We consider the problem of nonlinear oscillatory convection in a horizontal mushy layer rotating about a vertical axis. Under a near-eutectic approximation and the limit of large far-field temperature, we determine the stable and unstable oscillatory solutions of the weakly nonlinear problem by using perturbation and stability analyses. It was found that depending on the values of the parameters, supercritical simple travelling modes of convection in the form of hexagons, squares, rectangles or rolls can become stable and preferred, provided the value of the rotation parameter τ is not too small and is below some value, which can depend on the other parameter values. Each supercritical form of the oscillatory convection becomes subcritical as τ increases beyond some value, and each subcritical form of the oscillatory convection is unstable. In contrast to the non-rotating case, qualitative properties of the lefttravelling modes of convection are different from those of the right-travelling modes, and such qualitative difference is found to be due to the interactions between the local solid fraction and the Coriolis term in the momentum-Darcy equation.
IntroductionRiahi (2003) extended the steady problem of convection in rotating mushy layers treated by Guba (2001) by following Anderson & Worster (1995) in assuming a much wider range ε δ for the amplitude of convection, taking into account the interactions between the local solid fraction and the convection associated with the Coriolis term in the momentum-Darcy equation and carrying out stability analysis of the finiteamplitude steady solutions. It was found, in particular that over most of the range of the parameter values, subcritical down-hexagons with down-flow at the cell centres and up-flow at the cell boundaries can be preferred over up-hexagons, where flow is upward at the cell centres and downward at the cell boundaries.Riahi (2002) extended the linear oscillatory problem of convection in mushy layers and in the absence of rotation due to Anderson & Worster (1996) by employing weakly nonlinear and stability analyses to determine the stable finite-amplitude oscillatory solutions. He found, in particular, that depending on the values of the parameters, only supercritical simple travelling modes of convection in the form of either righttravelling rolls (where the phase velocity of the rolls is in the direction of the component of the position vector along the wavenumber vector) or left-travelling rolls, (where the phase velocity of the rolls is in the direction opposite to that of the component of the position vector along the wavenumber vector) or supercritical standing rolls can be stable. The weakly nonlinear and stability properties of the righttravelling mode were found to be the same as those of the left-travelling mode. The author is grateful to the editor and two referees for pointing out an error due to the