Citation: | YANG Pu, FANG Xiaoyu, WANG Ziwen, HUANG Shirui, LYU Yanxin, YANG Bo. The impact of water injection simulation on CO2 storage capacity in offshore saline aquifers[J]. Marine Geology Frontiers, 2025, 41(3): 99-106. doi: 10.16028/j.1009-2722.2024.237 |
Continuous or alternating water injection into saline aquifers can accelerate CO2 dissolution and increase the safety of CO2 storage. However, the hydrodynamic effect may interfere with the development of CO2 plumes, affecting indirectly the actual storage capacity of the aquifer, to which available engineering solution remain very limited. We studied the potential water injection strategies and the influence of key operational parameters on the storage safety and capacity during CO2 injection using a single well in an open saline aquifer. Results show that continuous water injection above the gas injection layer after a certain period could enhance significantly the storage intensity and increase the capacity. The early the water injection starts, the better the results. The storage capacity increases with the increase in water injection rate during gas injection. The temporal effect of water injection post gas injection on storage capacity needs to be evaluated case by case. Under a given total water injection volume, high-rate water injection during gas injection is more effective to enhance the storage capacity than low-rate and prolonged water injection. Reducing the spatial interval between the water injection layer and gas injection layer could enhance the actual storage capacity. Meanwhile, water injection could effectively reduce the CO2 saturation near the injection well, and mitigate the risk of wellbore leakage.
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Development and evolution process of CO2 plume in saline aquifer
Plan view of grid used for simulation
Comparison of plume distribution under different base conditions
Variation in storage intensity in different water injection schemes
Numerical simulation of CO2 storage capacity of various storage mechanisms in saline aquifer for 100 years
Plume distribution of CO2 in saline aquifer after 100 years of sequestration for Scheme 1
Plume distribution after 20 years of CO2 injection and 100 years of sequestration for Scheme 1
Variation in storage intensity with different water injection parameters
Evolution process of CO2 solubility trapping in different schemes
Curve of CO2 plume area growth over time at the top of the saline aquifer
Comparison of plume distribution on the wellbore profile at the end of CO2 injection