On the structure of solutions of multidimensional conservation laws with discontinuous flux
Graziano Crasta
Universit`a di Roma “La Sapienza”
11th Meeting on Nonlinear Hyperbolic PDEs and Applications On the occasion of the 60th birthday of Alberto Bressan
SISSA, Trieste, June 13–17, 2016
Based on joint works with V. De Cicco, G. De Philippis, F. Ghiraldin
Outline
1 Introduction to conservation laws with discontinuous flux
2 Assumptions on the flux
3 Weak entropy solutions (WES)
4 Existence of (generalized) traces
5 Generalized Kato inequality
Introduction to conservation laws with discontinuous flux
Conservation laws with discontinuous flux
. Scalar multi-dimensional conservation law with discontinuous flux:
(*) ut+ divxF (t, x , u) = 0, (t, x ) ∈ (0, +∞) × RN.
The vector fieldF : (0, +∞) × RN× R → RN ispossibly discontinuous in (t, x ).
. Motivations: vehicular traffic models, flows in porous media, etc.
. Our results: structure of solutions of (*) and applications to uniqueness of solutions to the Cauchy problem
(ut+ divxF (t, x , u) = 0, (t, x ) ∈ (0, +∞) × RN, u(0, x ) = u0(x ), x ∈ RN.
. Beware: in this talk we do not address the existence issue!
Introduction to conservation laws with discontinuous flux
Basic model
. Most studied: one space variable (N = 1), one point of discontinuity at the origin:
F (t, x , u) = F−(u) 1{x<0}+ F+(u) 1{x>0}, with F± regular functions.
. The flux is regular in the two regionsΩ±:= {(t, x ) : t > 0, ±x > 0}.
Discontinuities are located along the interfaceN := (0, +∞) × {0}.
. A typical definition of entropy solution requires that:
(i) the restrictions of u toΩ± are Kruˇzkov entropy solutions;
(ii) along the interfaceN the strong tracesu±of u satisfy some additional condition.
Introduction to conservation laws with discontinuous flux
Consequences of the first requirement:
(i) the restrictions of u toΩ± are Kruˇzkov entropy solutions.
. Existence of strong traces ofu alongN follows from genuine nonlinearity of F± (Panov, Vasseur, ...)
. Ifu andv are two bounded distributional solutions satisfying (i), then Z
|u(T ) − v (T )| dx ≤ Z
|u0− v0| dx + Z
NT
W (u±, v±) d HN where NT := N ∩ ((0, T ) × RN).
. In this Kato–like inequality, the additional term concentrated onN can be characterized in terms of the traces u±, v±:
W (u±, v±) := q+(u+, v+) − q−(u−, v−), where q± are the Kruˇzkov entropy fluxes
q±(u, v ) := sign(u − v ) [F±(u) − F±(v )].
Introduction to conservation laws with discontinuous flux
• Kato–like inequality
• W ≤ 0 on N
=⇒ contractivity of the semigroup and uniqueness
The additional condition in (ii) is used to show that, if u,v are entropy solutions, thenW (u±, v±) ≤ 0 along the interfaceN.
. It can be coded algebraically using the notion of germ (Andreianov, Karlsen, Risebro 2011) or of dissipative Riemann solver (Garavello, Natalini, Piccoli, Terracina 2007), or of transmission map (Andreianov, Canc`es 2015).
Introduction to conservation laws with discontinuous flux
Main objectives
. Notion ofweak entropy solution (WES) (including requirement (i) as a special case) for fluxes with a general set of discontinuities in several space variables.
. Structure resultsfor WES, including:
• existence of traces u± of a WES u on the setN of discontinuities of the fluxF;
• Kato–like contraction inequality: if u andv are WES, then Z
|u(T ) − v (T )| dx ≤ Z
|u0− v0| dx + Z
NT
W (u±, v±) d HN where
• NT := N ∩ ((0, T ) × RN)
• W (u±, v±) := q+(u+, v+) − q−(u−, v−)
• q±(u, v ) := sign(u − v ) hF±(t, x , u) − F±(t, x , v ), ν(t, x )i, andν is the normal vector field toN.
Assumptions on the flux
Assumptions on the flux
Our assumptions on F are mainly modeled on the case F (t, x , u) = bF (h(t, x ), u), with F : R × R → Rb N regular,h in SBV.
. The jump setN ⊂ (0, +∞) × RN ofF (·, ·, u) is independent ofu. . N is a countably HN–rectifiable set.
In the following, we consider the more general equation
divzA(z, u) = 0, z ∈ Rn (n = N + 1, z = (t, x ), A = (u, F )).
Assumptions on the flux
divzA(z, u) = 0, z ∈ Rn.
• A(·, v ) ∈ SBV (Rn, Rn),A(z, ·) ∈ C1(R, Rn).
Notation: DzA(z, v ) = ∇A(z, v ) Ln+ DjA(z, v )
• |∂vA(z, v )| ≤ M for every (z, v ), and∃ ω modulus of continuity s.t.
|∂vA(z, v ) − ∂vA(z, u)| ≤ ω(|v − u|), ∀z, u, v .
• ∃ g ∈ L1(Rn) s.t. |∇A(z, u) − ∇A(z, v )| ≤ g (z) |u − v |, ∀z, u, v .
• The following measure is finite:
σ := _
u∈R
|DzA(·, u)|
(σ is the smallest measure greater thansupu|DzA(·, u)|.)
Assumptions on the flux
The last assumption permits to define a universal (in u) jump set forA:
N :=n
z ∈ Rn: lim inf
r →0
σ(Br(z)) rn−1 > 0o
. σ finite =⇒ N countablyHn−1 rectifiable set.
For Hn−1–a.e. z ∈ N and every v ∈ R the traces A± ofA anda± of a := ∂vA are well defined.
Finally, we assume that
• Ais genuinely nonlinear, i.e.
L1 {v : a±(z, v ) · ξ = 0} = 0 for every ξ ∈ Sn−1 and forHn−1–a.e. z ∈ N.
Weak entropy solutions (WES)
Weak entropy solutions (WES) – 1D model
F (t, x , u) = F−(u) 1{x<0}+ F+(u) 1{x>0}
. A bounded distributional solutionu satisfies (i), i.e. its restrictions to Ω± are Kruˇzkov entropy solutions, iff
(i’) ∃ C ≥ 0s.t. for every k ∈ R,
∂t|u − k| + ∂x sign(u − k)[F (t, x , u) − F (t, x , k)] ≤ µ where µ(t, x ) := C δ0(x ) is a measure concentrated on the interfaceN. . IfA = (u, F ) andz = (t, x ), this condition gives
divz
sign(u − k)[A(z, u) − A(z, k)]
≤ µ.
. We shall call weak entropy solutions the bounded distributional solutions satisfying (i’).
Weak entropy solutions (WES)
Weak entropy solutions (WES) – General case
u ∈ L∞(Rn)is a weak entropy solution (WES) of
(*) divzA(z, u) = 0, z ∈ Rn
if u is a distributional solution of (*) and for everyk ∈ R it holds (EC) divz
sign(u − k)[A(z, u) − A(z, k)]
+ sign(u − k) divazA(z, k) ≤ µ, where µis a non-negative Radon measure independent ofk and such that µ(Rn\ N ) = 0.
Remark: divazA(z, k) = tr∇A(z, k) is the absolutely continuous part of divzA(·, k).
Weak entropy solutions (WES)
Comparison with other entropy conditions
. Kruˇzkov: Aregular in both variables divz
sign(u − k)[A(z, u) − A(z, k)]
+ sign(u − k) divzA(z, k) ≤ 0
=⇒ existence and uniqueness for evolutionary equation . Panov: divzA(·, k)locally finite Borel measure divz
sign(u−k)[A(z, u)−A(z, k)]
+sign(u−k) divazA(z, k) ≤ | divszA(z, k)|
=⇒ existence for evolutionary equation
. Vanishing viscosity(Diehl, Andreianov–Mitrovic, ...): ∃ ˆu everywhere defined representative of u s.t.
divz
sign(u − k)[A(z, u) − A(z, k)]
+ sign(u − k) divazA(z, k)
≤ sign( ˆu − k) divszA(z, k)
Existence of (generalized) traces
Generalized traces
Definition (Traces)
u ∈ L∞(Rn),J ⊂ Rn Hn−1–rectifiable set oriented by ν.
Set of traces of u atz0 ∈ J: Γu,J(z0) :=
n
(c−, c+) : ∃rk ↓ 0 : uz0,rk → c−1H−+ c+1H+ in L1loc o
, where uz0,r(z) := u(z0+ rz),H±:= {z ∈ Rn: ±hz − z0, ν(z0)i ≥ 0}.
Remark: if
uz0,r → c−1H−+ c+1H+ in L1loc, for r ↓ 0,
then Γu,J(z0) = {(c−, c+)}where(c−, c+) are the usual strong traces.
Existence of (generalized) traces
Existence of (generalized) traces
Theorem (Existence of traces)
Ifu is a WES, then for Hn−1 almost everyz0 ∈ N Γu,N(z0) 6= ∅.
. If(c−, c+) ∈ Γu,N(z0) satisfiesc−6= c+ then the traces are unique:
Γu,N(z0) = {(c−, c+)}.
. OtherwiseΓu,N(z0) = {(v , v ) : v ∈ [a, b]} for somea ≤ b.
. The Rankine–Hugoniot condition holds:
A−(z0, c−) · ν(z0) = A+(z0, c+) · ν(z0) ∀ (c−, c+) ∈ Γu,N(z0).
Existence of (generalized) traces
Sketch of the proof
Kinetic formulation
. For everyk ∈ R, the distribution ηk := divz
sign(u − k)[A(z, u) − A(z, k)]
+ sign(u − k) divazA(z, k) is a Radon measure in Rn (recall ηk ≤ µ), and
Cc∞(Rn× R) 3 Φ 7→ hη, Φi :=
Z Z
Rn×R
Φ(z, k) d ηk(z) dk is a Radon measure in Rn+1.
. The function(k, z) 7→ χ(k, u(z)) := sign(u(z) − k) is a distributional solution of the kinetic equation
divz[χ(k, u)∂vA(z, k)] − ∂k[χ(k, u) divazA(z, k)] = −∂kη in D0(Rn+1).
Existence of (generalized) traces
Blow-up in kinetic equation
ur(z) := u(z0+ rz), Ar(z, v ) := A(z0+ rz, v ), ηk,r(V ) := ηk(z0+ rV ) rn−1 . Strong pre-compactness of blow-ups: divzAr(z, ur) = 0 =⇒ (ur)r is pre-compact in L1(B1) (Panov).
. u∞ cluster point of (ur): from kinetic equation we get
divzχ(k, u∞)∂vAz0(z, k) = −∂k h(z0) λz0(k) Hn−1 ∂H+) where∂vAz0(z, k) = a+(k) 1H+(z) + a−(k) 1H−(z),a±(k) := ∂vA±(z0, k).
. InH+ this is the transport equation a+(k) · ∇zχ(k, u∞) = 0.
By GNL =⇒ u∞= const =: u+ in H+. Similarly, u∞= const =: u− inH−.
Generalized Kato inequality
Generalized Kato inequality
Theorem (Generalized Kato Inequality)
Let u and v be WES. Then there exists a Borel function ρ : N → R such that the following Kato inequality holds true:
divz
sign(u − v )[A(z, u) − A(z, v )]
≤ ρ Hn−1 N .
. Representation ofρ: for Hn−1 a.e. z ∈ N1 := {z ∈ N : ρ(z) 6= 0},u and v admit unique traces at z and
ρ = W (u±, v±) := q+(u+, v+) − q−(u−, v−).
Generalized Kato inequality
Sketch of the proof
1. Doubling of variables Weak entropy condition
(EC) divz
sign(u − k)[A(z, u) − A(z, k)]
+ sign(u − k) divazA(z, k) ≤ µ, for u(z) with k = v (z0)and forv (z0) withk = u(z).
Use test function Φ(z, z0) = δε(z − z0) ϕ(z + z0),ϕ ∈ Cc1(Rn), δε(ζ) = ε1nψ(ζε) standard family of mollifiers, and sum up:
[All that you expect at l.h.s. from doubling of variables]
≥ −2 Z Z
Φ(z, z0) dz0d µ(z) i.e.
I1ε− I2ε+ I3ε≥ −2 Z Z
Φ(z, z0) dz0d µ(z).
Generalized Kato inequality
(z0 = z − εw) I1ε=
Z Z
ψ(w )∇ϕ(2z − εw ) sign (u(z) − v (z − εw )×
×n
A(z, u(z)) + A(z − εw , u(z))
− A(z, v (z − εw )) − A(z − εw , v (z − εw ))o dwdz, I2ε=
Z Z
ϕ(2z − εw ) sign u(z) − v (z − εw )×
×n
∇ψ(w )A(z − εw , u(z)) − A(z, u(z)) ε
− ψ(w ) divazA(z − εw , u(z))o dwdz, I3ε=
Z Z
ϕ(2z + εw ) sign u(z + εw ) − v (z)
×n
∇ψ(w )A(z, v (z)) − A(z + εw , v (z)) ε
Generalized Kato inequality
2. Limit as ε → 0
I1ε= Z Z
ψ(w )∇ϕ(2z − εw ) sign (u(z) − v (z − εw )×
×n
A(z, u(z)) + A(z − εw , u(z))
− A(z, v (z − εw )) − A(z − εw , v (z − εw ))o dwdz.
Not difficult to show that
I1ε→ 2 Z
∇ϕ(2z) sign (u(z) − v (z)
A(z, u(z)) − A(z, v (z)) dz.
Generalized Kato inequality
. To pass to the limit inI2ε andI3ε we need a modification ofAmbrosio’s lemma on differential quotients:
For every w ∈ Rn there exists a null setD ⊂ Rn s.t.
A(z + εw , v ) − A(z, v )
ε = A1ε(z, v ) + A2ε(z, v ) where A1ε andA2ε satisfy the following properties:
(i) lim
ε↓0A1ε(z, v ) = ∇zA(z, v ) · w , ∀v ∈ R and z ∈ Rn\ D;
(ii) hε(z) := |w | sup
v ∈R
A1ε(z, v )
is equi-integrable;
(iii) For every compact set K ⊂ Rn we have Z
K
sup
v ∈R
A2ε(z, v )
dz ≤ |w | σs(K + Bε|w |).
Generalized Kato inequality
I2ε= Z Z
ϕ(2z − εw ) sign u(z) − v (z − εw )×
×n
∇ψ(w )A(z − εw , u(z)) − A(z, u(z)) ε
− ψ(w ) divazA(z − εw , u(z)) o
dwdz Ambrosio’s lemma:
A(z − εw , u(z)) − A(z, u(z))
ε = A1ε,w(z) + A2ε,w(z) where
A1ε,w(z) L
1
−→ −∇A(z, u(z)) · wloc
and Z
|A2ε,w(z)|ϕ(z) dz ≤ |w | kϕk∞|σs|(spt ϕ + Bε|w |) .
Generalized Kato inequality
Hence
I2ε= Z Z
ϕ(2z − εw ) sign u(z) − v (z − εw )
× − ∇ψ(w )∇A(z, u(z)) · w − ψ(w ) divazA(z, u(z)) dw dz + Rε, where
lim sup
ε→0
|Rε| ≤ C (ψ)kϕk∞|σs|(spt ϕ).
Passing to the limit:
Z Z . . . →
Z Z
ϕ(2z) sign u(z) − v (z)×
×∇ψ(w )∇A(z, u(z)) · w + ψ(w ) divazA(z, u(z)) dwdz
= [integrate by parts in w ] = 0.
Generalized Kato inequality
3. Conclusion
. Same estimate forI3ε. . Putting all together:
divz
sign (u(z) − v (z)
A(z, u(z)) − A(z, v (z))
≤ 2µ + C |σs| =: β
. Sinceβ(Rn\ N ) = 0, the vector field B(z) := sign (u(z) − v (z)
A(z, u(z)) − A(z, v (z))
has divergence–measure, div B Hn−1 and its generalized traces on N are
B±(z) = sign u±(z) − v±(z)
A±(z, u±(z)) − A±(z, v±(z))
Generalized Kato inequality
Open problems
. Well posedness: existence and uniqueness of solutions in the general setting.
(Partial well posedness results are known in the case of the vanishing viscosity germ and flux with a regular discontinuity set.)
. Relax assumptions on the flux A:
divzA(·, k) measure ∀k σ := _
k∈R
| divzA(·, k)| finite measure, N rectifiable.
Generalized Kato inequality
References:
. L. Ambrosio, G. Crasta, V. De Cicco, and G. De Philippis, A
nonautonomous chain rule in W1,p andBV, Manuscripta Math. 140 (2013), pp. 461–480.
. B. Andreianov, K.H. Karlsen, and N.H. Risebro, A theory of
L1-dissipative solvers for scalar conservation laws with discontinuous flux, Arch. Rational Mech. Anal. 201 (2011), pp. 27–86.
. G. Crasta, V. De Cicco, G. De Philippis and F. Ghiraldin, Structure of solutions of multidimensional conservation laws with discontinuous flux and applications to uniqueness, Arch. Rational Mech. Anal. 221 (2016), pp. 961-985.