1973
DOI: 10.1016/0017-9310(73)90183-x
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Calculation of turbulent boundary layers over flat plates with different phenomenological theories of turbulence and variable turbulent Prandtl number

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Cited by 37 publications
(9 citation statements)
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“…For P r = 0.025, however, it increases from the wall to a maximum value of 3.27 at y+ = 37 and then decreases gradually toward the channel centre. Although the profile of P r t in the vicinity of the wall has been a m atter of conjecture, the two numerical simulations do not show a marked increase toward the wall th at is seen in the previous empirical and experimental results (Wassel & Catton 1973;Kays & Crawford 1980). The time scale ratio R, which is the ratio of tem perature dissipation time scale tq to veloc dissipation time scale tu, is often used in scalar flux modelling.…”
Section: ____mentioning
confidence: 57%
“…For P r = 0.025, however, it increases from the wall to a maximum value of 3.27 at y+ = 37 and then decreases gradually toward the channel centre. Although the profile of P r t in the vicinity of the wall has been a m atter of conjecture, the two numerical simulations do not show a marked increase toward the wall th at is seen in the previous empirical and experimental results (Wassel & Catton 1973;Kays & Crawford 1980). The time scale ratio R, which is the ratio of tem perature dissipation time scale tq to veloc dissipation time scale tu, is often used in scalar flux modelling.…”
Section: ____mentioning
confidence: 57%
“…Variable P r t models have had difficulty matching experimental data. [11][12][13][14] Scale resolving simulations (SRS) have become a major focus in recent years. Detached Eddy Simulation (DES) and Large Eddy Simulation (LES) allow the largest scales of turbulence to be resolved while filtering (implicitly or explicitly) the smallest scales.…”
Section: B Numerical Backgroundmentioning
confidence: 99%
“…Furthermore, the mean scalar gradient of the two-part model directly influences the evaluation of SGS scalar fluxes, although this is surprising since the SGS scalar fluxes must be determined locally (Horiuti 1987). A significant difference in k, near the wall by Wassel & Catton (1973) are included. The Pr, profile from Case 1 is in fairly good agreement with Hishida et al (1986), except in the channel central region.…”
Section: (4b)mentioning
confidence: 99%