Existence and nonuniqueness of rectangular solutions of the Bénard problem
Existence and nonuniqueness of rectangular solutions of the Bénard problem
复制标题
DOI:
10.1007/bf00256457
复制
发表时间:
1968
影响因子:
2.5
通讯作者:
P. Rabinowitz
中科院分区:
文献类型:
--
作者:
P. Rabinowitz
In this paper we will study the B6nard problem which is a relatively simple convection problem. We want a mathematical description of the following idealized experiment: An infinite horizontal layer of viscous fluid initially at rest lies between two rigid perfectly conducting walls. A constant temperature gradient is maintained between the walls, the lower wall being warmer. If the temperature gradient is small, the fluid remains at rest and heat is transported through the fluid only by conduction. However when the temperature gradient is increased beyond a certain critical value, the fluid undergoes time independent motions called convection corrents. Heat is now transported through the fluid by convection as well as conduction. In actual experiments, the fluid arranges itself in a regular cellular pattern, and motions take place only within the cells [1, 2]. The shape of the cells seems to depend strongly on the shape of the container [2]. One can give a simple qualitative explanation of the above phenomena. The bottom portion of the fluid expands because of the heating and becomes less dense. It therefore tends to rise. However the fluid, being viscous, resists this buoyancy force. If the temperature gradient is small the viscous forces are dominant and the fluid remains at rest, heat being transported only by conduction. On exceeding the critical temperature gradient, the buoyancy force becomes large enough to overcome the viscosity of the fluid and convection begins. B~ NARD conducted the original experiments in this area. His fluid had a free upper surface and he found the cells to be in the shape of hexagons [2]. However this effect was later shown [3] to be due primarily to surface tension, which plays a negligible role in the problem we consider here. We seek to show that the above convective phenomena can be obtained mathematically from the equations of motion of the fluid. The conduction solution is easily obtained and exists for all values of the temperature gradient. Thus the problem mathematically becomes one of nonuniqueness. We must show that on exceeding a critical temperature gradient, new solutions of the equations, corresponding to convection branch or bifurcate from the conduction solution. Actually we will give a much more complete picture of the structure of these equations. An examination of the corresponding linearized equations shows that the temperature gradient appears as an eigenvalue. Our main result will be the existence of" convective" solutions for temperature gradients near the eigenvalues of linear theory. Of course the solutions of major physical interest are those which