Geodesic
Two-temperature simulation of hydrate-bearing rock
Matematičeskoe modelirovanie, Tome 22 (2010) no. 4, pp. 23-31.

Voir la notice de l'article provenant de la source Math-Net.Ru

Two-temperature mathematical model for a description of the temperature field of the heat source in hydrate-bearing rock is proposed. For the phase “water/ice” enthalpy form of the Stephan problem is used. Numerical model is implemented within finite element method.
Keywords: two-temperature model, finite element method, the Stephan problem. 
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Yu. M. Laevsky; A. A. Kalinkin. Two-temperature simulation of hydrate-bearing rock. Matematičeskoe modelirovanie, Tome 22 (2010) no. 4, pp. 23-31. http://geodesic.mathdoc.fr/item/MM_2010_22_4_a1/

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