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The heat smoothing time exponent is forced by scaling

Example

Assume Countable Choice. For n≥1 and 1≤p≤q≤∞, an estimate ∥Htf∥q≤Ct−β∥f∥p valid for every t>0 and every f∈Lp(Rn) with a finite constant C independent of t,f requires β=n2(1p−1q). This asserts the necessary power, not the optimal Young constant.

Facts & Assumptions

Given: Countable Choice, n≥1, 1≤p≤q≤∞, a real β, a finite constant C with ∥Htf∥q≤Ct−β∥f∥p for all t>0 and all f∈Lp(Rn), and λ>0.

[A1]

Countable Choice is the hypothesis carried by the evolution and integration suppliers below (The Axiom of Countable Choice (ACω)).

[F1]

Htf is the Lp (respectively Lq) class of Γt∗f whenever f lies in the corresponding space (The heat evolution Ht of initial data).

[F2]

For every s>0 the kernel satisfies Γ(z,s)=(4πs)−n/2e−∣z∣2/(4s) and the scaling identity Γ(λu,λ2s)=λ−nΓ(u,s); it is positive with unit mass (Normalisation, parabolic scaling, heat equation and derivative bounds for the heat kernel).

[F3]

For 1≤p≤q≤∞ the heat flow satisfies ∥H1g∥q≤Cn,p,q∥g∥p with a finite constant, so ∥H1g∥q<∞ for every g∈Lp (Lp to Lq smoothing estimate for the heat flow).

[F4]

For a measurable g≥0, ∫Rng=0 if and only if g=0 almost everywhere (A nonnegative measurable function has integral 0 exactly when it vanishes almost everywhere).

[F5]

The unit ball B1⊆Rn is measurable with 0<∣B1∣<∞ (Euclidean balls have positive finite Lebesgue measure), so its indicator is measurable (An indicator function is measurable exactly when its set is measurable).

[F6]

For a C1 diffeomorphism T of open sets and g∈L1(V), ∫Vg(y) dy=∫Ug(T(x))∣det⁡DT(x)∣ dx (A C^1 diffeomorphism satisfies the change-of-variables formula for L^1 functions); the mutually inverse maps x↦λx and z↦λ−1z used below qualify with ∣det⁡DT∣=λ±n.

Verification

technique · direct
1.1A1F5given

The base datum: put f:=1B1. By [F5] the function f is measurable, nonnegative and nonzero, and ∥f∥p=∣B1∣1/p for 1≤p<∞ while ∥f∥∞=1, so f∈Lp(Rn) with 0<∥f∥p<∞ for every 1≤p≤∞ (with the usual 1/∞=0 reading of the exponent).

2.1step 1.1F6givenalgebra

Dilated data: for λ>0 put fλ(x):=f(λx). Substituting z=λx in the Lp integral through [F6] gives ∥fλ∥p=λ−n/p∥f∥p for 1≤p<∞, and ∥fλ∥∞=∥f∥∞=1 for p=∞; in both cases ∥fλ∥p=λ−n/p∥f∥p with 1/∞=0.

2.2step 1.1F1F2F6givenalgebra

Parabolic scaling of the flow: substituting z=λy in the defining convolution of [F1] and using the kernel scaling identity of [F2] with λ replaced by λ−1, Γ(x−λ−1z,λ−2)=λnΓ(λx−z,1), gives Hλ−2fλ(x)=∫Γ(x−λ−1z,λ−2)f(z)λ−n dz=∫Γ(λx−z,1)f(z) dz=H1f(λx) for every x.

3.1step 1.1step 2.2F3F4givenalgebra

Norm of the scaled flow: substituting w=λx in the defining integral of ∥Hλ−2fλ∥qq through [F6] and using step 2.2 gives ∥Hλ−2fλ∥q=λ−n/q∥H1f∥q for 1≤q<∞, and step 2.2 directly gives ∥Hλ−2fλ∥∞=∥H1f∥∞; moreover 0<∥H1f∥q<∞, because the finiteness is [F3] with g=f∈Lp, and the strict positivity follows from H1f>0 everywhere (the integrand Γ(x−y,1)f(y) is positive on the positive-measure set B1) together with [F4] applied to H1f≥0 when q<∞ and with the fact that a zero essential supremum would force H1f=0 almost everywhere, contradicting positivity everywhere when q=∞.

4.1step 3.1givenalgebra

Forcing the exponent: apply the hypothesised estimate to fλ at time t=λ−2: by steps 2.1 and 3.1, λ−n/q∥H1f∥q≤Cλ2βλ−n/p∥f∥p, that is, 0<∥H1f∥q∥f∥p≤Cλ2β−n(1/p−1/q) for every λ>0. If 2β−n(1p−1q) were positive, letting λ↓0 would give the contradiction 0<L≤0; if it were negative, letting λ→∞ would give the same contradiction; hence 2β=n(1p−1q) and β=n2(1p−1q).

5.1step 1.1step 2.1step 2.2step 3.1step 4.1F3given∎

Steps 1.1, 2.1, 2.2, 3.1 and 4.1 exhibit a single nonzero nonnegative datum whose parabolic dilates force the time exponent to equal n2(1p−1q) in any estimate of the stated form; this determines the necessary power and says nothing about the optimal constant, whose optimality is not asserted by [F3].

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