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- W2074906128 abstract "Thermal convection in a two-layer system with the presence of a plane Couette flow is investigated. The system comprises a fluid layer overlying a porous layer saturated with the same fluid and the lower plate is maintained warmer than the upper. A shear is generated by moving the upper wall horizontally at a constant speed. Both convection modes including longitudinal and transverse rolls are considered. Numerical results show that the neutral curves of both modes may be bimodal which depends on the depth ratio (i.e., the ratio of the depth of fluid layer to that of porous layer). The longitudinal rolls are always preferred at the onset of convection and the stability of this mode is independent of Reynolds and Prandtl numbers. But the transverse rolls may have the same stability as the longitudinal rolls when Reynolds number or Prandtl number approaches zero. Either increase of Reynolds number or Prandtl number raises its stability, and both produce the same effects on the stability behaviors of transverse rolls and the critical convection mode of transverse rolls tends to be within the porous layer with long wavelength." @default.
- W2074906128 created "2016-06-24" @default.
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- W2074906128 date "2005-06-01" @default.
- W2074906128 modified "2023-09-25" @default.
- W2074906128 title "Thermal convection in superposed fluid and porous layers subjected to a horizontal plane Couette flow" @default.
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- W2074906128 doi "https://doi.org/10.1063/1.1932312" @default.
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