Top-down and bottom-up estimates of CO (sub 2) storage capacity in the United Kingdom sector of the southern North Sea Basin
Top-down and bottom-up estimates of CO (sub 2) storage capacity in the United Kingdom sector of the southern North Sea Basin
Environmental Geosciences (June 2006) 13 (2): 71-84
- Atlantic Ocean
- basins
- Bunter
- carbon dioxide
- clastic rocks
- Europe
- gas injection
- global
- greenhouse effect
- ground water
- industrial waste
- injection
- Leman Sandstone Formation
- Lower Permian
- Lower Triassic
- Mesozoic
- North Atlantic
- North Sea
- oil and gas fields
- Paleozoic
- Permian
- pollution
- porous materials
- remediation
- reservoir rocks
- sandstone
- sedimentary basins
- sedimentary rocks
- simulation
- storage
- storage coefficient
- stratigraphy
- substrates
- Triassic
- United Kingdom
- waste disposal
- Western Europe
- Bunter Sandstone Aquifer
Calculations of the CO (sub 2) storage capacity in the Leman Sandstone Formation and the Bunter Sandstone Formation in the data-rich southern North Sea basin, using structure contour, porosity, and isopach maps and a simulation of CO (sub 2) injection, suggest that their CO (sub 2) storage capacities are approximately 3 and up to 15 Gt CO (sub 2) , respectively. It is recognized that such data are not available for most sedimentary basins, and a simple top-down method of calculating CO (sub 2) storage capacity would be highly desirable from a policy maker's perspective, so that the storage capacity of a basin, region, or jurisdiction could readily be estimated. Therefore, the above estimates were used to calculate the amount of CO (sub 2) stored per unit area and the amount of CO (sub 2) stored per unit of pore volume in the Leman Sandstone and Bunter Sandstone formations. The results were compared to similar calculations, derived from published data, for the Utsira Sand, a CO (sub 2) storage reservoir in the northern North Sea. The mean CO (sub 2) stored per unit area of the formation is 140 kg m (super -2) , and the range is 42-260 kg m (super -2) . The mean CO (sub 2) stored per unit pore volume is 6.3 kg m (super -3) , and the range is 1.8-10.0 kg m (super -3) . Two important factors that vary widely between these three North Sea reservoir formations are the total pore volume in traps and the achievable CO (sub 2) saturation; neither can be determined without detailed data.