Experimental study of turbulent flow over and within cubically packed walls of spheres: Effects of topography, permeability and wall thickness

被引:31
作者
Kim, Taehoon [1 ,2 ]
Blois, Gianluca [2 ]
Best, James L. [1 ,4 ,5 ,6 ,7 ]
Christensen, Kenneth T. [2 ,3 ,8 ]
机构
[1] Univ Illinois, Dept Mech Sci & Engn, Champaign, IL 61820 USA
[2] Univ Notre Dame, Dept Aerosp & Mech Engn, Notre Dame, IN 46556 USA
[3] Univ Notre Dame, Dept Civil & Environm Engn & Earth Sci, Notre Dame, IN 46556 USA
[4] Univ Illinois, Dept Geol, Champaign, IL 61820 USA
[5] Univ Illinois, Dept Geog, Champaign, IL 61820 USA
[6] Univ Illinois, Dept Geog Informat Sci, Champaign, IL 61820 USA
[7] Univ Illinois, Ven Te Chow Hydrosyst Lab, Champaign, IL 61820 USA
[8] Kyushu Univ, Int Inst Carbon Neutral Energy Res WPI I2CNER, Fukuoka, Fukuoka, Japan
基金
美国国家科学基金会;
关键词
Turbulent flow; Permeable wall; Flow interaction; PIV measurement; Refractive-index matching; DIRECT NUMERICAL-SIMULATION; BOUNDARY-LAYERS; REFRACTIVE-INDEX; CHANNEL FLOW; TRANSPORT; EXCHANGE; SMOOTH; BEDS;
D O I
10.1016/j.ijheatfluidflow.2018.06.004
中图分类号
O414.1 [热力学];
学科分类号
摘要
Results of high-resolution particle-image velocimetry (PIV) measurements are presented to explore how turbulent flow overlying a permeable wall is linked to the underlying pore flow and how their interplay is controlled by the topography of the wall interface and wall thickness. Two permeable walls were constructed from uniform spherical elements (25.4 mm diameter) in a cubically packed arrangement (porosity similar to 48%): one with two layers of spheres and the other with five layers. In addition, an impermeable rough wall with identical topography was considered as a baseline of comparison in order to explore the structural modifications imposed by permeability in the near-wall region. First- and second-order velocity statistics provide a quantitative assessment of such modifications of the local flow. A double-averaging approach allowed investigation of the global representation of the flow and assessment of conventional scaling parameters. A momentum deficit in the first pore layer and subsequent recovery beneath is observed, consistent with previous studies, as is a decay of the turbulent fluctuations. The transitional layer resides at the wall interface where free flow and pore flow interact, exchanging mass and momentum through intermittent turbulent events. Statistical investigation based on conditional averaging reveals that upwelling and down-welling flow events are associated with the passage of large-scale, low and high streamwise momentum free flow near the wall, respectively.
引用
收藏
页码:16 / 29
页数:14
相关论文
共 43 条
[1]  
Adrian R J., 2011, Particle Image Velocimetry
[2]   RESPONSE OF A TURBULENT BOUNDARY LAYER TO A STEP CHANGE IN SURFACE ROUGHNESS .1. SMOOTH TO ROUGH [J].
ANTONIA, RA ;
LUXTON, RE .
JOURNAL OF FLUID MECHANICS, 1971, 48 (AUG27) :721-&
[3]   ROUGH-WALL TURBULENT BOUNDARY-LAYERS IN THE TRANSITION REGIME [J].
BANDYOPADHYAY, PR .
JOURNAL OF FLUID MECHANICS, 1987, 180 :231-266
[4]  
Best J., 2005, J GEOPHYS RES, V110
[5]   Measurements of turbulence characteristics in an open-channel flow over a transitionally-rough bed using particle image velocimetry [J].
Bigillon, F. ;
Nino, Y. ;
Garcia, M. H. .
EXPERIMENTS IN FLUIDS, 2006, 41 (06) :857-867
[6]  
Blois G., 2012, 50 AM I AER ASTR AIA
[7]  
Bomminayuni S., 2011, J HYDRAUL ENG
[8]   The influence of wall permeability on turbulent channel flow [J].
Breugem, W. P. ;
Boersma, B. J. ;
Uittenbogaard, R. E. .
JOURNAL OF FLUID MECHANICS, 2006, 562 :35-72
[9]   REFRACTIVE-INDEX MATCHING METHODS FOR LIQUID FLOW INVESTIGATIONS [J].
BUDWIG, R .
EXPERIMENTS IN FLUIDS, 1994, 17 (05) :350-355
[10]   Velocity-defect scaling for turbulent boundary layers with a range of relative roughness [J].
Connelly, JS ;
Schultz, MP ;
Flack, KA .
EXPERIMENTS IN FLUIDS, 2006, 40 (02) :188-195