A direct numerical simulation of natural convection between two infinite vertical differentially heated walls scaling laws and wall functions

Citation
Tam. Versteegh et Ftm. Nieuwstadt, A direct numerical simulation of natural convection between two infinite vertical differentially heated walls scaling laws and wall functions, INT J HEAT, 42(19), 1999, pp. 3673-3693
Citations number
23
Categorie Soggetti
Mechanical Engineering
Journal title
INTERNATIONAL JOURNAL OF HEAT AND MASS TRANSFER
ISSN journal
00179310 → ACNP
Volume
42
Issue
19
Year of publication
1999
Pages
3673 - 3693
Database
ISI
SICI code
0017-9310(199910)42:19<3673:ADNSON>2.0.ZU;2-K
Abstract
A direct numerical simulation has been performed for the case of a natural convection flow between two differentially heated vertical walls for a rang e of Rayleigh numbers (5.4 x 10(5) < Ra < 5.0 x 10(6)). The simulation data are compared with experimental data of Dafa-Alla and Betts [Experimental s tudy of turbulent natural convection in a tall cavity, Exp. Heat Transfer 9 (1996) 165-194] and the agreement is found to be acceptable, Given the num erical data we consider the scaling behaviour of the mean temperature, the mean velocity profile and of the profiles of various turbulence statistics. Point of departure is the approach proposed by George and Capp [A theory f or natural convection turbulent boundary layers next to heated vertical sur faces, Int. J. Heat Mass Transfer 22 (1979) 813-826] who have formulated sc aling relationships valid, respectively, in the near-wall inner layer and i n the outer layer in the centre region of the channel. Matching of the scal ing relationships in the overlap between the inner and outer region leads t o explicit expressions which can be used as wall functions in computational procedures, The DNS data confirm the results of George and Capp for the sc aling of the mean temperature profile. For the mean velocity profile our DN S data support another scaling in terms of a defect law for the velocity gr adient in the inner layer. The scaling of George and Capp is also found to apply to the Reynolds stress, the temperature variance and the temperature fluxes. However, the velocity variances again seem to follow a different sc aling. (C) 1999 Elsevier Science Ltd. All rights reserved.