Feedback control stabilization of the no-motion state of a fluid confined in a horizontal porous layer heated from below
- 1 December 1993
- journal article
- research article
- Published by Cambridge University Press (CUP) in Journal of Fluid Mechanics
- Vol. 257 (-1) , 485-505
- https://doi.org/10.1017/s0022112093003179
Abstract
We consider a horizontal three-dimensional saturated porous layer, confined in an upright cubic box, heated from below and cooled from above. In the absence of a controller, the fluid maintains a no-motion state for subcritical Rayleigh numbers R < Rc, where Rc depends on the box's aspect ratio. Once this critical number is exceeded, fluid motion ensues. We demonstrate that, with the use of feedback control strategies which suppress flow instabilities, one can maintain a stable no-motion state for Rayleigh numbers far exceeding the classical critical one for the onset of convection. To preserve the equilibrium no-motion state of the classical problem, the controller alters the system's dynamics so as to stabilize an otherwise non-stable state.Keywords
This publication has 12 references indexed in Scilit:
- Stabilization of the no-motion state in Rayleigh-Bénard convection through the use of feedback controlPhysical Review Letters, 1993
- Hexagonal and roll flow patterns in temporally modulated Rayleigh-Bénard convectionPhysical Review A, 1992
- Stabilization of Rayleigh–Bénard convection by means of a slow nonplanar oscillatory flowPhysics of Fluids A: Fluid Dynamics, 1992
- Active control of convectionPhysics of Fluids A: Fluid Dynamics, 1991
- Controlling a chaotic systemPhysical Review Letters, 1991
- Bénard convection with time-periodic heatingPhysics of Fluids, 1984
- Low Rayleigh Number Thermal Convection in a Vertical Cylinder Filled With Porous Materials and Heated From BelowJournal of Heat Transfer, 1982
- The Stability of Time-Periodic FlowsAnnual Review of Fluid Mechanics, 1976
- Convection in a Box of Porous Material Saturated with FluidPhysics of Fluids, 1972
- Criterion for the onset of convective flow in a fluid in a porous mediumInternational Journal of Heat and Mass Transfer, 1967