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- W2016164094 abstract "The effect of a salinity gradient on the instability of natural convection in a vertical fluid layer between two parallel plates is investigated theoretically. Temperatures of the two plates are different by 2 T 0 and both a stable temperature gradient, β>0, and an unstable salinity gradient, β s >0, are present in the vertical direction. The stability is investigated for various values of β and β s in the case of the Prandtl number P r =7 and the Schmidt number S c =700, which corresponds to weak salt water. It is found that the stationary mode dominates the onset of instability if both β and β s are moderate, otherwise the travelling mode governs it." @default.
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- W2016164094 title "The Effect of a Salinity Gradient on the Instability of Natural Convection in a Vertical Fluid Layer" @default.
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- W2016164094 doi "https://doi.org/10.1143/jpsj.54.3747" @default.
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