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The evolution of woody plants has solved the problem of capture (photosynthesis) and storage (formation of durable cells) at minimal cost.
Subsequently, the study was expanded to understand the effect of caprock permeability and the heterogeneity preserved in the storage formation.
When projects are designed as CCS from the start, there is typically a site evaluation process to review the storage formation according to best practice criteria for CCS.
Thirdly, the nature of the strata underlying the storage formation is critical to the pressure increase in response to the fluid injection.
The approach consists of extracting brine from the storage formation and then re-injecting it so that it mixes with CO2 at depth in the injection well.
This paper demonstrates an approach to identify optimal monitoring designs that minimize the time to first detection of CO2 leakage from a subsurface storage formation.
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As such, detection and characterization of leakage pathways from storage formations into overlying formations are required.
Geological monitoring is mostly related to large scale migration of the injected CO2 in the storage formations.
Relative permeability curves measured on samples from seven potential storage formations are used to illustrate the effect on the CoPs.
Monitoring of geochemical changes induced by CO2 intrusion in freshwater aquifers which are located between storage formations and close-to-surface compartments can enable the early detection of CO2 leakage events and ensure the safety of freshwater resources.
The relative permeability, capillary pressure, and residual trapping determine the rate of CO2 injection, the spread of injected CO2 in subsurface storage formations, and the long-term immobilization of injected fluid after injection has completed.
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