Abstract
The steady motion of water in an enclosed rectangular cavity with differentially heated vertical end walls was studied experimentally, and the results are compared with the findings of parts 1 and 2. The depth-to-length ratios of the cavities were 102 and 1·9 × 102, and the Rayleigh number was allowed to vary sufficiently to enable a study to be made of the transition from a flow driven by the vertical wall boundary layers to one sustained by a longitudinal temperature gradient in the central sections of the cavity.
Publisher
Cambridge University Press (CUP)
Subject
Mechanical Engineering,Mechanics of Materials,Condensed Matter Physics
Reference13 articles.
1. Hart, J. E. 1971 J. Fluid Mech. 47,547–576.
2. Logan, W. B. & Cebulski, D. E. 1970 Am. Ass. Petroleum Geol. Mem. no. 13.
3. Cormack, D. E. , Leal, L. G. & Seinfeld, J. H. 1974 J. Fluid Mech. 65,231.
4. Fischer, H. B. 1972 J. Fluid Mech. 53,671–687.
5. Eckert, E. R. G. & Carlson, W. O. 1961 Int. J. Heat Mass Transfer,2,106–120.
Cited by
144 articles.
订阅此论文施引文献
订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献