Abstract
A two-temperature model for describing the temperature field of a heat source in a hydrate-bearing rock is proposed. For the water/ice phase, the enthalpy formulation of the Stefan problem is used. Numerical simulation is accomplished through the finite element method.
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Original Russian Text © Yu.M. Layevskii, A.A. Kalinkin, 2010, published in Matematicheskoe Modelirovanie, 2010, Vol. 22, No. 4, pp. 23–31.
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Layevskii, Y.M., Kalinkin, A.A. A two-temperature model of hydrate-bearing rock. Math Models Comput Simul 2, 753–759 (2010). https://doi.org/10.1134/S2070048210060104
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DOI: https://doi.org/10.1134/S2070048210060104