Flow structure and turbulence characteristics downstream of a spanwise suspended linear array

被引:8
|
作者
Qiao, J. D. [1 ]
Delavan, S. K. [1 ]
Nokes, R. I. [2 ]
Plew, D. R. [3 ]
机构
[1] SUNY Buffalo, Civil Struct & Environm Engn, Buffalo, NY 14260 USA
[2] Univ Canterbury, Civil & Nat Resources Engn, Christchurch, New Zealand
[3] Natl Inst Water & Atmospher Res, NIWA, Christchurch, New Zealand
关键词
Suspended linear array; Sub-layers; Shear layer; TKE decay; Momentum transport; HYACINTH EICHHORNIA-CRASSIPES; WATER-FLOW; MUSSEL; MYTILUS; AQUACULTURE; PATTERNS; DECAY;
D O I
10.1007/s10652-016-9465-0
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Laboratory experiments are conducted to quantify the mean flow structure and turbulence properties downstream of a spanwise suspended linear array in a uniform ambient water flow using Particle Tracking Velocimetry. Eighteen experimental scenarios, with four depth ratios (array depth to water column depth) of 0.35, 0.52, 0.78, and 0.95 and bulk Reynolds number (length scale is the array depth) from 11,600 to 68,170, are investigated. Three sub-layers form downstream of the array: (1) an internal wake zone, where the time-averaged velocity decreases with increasing distance downstream, (2) a shear layer which increases in vertical extent with increasing distance downstream of the array, and the rate of the increase is independent of the bulk Reynolds number or the depth ratio, and (3) an external wake layer with enhanced velocity under the array. The location of the shear layer is dependent on the depth ratio. The spatially averaged and normalized TKE of the wake has a short production region, followed by a decay region which is comparable to grid turbulence decay and is dependent on the depth ratio. The results suggest that the shear layer increases the transfer of horizontal momentum into the internal wake zone from the fluid outside of the array and that the turbulence in the internal wake zone can be modeled similarly to that of grid turbulence.
引用
收藏
页码:1021 / 1041
页数:21
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