Geomechanical response of permafrost-associated hydrate deposits to depressurization-induced gas production

• Published in: Journal of Petroleum Science and Engineering
• Main Authors: Rutqvist, J., Moridis, G.J., Grover, T., Collett, T.
• Other Authors: Lawrence Berkeley National Laboratory. Earth Sciences Division.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Lawrence Berkeley National Laboratory 2009
• Subjects: Canada; 58; Sediments; Layers; 54; Zones; Deposits; Hydrates; Simulation; Wells; Thermodynamics; Depth; Production; Failures; Stresses; Overburden; Depressurization; Dissociation; Permafrost; Shear; Alaska; Northwest Territories; permafrost
• Online Access: https://doi.org/10.1016/j.petrol.2009.02.013; https://digital.library.unt.edu/ark:/67531/metadc932396/

In this simulation study, we analyzed the geomechanical response during depressurization production from two known hydrate-bearing permafrost deposits: the Mallik (Northwest Territories, Canada) deposit and Mount Elbert (Alaska, USA) deposit. Gas was produced from these deposits at constant pressure using horizontal wells placed at the top of a hydrate layer (HL), located at a depth of about 900 m at the Mallik and 600 m at the Mount Elbert. The simulation results show that general thermodynamic and geomechanical responses are similar for the two sites, but with substantially higher production and more intensive geomechanical responses at the deeper Mallik deposit. The depressurization-induced dissociation begins at the well bore and then spreads laterally, mainly along the top of the HL. The depressurization results in an increased shear stress within the body of the receding hydrate and causes a vertical compaction of the reservoir. However, its effects are partially mitigated by the relatively stiff permafrost overburden, and compaction of the HL is limited to less than 0.4%. The increased shear stress may lead to shear failure in the hydrate-free zone bounded by the HL overburden and the downward-receding upper dissociation interface. This zone undergoes complete hydrate dissociation, and the cohesive strength of the sediment is low. We determined that the likelihood of shear failure depends on the initial stress state as well as on the geomechanical properties of the reservoir. The Poisson's ratio of the hydrate-bearing formation is a particularly important parameter that determines whether the evolution of the reservoir stresses will increase or decrease the likelihood of shear failure.