Author:
Kelly R. E.,Redekopp L. G.
Abstract
The development of the boundary layer on the upper surface of a horizontal flat plate in a non-diffusive, stratified flow is described. It is shown that the flow can be characterized by two basic parameters, the Reynolds (RL) and Russell (RuL) numbers, and that, depending on the relative magnitude of these two parameters, three different régimes of flow can be defined. The delineation of these régimes and the description of the flow in each of them is obtained by deriving a uniformly valid first approximation to the Boussinesq equations of motion for a flow contained in the two-dimensional parameter spaceRuL> 0,RL> 1. The critical stratification for the self-blocking of a horizontal boundary layer is shown to be given by the conditionRuL=O(RL½).
Publisher
Cambridge University Press (CUP)
Subject
Mechanical Engineering,Mechanics of Materials,Condensed Matter Physics
Reference14 articles.
1. Pao, Y.-H. 1968 Laminar flow of a stably stratified fluid past a flat plate.J. Fluid Mech. 34,795–808.
2. Martin, S. & Long, R. R. 1968 The slow motion of a flat plate in a viscous stratified fluid.J. Fluid Mech. 31,669–688.
3. Van Dyke, M. D. 1964 Perturbation Methods in Fluid Mechanics .New York:Academic.
4. Long, R. R. 1955 Some aspects of the flow of stratified fluids. III. Continuous density gradients.Tellus,7,432–457.
5. Rosenhead, L. (Ed.)1963 Laminar boundary layers .Oxford University Press.
Cited by
11 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