Abstract
A self-similar solution is obtained, showing the contradictions of the front model of phase transition. A mathematical model taking account of the formation of an extended frozen region is constructed.
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Translated from Inzhenerno-Fizicheskii Zhurnal, Vol. 55, No. 3, pp. 435–441, September, 1988.
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Maksimov, A.M., Tsypkin, G.G. Formation of a two-phase zone in the interaction of wet rocks with cooled salt solution. Journal of Engineering Physics 55, 1014–1019 (1988). https://doi.org/10.1007/BF00870486
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DOI: https://doi.org/10.1007/BF00870486