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FutureGen in Kentucky A slide show explaining a KGS preliminary assessment of geologic sequestration potential for future power plants in Kentucky
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FutureGen is a DOE program to design a power plant that will integrate advanced coal gasification to produce hydrogen and electric power with CO2 capture and storage (also called sequestration)
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FutureGen in Kentucky Geologic sequestration potential
Why FutureGen? Concerns about climate change resulting in a need to reduce CO2 emissions FutureGen will be a near-zero emissions power plant funded by DOE and industry FutureGen will incorporate geologic carbon sequestration to reduce CO2
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Limiting future carbon emissions from power plants is a critical component of DOE- sponsored energy research including FutureGen. “the captured CO2…would then be permanently sequestered in a geologic formation.” Validating the integrated operation of gasification technology Proving effectiveness, permanence, and safety of sequestration in a geologic formation From the DOE FutureGen fact sheet: Major goals include:
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The Kentucky Geological Survey is part of three Phase II partnerships
Midwest Regional Carbon Sequestration Partnership Midwest (Illinois Basin) Geological Sequestration Consortium Southeast Regional Carbon Sequestration Partnership More info at DOE’s
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Geologic carbon sequestration possibilities
After Harper (2004) Unmineable coals Organic-rich shales Depleted oil and gas reservoirs Deep saline aquifers Power plant Pipeline Multiple options at different locations Regional DOE partnerships are assessing several types of geologic reservoirs Enhanced oil and gas recovery may be possible for unmineable coals, organic-rich shales, and depleted oil and gas reservoirs
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Geologic carbon sequestration possibilities
FutureGen Unmineable Coal Beds Injection into unmineable coal beds might allow secondary recovery of methane in some (not all) areas Images modified from Midwest Regional Carbon Sequestration Partnership (2005)
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Geologic carbon sequestration possibilities
FutureGen Oil and Gas Reservoirs Injection into depleted oil or gas reservoirs might allow secondary recovery of oil or gas Images modified from Midwest Regional Carbon Sequestration Partnership (2005)
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Geologic carbon sequestration possibilities
FutureGen Deep Saline Aquifers Injection into deep saline aquifers offers possibility of storage without negating a potential resource Images modified from Midwest Regional Carbon Sequestration Partnership (2005)
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Geologic carbon sequestration possibilities
Minimal transport distance Minimal transport distance Multiple reservoirs Power plant Pipeline Enough depth to minimize leakage and to keep CO2 in supercritical phase Coals + Oil and gas reservoirs + Saline aquifers After Harper (2004) Optimal sites might have multiple reservoirs (stacked or at several locations) at depth, within some distance of the plant based on the transport costs of CO2
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Geologic carbon sequestration possibilities
FutureGen Preliminary requirements: Large storage volume For a FutureGen–type plant, DOE estimates 1 million tons CO2 /year for 30 years = 30 million tons CO2 Could be one large or multiple reservoirs Image modified from Midwest Regional Carbon Sequestration Partnership (2005)
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Geologic carbon sequestration possibilities
FutureGen Preliminary requirements: Depth (> 2,500’) for existing depleted oil and gas reservoirs In our area, this is the depth needed to keep any injected CO2 in liquid form (miscible)* Injection into unmineable coals could be shallower because of a different sequestration mechanism Image modified from Midwest Regional Carbon Sequestration Partnership (2005) * Greater depth also provides more seals to prevent leakage
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Geologic carbon sequestration possibilities
FutureGen Preliminary requirements: Proximity to existing energy infrastructure and likely a waterway Most existing KY power plants are near large rivers Image modified from Midwest Regional Carbon Sequestration Partnership (2005)
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Existing and proposed power plants
Existing power plants Proposed plants Most along rivers Power plant siting involves many non-geologic decisions By using existing plant locations to define the study area we incorporated those decisions with the geologic assessment.
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Existing and proposed power plant counties
Existing power plants Proposed plants Future power plants are likely to have at least the existing requirements relative to water. Study area limited to counties with known and proposed plants, similar water supplies, or large coal resources* *these might not have water needs for some types of plants
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Existing and proposed power plant counties
Existing power plants Proposed plants Areas might include a 25-mile radius around existing and proposed plants as examples of hypothetical transport areas around each Circles show possibility for pipeline transport
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Existing and proposed power plant counties
NATCARB Pipeline cost calculator Result Cost is: $2,860,898 Distance is: 28 miles The reason for examining the radius around some areas is that pipeline transport to a sequestration site might be needed.
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Seismicity Seismic potential is greatest in far western Kentucky
Magnitude Peak ground acceleration >0.3g 3.0 4.0 5.0 + Seismic potential is greatest in far western Kentucky Seismic potential may be concern for building future large, Federally funded (or co-funded) construction projects Faults (red lines) will also need to be considered (not for seismic potential but for reservoir leakage and seal potential)
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Kentucky “unmineable” coal potential
2003 Coal production (Mt) 15+ No production in study area 10-15 5-10 1-5 0-1 Kentucky has two coal fields (the Eastern Kentucky Coal Field and the Western Kentucky Coal Field) Coal is mined at 1000 ft in western Kentucky Coal is mined at depths beneath surface of more than 1000 ft in eastern Kentucky, but in some places that is still “above drainage”
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Kentucky “unmineable” coal potential
Areas with multiple deep coals below drainage Gray: Coals > 500 ft deep Red: Coals > 1,000 ft deep Surface fracturing extends 400 to 500 feet beneath the surface, so potential coals would need to be at least 500 feet beneath drainage Areas of coals at depth are smaller than the total area of the coal fields Definition of “unmineable” is variable and will influence potential
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Known Kentucky oil and gas reservoirs
Operating and abandoned oil and gas fields Oil Gas Waterflood Kentucky has hundreds of oil and gas fields Not all are within the electric power infrastructure area Not all fields are likely sequestration targets
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Known Kentucky oil and gas reservoirs
Fields with sufficient depth or volume Volumes >15 MM tons (20 fields) 2,500 ft or deeper Known fields have demonstrated reservoir and trap properties 9 have >30 MM tons estimated capacity for CO2 storage Many of these fields are not abandoned
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Known Kentucky oil and gas reservoirs
Western KY Central KY Eastern KY Oil field (generalized) Gas field (generalized) 2,500 feet Kentucky’s geology controls the depth of the known oil and gas fields. Major oil- and gas-bearing units are shallower than 2,500 feet in the central part of the state. There are speculative possibilities deeper.
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Additional potential oil and gas reservoirs
Organic shales: a different type of potential CO2 reservoir Red has most potential Blue has least potential Tan has no potential KGS is currently funded by DOE to investigate the potential of black (organic-rich) shales to adsorb CO2 as a sequestration mechanism The black shales are widespread with large potential capacity Not a proven CO2 sequestration reservoir; behaves like coals
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Kentucky potential deep saline reservoirs
Deep sands (saline aquifers) Net Sand Thickness Red is thickest Blue is thinnest Tan is no sand DOE partnerships have shown that deep saline aquifers (mostly sandstone) have greatest potential for large storage volume Possible cumulative thickness is > 800 ft in western KY Limited well penetrations and reservoir data in KY
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Rock units beneath Kentucky
“Vuggy” Copper Ridge Rose Run Strata vary in characteristics Some are known reservoirs Some are potential reservoirs Some are seals Deep saline reservoirs shown with arrows Mt. Simon Rome sands Middle Run/ Four Sand Diagram from MRCSP research St. Peter
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Kentucky potential deep saline reservoirs
Mount Simon Sandstone Isopach Map No Mt. Simon south of the Kentucky River and Rough Creek FZs Based on ~20 wells Potential for as much as 6 Bmt capacity
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Kentucky potential deep saline reservoirs
Thick, Porous Rome Sandstone Wedge ( up to 700’ thick) Contour Interval = 50 ft Deep sands south of the Kentucky River Fault Zone
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Kentucky potential deep saline reservoirs
150 ft contour interval Top Conasauga Structure Map Possibility for closed structure traps in Rome Trough Depth here 4,000 to 5,000 ft Potential capacity 3.5 Bmt CO2
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Kentucky potential deep saline reservoirs
Middle Run (“4 Sand”) Reservoir N S 3 4 S 4 1mi 5 Precambrian Unconformity Paleozoic “4 Sand” (4S) is a mappable seismic sequence Reflection seismic will be needed for sequestration site evaluations and for monitoring after CO2 injection
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Kentucky potential deep saline reservoirs
Middle Run (“4 Sand”) Reservoir 81 sq. mi. lens in Hart Co. Averages 440 ft. thick 7,000-9,500 feet depth ~3 Bmt potential capacity Are there other similar lenses? Additional study needed N 100 ft contour interval
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Assessment of carbon sequestration options along the power plant infrastructure areas
Seismic concern area Next we will compare the infrastructure area (in tan) to the number of known and speculative sequestration options by county
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Areas with known oil and gas field options
Outside study area Study area (no large oil and gas fields)* 1 option 2 options This area is away from large water supplies Known = O&G fields >15 MM tons O&G fields >2,500’ deep Areas with no “known” options do have potential/speculative options.
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Areas with known and possible/speculative geologic options
Outside study area Fewest (1) Most (6) Based on: O&G fields >15 MM tons O&G fields >2,500’ deep Coals below 1,000 ft Number of deep sands Potential in black shale Other speculative reservoirs
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Preliminary Summary There are areas with multiple sequestration options in both eastern and western KY along existing river corridors or within coal fields for short fuel-transport distances There are known and more speculative (but possible) reservoir options in the same regions
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Preliminary Summary All reservoirs would need further testing to determine reservoir characteristics (permeability, water chemistry, etc.) for reservoir modeling Permitting and regulations for test (small quantity) and future large quantity CO2 injections will be important in determining the potential future application of this technology in Kentucky
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Potentially, some of the best areas for sequestration in saline formations (at depth) near power plants Best Good Thick, but deep Thin and/or shallow Based on: Thickness of Mt. Simon Depth of Mt. Simon Depth of vuggy Copper Ridge Thickness of Rome Ss. Depth of Rome Ss St. Peter and Rose Run Ss Thickness of Middle Run Ss Depth of Middle Run Ss More explanation follows
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Potentially, some of the best areas for sequestration in saline formations (at depth) near power plants Best Good Thick, but deep Thin and/or shallow Best here, is the area in the river corridor that had the most options at optimal depths, i.e. moderately deep (5,000-8,000 ft) and thick ( ft) Mt. Simon Sandstone and thin St. Peter (<60 ft) and Rose Run (<80 ft) at moderate depth (3,000-4,000 ft)
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Potentially, some of the best areas for sequestration in saline formations (at depth) near power plants Best Good Thick, but deep Thin and/or shallow Good here, are the areas in the infrastructure region that had some deep saline reservoir potential (but with fewer options, i.e. thinner, or deeper potential reservoirs) in combination with other known or speculative options
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Final Summary In terms of potential volume, deep saline reservoirs are likely the best option for large-scale, permanent CO2 storage Several lie in central and eastern Kentucky on or near navigatible waterways These reservoirs would require further testing to determine reservoir characteristics (permeability, water chemistry, etc.) for reservoir modeling
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Acknowledgements This presentation was developed by the Energy and Mineral Section of the Kentucky Geological Survey Contributors: Stephen F. Greb Brandon C. Nuttall James A. Drahovzal James C. Cobb Cortland F. Eble John B. Hickman Paul D. Lake Thomas M. Parris Michael P. Solis Kathryn G. Takacs
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For more information: DOE Carbon Sequestration Program
MRCSP Partnership DOE FutureGen Initiative MGSC (Illinois Basin) Partnership DOE Carbon Sequestration Technology Roadmap and Program Plan for 2005 SECARB Partnership DOE Carbon Sequestration Technology Roadmap and Program Plan for 2005
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