A Fully Coupled Thermo-Hydro-Mechanical Model For Methane Hydrate Reservoir Simulations

Author(s):  
Huo-Lang Fang
2018 ◽  
Author(s):  
Saurav Parashar ◽  
Raghvendra Pratap Singh ◽  
Malay Kumar Das

2001 ◽  
Author(s):  
Jinghong Fan

Abstract A three-dimensional, meso-electro-mechanical model has been formulated for description of PMN-PT-BT ceramics. Unlike the experimentally fit models and phenomenological models which are based on state variables and/or empirical relationships, this fully coupled, computational mesomechanics model for polycrystalline PMN-PT-BT ceramics is developed based on considerations of constitutive behavior of single crystals. Specifically, domain wall nucleation and evolution rate equations are proposed in this work to describe the nonlinear hysteresis behavior of these ceramics near the phase transition temperature with maximum permittivity.


2011 ◽  
Author(s):  
Than Tin Aung ◽  
Satoshi Noguchi ◽  
Nobutaka Oikawa ◽  
Takayuki Kanno ◽  
Machiko Tamaki ◽  
...  

Energy ◽  
2019 ◽  
Vol 166 ◽  
pp. 834-844 ◽  
Author(s):  
Tao Yu ◽  
Guoqing Guan ◽  
Abuliti Abudula ◽  
Akihiro Yoshida ◽  
Dayong Wang ◽  
...  

2002 ◽  
Vol 24 (6) ◽  
pp. 499-512 ◽  
Author(s):  
Wonmo Sung ◽  
Hoseob Lee ◽  
Huen Lee ◽  
Chulsoo Lee

Entropy ◽  
2020 ◽  
Vol 22 (11) ◽  
pp. 1212 ◽  
Author(s):  
Bo Li ◽  
Wen-Na Wei ◽  
Qing-Cui Wan ◽  
Kang Peng ◽  
Ling-Ling Chen

The purpose of this study is to analyze the dynamic properties of gas hydrate development from a large hydrate simulator through numerical simulation. A mathematical model of heat transfer and entropy production of methane hydrate dissociation by depressurization has been established, and the change behaviors of various heat flows and entropy generations have been evaluated. Simulation results show that most of the heat supplied from outside is assimilated by methane hydrate. The energy loss caused by the fluid production is insignificant in comparison to the heat assimilation of the hydrate reservoir. The entropy generation of gas hydrate can be considered as the entropy flow from the ambient environment to the hydrate particles, and it is favorable from the perspective of efficient hydrate exploitation. On the contrary, the undesirable entropy generations of water, gas and quartz sand are induced by the irreversible heat conduction and thermal convection under notable temperature gradient in the deposit. Although lower production pressure will lead to larger entropy production of the whole system, the irreversible energy loss is always extremely limited when compared with the amount of thermal energy utilized by methane hydrate. The production pressure should be set as low as possible for the purpose of enhancing exploitation efficiency, as the entropy production rate is not sensitive to the energy recovery rate under depressurization.


2010 ◽  
Vol 75 (1) ◽  
pp. 72-83 ◽  
Author(s):  
Hisanao Ouchi ◽  
Masanori Kurihara ◽  
Akihiko Sato ◽  
Yoshihiro Masuda ◽  
Hideo Narita ◽  
...  

2010 ◽  
Vol 126 (4/5) ◽  
pp. 138-147
Author(s):  
Yasuhide SAKAMOTO ◽  
Hironori HANEDA ◽  
Taro KAWAMURA ◽  
Norio TENMA ◽  
Kazuo AOKI ◽  
...  

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