--> Abstract: Evaluating Seal Capacity of Caprocks and Intraformational Barriers for Carbon Dioxide Containment, by Richard (Ric) Daniel and John Kaldi; #90082 (2008)
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Evaluating Previous HitSealNext Hit Capacity of Caprocks and Intraformational Barriers for Carbon Dioxide Containment

Richard (Ric) Daniel and John Kaldi
Cooperative Research Centre for Greenhouse Technologies, at the Australian School of Petroleum, The University of Adelaide, Adelaide, SA, Australia

The petrophysical properties of cap rocks and intraformational barriers can constrain the CO2 containment volumes of potential geosequestration sites and requires an understanding of the Previous HitsealNext Hit capacity, which is the capillary pressure at which a trapped fluid commences to leak or move through a Previous HitsealNext Hit rock. Previous HitSealNext Hit rocks are effective because of very fine pore and pore-throat sizes that result in low porosities and permeabilities, which in turn generate high capillary threshold pressures. These pressures, together with wettability and interfacial tension (IFT) properties, determine the final column height that a Previous HitsealNext Hit can support. A review is presented on the role of wettability and IFT in the geological storage of CO2 and its effect on Previous HitsealNext Hit capacity (CO2 column height) with respect to capillary pressure, the potential for the movement of CO2 through the Previous HitsealNext Hit and the effect on reservoir storage volumes.

Mercury injection capillary pressure analysis has been used extensively in the petroleum industry to determine the effectiveness of the top Previous HitsealNext Hit in relation to hydrocarbon column height retention. With the burgeoning interest in geological storage of carbon dioxide (CO2), this technology can be applied to establish the suitability of a top Previous HitsealTop for containment of CO2; however, the role of IFT and wettability in the CO2-water-rock systems is not well understood. It is unclear how supercritical CO2 (scCO2) effects these two properties, especially as the water front becomes saturated with scCO2 and eventually becomes miscible with the scCO2 at reservoir conditions.

Literature-to-date shows that wettability and IFT of the CO2-water-rock system may be more significant than in the hydrocarbon-water-rock systems and that calculated CO2 column heights based on non-wetting assumptions could result in column heights being as much as 50% less than otherwise predicted.

AAPG International Conference and Exhibition, Cape Town, South Africa 2008 © AAPG Search and Discovery