Abstract:
Objective To clarify the potential impacts of large-scale CO2 injection and the leakage of injected CO2 along with reservoir brine on shallow groundwater, thereby supporting risk prevention and control for leakage in CO2 geological storage projects and the protection of shallow groundwater.
Methods This paper employs the literature analysis method to systematically summarize research progress on the impacts of large-scale CO2 geological storage injection and reservoir fluid leakage migration on shallow groundwater flow fields and water quality.
Results Large-scale CO2 injection leads to reservoir pressure accumulation and pressure disturbance transmission into shallow aquifers, resulting in phenomena such as rising groundwater levels, increased pressure, and enhanced evapotranspiration. The leakage of CO2 or reservoir brine to shallow aquifers can lead to a decrease in pH and ORP, an increase in parameters such as alkalinity and electrical conductivity, elevated concentrations of major ions like Ca-Mg-K, release and migration of toxic trace metals, and alterations in the biodiversity and metabolic diversity of microbial communities. These complex biogeochemical processes are influenced by factors such as the intensity of CO2 or reservoir brine leakage and the hydrogeological conditions of the shallow aquifer. Adsorption and desorption, dissolution and precipitation, and redox reactions are the primary mechanisms governing changes in groundwater quality following CO2 intrusion .
Conclusions Shallow groundwater serves not only as a risk receptor for potential leakage in CO2 geological storage projects but also as an information carrier for assessing storage safety and effectiveness. Therefore, greater emphasis should be placed on researching the impacts and monitoring of shallow groundwater in large-scale CO2 geological storage projects, both to prevent environmental incidents and to provide support for verifying storage effectiveness .
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