EVALUATION OF POTENTIAL GEOLOGIC CARBON DIOXIDE SEQUESTRATION SITES: TRAP VALIDATION CONCEPTS FROM THE PETROLEUM INDUSTRY
Characteristics of successful hydrocarbon traps that are applicable to subsurface carbon dioxide storage include presence of a porous and permeable reservoir, a geometric trapping configuration of the reservoir, and a robust seal envelope (base, lateral, and top seal) that can maintain a buoyant fluid column over geologically significant periods of time. Identification of a geologic trap, which may comprise both stratigraphic and structural trapping elements, is the first step in the investigation. The second step is to analyze the geologic seal around a trap. Elements of seal to be considered include seal mechanical strength, seal capillary entry pressure, and fault leak. The mechanical capacity of a seal is compromised when the absolute pressure of the non-aqueous phase on the seal unit exceeds either its opening mode tensile strength or the minimum stress. In contrast, capillary seal failure occurs when the buoyant pressure of the non-aqueous phase exceeds the capillary entry pressure of the seal, a function of seal pore throat size, interfacial tension, and wetting properties. Fault seal for long time periods is primarily a matter of what rock type is juxtaposed with the reservoir rock across a fault.
The best forward prediction of carbon dioxide storage capacity over the long-term will result from full integration of fluid and bed seal properties, fracture gradients, and structural and stratigraphic models. Such a prediction requires simultaneous evaluation of all elements that control fill capacity. Confidence may be improved in petroliferous basins that have been “leak-tested” by hydrocarbons, or where other traps along a leak pathway will capture carbon dioxide escaped from the injection site. Implementation of this integrated approach will help identify safe long-term carbon dioxide storage sites and assist in the management of any commissioned site.