scholarly journals Micromechanical Investigation of Stress Relaxation in Gas Hydrate-Bearing Sediments Due to Sand Production

Energies ◽  
2019 ◽  
Vol 12 (11) ◽  
pp. 2131 ◽  
Author(s):  
Eitan Cohen ◽  
Assaf Klar ◽  
Koji Yamamoto

Past experience of gas production from methane-hydrate-bearing sediments indicates that sand migration is a major factor restricting the production of gas from methane-hydrate reservoirs. One important geotechnical aspect of sand migration is the influence of grain detachment on the existing stresses. This paper focuses on understanding and quantifying the nature of this aspect using different approaches, with a focus on discrete element method (DEM) simulations of sand detachment from hydrate-bearing sand samples. The investigation in the paper reveals that sand migration affects isotropic and deviatoric stresses differently. In addition, the existence of hydrate moderates the magnitude of stress relaxation. Both of these features are currently missing from continuum-based models, and therefore, a new constitutive model for stress relaxation is suggested, incorporating the research findings. Model parameters are suggested based on the DEM simulations. The model is suitable for continuum mechanics-based simulations of gas production from hydrate reservoirs.

Author(s):  
Ah-Ram Kim ◽  
Gye-Chun Cho ◽  
Joo-Yong Lee ◽  
Se-Joon Kim

Methane hydrate has been received large attention as a new energy source instead of oil and fossil fuel. However, there is high potential for geomechanical stability problems such as marine landslides, seafloor subsidence, and large volume contraction in the hydrate-bearing sediment during gas production induced by depressurization. In this study, a thermal-hydraulic-mechanical coupled numerical analysis is conducted to simulate methane gas production from the hydrate deposits in the Ulleung basin, East Sea, Korea. The field-scale axisymmetric model incorporates the physical processes of hydrate dissociation, pore fluid flow, thermal changes (i.e., latent heat, conduction and advection), and geomechanical behaviors of the hydrate-bearing sediment. During depressurization, deformation of sediments around the production well is generated by the effective stress transformed from the pore pressure difference in the depressurized region. This tendency becomes more pronounced due to the stiffness decrease of hydrate-bearing sediments which is caused by hydrate dissociation.


Energy ◽  
2019 ◽  
Vol 166 ◽  
pp. 1106-1119 ◽  
Author(s):  
Yongchang Feng ◽  
Lin Chen ◽  
Anna Suzuki ◽  
Takuma Kogawa ◽  
Junnosuke Okajima ◽  
...  

Energy ◽  
2015 ◽  
Vol 82 ◽  
pp. 686-696 ◽  
Author(s):  
Piyush Bhade ◽  
Jyoti Phirani

2019 ◽  
Vol 184 ◽  
pp. 194-204 ◽  
Author(s):  
Yongchang Feng ◽  
Lin Chen ◽  
Anna Suzuki ◽  
Takuma Kogawa ◽  
Junnosuke Okajima ◽  
...  

2016 ◽  
Vol 108 ◽  
pp. 439-445 ◽  
Author(s):  
Yoshihiro Konno ◽  
Yoshihiro Masuda ◽  
Koya Akamine ◽  
Motoyoshi Naiki ◽  
Jiro Nagao

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