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- W2032055966 abstract "Abstract An analysis is made of the effect of vertical throughflow on the onset of thermal convection in a horizontal layer of an electrically conducting fluid contained between two rigid permeable plates and heated from below in the presence of a uniform vertical magnetic field. The constant throughflow is measured by Peclet number Q and at both boundaries heat flux is held constant. It is found that when both boundaries are perfectly electrically conducting, the critical value of Rayleigh number R c t at the onset of steady convection increases with increase in Q for given values of the magnetic parameter R h , the Prandtl number p 1 and the magnetic Prandtl number p 2 with p 1 > p 2 . It is observed that the magnetic field inhibits the onset of steady convection. The analysis further reveals that R c t is independent of the sign of Q . When the lower plate is electrically non-conducting and the upper plate is perfectly electrically conducting, R c t is greater than the corresponding value of R c t for perfectly conducting plates for given values of Q , R h , p 1 and p 2 . It is also found that the positive throughflow ( Q > 0 ) is more stabilizing than the negative one ( Q 0 ) . The results are exemplified by considering some realistic cases e.g., liquid sodium and gallium." @default.
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- W2032055966 date "2012-07-01" @default.
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- W2032055966 title "Magnetohydrodynamic thermal instability in a conducting fluid layer with throughflow" @default.
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- W2032055966 doi "https://doi.org/10.1016/j.ijnonlinmec.2011.10.006" @default.
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