Abstract

The effect of feedback control on the onset of steady and oscillatory surface tension-driven (Marangoni) instability in a rotating horizontal fluid layer is considered theoretically using linear stability theory. It is demonstrated that generally the critical Marangoni number for transition from the no-motion (conduction) to the motion state can be drastically increased by the combined effects of feedback control and rotation. Some cases in which increasing the controller gain parameter can be ineffective are also presented. The thresholds and codimension-2 points for the onset of steady and oscillatory convection are determined. We show how the Pr–Ta parameter space is divided into regions in which steady or oscillatory convection is preferred.

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