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The Hamilton--Jacobi correspondence in one dimension

Statement

Assume Countable Choice and Dependent Choice (The Axiom of Countable Choice (ACω), The axiom of dependent choice: a relation in which every element is related to something admits an N-indexed chain) for the heat-kernel, L1 completeness and vanishing-viscosity extraction interfaces used below. Let f∈C2(R) be strictly convex and superlinear, with f(p)/∣p∣→∞ as ∣p∣→∞.

(i) Let U0∈C0,1(R)∩L∞(R) and let u0=U0′ be its a.e. derivative. The Hopf--Lax function V(t,x)=QtU0(x)=inf⁡y∈R{U0(y)+tL ⁣(x−yt)},t>0,V(0,x)=U0(x), where L=f∗, is the unique viscosity solution of Vt+f(Vx)=0 with initial datum U0 among functions bounded and uniformly continuous on [0,S]×R for every finite S>0 (The Hamilton--Jacobi Cauchy problem and its classical solutions, Discontinuous viscosity solutions through the two envelopes). Its a.e. spatial derivative v=Vx is the bounded Kruzhkov entropy solution of vt+∂xf(v)=0 with initial datum u0.

(ii) Conversely, let u0∈L1(R)∩L∞(R) have compact support and let u be its bounded Kruzhkov entropy solution, using the strong local L1 initial trace. With U0(x)=∫−∞xu0(y) dy,U(t,x)=∫−∞xu(t,y) dy−tf(0), the function U is the unique viscosity solution of Ut+f(Ux)=0 with datum U0 in the same finite-slab class as in (i), and Ux=u almost everywhere. In the compactly supported datum class of (ii), differentiation and the normalized primitive are inverse correspondences (Kruzhkov entropy solutions, Existence of bounded Kruzhkov entropy solutions).

Facts & Assumptions

Given: Countable and Dependent Choice, a strictly convex superlinear C2 flux f, its conjugate L, and the two datum classes in the statement.

[F2]

The normalized flux g=f−f(0) gives the same conservation law. For smooth compactly supported data its viscous solutions are mild classical solutions, obey the range and L1 bounds, and are locally precompact in space--time L1, with limits continuous into local L1. The existence proof passes their weak and entropy identities to the unique entropy solution (The viscous scalar Cauchy problem with smooth data has a global classical solution, Uniform L-infinity, mass and energy bounds for the viscous approximations, Vanishing-viscosity families are locally precompact in L1, Existence of bounded Kruzhkov entropy solutions, Kruzhkov entropy solutions, Distributional weak solutions of the Cauchy problem).

[F3]

The heat kernels have unit mass, solve the heat equation, have Gaussian derivative estimates, and give the heat evolution; smooth cutoffs have derivatives O(R−1) and O(R−2) (The heat evolution Ht of initial data, Normalisation, parabolic scaling, heat equation and derivative bounds for the heat kernel, Explicit compactly supported smooth cutoffs). Fubini, dominated convergence and FTC justify the kernel calculations (Fubini's theorem for L^1 functions on a sigma-finite product, Dominated convergence, The second fundamental theorem: if G is differentiable on [a,b] with G′=f and f is integrable, then ∫abf=G(b)−G(a)).

[F4]

Entropy solutions contract in global L1 at every time for their continuous representatives, and locally on shrinking balls; they are unique in the bounded class. Compactly supported data stay supported in a common bounded interval on every finite horizon (Global L1 contraction from the local estimate, Local L1 contraction for two entropy solutions, Uniqueness, comparison and order preservation of entropy solutions, Finite propagation for scalar conservation laws).

Proof

technique · direct
1.1F1

Conjugate calculus and localization. Strict convexity makes f′ strictly increasing: convex secant inequalities give monotonicity, and equality at two distinct points would make f affine between them. Superlinearity makes its limits ±∞ (a finite derivative bound at either end would bound f linearly there). Thus p(q):=(f′)−1(q) is continuous, and is the unique maximiser of pq−f(p). The inequalities p(q)h≤L(q+h)−L(q)≤p(q+h)h for h>0, and their reversed versions for h<0, show that L′(q)=p(q). If W is M-Lipschitz and y minimises W(y)+tL((x−y)/t), perturb y in each direction and use the Lipschitz bound to obtain ∣L′((x−y)/t)∣≤M. Hence ∣x−y∣≤Ct, where C=max⁡∣p∣≤M∣f′(p)∣. Translating competitors shows that QtW is M-Lipschitz in x. Moreover L(v)−M∣v∣≥−C0, where C0=max⁡{f(M),f(−M)} by the conjugate definition, and the competitor y=x gives QhW−W≤hL(0). These bounds and the semigroup law give a uniform time Lipschitz bound on finite horizons. Also L(q)≥−f(0) for all q, with equality at q=f′(0), so Qt0=−tf(0). Sup contraction therefore gives ∥QtU0+tf(0)∥∞≤∥U0∥∞, proving boundedness on each finite slab, with no time-uniform bound asserted.

1.2F2F3

Viscous primitives for a smooth compact datum. Let a∈Cc∞, P0(x)=∫−∞xa, and let uε be [F2]'s viscous solution for g=f−f(0). Define Wε(t)=HεtP0−∫0tHε(t−s)f(uε(s)) ds. Differentiating in x gives exactly the mild identity for uε, so Wxε=uε. Heat-potential cancellation as in the viscous construction makes Wε classical at positive times, and its equation is Wtε+f(Wxε)=εWxxε. At x→−∞ its initial heat term tends to zero, while the integral tends to tf(0): g(uε(s))∈L1, and convolution of an L1 function with a bounded Gaussian tends to zero at spatial infinity; boundedness dominates the finite time integral. Thus Wε(t,x)=∫−∞xuε(t,y)dy−tf(0). Testing the smoothed ∣uε∣ balance with an exterior cutoff, then removing a second outer cutoff, gives ∫∣uε(t)∣(1−χR)≤∫∣a∣(1−χR)+CT(R−1+R−2)∥a∥1(0≤t≤T, 0<ε≤1). This is the cutoff calculation of the L1 bound in [F2], with ∣g(u)∣≤C∣u∣ and [F3]'s derivative bounds. It supplies uniform tails.

2.1F2F3step 1.2

A time modulus for the viscous primitives. The Gaussian convolution identity HrHs=Hr+s follows by completing the square in the kernel product and using unit mass and Fubini. Applying it to the definition in step 1.2 gives Wε(t+h)=HεhWε(t)−∫tt+hHε(t+h−s)f(uε(s)) ds. Put M=∥a∥∞ and B=max⁡∣z∣≤M∣f(z)∣. Since Wxε=uε, these primitives are M-Lipschitz in x, including at t=0. Gaussian scaling gives ∫∣z∣Γ(z,r) dz=Cr, with C<∞ by the Gaussian bound. Hence unit mass gives ∥HrWε(t)−Wε(t)∥∞≤CMr, and heat contraction bounds the time integral by Bh. Thus ∥Wε(t+h)−Wε(t)∥∞≤CMh+Bh for 0≤t<t+h≤T, uniformly in 0<ε≤1.

3.1F2F3step 1.2step 2.1

Uniform convergence of primitives. By [F2], choose a subsequence uε→u locally in space--time L1, where u is the entropy solution of datum a, continuous into local L1. A further subsequence converges on almost every time slice locally in L1. The uniform tails of step 1.2 pass to these slices by monotone exhaustion, and to every time by local continuity on bounded annuli followed by exhaustion. They imply u(t)∈L1 with uniformly small tails; local continuity then gives global L1 continuity on [0,T]. Moreover ∫0T∥uε(t)−u(t)∥1dt→0: the tails are uniformly small outside large intervals, the compact space--time convergence handles times away from 0,T, and the bound ∣uε∣,∣u∣≤M controls the remaining small time intervals on the fixed spatial interval. For P(t,x)=∫−∞xu(t,y) dy−tf(0), the primitive formula of step 1.2 gives ∥Wε(t)−P(t)∥∞≤∥uε(t)−u(t)∥1, so the integral in time of the left side tends to zero. The function P is continuous in time in the supremum norm by global L1 continuity. Together with the common modulus of step 2.1, this implies uniform convergence on [0,T]×R: a discrepancy of size d>0 at any time would persist with size at least d/2 on a one-sided interval of length bounded below independently of ε, contradicting that vanishing time integral.

4.1F1F2F3step 1.2step 3.1

The viscosity limit. At a strict local maximum of P−ϕ, with smooth ϕ, step 3.1 gives nearby local maxima of Wε−ϕ. The classical equation in step 1.2 gives ϕt+f(ϕx)≤εϕxx there; passing to the limit proves the subsolution inequality. Local minima give the supersolution inequality. Adding a fourth-power distance term makes a contact strict without changing its first derivatives; approximation in C1 on a compact contact neighbourhood reduces C1 tests to smooth tests. Thus P is a viscosity solution with initial datum P0. It is bounded by ∥a∥1+T∣f(0)∣, spatially M-Lipschitz, and uniformly continuous in time on [0,T] by step 3.1. Uniqueness in [F1] gives P=QtP0.

5.1F1F4F5step 4.1

Compactly supported bounded data. For compactly supported a∈L1∩L∞, choose smooth compactly supported aj→a in L1 with ∥aj∥∞≤∥a∥∞, using [F5]. Their primitives converge uniformly since sup⁡x∣∫−∞x(aj−a)∣≤∥aj−a∥1. By [F4], their entropy solutions converge uniformly in time in L1 to the solution of datum a; their normalized primitives therefore converge uniformly as well. The Hopf--Lax sup contraction in [F1] passes the identity of step 4.1 to P(t)=QtP0. In particular Px=u a.e. by [F5]. This proves (ii), including the normalization −tf(0).

6.1F1F4F5step 1.1step 5.1

A bounded Lipschitz primitive with nonintegrable derivative. Let U0 be as in (i), and set U0R(x)=U0(max⁡{−R,min⁡{x,R}}). It has the same sup and Lipschitz bounds, and derivative u0R=u01(−R,R) a.e. The difference between U0R and the normalized primitive of u0R is its constant value U0(−R); adding this constant commutes with Hopf--Lax. Thus step 5.1 shows that (QtU0R)x is an entropy solution with datum u0R. Step 1.1 places every minimiser for both U0 and U0R within Ct of x. Consequently QtU0R(x)=QtU0(x) whenever ∣x∣+Ct<R, since all those competitors see identical data. Every compact positive-time cylinder is contained in such a region for large R, so the a.e. derivative v=(QtU0)x is bounded by M and obeys the weak equation and every entropy inequality locally, hence globally. For a compact spatial set, fix R large enough that this equality holds throughout 0≤t≤T on that set; the strong local trace of the compact-data solution supplies the trace of v equal to u0. This proves (i), with entropy uniqueness from [F4].

7.1step 5.1step 6.1∎

Conclusion. Step 6.1 proves the derivative correspondence for the entire bounded Lipschitz primitive class, including nonintegrable derivatives, while step 5.1 proves the normalized primitive correspondence for compactly supported integrable data. In that latter class, a.e. differentiation returns u, and integration from −∞ with the time shift −tf(0) returns the prescribed viscosity potential. All arguments hold on an arbitrary finite horizon; [F1] gives viscosity uniqueness on each such slab, while [F4] gives compatibility of the entropy solutions on overlapping horizons. These are the global solutions and inverse correspondences asserted.

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