A gauge identity for interscale transfer in inhomogeneous turbulence
Khalid M. Saqr
Abstract
The local definition of interscale energy transfer is missing in inhomogeneous turbulence research. This manifests as a discrepancy between the subgrid-scale production $Π^{\mathrm{SGS}}$ and the increment-based transfer density $Π^{\mathrm{KHMH}}$. Here, this missing definition is found by identifying a gauge freedom in the spatial transport of energy, yielding the identity: $Π^{\mathrm{SGS}} = \int G_\ell Π^{\mathrm{KHMH}} \, d\boldsymbol{r} + \nabla \cdot \boldsymbol{J}_{\mathrm{gauge}}$. The formulations are proven to differ strictly by the divergence of the current $\boldsymbol{J}_{\mathrm{gauge}}$. Validation against the analytical Womersley solution confirms the identity to within machine precision ($<10^{-14}$). The current $\boldsymbol{J}_{\mathrm{gauge}}$ is identified as the mechanism for redistribution toward compliant boundaries. Both measures are shown to converge to the unique Duchon--Robert dissipation $D(u)$, unifying the theoretical framework for non-stationary turbulence.
