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- W2892862373 abstract "Gas hydrate buried in reservoir rock at low temperature and high pressure conditions is solid clathrate compound in which gas molecules are lodged within ice crystals. Two approaches, increasing the temperature and decreasing the pressure, are commonly used in exploiting gas hydrate. With temperature increasing, phase transition of pore ice will reduce the strength of permafrost. When it occurs, the heat is transferred in the form of specific heat and latent heat. Moreover, the melting point is not constant but depends on the pore size of porous solids. Considering these features, the process of heat transfer of sandstone in situ was governed by heat transfer equation with phase transition. This study addresses the forming conditions of hydrates and establishes a governing equation with phase transition. The process was simulated and discussed through temperature evolution." @default.
- W2892862373 created "2018-10-05" @default.
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- W2892862373 date "2018-09-25" @default.
- W2892862373 modified "2023-10-17" @default.
- W2892862373 title "Heat Transfer in Gas Hydrate Sediment" @default.
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- W2892862373 doi "https://doi.org/10.1007/978-981-13-2306-5_78" @default.
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