ˆ uε(s2)) = E(ˆ tε(s1), ˆ uε(s1)) + Z s2

s1

∂tE(ˆ tε, ˆ uε)ˆ t′

ε

converges to (ˆ t, ˆ u) ∈ C0

Lip([0, b

T]; [0, T] × B1) Z s2

s1

|ˆ u′|1 + Z s2

s1

M0 `ˆ t′, ˆ u′2, −∂E(ˆ t, ˆ u) ´ + E(ˆ t(s2), ˆ u(s2)) = E(ˆ t(s1), ˆ u(s1)) + Z s2

s1

∂tE(ˆ t, ˆ u)ˆ t′ (|ˆ u′|1 metric derivative of ˆ u!), with M0 `ˆ t′, ˆ u′2, −∂E(ˆ t, ˆ u) ´ = ( ˆ u′2 · d2 ` −∂E(ˆ t, ˆ u), K ∗´ se ˆ t′ = 0 I{0} ` d2 ` −∂E(ˆ t, ˆ u), K ∗´´ se ˆ t′ > 0

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The asymptotic analysis as ε ↓ 0

Theorem [Mielke, R., Savar´ e’09] Up to a subsequence, as ε ց 0 the trajectory {(ˆ tε, ˆ uε)} Z s2

s1

|ˆ u′

ε|1 +

Z s2

s1

ε 2ˆ t′

ε

ˆ u′

ε2 2 +

ˆ t′

ε

2εd2 ` −∂E(ˆ tε, ˆ uε), K ∗´2 + E(ˆ tε(s2), ˆ uε(s2)) = E(ˆ tε(s1), ˆ uε(s1)) + Z s2

s1

∂tE(ˆ tε, ˆ uε)ˆ t′

ε

converges to (ˆ t, ˆ u) ∈ C0

Lip([0, b

T]; [0, T] × B1) Z s2

s1

|ˆ u′|1 + Z s2

s1

M0 `ˆ t′, ˆ u′2, −∂E(ˆ t, ˆ u) ´ + E(ˆ t(s2), ˆ u(s2)) = E(ˆ t(s1), ˆ u(s1)) + Z s2

s1

∂tE(ˆ t, ˆ u)ˆ t′ (|ˆ u′|1 metric derivative of ˆ u!), with M0 `ˆ t′, ˆ u′2, −∂E(ˆ t, ˆ u) ´ = ( ˆ u′2 · d2 ` −∂E(ˆ t, ˆ u), K ∗´ se ˆ t′ = 0 I{0} ` d2 ` −∂E(ˆ t, ˆ u), K ∗´´ se ˆ t′ > 0 + “normalization condition” ˆ t′ + |ˆ u′|1 + ˆ u′2 · d2 ` −∂E(ˆ t, ˆ u), K ∗´ ≡ 1

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Two key ideas

Proof based on:

◮ reparametrization of trajectories ◮ energy identity: need for a notion of subdifferential for which the chain rule holds.. Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Remarks on the limit problem

(ˆ t, ˆ u) ∈ C0

Lip([0, b

T]; [0, T] × B1), ˆ t(0) = 0, ˆ t(b T) = T Normalization: ˆ t′ + |ˆ u′|1 + ˆ u′2 · d2 ` −∂E(ˆ t, ˆ u), K ∗´ ≡ 1 Energy id.: d ds E(ˆ t(s), ˆ u(s)) − ∂tE(ˆ (s), ˆ u(s))ˆ t′(s) = −−∂E(ˆ t(s), ˆ u(s)), ˆ u′(s) = −|ˆ u′(s)|1 − ˆ u′(s)2 · d2 ` −∂E(ˆ t(s), ˆ u(s)), K ∗´ for a.a. s ∈ (0, b T) Constraint: M0 `ˆ t′, ˆ u′2, −∂E(ˆ t, ˆ u) ´ ≡ ˆ u′2 · d2 ` −∂E(ˆ t, ˆ u), K ∗´

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Remarks on the limit problem

(ˆ t, ˆ u) ∈ C0

Lip([0, b

T]; [0, T] × B1), ˆ t(0) = 0, ˆ t(b T) = T Normalization: ˆ t′ + |ˆ u′|1 + ˆ u′2 · d2 ` −∂E(ˆ t, ˆ u), K ∗´ ≡ 1 Energy id.: d ds E(ˆ t(s), ˆ u(s)) − ∂tE(ˆ (s), ˆ u(s))ˆ t′(s) = −−∂E(ˆ t(s), ˆ u(s)), ˆ u′(s) = −|ˆ u′(s)|1 − ˆ u′(s)2 · d2 ` −∂E(ˆ t(s), ˆ u(s)), K ∗´ for a.a. s ∈ (0, b T) Three regimes: 8 > > > > > > > < > > > > > > > : ˆ t′(s) = 1 ( ⇔ ˆ u′(s) = 0 ) ⇒ | − ∂E(r, u(r))|1,∗ ≤ 1 ˆ t′(s) ∈ (0, 1) ( ⇔ |ˆ u′(s)|1 ∈ (0, 1) ) ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ = 1 ˆ t′(s) = 0 ( ⇔ |ˆ u′(s)|1 + ˆ u′(s)2 · d2 ` −∂E(ˆ t(s), ˆ u(s)), K ∗´ = 1 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ ≥ 1

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Parametrized rate-independent evolutions

Definition

We call parametrized rate-independent evolution a pair (ˆ t, ˆ u) ∈ AC([0, b T]; [0, T] × B1), ˆ t(0) = 0, ˆ t(b T) = T, satisfying Nondegeneracy: ˆ t′(s) + |ˆ u′(s)|1 > 0 for a.a. s ∈ (0, b T), Energy id.: d ds E(ˆ t(s), ˆ u(s)) − ∂tE(ˆ (s), ˆ u(s))ˆ t′(s) = −−∂E(ˆ t(s), ˆ u(s)), ˆ u′(s) = −|ˆ u′(s)|1 − ˆ u′(s)2 · d2 ` −∂E(ˆ t(s), ˆ u(s)), K ∗´ for a.a. s ∈ (0, b T) Three regimes: 8 > > > < > > > : ˆ t′(s) > 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ ≤ 1 ˆ t′(s) |ˆ u′(s)|1 > 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ = 1 ˆ t′(s) = 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ ≥ 1

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Properties of parametrized rate-independent evolutions

Nondegeneracy: ˆ t′(s) + |ˆ u′(s)|1 > 0 for a.a. s ∈ (0, b T), Energy id.: d ds E(ˆ t(s), ˆ u(s)) − ∂tE(ˆ (s), ˆ u(s))ˆ t′(s) = −−∂E(ˆ t(s), ˆ u(s)), ˆ u′(s) = −|ˆ u′(s)|1 − ˆ u′(s)2 · d2 ` −∂E(ˆ t(s), ˆ u(s)), K ∗´ for a.a. s ∈ (0, b T) Three regimes: 8 > > > < > > > : ˆ t′(s) > 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ ≤ 1 ˆ t′(s) |ˆ u′(s)|1 > 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ = 1 ˆ t′(s) = 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ ≥ 1

◮ Intrinsically rate-independent notion: invariant for time-rescalings ◮ Arises in the vanishing viscosity limit ◮ Under conditions on B1, notion equivalent to the doubly nonlinear PDE

formulation

◮ Stability w.r.t. the problem data Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Properties of parametrized rate-independent evolutions

Nondegeneracy: ˆ t′(s) + |ˆ u′(s)|1 > 0 for a.a. s ∈ (0, b T), Energy id.: d ds E(ˆ t(s), ˆ u(s)) − ∂tE(ˆ (s), ˆ u(s))ˆ t′(s) = −−∂E(ˆ t(s), ˆ u(s)), ˆ u′(s) = −|ˆ u′(s)|1 − ˆ u′(s)2 · d2 ` −∂E(ˆ t(s), ˆ u(s)), K ∗´ for a.a. s ∈ (0, b T) Three regimes: 8 > > > < > > > : ˆ t′(s) > 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ ≤ 1 ˆ t′(s) |ˆ u′(s)|1 > 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ = 1 ˆ t′(s) = 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ ≥ 1

◮ Intrinsically rate-independent notion: invariant for time-rescalings ◮ Arises in the vanishing viscosity limit ◮ Under conditions on B1, notion equivalent to the doubly nonlinear PDE

formulation

◮ Stability w.r.t. the problem data ◮ Three regimes reflect the different types of evolution of the system Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The three regimes

8 > < > : ˆ t′(s) > 0, |ˆ u′(s)|1 = 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ ≤ 1 (sticking) ˆ t′(s) |ˆ u′(s)|1 > 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ = 1 (sliding) ˆ t′(s) = 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ ≥ 1 (viscous slip)

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The three regimes

8 > < > : ˆ t′(s) > 0, |ˆ u′(s)|1 = 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ ≤ 1 (stationarity) ˆ t′(s) |ˆ u′(s)|1 > 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ = 1 (rate-independent) ˆ t′(s) = 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ ≥ 1 (jump)

Stationarity

◮ local stability condition

| − ∂E(ˆ t(s0), ˆ u(s0))|1,∗ ≤ 1 vs. E(s0, u(s0)) − E(s0, z) D(u(s0), z) ≤ 1 ∀ z

◮ in a neighbourhood I(s0) there hold ˆ

u(s) ≡ ˆ u(s0) and the energy identity E(ˆ t(s2), ˆ u(s0)) − E(ˆ t(s1), ˆ u(s0)) = Z s2

s1

∂tE(ˆ t(s), ˆ u(s0))ˆ t′(s) ds ∀ s1 ≤ s2 ∈ I(s0) .

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

The three regimes

8 > < > : ˆ t′(s) > 0, |ˆ u′(s)|1 = 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ ≤ 1 (stationarity) ˆ t′(s) |ˆ u′(s)|1 > 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ = 1 (rate-independent) ˆ t′(s) = 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ ≥ 1 (jump)

Rate-independent evolution

◮ local stability condition

| − ∂E(ˆ t(s0), ˆ u(s0))|1,∗ = 1 ∼ −∂E(ˆ t(s0), ˆ u(s0)) ∈

Sign(ˆ u′(s0))

z }| { ∂Ψ1(ˆ u′(s0))

◮ in a neighbourhood I(s0) energy identity ∀ s1 ≤ s2 ∈ I(s0)

E(ˆ t(s2), ˆ u(s2)) − E(ˆ t(s1), ˆ u(s1)) = Z s2

s1

` ∂tE(ˆ t(s), ˆ u(s))ˆ t′(s) − |ˆ u′(s)|1 ´ ds .

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The three regimes

8 > < > : ˆ t′(s) > 0, |ˆ u′(s)|1 = 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ ≤ 1 (stationarity) ˆ t′(s) |ˆ u′(s)|1 > 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ = 1 (rate-independent) ˆ t′(s) = 0 ⇒ | − ∂E(ˆ t(s), ˆ u(s))|1,∗ ≥ 1 (jump)

Jump regime

◮ in a neighbourhood I(s0) there hold ˆ

t(s) ≡ ˆ t(s0) and energy identity ∀ s1 ≤ s2 ∈ I(s0) E(ˆ t(s0), ˆ u(s2))−E(ˆ t(s0), ˆ u(s1)) = Z s2

s1

` −|ˆ u′(s)|1 − ˆ u′(s)2 · d2 ` −∂E(ˆ t(s0), ˆ u(s)), K ∗´´ ds .

◮ With a rescaling which depends on the

viscous quantities ˆ u′2 & d2 ` −∂E(ˆ t, ˆ u), K ∗´ we pass from ˆ u(s) to ˜ u(σ) solution of the viscous doubly nonlinear equation ∂Ψ1(˜ u′(σ)) + ∂Ψ2(˜ u′(σ)) + ∂E(ˆ t(s0), u(σ)) ∋ 0

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Differential characterization

In the case B1 has the Radon Nikod´ ym property (hence we have pointwise derivatives!! But L1 is forbidden) &

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Differential characterization

In the case B1 has the Radon Nikod´ ym property (hence we have pointwise derivatives!! But L1 is forbidden) & E(t, u) = E(u) − ℓ(t), u

Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Differential characterization

In the case B1 has the Radon Nikod´ ym property (hence we have pointwise derivatives!! But L1 is forbidden) & E(t, u) = E(u) − ℓ(t), u then (ˆ t, ˆ u) ∈ AC([0, b T]; [0, T] × B1) is a parametrized rate-independent evolution if and only if ∃ λ : (0, b T) → R+ : for a.a. s ∈ (0, b T) 8 > < > : ∂Ψ1(ˆ u′(s)) + λ(s)∂Ψ2(ˆ u′(s)) + ∂E(ˆ u(s)) ∋ ℓ(ˆ t(s)) λ(s)ˆ t′(s) = 0

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Differential characterization

In the case B1 has the Radon Nikod´ ym property (hence we have pointwise derivatives!! But L1 is forbidden) & E(t, u) = E(u) − ℓ(t), u then (ˆ t, ˆ u) ∈ AC([0, b T]; [0, T] × B1) is a parametrized rate-independent evolution if and only if ∃ λ : (0, b T) → R+ : for a.a. s ∈ (0, b T) 8 > < > : ∂Ψ1(ˆ u′(s)) + λ(s)∂Ψ2(ˆ u′(s)) + ∂E(ˆ u(s)) ∋ ℓ(ˆ t(s)) λ(s)ˆ t′(s) = 0 The “Lagrange multiplier” λ (and thus viscous dissipation) is activated by ˆ t′(s) = 0, i.e. at jumps

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

BV rate-independent evolutions

From virtual to real jumps

With a suitable rescaling, we pass from (ˆ t, ˆ u) parametrized rate-independent evolution ⇓ ⇑ to u BV rate-independent evolution in jump points it follows the trajectory of a viscous doubly nonlinear equation

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

BV rate-independent evolutions

From virtual to real jumps

With a suitable rescaling, we pass from (ˆ t, ˆ u) parametrized rate-independent evolution ⇓ ⇑ to u BV rate-independent evolution in jump points it follows the trajectory of a viscous doubly nonlinear equation

Approximation by time discretization

Existence of BV rate-independent evolutions: passing to the limit in the discretization scheme: ( Un

τ ∈ ArgminU∈B2

n |U − Un−1

τ

|1 + ε(τ)

τ U − Un−1 τ

2

2 + E(tn, U)

  • .

with ε(τ) → 0 & ε(τ)

τ

↑ ∞ as τ ↓ 0

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Metric analysis popping out

Z s2

s1

|ˆ u′|1 + Z s2

s1

M0 `ˆ t′, ˆ u′2, −∂E(ˆ t, ˆ u) ´ + E(ˆ t(s2), ˆ u(s2)) = E(ˆ t(s1), ˆ u(s1)) + Z s2

s1

∂tE(ˆ t, ˆ u)ˆ t′ BUT: B1 ∼ L1 does not have the Radon-Nikod´ ym property

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Metric analysis popping out

Z s2

s1

|ˆ u′|1 + Z s2

s1

M0 `ˆ t′, ˆ u′2, −∂E(ˆ t, ˆ u) ´ + E(ˆ t(s2), ˆ u(s2)) = E(ˆ t(s1), ˆ u(s1)) + Z s2

s1

∂tE(ˆ t, ˆ u)ˆ t′ BUT: B1 ∼ L1 does not have the Radon-Nikod´ ym property

◮ Need to replace pointwise derivative |ˆ

u′|1 by metric derivative

◮ Metric analysis, theory of gradient flows in metric spaces: ◮ De Giorgi, Marino, Saccon, Tosques, Degiovanni, Ambrosio ’80 ∼ ’90 theory of

Curves of Maximal Slope and Minimizing Movements

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Metric analysis popping out

Z s2

s1

|ˆ u′|1 + Z s2

s1

M0 `ˆ t′, ˆ u′2, −∂E(ˆ t, ˆ u) ´ + E(ˆ t(s2), ˆ u(s2)) = E(ˆ t(s1), ˆ u(s1)) + Z s2

s1

∂tE(ˆ t, ˆ u)ˆ t′ BUT: B1 ∼ L1 does not have the Radon-Nikod´ ym property

◮ Need to replace pointwise derivative |ˆ

u′|1 by metric derivative

◮ Metric analysis, theory of gradient flows in metric spaces: ◮ De Giorgi, Marino, Saccon, Tosques, Degiovanni, Ambrosio ’80 ∼ ’90 theory of

Curves of Maximal Slope and Minimizing Movements

◮ [ Gradient flows in metric spaces, Ambrosio-Gigli-Savar´

e 2005] systematic theory of existence, approximation & uniqueness of solutions of metric gradient flows, with applications to gradient flows in Wasserstein spaces.

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Metric analysis popping out

Z s2

s1

|ˆ u′|1 + Z s2

s1

M0 `ˆ t′, ˆ u′2, −∂E(ˆ t, ˆ u) ´ + E(ˆ t(s2), ˆ u(s2)) = E(ˆ t(s1), ˆ u(s1)) + Z s2

s1

∂tE(ˆ t, ˆ u)ˆ t′ BUT: B1 ∼ L1 does not have the Radon-Nikod´ ym property

◮ Need to replace pointwise derivative |ˆ

u′|1 by metric derivative

◮ Metric analysis, theory of gradient flows in metric spaces: ◮ De Giorgi, Marino, Saccon, Tosques, Degiovanni, Ambrosio ’80 ∼ ’90 theory of

Curves of Maximal Slope and Minimizing Movements

◮ [ Gradient flows in metric spaces, Ambrosio-Gigli-Savar´

e 2005] systematic theory of existence, approximation & uniqueness of solutions of metric gradient flows, with applications to gradient flows in Wasserstein spaces.

◮ subdifferentials replaced by slopes, doubly nonlinear equations formulated in a

metric setting [R., Mielke, Savar´ e’08], [Mielke, R., Savar´ e’08]

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Introduction “Viscous” doubly nonlinear equations Vanishing viscosity analysis Parametrized rate-independent evolutions Conclusions

Future developments

◮ applications of this general method to “concrete” problems in continuum

mechanics..

◮ from two norms to two metrics.. Riccarda Rossi Interplay of viscosity and dry friction in rate-independent evolutions with nonconvex energies