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

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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. 
@article{MM_2010_22_4_a1,
     author = {Yu. M. Laevsky and A. A. Kalinkin},
     title = {Two-temperature simulation of hydrate-bearing rock},
     journal = {Matemati\v{c}eskoe modelirovanie},
     pages = {23--31},
     publisher = {mathdoc},
     volume = {22},
     number = {4},
     year = {2010},
     language = {ru},
     url = {http://geodesic.mathdoc.fr/item/MM_2010_22_4_a1/}
}
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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/