2005
DOI: 10.1016/j.expthermflusci.2005.02.002
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Experimental investigation of the grid-generated turbulence features in a free surface flow

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Cited by 21 publications
(19 citation statements)
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“…Schematics of the experimental setup and test rig with PIV equipment are shown in Figure 1a,b. As previous studies with similar test condition and flow regime show [19], the flow in main flow region around mid-depth of the channel far downstream of the obstacle is generally homogeneous in water depth direction. In this work, honeycombs and wave-breaking plates were installed at the tunnel entrance far enough (about 10 m) upstream of the test section to ensure a vertically uniform base flow away from boundaries without grid more certainly [25,26].…”
Section: Experimental Facilitysupporting
confidence: 73%
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“…Schematics of the experimental setup and test rig with PIV equipment are shown in Figure 1a,b. As previous studies with similar test condition and flow regime show [19], the flow in main flow region around mid-depth of the channel far downstream of the obstacle is generally homogeneous in water depth direction. In this work, honeycombs and wave-breaking plates were installed at the tunnel entrance far enough (about 10 m) upstream of the test section to ensure a vertically uniform base flow away from boundaries without grid more certainly [25,26].…”
Section: Experimental Facilitysupporting
confidence: 73%
“…The distribution and value of velocity, turbulence intensity, integral scale and space-time correlation are presented in detail to reveal the transition properties of flow and turbulence distribution, which would be beneficial to the engineering determination of the channel dimension and configuration of the downstream filter device. As the distributions for both mean and fluctuating velocities x/M > 20 have shown few changes in the open water channel [19] (similar to the current case), the results in this paper are also useful to infer the flow distribution at a farther downstream distance. The flow diversity in water depth direction due to the influence of free surface and flow structures from the turbulence boundary layer (TBL) of the channel bottom is also analyzed, which is important for sediment transport.…”
Section: Introductionsupporting
confidence: 65%
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“…The classical approach to generate turbulence in the laboratory is the so-called grid method [1][2][3][4][5], in which fluid flow is forced through a mesh grid to generate turbulence. The main feature of grid turbulence is that it produces single-length turbulence scales at any instant.…”
Section: Introductionmentioning
confidence: 99%
“…The hydrodynamics of these turbulent flows are similar, however. It has been well established that turbulence in a stationary grid is driven by the mean flow which decays by a power law (Murzyn and Bélorgey 2005), but an oscillating grid generates zero-mean turbulence (Hwang and Eaton 2004). There are also differences in the functional relationships that describe turbulence parameters.…”
Section: Introductionmentioning
confidence: 99%