TY - GEN
T1 - Detailing History and Non-equilibrium Effects in Adverse Pressure Gradient Turbulent Boundary Layers
AU - Romero, S.
AU - Zimmerman, S.
AU - Philip, J.
AU - Klewicki, J.
N1 - Publisher Copyright: © The Author(s), under exclusive license to Springer Nature Switzerland AG 2024.
PY - 2024
Y1 - 2024
N2 - Utilizing the stress balance and a wall shear stress and pressure based velocity scale, uhyb, introduced in Romero et al. (2022) non-equilibrium effects in adverse pressure gradient turbulent boundary layers are studied. Data from canonical flows, i.e. zero pressure gradient turbulent boundary layers, are used to provide context for this adverse pressure gradient turbulent boundary layer analysis. Adverse pressure gradient flows at varying Clauser pressure-gradient parameter β are studied. This parameter can be defined as the ratio of time-scales, β=tΔ/tPG, characteristic of the turbulence and pressure gradient. Here, tΔ=Δ/uτ, where Δ=(U∞/uτ)δ∗ is the Rotta-Clauser thickness, δ∗ is the displacement thickness, and uτ is the friction velocity. tPG=-(dU∞/dx)-1, where U∞ is the free-stream velocity. For the adverse pressure gradient flow to achieve self-similarity, β, the ratio of two time-scales, has to be a constant. Therefore, under a non-constant β the flow takes time to reach self-similarity and history effects become apparent. From studying non-constant β cases, this study hypothesizes a link between the cross-over from equilibrium to non-equilibrium with a corresponding qualitative change to the internal leading order stress balance.
AB - Utilizing the stress balance and a wall shear stress and pressure based velocity scale, uhyb, introduced in Romero et al. (2022) non-equilibrium effects in adverse pressure gradient turbulent boundary layers are studied. Data from canonical flows, i.e. zero pressure gradient turbulent boundary layers, are used to provide context for this adverse pressure gradient turbulent boundary layer analysis. Adverse pressure gradient flows at varying Clauser pressure-gradient parameter β are studied. This parameter can be defined as the ratio of time-scales, β=tΔ/tPG, characteristic of the turbulence and pressure gradient. Here, tΔ=Δ/uτ, where Δ=(U∞/uτ)δ∗ is the Rotta-Clauser thickness, δ∗ is the displacement thickness, and uτ is the friction velocity. tPG=-(dU∞/dx)-1, where U∞ is the free-stream velocity. For the adverse pressure gradient flow to achieve self-similarity, β, the ratio of two time-scales, has to be a constant. Therefore, under a non-constant β the flow takes time to reach self-similarity and history effects become apparent. From studying non-constant β cases, this study hypothesizes a link between the cross-over from equilibrium to non-equilibrium with a corresponding qualitative change to the internal leading order stress balance.
KW - Adverse pressure gradients
KW - Tuburlent boundary layers
UR - https://www.scopus.com/pages/publications/85202154592
U2 - 10.1007/978-3-031-55924-2_11
DO - 10.1007/978-3-031-55924-2_11
M3 - Conference contribution
SN - 9783031559235
T3 - Springer Proceedings in Physics
SP - 83
EP - 88
BT - Progress in Turbulence 10 - Proceedings of the iTi Conference on Turbulence 2023
A2 - Örlü, Ramis
A2 - Talamelli, Alessandro
A2 - Peinke, Joachim
A2 - Oberlack, Martin
PB - Springer Science and Business Media Deutschland GmbH
T2 - 10th Conference on Interdisciplinary Turbulence Initiative, iTi 2023
Y2 - 24 June 2023 through 26 June 2023
ER -