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Thermocapillary-buoyancy Convection Driven by a Horizontal Temperature Gradient in a Thin Liquid Layer: The Effect of Evaporation

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Abstract

The effects of phase change on the stability of a horizontally heated liquid layer are studied experimentally in this paper. Results are obtained for two volatile liquids with similar Prandtl numbers in a rectangular geometry with different temperature differences. Three different flow states occur with the variation of the liquid depth, namely oscillating multicellular convection, hydrothermal waves and steady flow. The critical conditions for the transition between the different flow states are identified and discussed. In addition, the presence of evaporation at the interface plays an essential role in the flow instabilities. The results show that evaporation at the surface and associated surface deformation tend to inhibit the development of a hydrothermal wave but conversely promote the transition of oscillating multicellular convection. Furthermore, the transient nature of HTWs is shown to be little affected by the phase change.

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Acknowledgements

This work was financially supported by the National Natural Science Foundation of China (Grants No. 11532015, No. 11302236), by the Strategic Priority Research Program on Space Science, Chinese Academy of Sciences (Grants No. XDA04073000, XDA04020202-02) and China Manned Space Program (TZ-1).

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Correspondence to Qiu-Sheng Liu.

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This article is part of the Topical Collection on The Effect of Gravity on Non-equilibrium Processes in Fluids

Guest Editors: Tatyana Lyubimova, Valentina Shevtsova

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Qin, J., Liu, QS., Tao, YQ. et al. Thermocapillary-buoyancy Convection Driven by a Horizontal Temperature Gradient in a Thin Liquid Layer: The Effect of Evaporation. Microgravity Sci. Technol. 34, 66 (2022). https://doi.org/10.1007/s12217-022-09976-x

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  • DOI: https://doi.org/10.1007/s12217-022-09976-x

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