TY - JOUR
T1 - The three effects of the pressure force on turbulent boundary layers
AU - Gungor, Taygun Recep
AU - Gungor, Ayse Gul
AU - Maciel, Yvan
N1 - Publisher Copyright:
© 2025 The Authors
PY - 2025/12
Y1 - 2025/12
N2 - This study aims to isolate the three effects of the pressure force on the inner and outer layers: the local direct impact (characterized by the pressure gradient parameter, β), the local disequilibrating effect (represented here by the normalized streamwise derivative dβ/dX), and the upstream cumulative effect, while also accounting for the inevitable Reynolds number influence. To achieve this objective, we draw on several non-equilibrium and near-equilibrium databases from the literature, and employ a methodology based on the selection of pressure-gradient parameters — distinct for the inner and outer layers — that capture the local direct impact and the local disequilibration effect of the pressure gradient. The pressure force impact on the inner and outer regions is represented by two parameters: the friction–viscous pressure-gradient parameter, βi, and the pressure-gradient parameter based on Zagarola–Smits velocity, βZS, respectively. In the non-equilibrium flow cases, both βi and βZS exhibit similar distributions, initially increasing and then decreasing. However, the rate of change of these parameters along the streamwise direction varies among the flows, indicating differing levels of pressure force disequilibration. In addition, we employ two near-equilibrium cases with minimal variations of the pressure gradient parameters for comparisons. In the outer layer, it is found that both the local and cumulative disequilibrating effects modify the mean velocity and Reynolds stress profiles at identical βZS values. The faster the variations in pressure force impact, the more delayed the response of both mean flow and turbulence. Cumulative effects prove to be significant. In the inner layer, which responds much faster to changes in pressure force, the local disequilibrating effect still modifies the mean velocity profile in the viscous sublayer. Notably, when the mean velocity defect is significant, the behavior of u-structures in the inner layer appears to be governed by how outer turbulence responds to pressure force effects. In contrast, the size of uv-structures in the inner layer scales with the mixed pressure-friction length (ν/uτ+ν/upi). Unlike inner u-structures, they are independent of large-scale outer structures and flow history.
AB - This study aims to isolate the three effects of the pressure force on the inner and outer layers: the local direct impact (characterized by the pressure gradient parameter, β), the local disequilibrating effect (represented here by the normalized streamwise derivative dβ/dX), and the upstream cumulative effect, while also accounting for the inevitable Reynolds number influence. To achieve this objective, we draw on several non-equilibrium and near-equilibrium databases from the literature, and employ a methodology based on the selection of pressure-gradient parameters — distinct for the inner and outer layers — that capture the local direct impact and the local disequilibration effect of the pressure gradient. The pressure force impact on the inner and outer regions is represented by two parameters: the friction–viscous pressure-gradient parameter, βi, and the pressure-gradient parameter based on Zagarola–Smits velocity, βZS, respectively. In the non-equilibrium flow cases, both βi and βZS exhibit similar distributions, initially increasing and then decreasing. However, the rate of change of these parameters along the streamwise direction varies among the flows, indicating differing levels of pressure force disequilibration. In addition, we employ two near-equilibrium cases with minimal variations of the pressure gradient parameters for comparisons. In the outer layer, it is found that both the local and cumulative disequilibrating effects modify the mean velocity and Reynolds stress profiles at identical βZS values. The faster the variations in pressure force impact, the more delayed the response of both mean flow and turbulence. Cumulative effects prove to be significant. In the inner layer, which responds much faster to changes in pressure force, the local disequilibrating effect still modifies the mean velocity profile in the viscous sublayer. Notably, when the mean velocity defect is significant, the behavior of u-structures in the inner layer appears to be governed by how outer turbulence responds to pressure force effects. In contrast, the size of uv-structures in the inner layer scales with the mixed pressure-friction length (ν/uτ+ν/upi). Unlike inner u-structures, they are independent of large-scale outer structures and flow history.
KW - Pressure gradient
KW - Turbulent boundary layer
UR - https://www.scopus.com/pages/publications/105008508538
U2 - 10.1016/j.ijheatfluidflow.2025.109898
DO - 10.1016/j.ijheatfluidflow.2025.109898
M3 - Article
AN - SCOPUS:105008508538
SN - 0142-727X
VL - 116
JO - International Journal of Heat and Fluid Flow
JF - International Journal of Heat and Fluid Flow
M1 - 109898
ER -