Characterizing developing adverse pressure gradient flows subject to surface roughness

被引:14
作者
Brzek, Brian [1 ]
Chao, Donald [1 ]
Turan, Oezden [2 ]
Castillo, Luciano [1 ]
机构
[1] Rensselaer Polytech Inst, Troy, NY 12180 USA
[2] Victoria Univ Technol, Melbourne, Vic 3000, Australia
基金
美国国家科学基金会;
关键词
TURBULENT-BOUNDARY-LAYERS; MEAN-VELOCITY PROFILE; TRANSITIONALLY ROUGH; UPSTREAM CONDITIONS; SIMILARITY ANALYSIS; OUTER FLOW; WALL; SMOOTH;
D O I
10.1007/s00348-009-0759-6
中图分类号
TH [机械、仪表工业];
学科分类号
0802 ;
摘要
An experimental study was conducted to examine the effects of surface roughness and adverse pressure gradient (APG) on the development of a turbulent boundary layer. Hot-wire anemometry measurements were carried out using single and X-wire probes in all regions of a developing APG flow in an open return wind tunnel test section. The same experimental conditions (i.e., T (a), U (ref), and C (p)) were maintained for smooth, k (+) = 0, and rough, k (+) = 41-60, surfaces with Reynolds number based on momentum thickness, 3,000 < Re (theta) < 40,000. The experiment was carefully designed such that the x-dependence in the flow field was known. Despite this fact, only a very small region of the boundary layer showed a balance of the various terms in the integrated boundary layer equation. The skin friction computed from this technique showed up to a 58% increase due to the surface roughness. Various equilibrium parameters were studied and the effect of roughness was investigated. The generated flow was not in equilibrium according to the Clauser (J Aero Sci 21:91-108, 1954) definition due to its developing nature. After a development region, the flow reached the equilibrium condition as defined by Castillo and George (2001), where I > = const, is the pressure gradient parameter. Moreover, it was found that this equilibrium condition can be used to classify developing APG flows. Furthermore, the Zagarola and Smits (J Fluid Mech 373:33-79, 1998a) scaling of the mean velocity deficit, U (a)delta*/delta, can also be used as a criteria to classify developing APG flows which supports the equilibrium condition of Castillo and George (2001). With this information a 'full APG region' was defined.
引用
收藏
页码:663 / 677
页数:15
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