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Mean and fluctuation energy exchange
Statement
Let be an open interval, let and be integers, and define the flat torus , with integration using Lebesgue measure on a periodic cell . Fix constants with and a common constant . For , let be continuously differentiable in with continuous second spatial derivatives, and let be continuously differentiable. Require these fields to be -periodic in each spatial coordinate, so they descend to . Suppose they are unforced and satisfy pointwise on
Use , for a matrix field , and componentwise Laplacian. For set . Define , , , and
For a matrix and vector field , set and . Then for every ,
For every in , the endpoint identities are
The transfer term has opposite signs in the two balances and cancels in their sum. No sign is asserted for .
Statement references
Facts & Assumptions
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 .
Exact finite Reynolds averaged equation: The fixed-weight fluctuations have zero weighted mean, .
Exact finite Reynolds averaged equation: The pointwise kinetic-energy split is .
The periodic lifts are maps on satisfying the Statement’s regularity, fixed-weight, common-viscosity, divergence, and unforced equation hypotheses. Thus [F1] applies with its open spatial domain ; 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
By [F1], the mean field satisfies with . Differentiate under the integral, which is valid by the stated regularity and compactness of the periodic cell. For every continuously differentiable periodic scalar , , since integration over gives equal endpoint values. Thus the convection and pressure terms integrate to zero because they are respectively and ; periodic integration by parts gives and . This proves the mean-energy identity.
Dot the th equation in [A1] with , integrate, and multiply by . The time term is . The convection and pressure terms are periodic divergences, respectively and , because ; their integrals vanish by the periodic-cell argument in step 1.1. Periodic integration by parts gives the viscous contribution . Summing over yields .
Fixed weights and [F2] give , while [F3] gives . Expanding and summing squared norms therefore gives . 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.
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 in 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.