Turbulent kinetic energy transport in a corner formed by a solid wall and a free surface

被引:32
作者
Hsu, TY
Grega, LM
Leighton, RI
Wei, T
机构
[1] Rutgers State Univ, Dept Aerosp & Mech Engn, Piscataway, NJ 08854 USA
[2] USN, Surface Warfare Ctr W, Struct Acoust & Hydroacoust Branch, Bethesda, MD 20817 USA
[3] USN, Res Lab, Div Remote Sensing, Washington, DC 20375 USA
关键词
D O I
10.1017/S0022112099008125
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
High-resolution DPIV and LDV measurements were made in a turbulent mixed boundary corner, i.e, a turbulent boundary layer generated by horizontal flow of water along a vertical wall in the vicinity of a horizontal free surface. This work is an extension of an earlier numerical/experimental study which established the existence of inner and outer secondary flow regions in the corner. The inner secondary motion is characterized by a weak, slowly evolving vortex with negative streamwise vorticity. The outer secondary motion is characterized by an upflow along the wall and outflow away from the wall at the free surface. The objective of the current investigation, then, was to understand the combined effects of a horizontal, shear-free, free surface and a vertical, rigid, no-slip boundary on turbulent kinetic energy transport. The context of this work is providing physical insights and quantitative data for advancing the state of the art in free-surface turbulence modelling. Experiments were conducted in a large free-surface water tunnel at momentum-thickness Reynolds numbers, Re-theta, of 670 for the DPIV studies, and 1150 for the LDV measurements. A high-resolution, two-correlation DPIV program was used to generate ensembles of vector fields in planes parallel to the free surface. These data were further processed to obtain profiles of turbulent kinetic energy transport terms, such as production and dissipation. In addition, profiles of streamwise and surface-normal velocity were made (as functions of distance from the wall) using two-component LDV. Key findings of this study include the fact that both turbulent kinetic energy production and dissipation are dramatically reduced close to the free surface. Far from the wall, this results in an increase in surface-parallel fluctuations very close to the free surface. The degree of this anisotropy and the spatial scales over which it exists are critical data for improved free-surface turbulence models.
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页码:343 / 366
页数:24
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