Log-linear law of the mean streamwise velocity in turbulent boundary layers with moderate adverse pressure gradients
Fuzhou Lyu, Lihao Zhao, Weixi Huang, Chunxiao Xu
TL;DR
The classical log law for mean velocity in wall-bounded turbulence does not hold under moderate adverse pressure gradients. The authors derive a log--linear law from the total shear-stress balance and a β-dependent eddy-viscosity scaling, yielding a closed-form expression for $U^+$ that includes both logarithmic and linear terms and recovers the traditional log law as $\beta \to 0$. Validation against diverse incompressible APG TBL datasets with $0.73 \le \beta \le 9.0$ shows substantially better agreement than the classical log law, with the diagnostic function $\Phi_2$ remaining near unity across cases. The approach preserves the classical Kármán constant $\kappa \approx 0.41$, introduces no extra empirical coefficients, and offers a simple, robust enhancement for predicting APG TBLs in RANS/WMLES applications.
Abstract
An essential feature of canonical zero-pressure-gradient (ZPG) turbulent boundary layers (TBLs) is that the mean streamwise velocity exhibits a logarithmic dependence on the wall-normal distance, known as the log law. In this study, we demonstrate that this conventional log law is not suitable for turbulent boundary layers subjected to pressure gradients (PGs). Instead, a log--linear law is theoretically derived for TBLs under moderate adverse pressure gradients (APGs), based on the total shear-stress balance and a rescaled eddy-viscosity model. The validity of the proposed log--linear law is assessed using available datasets of incompressible APG TBLs with the Clauser pressure-gradient parameter $β$ ranging from 0.73 to 9.0. Compared with the conventional log law, the present log--linear formulation shows significantly improved agreement with the measured mean velocity profiles. In the limiting case of $β\to 0$, the proposed law naturally recovers the classical log law.
