Abstract
It is shown that at the moment a quasisteady disintegration regime is established, the thickness of the layer of material carried off from the surface is roughly equal to the depth of heating.
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Translated from Inzhenerno-Fizicheskii Zhurnal, Vol. 52, No. 3, pp. 357–362, March, 1987.
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Polezhaev, Y.V., Frolov, G.A. Transient regime in the thermal and erosional destruction of materials. Journal of Engineering Physics 52, 255–259 (1987). https://doi.org/10.1007/BF00872500
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DOI: https://doi.org/10.1007/BF00872500