The Minimal Attached Eddy in Wall Turbulence: Statistical Foundations, Inverse Identification and Influence Kernels
Karthik Duraisamy
TL;DR
This work extends Townsend's attached-eddy hypothesis by formulating an inverse problem to recover ideal single-eddy influence functions from DNS moments, then building a minimal Biot–Savart-consistent hairpin eddy template anchored to the inferred kernels. A spectral Influence kernel is introduced to map self-similar eddy footprints to the 1D energy spectrum, clarifying the origin of the $k_x^{-1}$ scaling and the log-layer behavior. The square hairpin with wall image reproduces mean and Reynolds-stress statistics across a range of Reynolds numbers, supporting the view that eddy morphology is secondary to kinematic influence functions once mean anchoring is fixed. The framework provides a transparent link between morphology, influence kernels, and spectra, offering a pathway to more sophisticated, yet parsimonious, models of wall turbulence and a direction for future inverse-design of eddy populations.
Abstract
Townsend's attached eddy hypothesis models the logarithmic region of high Reynolds number wall turbulence as a random superposition of wall-attached, geometrically self-similar eddies whose sizes obey a scale-invariant population law. Building on the statistical framework of Woodcock and Marusic (2015), the present work (i) poses an inverse problem to infer the ideal single-eddy contribution (influence) functions for the mean velocity and Reynolds stresses from DNS moments, (ii) uses these inferred kernels to guide a minimal Biot-Savart-consistent hairpin-type eddy built from Rankine vortex rods together with an inviscid image system, and (iii) introduces a spectral Influence kernel that maps a self-similar eddy footprint to its one-dimensional energy spectrum. The Influence-kernel viewpoint yields a transparent explanation for the emergence (and limitations) of the linear part of the energy spectrum, provides a clear scale-by-scale decomposition and helps rationalize why simple eddy templates can reproduce a broad set of log-layer statistics once the mean-flow anchoring is fixed.
