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Mean and fluctuation energy exchange

Statement

Let I⊆R be an open interval, let d≥2 and N≥1 be integers, and define the flat torus Td:=(R/2πZ)d, with integration using Lebesgue measure on a periodic cell [0,2π]d. Fix constants aj≥0 with ∑j=1Naj=1 and a common constant ν≥0. For j=1,…,N, let uj:I×Rd→Rd be continuously differentiable in (t,x) with continuous second spatial derivatives, and let pj:I×Rd→R be continuously differentiable. Require these fields to be 2π-periodic in each spatial coordinate, so they descend to Td. Suppose they are unforced and satisfy pointwise on I×Rd

div⁡uj=0,∂tuj+div⁡(uj⊗uj)+∇pj=νΔuj.

Use (u⊗v)rs=urvs, (div⁡A)r=∑s∂xsArs for a matrix field A, and componentwise Laplacian. For A∈Rd×d set tr⁡A:=∑rArr. Define uˉ=∑jajuj, vj=uj−uˉ, R=∑jajvj⊗vj, and

Em(t):=12∫Td∣uˉ(t,x)∣2 dx,Ef(t):=12∫Tdtr⁡R(t,x) dx=12∫Td∑jaj∣vj(t,x)∣2 dx.

For a matrix A and vector field q, set A:∇q:=∑r,s=1dArs∂xsqr and ∣∇q∣2:=∑r,s=1d∣∂xsqr∣2. Then for every t∈I,

dEmdt=−ν∫Td∣∇uˉ∣2 dx+∫TdR:∇uˉ dx,

dEfdt=−ν∫Td∑jaj∣∇vj∣2 dx−∫TdR:∇uˉ dx.

For every t0<t1 in I, the endpoint identities are

Em(t1)−Em(t0)=−ν∫t0t1∫Td∣∇uˉ∣2 dx dt+∫t0t1∫TdR:∇uˉ dx dt,

Ef(t1)−Ef(t0)=−ν∫t0t1∫Td∑jaj∣∇vj∣2 dx dt−∫t0t1∫TdR:∇uˉ dx dt.

The transfer term has opposite signs in the two balances and cancels in their sum. No sign is asserted for ∫TdR:∇uˉ dx.

Facts & Assumptions

[F1]

Exact finite Reynolds averaged equation: For fixed nonnegative normalized weights and a smooth finite family of divergence-free solutions with common viscosity, the weighted mean satisfies the exact averaged equation with covariance term −div⁡R.

[F2]

Exact finite Reynolds averaged equation: The fixed-weight fluctuations have zero weighted mean, ∑jajvj=0.

[F3]

Exact finite Reynolds averaged equation: The pointwise kinetic-energy split is ∑jaj∣uj∣2=∣uˉ∣2+tr⁡R.

[A1]

The periodic lifts are maps on Rd satisfying the Statement’s regularity, fixed-weight, common-viscosity, divergence, and unforced equation hypotheses. Thus [F1] applies with its open spatial domain Ω=Rd; the periodic cell is used only for the energy integrals.

Given: The data in the Statement, including [A1] and the finite Reynolds averaged equation and energy split [F1].

Proof

1.1givenA1F1algebra

By [F1], the mean field satisfies ∂tuˉ+div⁡(uˉ⊗uˉ)+∇pˉ=νΔuˉ−div⁡R with div⁡uˉ=0. Differentiate Em under the integral, which is valid by the stated regularity and compactness of the periodic cell. For every continuously differentiable periodic scalar g, ∫Td∂xsg dx=0, since integration over xs∈[0,2π] gives equal endpoint values. Thus the convection and pressure terms integrate to zero because they are respectively div⁡(∣uˉ∣2uˉ/2) and div⁡(pˉuˉ); periodic integration by parts gives ∫uˉ⋅Δuˉ=−∫∣∇uˉ∣2 and −∫uˉ⋅div⁡R=∫R:∇uˉ. This proves the mean-energy identity.

2.1givenA1step 1.1algebra

Dot the jth equation in [A1] with uj, integrate, and multiply by aj. The time term is 12ajddt∫∣uj∣2. The convection and pressure terms are periodic divergences, respectively div⁡(∣uj∣2uj/2) and div⁡(pjuj), because div⁡uj=0; their integrals vanish by the periodic-cell argument in step 1.1. Periodic integration by parts gives the viscous contribution −νaj∫∣∇uj∣2. Summing over j yields ddt(12∫∑jaj∣uj∣2)=−ν∫∑jaj∣∇uj∣2.

3.1F2F3step 1.1step 2.1algebra

Fixed weights and [F2] give ∑jaj∇vj=∇(∑jajvj)=0, while [F3] gives 12∫∑jaj∣uj∣2=Em+Ef. Expanding ∇uj=∇uˉ+∇vj and summing squared norms therefore gives ∑jaj∣∇uj∣2=∣∇uˉ∣2+∑jaj∣∇vj∣2. Subtracting step 1.1's mean-energy balance from step 2.1's total balance yields the stated fluctuation-energy balance with the transfer term's opposite sign.

4.1givenA1step 1.1step 3.1algebra∎

Both energies and the transfer integrand are continuous in time under [A1]. Integrating the two derivative identities from step 3.1 and step 1.1 between any t0<t1 in I by the fundamental theorem of calculus gives the stated finite-time identities. Adding them cancels the transfer integrals exactly; no sign restriction on either transfer integral was used.

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