期刊
EXPERIMENTAL THERMAL AND FLUID SCIENCE
卷 129, 期 -, 页码 -出版社
ELSEVIER SCIENCE INC
DOI: 10.1016/j.expthermflusci.2021.110469
关键词
High spatial resolution; PIV; Large scale motions; Turbulent boundary layer; Adverse pressure gradient; Zero pressure gradient
资金
- Australian Government of this research through an Australian Research Council Discovery grant
- ARC Discovery Early Career Researcher Award (DECRA) fellowship
- Punjab Educational Endowment Fund (PEEF), Punjab, Pakistan
- Australian Government Research Training Program (RTP) Scholarship
- Australian Government
- NCMAS grant
- Monash University through an ARC LIEF grant
- Multi-modal Australian ScienceS Imaging and Visualisation Environment (MASSIVE)
High-spatial-resolution two-component, two-dimensional particle-image-velocimetry measurements were taken in a high Reynolds number Boundary Layer Wind Tunnel to study zero-pressure-gradient and adverse-pressure-gradient turbulent boundary layers. The large-scale motions were found to be energized in the outer-layer, with adverse-pressure-gradient making them stronger.
High-spatial-resolution (HSR) two-component, two-dimensional particle-image-velocimetry (2C-2D PIV) measurements of a zero-pressure-gradient (ZPG) turbulent boundary layer (TBL) and an adverse-pressure-gradient (APG)-TBL were taken in the Laboratoire de Mecanique des Fluides de Lille (LMFL) High Reynolds number Boundary Layer Wind Tunnel. The ZPG-TBL has a momentum-thickness based Reynolds number Re-delta 2 = delta(2) U-e/nu = 7, 750 (where delta(2) is the momentum thickness and U-epsilon is the edge velocity), while the APG-TBL has a Re delta(2) = 16, 240 and a Clauser's pressure gradient parameter beta= delta(1) P-x/tau(omega) = 2.27 (where.. 1 is the displacement thickness, P-x is the pressure gradient in streamwise direction and tau(omega) is the wall shear stress). The 2C fluctuating flow field of each TBL was decomposed using proper orthogonal decomposition (POD) to investigate the large-scale motions (LSMs). The LSMs are found to be energized in the outer-layer, becoming stronger in the presence of the adverse-pressure-gradient. Profiles of the conditionally averaged Reynolds stresses show that high-momentum LSMs contribute more to the Reynolds stresses than low-momentum LSMs from the wall to the end of the log-layer while the opposite is found in the wake region. The cross-over point between the profiles of the conditionally averaged Reynolds stresses from the high- and low-momentum LSMs always has a higher value than the corresponding Reynolds stress from the unconditional ensemble average at the same wall-normal location. This difference is up to 80% in the Reynolds streamwise and shear stresses and up to 15% in the Reynolds wall-normal stresses. Furthermore, the cross-over point in the APG-TBL is found to be further from the wall than in the ZPG-TBL. The conditional Reynolds streamwise and shear stresses without the LSMs are reduced by up to 42% in the ZPG-TBL and by up to 50% in the APG-TBL, while having a minimal effect on the conditional Reynolds wall-normal stress without the LSMs in both the ZPG- and APG-TBL.
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