What to do with CO 2 – the knowns and unknowns of geologic sequestration and CO 2 EOR in greenhouse gas context Susan Hovorka, Gulf Coast Carbon Center,

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What to do with CO 2 – the knowns and unknowns of geologic sequestration and CO 2 EOR in greenhouse gas context Susan Hovorka, Gulf Coast Carbon Center, Bureau of Economic Geology, Jackson School of Geosciences, The University of Texas at Austin Presented to Austin Professional Landmen's Association May 30, 2008 Austin, TX

CO 2 Increasing in the Atmosphere CO 2 is produced by burning fossil fuels CO 2 has been building up in the atmosphere during the industrial revolution As more people world-wide improve their standard of living, the amount of CO 2 released will increase, causing additional build-up in the atmosphere Recent increase in CO 2 concentration

Risks from CO 2 Build-up in the Atmosphere Recent increase in average global temperature CO 2 is one of the greenhouse gases that control how much of the solar energy that hits the Earth is retained as heat. Higher atmospheric concentrations of CO 2 will force the climate toward warmer average global conditions. Risks associated with warmer climate include coastal flooding, more severe tropical storms, desertification, and increased width of tropics.

US Gulf Coast: Unique risks from greenhouse Gas emission Unique contribution to the solution Southeast US is vulnerable to damage resulting from climate change –Hurricane landfall around Gulf of Mexico –Risk of tropical species invasion –Much of US low relief coastline – inundation by sea level rise Southeast has unique sequestration potential –Energy industry center (refinery and oil production) –Very well known, thick wedge of high permeability sandstones, excellent seals –Initiated by CO 2 EOR Anthropogenic sources overlie thick subsurface Flooded by 50 ft sea level rise Fire ant Invasion, USDA SECARB lead by Southern States Energy Board Funded by DOE - NETL

Options to Reduce CO 2 in the Atmosphere Conservation and energy efficiency Fuel switching—e.g., natural gas for coal Alternative energy—e.g., wind, solar, nuclear Terrestrial sequestration—e.g., rainforest preservation, tree farms, no-till farming. Ocean disposal Mineral sequestration Geologic storage” sequestration” “Novel concepts” Which Is Best? To reduce the large volumes of CO 2 that are now and will be in the future released to the atmosphere, multiple options must be brought to maturation.

To reduce CO 2 emissions to air from point sources.. Carbon extracted from a coal or other fossil fuel… is currently burned and emitted to air CO 2 is shipped as supercritical fluid via pipeline to a selected, permitted injection site CO 2 injected at pressure into pore space at depths below and isolated (sequestered) from potable water. CO 2 stored in pore space over geologically significant time frames. Geologic Sequestration (Storage) of Carbon – Put it back Return it to the Earth where it came from

Assuring CO 2 Stays Underground Capture Land surface > 800 m Underground Sources of Drinking Water Injection Zone Seal = capillary or pressure barrier to flow CO 2 Seal limits CO 2 rise under buoyancy

Complex! Monitoring to Assure that CO 2 remains where it is placed Atmosphere –Ultimate receptor but dynamic Biosphere –Assurance of no damage but dynamic Soil and Vadose Zone –Integrator but dynamic Aquifer and USDW –Integrator, slightly isolated from ecological effects Above injection monitoring zone –First indicator, monitor small signals, stable. In injection zone - plume –Oil-field type technologies. Will not identify small leaks In injection zone - outside plume –Assure lateral migration of CO 2 and brine is acceptable Aquifer and USDW Atmosphere Biosphere Vadose zone & soil Seal Monitoring Zone CO 2 plume Pressure monitoring “box”

GCCC Field Tests for Monitoring and Verification Technologies DOE NETL support SECARB Phase II&II Cranfield Frio Test Site SACROC Southwest Partnership NM Tech

Cranfield unit boundary Oil ring Gas cap Sonat CO2 pipeline Denbury early injectors Denbury later Injectors shown schematically CO 2 used for EOR – bringing old fields back to life Example Denbury Cranfield unit, MS Unit boundary

CO 2 Sequestration Capacity in Miscible Oil Reservoirs along the Gulf Coast Bureau of Economic Geology Mark Holtz 2005 NATCARB Atlas 2007 Estimated annual regional point source CO 2 emissions

Cranfield unit boundary Oil ring Gas cap Sonat CO2 pipeline Denbury early injectors Denbury later Injectors shown schematically Saline aquifer within Cranfield unit End of EOR: using space for sequestration of CO 2 Example Denbury Cranfield unit, MS

Injection into a down-dip brine- very large volumes CO 2 plume

Role of EOR in Sequestration Volume of CO 2 Time EOR Brine sequestration EOR Significant volumes: only a fraction of all point source CO 2 can be sold for EOR Offset some of cost of capture Pipeline development, site characterization Public acceptance

Evolution from EOR to storage in brine: increase in volume of subsurface used CO 2 plumeElevated pressure CO 2 injection (no production) pressure plume extends beyond the CO 2 injection area In EOR CO 2 injection is approximately balanced by oil, CO 2, and brine production no pressure plume beyond the CO 2 injection area Elevated pressure

How does EOR compare to brine sequestration? EOR Recycle with production Confined area –Trap –Pressure control Residual oil- CO2 very soluble Many well penetrations = leakage risk Brine Reservoir Pure storage Large area –May not use a trap –Pressure area increase Brine – Co2 weakly soluble Few well penetrations = lower confidence

Issues where Landman expertise is needed Ownership and process for leasing pores space –Early projects: CO2 EOR –Evolution to CO2 storage Who owns the pore space? How is permission to inject and add pressure obtained?

Two areas are involved in sequestration Injection well Plume of injected CO 2 Footprint of area over CO 2 Footprint of area of elevated pressure What area is leased? 1 2

Monitoring Goals For Commercial Sequestration Show that: Storage capacity and injectivity are sufficient for the volume via history match between observed and modeled CO 2 will be contained in the target formation not damage drinking water or be released to the atmosphere Know aerial extent of the plume elevated pressure effects compatible with other uses minimal risk to resources, humans, & ecosystem Advance warning of hazard allow mitigation if needed Public acceptance provide confidence in safe operation Modified from J. Litynski, NETL

Gulf Coast Carbon Center (GCCC) GCCC Research Team: Susan Hovorka, Tip Meckel, J. P. Nicot, Ramon Trevino, Jeff Paine, Becky Smyth; Post-docs and students Associate Director Ian Duncan Director Scott Tinker