2017
DOI: 10.1016/j.ijheatmasstransfer.2017.02.024
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Heat transfer in production and decay regions of grid-generated turbulence

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Cited by 20 publications
(28 citation statements)
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“…However, it has been later realized to vary dramatically depending on grid geometry, inflow conditions and experimental facility, etc. [16][17][18]24,25]. The flow structure and turbulence statistics, in Sections 3.1 and 3.2, evidenced the importance of the smaller scales in addition to the largest scale.…”
Section: Revisit the Wake Interaction Length Scale Modelmentioning
confidence: 86%
See 2 more Smart Citations
“…However, it has been later realized to vary dramatically depending on grid geometry, inflow conditions and experimental facility, etc. [16][17][18]24,25]. The flow structure and turbulence statistics, in Sections 3.1 and 3.2, evidenced the importance of the smaller scales in addition to the largest scale.…”
Section: Revisit the Wake Interaction Length Scale Modelmentioning
confidence: 86%
“…Previously, the magnitude of the peak turbulence intensity was proposed to be proportional to c d t 0 /L 0 for fractal square grids, where c d is the drag coefficient of the largest bars of the grid [17]. Subsequent research focused on the largest scale being the dominant factor to determine the peak turbulence intensity magnitude, i.e., Tu peak ∝ c d t 0 /L 0 [18,25]. This relation has shown to be true for both multi-scale and single-scale grids having different ratios of t 0 /L 0 .…”
Section: Revisit the Wake Interaction Length Scale Modelmentioning
confidence: 99%
See 1 more Smart Citation
“…However, the effect of the grid parameters on the turbulent field was ignored. Melina [23], Ahmadi-Baloutaki [24], and Wang [25] applied the gridgenerated turbulence directly, without studying the turbulence characteristics.…”
Section: State Of the Artmentioning
confidence: 99%
“…Since Rouse (1939) first used OGT to study sediment suspension [20], the OGT was employed to explore the mechanics of the sediment transport [21,22], the interfacial mixing in stratified flows [2,23], the mass transfer across a shear-free water-air interface [24,25], the desorption of contaminants from sediment [26,27], the rate of frazil ice growth [28] and the turbulent thermal diffusion effect [6]. With so many application experiences, despite the emergence of the alternative loudspeaker and jet approaches which are relatively expensive, the OGT was still widely used in recent years [5,[29][30][31][32][33][34].…”
Section: Introductionmentioning
confidence: 99%