Simulations of zero pressure-gradient turbulent boundary layers over riblets
Vishal Kumar, Amirreza Rouhi, Oriol Lehmkuhl, Wen Wu, Melissa Kozul, Alexander J. Smits
TL;DR
This work investigates how zero-pressure-gradient turbulent boundary layers respond to streamwise step changes between smooth walls and riblets, focusing on drag-increasing triangular riblets with $s^+ \approx 50$. It employs large-eddy simulations with a novel grid-generation strategy for unstructured spectral-element codes and an inflow precursor to realize a ZPG TBL over riblets, enabling controlled step-change experiments. The study reveals that the internal equilibrium layer thickness $\delta_{IEL}$ grows to $0.4\delta_0$ within $4$–$12\delta_0$ depending on transition direction, but the wake remains history-locked (frozen) and the skin-friction coefficient $C_f$ does not reach its equilibrium value even at $\sim 45\delta_0$. These findings highlight persistent history effects in riblet-textured boundary layers and inform both drag predictions and the modeling of texture transitions in engineering applications, with implications for riblet design and flow-control strategies. $Re_{\theta,0} \simeq 680$ and $Re_\tau \simeq 283$ characterize the upstream state, while the flows evolve toward $Re_{\theta} \sim 1000$ downstream.$
Abstract
We computationally study the response of zero-pressure-gradient (ZPG) turbulent boundary layers (TBLs) to streamwise step changes from a smooth wall to riblets (S-R), and vice versa (R-S). We consider triangular riblets with tip angle $90^o$ (T9), that increase drag, with viscous-scaled spacing $50$. A novel grid-generation approach is developed for unstructured spectral-element codes, consistent with the size of turbulent scales across the TBL. We generate a ZPG TBL upstream of the step change (with thickness $δ_0$) with momentum thickness Reynolds number $Re_{θ_0} \simeq 680$. The TBL departure from equilibrium due to the step change, and its subsequent relaxation, recall previous studies on step changes in surface roughness. Downstream of the R-S step change, the internal equilibrium layer thickness $δ_{IEL}$ reaches $0.4 δ_0$ within $12δ_0$. However, downstream of the S-R step change $δ_{IEL}$ reaches $0.4 δ_0$ within $4δ_0$. In all cases, $δ_{IEL}$ does not reach the boundary layer thickness, even up to a distance of $45δ_0$ downstream of the step change, owing to persistent history effects within the frozen wake region.
