“…We noted that, at the relevant scaling established by Anderson & Worster (1995, 1996, the linear system of the problem exhibits both stationary and oscillatory modes of convection at comparable critical values of the Rayleigh number for the onset of convection. Hence, to determine valid analytical results, which could also be compared with the available experimental results (Tait, Jahrling & Jaupart 1992), a nonlinear theory needed to be developed and analysed, which could account for both stationary and oscillatory modes of convection (Riahi 2002). However, prior to the present study, no nonlinear investigation of oscillatory convection alone in mushy layers had been carried out, and, thus, to understand its qualitative features the present investigation was necessary.…”