
This study analyzes the migration and dissolution of CO2 plumes in a stratified saline aquifer, with particular emphasis on how sandstone–shale system influences CO2 diffusion and dissolution. The cover illustration depicts the lateral and vertical spreading of CO2 plumes from the injection point, the buoyant rise, and accumulation beneath low-permeability shale. The magnified view on the right highlights that porosity and heterogeneity markedly reshape saturation patterns and plume fronts. Higher porosity promotes local accumulation, but limits radial advance, whereas higher permeability tends to extend the dissolution front. Together, the results illustrate how reservoir properties govern CO2 migration and dissolution efficiency in layered aquifers.
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