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Paper No. 11
Presentation Time: 4:35 PM

SIMULATION OF THE IMPACTS OF FAULTS ON CO2 INJECTION INTO SANDSTONE AQUIFERS


PASALA, Sangeetha Madhuri, Chemical Engineering, University of Utah, 50 S. Central Campus Drive, Room 3290, Salt Lake City, UT 84112-9203, FORSTER, Craig B., (Deceased), College of Architecture and Urban Planning, University of Utah, Salt Lake City, UT 84112, EVANS, James P., Dept. of Geology, Utah State University, 4505 Old Main Hill, Logan, UT 84322-4505 and DEO, Milind, Chemical Engineering, University of Utah, Salt Lake City, UT 84112, james.evans@usu.edu

Numerical flow simulations in the Navajo Sandstone explore how faults affect CO2 sequestration in high-porosity quartz sandstones. We examine regions where nature offers analogs of “successful” storage, and sites where leakage has occurred via fault breaches. Two end-member fault types are considered: low-permeability faults dominated by deformation-band networks, and high-permeability faults dominated by fracture networks in a damage zone adjacent to a clay-rich gouge zone. Equivalent permeability (k) values can range from less than 10-14 m2 (10 md) for deformation-band-dominated faults to greater than 10-12 m2 (1000 md) for fracture-dominated faults, regardless of the permeability of the unfaulted sandstone. Water-CO2 fluid-flow simulations model the injection of CO2 into high-k sandstone (5 x 10-13 m2 or 500 md) with low-k (5 x 10-17 m2 or 0.05 md) or high-k (5 x 10-12 m2 or 5000 md) fault zones that correspond to deformation-band- or fracture-dominated faults, respectively. After 500 days, the CO2 rises to produce an inverted cone of free and dissolved CO2 that spreads laterally away from the injection well. Free CO2 fills ≤ 41% of the pore space behind the advancing CO2 front, where dissolved CO2 is at or near geochemical saturation. The low-k fault zone exerts the greatest impact on the shape of the advancing CO2 front and restricts the dissolved and free CO2 to the region upstream of the barrier. In this high-k aquifer, the high-k fault zone exerts a small influence on the shape of the advancing CO2 front. In lower-permeability aquifers, high-permeability fault zones will become more important as pathways for CO2 to bypass unfaulted sandstone. Although high-permeability fault conduits might lead to reduced sequestration efficiency, aquifer compartmentalization by low-permeability fault barriers may lead to improved efficiency because the barriers restrict lateral CO2 migration and maximize the volume of CO2 emplaced in each fault-bound compartment.
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