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Vibrational convection in a plane layer with a longitudinal temperature gradient

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Abstract

An exact solution is obtained for the equations of vibrogravitational convection in an arbitrarily oriented plane fluid layer with a longitudinal component of the temperature gradient. It is shown that in the absence of a static field inclined vibration leads to the development of plane-parallel convective flow. On the other hand, gravitational plane-parallel convective flow can always be suppressed by an appropriate choice of the direction and amplitude of vibration.

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Literature cited

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    R. V. Birikh

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  1. R. V. Birikh
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Translated from Izvestiya Akademii Nauk SSSR, Mekhanika Zhidkosti i Gaza, No. 4, pp. 12–15, July–August, 1990.

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Birikh, R.V. Vibrational convection in a plane layer with a longitudinal temperature gradient. Fluid Dyn 25, 500–503 (1990). https://doi.org/10.1007/BF01049852

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  • DOI: https://doi.org/10.1007/BF01049852

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