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Effect of ice crystals on run-back ice evolution on a wing model

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Thermophysics and Aeromechanics Aims and scope

Abstract

The influence of ice crystals in an airflow on evolution of run-back ice on the surface of the wing model is numerically investigated for the conditions of experiment in an icing wind tunnel. The results confirm that a change in the mass of ice deposits upon introducing crystals into the flow observed experimentally is associated with absorption of some mass of ice crystals by the water film formed on the surface of a solid at low flow velocities and with film splashing at higher flow velocities. In the first case, the mass of the run-back ice increases; in the second case, it decreases.

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Authors and Affiliations

  1. Central Aerohydrodynamic Institute n.a. N.E. Zhukovsky, Zhukovsky, Moscow Region, Russia

    A. V. Kashevarov, A. B. Miller, Yu. F. Potapov & A. L. Stasenko

  2. Moscow Institute of Physics and Technology, Dolgoprudny, Moscow Region, Russia

    A. B. Miller & A. L. Stasenko

Authors
  1. A. V. Kashevarov
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  2. A. B. Miller
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  3. Yu. F. Potapov
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  4. A. L. Stasenko
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Corresponding author

Correspondence to A. V. Kashevarov.

Additional information

The work was carried out within the MUSIC-Haic project of the HORIZON 2020 EU program with financial support from the Ministry of Science and Higher Education of the Russian Federation in the framework of the federal target program “Research and Development in Priority Areas of Development of the Scientific and Technological Complex of Russia for 2014–2020”, unique project identifier RFMEFI62818X0010.

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Kashevarov, A.V., Miller, A.B., Potapov, Y.F. et al. Effect of ice crystals on run-back ice evolution on a wing model. Thermophys. Aeromech. 28, 21–28 (2021). https://doi.org/10.1134/S0869864321010030

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  • DOI: https://doi.org/10.1134/S0869864321010030

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