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ORIGINAL RESEARCH PAPER

On Leakage and Seepage from Geologic Carbon Sequestration Sites

Unsaturated Zone Attenuation

Earth Sciences Division 90-1116, Lawrence Berkeley National Laboratory, University of California, Berkeley, CA 94720
^* Corresponding author (cmoldenburg{at}lbl.gov).

Received 25 February 2003.

Geologic carbon sequestration is the direct injection of CO₂ into deep geologic formations for permanent disposal. Although numerous trapping mechanisms exist in the subsurface, it is possible that CO₂ will leak from the primary sequestration target and seep out of the ground. The unsaturated zone has the potential to attenuate leaking CO₂ and decrease seepage and near-surface CO₂ concentrations. Attenuation processes include permeability trapping, ponding as dense CO₂ spreads out on the water table, solubility trapping by infiltrating or residual water, and dilution through mixing with ambient soil gas. Numerical simulations of CO₂ flowing upward through a thick model unsaturated zone were performed to investigate the sensitivity of various unsaturated zone properties on CO₂ seepage flux and near-surface CO₂ gas concentrations. These two quantities are considered drivers for health and environmental risk due to exposure to CO₂. For the conceptual model considered, seepage flux and near-surface CO₂ gas concentrations are most strongly controlled by the leakage rate at the water table, followed by the source zone radius. Permeability and permeability anisotropy, as well as porosity and infiltration rate are also important, although to a lesser degree. Barometric pumping causes local maxima in seepage flux and near-surface CO₂ concentrations, but has negligible effect in a time-averaged sense. When the leakage source is turned off, the CO₂ plume attentuates through dissolution into infiltrating water. For the case of a constant leakage rate, the unsaturated zone can attenuate low leakage fluxes but should not be expected to attenuate large CO₂ leakage fluxes.