a Project Center for Energy Transition and ESG, Skolkovo Institute of Science and Technology (Skoltech), Bolshoy Boulevard 30, bld. 1, Moscow, 121205,
Russia
b Institute of Physics of the Earth, Russian Academy of Sciences, B. Gruzinskaya st., 10, Moscow, 123995, Russia
c Gazpromneft Science & Technology Center, 75-79 liter D Moika River Emb., St Petersburg, 190000, Russia
d Institute of Mechanics, Moscow State University, Michurinsky Pr., 1, Moscow, 119192, Russia
e Department of Civil and Resource Engineering, Dalhousie University, 1360 Barrington Street, Halifax, B3H 4R2, Nova Scotia, Canada
2025, 17(4): 1986-2008. doi:10.1016/j.jrmge.2024.04.016
Received: 2023-12-30 / Revised: 2024-04-22 / Accepted: 2024-04-27 / Available online: 2024-07-05
2025, 17(4): 1986-2008.
doi:10.1016/j.jrmge.2024.04.016
Received: 2023-12-30
Revised: 2024-04-22
Accepted: 2024-04-27
Available online: 2024-07-05
We study CO2 injection into a saline aquifer intersected by a tectonic fault using a coupled modeling approach to evaluate potential geomechanical risks. The simulation approach integrates the reservoir and mechanical simulators through a data transfer algorithm. MUFITS simulates non-isothermal multiphase flow in the reservoir, while FLAC3D calculates its mechanical equilibrium state. We accurately describe the tectonic fault, which consists of damage and core zones, and derive novel analytical closure relations governing the permeability alteration in the fault zone. We estimate the permeability of the activated fracture network in the damage zone and calculate the permeability of the main crack in the fault core, which opens on asperities due to slip. The coupled model is applied to simulate CO2 injection into synthetic and realistic reservoirs. In the synthetic reservoir model, we examine the impact of formation depth and initial tectonic stresses on geomechanical risks. Pronounced tectonic stresses lead to inelastic deformations in the fault zone. Regardless of the magnitude of tectonic stress, slip along the fault plane occurs, and the main crack in the fault core opens on asperities, causing CO2 leakage out of the storage aquifer. In the realistic reservoir model, we demonstrate that sufficiently high bottomhole pressure induces plastic deformations in the near-wellbore zone, interpreted as rock fracturing, without slippage along the fault plane. We perform a sensitivity analysis of the coupled model, varying the mechanical and flow properties of the storage layers and fault zone to assess fault stability and associated geomechanical risks.
Keywords: CO2 storage, Reservoir simulator, Mechanical simulator, Tectonic fault, Fault slip, Plastic deformations, Integrity loss, CO2 leakage
Evgenii Kanin
Evgenii Kanin obtained his BSc (2016) and MSc (2018) in applied physics and mathematics from Moscow Institute of Physics and Technology and MSc in petroleum engineering from Skolkovo Institute of Science and Technology (Skoltech) in 2019. He completed his PhD in Petroleum Engineering at Skoltech in 2022, defending the dissertation “Asymptotic Models of Coupled Geomechanics/Fluid Mechanics Phenomena of Hydraulic Fracture Growth”. Currently, Evgenii is a research scientist at the Project Center for Energy Transition and ESG at Skoltech, where he conducts research in the area of decarbonization and energy transition. His research interests include fluid mechanics, geomechanics, CO2 sequestration, mechanics of hydraulic fractures, and multiphase flow modeling.