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In many of the underground CO2 storage sites, the sedimentary reservoirs are not petrologically uniform. Reservoir formations usually comprise high-permeability layers and low-permeability interbeds. Such sedimentary structure has been observed in CO2 storage reservoirs; for example, the Utsira formation, Sleipner, Norway, and also in the Haizume formation, Nagaoka, Japan. During the upward migration...
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