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CO2 Sequestration and Climate: Forefront
Technologies in the Pacific Northwest


             B. Peter McGrail, Ph.D
               Laboratory Fellow
        Energy & Environment Directorate

Washington Society of Professional Engineer’s Conference
                  Seattle, Washington
                      May 15, 2009
Historical Record of Atmospheric
           CO2 Concentrations


                           400
CO2 Concentration (ppmv)




                           350


                           300


                           250


                           200


                           150
                            50000   40000   30000   20000   10000   0
                                             Time (yr BP)
Climate change is a long-term strategic
problem with implications for today                                                                   20




                                              Global Fossil Fuel Carbon Emissions Gigatons per Year
                                                                                                                                                                                                               Historical Emissions
Stabilizing atmospheric concentrations of                                                                                                                                                                      GTSP_750
                                                                                                                                                                                                               GTSP_650
greenhouse gases and not their annual                                                                 15                                                                                                       GTSP_550
                                                                                                                                                                                                               GTSP_450
emissions levels should be the strategic                                                                                                                                                                       GTSP Reference Case


goal of climate policy                                                                                10



A fixed and finite amount of CO2 can be                                                                   5
released to the atmosphere over the
course of this century                                                                                -
                                                                                                                 1850                                          1900     1950    2000     2050   2100    2150     2200     2250    2300
    Every ton of emissions released to the
    atmosphere reduces the budget left for                                                                                                                              Stabilization of CO2 at 550 ppm
                                                                                                                                                        1600
    future generations                                                                                                                                                    History                         Future
                                                                                                                                                                  Oil
                                                                                                                                                        1400
    As we move forward in time and the                                                                                                                            Natural Gas




                                                                                                          .
                                                                                                                                                                  Coal
    planetary emissions budget is drawn

                                                                                                          Global Primary Energy 1850-2100 (Exajoules)
                                                                                                                                                        1200      Biomass Energy
    down, the remaining allowable emissions                                                                                                                       Non-Biomass Renewable Energy
                                                                                                                                                        1000
    will become more valuable                                                                                                                                         Oil + CCS
                                                                                                                                                                      Natural Gas + CCS
CO2 capture and storage (CCS) plays a                                                                                                                   800
                                                                                                                                                                      Coal + CCS
                                                                                                                                                                      Nuclear Energy
large role but…                                                                                                                                         600           End-use Energy
    Government and industry must make
    adequate provision for its use                                                                                                                      400

    CCS is not a silver bullet
                                                                                                                                                        200



                                                                                                                                                          0
                                                                                                                                                          1850           1900          1950      2000          2050        2100
                                                                                                                                                                                                                                         3
Coal Gasification Integrated with CO2
Capture                                             Conventional Gas Cleanup                                     PRODUCT CO2
                                                 ABSORBER VENT
                                                                         Sulfur
                   Coal
           ASU
                 DEMIN WATER MAKEUP


                                                                                             CW



            CW
                                                         CW




                                                                       H2

                                                                                CO2 to
                                                                                  LP
                                                                             Sequestration                 LP
                                                       WGS                        STEAM
                                                                                                         STEAM
                                                      Reactor Gas Separator



FLUE GAS
FEED
                                                                                                  WASTE TO
EXCESS                                                                                            DISPOSAL
                                  CW
WATER


                                                                            SODA ASH



                                       MAKEUP
                                       SOLVENT
Metal-Organic Solid Sorbent Technology

 Several classes of organic solids (including
 clathrates) are stable at high temperatures
 (250°C+)
 Cage/pore properties can be tailored to
 targeted guest
 Molecular engineered selectivity for CO2
 (or other gases)
 Can be produced in engineered structures,
 i.e. thin films, membranes, microporous
 materials
 No covalent/ionic chemical bonds involved
 – gas separation and retrieval cycles
 performed without degradation of the host
New Technologies Offer Breakthroughs in
CO2 Capture Economics
Coordination solid based on
hydroxytetephalic acid and various metals




    Porous tubular network
    25 wt% CO2 uptake at 1 bar and RT (4X amine solvents)
    No uptake of N2 at 1 bar
    Absorbs SO2 without degradation of material
    Heat of regeneration <140 BTU/lb-CO2 versus 710 BTU/lb-CO2 for
    MEA
Worldwide Portfolio of CCS Projects




7
Generic Sequestration System
                                   CO2 Phase Diagram




8
Reservoir Simulation of CO2 Injection
The Sequestration System Design
“Pentagon”                     Capture system
                                                                                                          Pipeline
                                           ity                         Le                                 Wellbore
                                        bil                               ga
                                                                             l
                                     Lia                                         &
                                                                                     Lia                  Reservoir(s)
                                l&                  Monitoring
                              ga                    Verification                           bil
                                                                                              ity
                           Le                       Accounting
                                                     Systems

                                                                        Control and
                              Delivery                                    Data
                           Infrastructure                               Acquisition
                                                                         Systems
                     ity




                                                                                               Le
                iabil




                                                                                                 gal &
               L
         gal &




                                                                                                       Liabil
                                       Cost
       Le




                                                                   Permitting
                                     Estimation



                                                                                                             ity
                                                 Legal & Liability
The CCS and Power Plant Developer Nexus


 CCS introduces a new
 and unfamiliar paradigm         Outline of Incised Valley (>50
                                 ft Muddy thickness) Thins
                                 may indicate areas with
 for power plant                 preserved Rozet remnants


 developers
   Traditional siting factors
   (water, transmission lines,                 Rozet Member, largely
   fuel cost) no longer solely                 continuous to the east;
                                               variable porosity
   determine project viability                 should offer the
                                               possibility of multiple,
                                               segregated aquifers.

   Suitable geology for
   sequestration or buyer for                                             Gas - Red
                                                                          Oil - Green

   CO2 required                                                           Water - Blue

                                                         Production ratios tend to
                                                         distinguish Springen Ranch vs

 400 to 700 acre plant                                   Ute Members. No Rozet
                                                         production this immediate area.



 boundary expands to
 5000 to 10,000 acre AOI
Integrated Sequestration System Design

                                      Wellbore Design        Po          Pipeline Design
     Reservoir Simulation
                                Pb                           To     Po

                                &
                                m                            m&     To
                                                                    m&




                               TCO2                          TCO2
                                                                          Pipeline design
        Geological data                                                   specifications
        Hydrologic data
                                                                          Heat transfer
        Geochemical data                                                  parameters
        Initial and boundary           Well design parameters
        conditions                                                        Soil temperature
                                       Heat transfer parameters
                                                                          CO2 EOS
                                       Boundary conditions
                                       CO2 EOS

                                                                    • Plant specifications

12
Coupled Thermohydraulic Modeling

      One dimensional finite-difference flow model
      CO2 properties computed from equation of state (Span and Wagner,
      1996)
      Heat transfer from soil (pipeline) and surrounding rock (wellbore)

                               ⎡ 64 744 6447448 64 744 ⎤
                                     4
                                   frictional loss
                                                   8       gravity head
                                                                                  4            8
                                                                               flow acceleration
                          j +1 ⎢
                                 fG (Vi + Vi −1 )       (ρi + ρi −1 ) sin α + G (V − V ) ⎥
           p j = p1 − ΔL ∑ ⎢                         −g                                       i −1 ⎥
                                                                              ΔL
                                                                                      i
                         i =2 ⎢         4D                   2                                     ⎥
                               ⎢
                               ⎣                                                                   ⎥
                                                                                                   ⎦
                            ⎡ heat transfer 64 energy 64748 gravitational energy ⎤
                               }
                                              potential
                                                   74   8    kinetic energy
                       j +1 ⎢                                                6 74 ⎥
                                                                               4 8
                               Qi           ⎛ pi pi −1 ⎞ 1 2
           u j = u1 + ∑ ⎢            ΔL − ⎜ −            ⎟ − (Vi − Vi −1 ) + g ΔL sin α ⎥
                                                                          2

                      i =2 ⎢    m           ⎝  ρi ρi −1 ⎠ 2                             ⎥
                            ⎢
                            ⎣                                                           ⎥
                                                                                        ⎦


13
Major Features at Each Candidate Site

        Jewett                   Odessa                 Mattoon               Tuscola




Woodbine                     Delaware Sands         Mt. Simon              Mt. Simon
• 5K to 6K ft                  plus Queen           • 6K to 7K ft          • 6K to 7K ft
• 1 injection well           • 3K to 5K ft          • 1 injection well     • 1 injection well
                             • 10 vertical          • Injection on plant   • Install ~10-miles of
Travis Peak                    injection wells        site                   new pipeline
• R&D Potential
                             • Use all or part of   • No nearby wells      • No nearby wells
• 10K to 12K ft                existing pipeline      penetrate              penetrate primary
• 5 Wells (1 injector/4        (56 miles total)
   production                                         primary seal           seal
                             • Near-by wells
• Install ~30-miles of new
  pipeline
• Near-by wells
Depth In
 Feet


   1000
                                                       Major
                                                      Features:

                                                    Comparison
                                                     of Sites by
   5000                                                 Depth
                     5600’



                                    7750’
                                            8350’

                             Seal

                             Injection
  10000
           11,500’
Design Data Comparison By Site (130 MMscfd)

              Parameter              Units    Illinois    Illinois     Texas      Texas Odessa
                                              Mattoon     Tuscola      Jewett
                Pipeline             miles        0         11.0        52.5           86
         Well Connector Pipe         miles       0.5         2           1             8
                #Wells                           1           1           1             10
         Injection Tubing OD         inches      5.5         5.5         5.5          2.88
       Injection Tubing ID (Drift)   inches     4.55        4.55        4.55          2.17
          Depth to Reservoir          feet      6950        6150        4800          2900
        Pipeline Inlet Pressure       psi     2140-2160   1720-2030   1800-2160    1410-1630
          Wellhead Pressure           psi     2140-2160   1690-2010   1740-2100    1320-1520
            Required BHP              psi       3096        2790        2760          2190
         In situ Temperature           °F       138         130         153           107

           Predicted Temp             °F       117-118     90-114      69-109        62-101

            Pipe Diameter            inches      16          16          18            18



            Operating at lower pressure in winter can save
            $300K to $400K per year in compression costs
16
Nonisothermal Simulations with STOMP-CO2
     • Woodbine formation, Brazos, Texas
     • Field temperature of 68° C with a geothermal gradient
     • Injection temperature between 21° C and 43° C
     • 50 MMT Injection for 27.34 years with two 28-day plant shutdowns per year
     • 50-year simulation period




                         Temperature, 20° C (blue) - 70° C (red)



17
Nonisothermal Simulations with
STOMP-CO2e
• Woodbine formation, Brazos, Texas
• Field temperature of 68° C with a
geothermal gradient
• Injection temperature between 21° C and
43° C
• 50 MMT Injection for 27.34 years with two
28-day plant shutdowns per year
• 50-year simulation period




                       Dissolved CO2 Concentration, 0.0 (blue) - 0.07 gm/cm3 (red)
18
Liquid CO2 (~2500 ppmw H2O, 298 ppmw H2S)
CO2 Purity Effects
  Pipeline regulations vary widely
  for H2S                                                                     Pipeline
     20 ppm K-M Central Basin system                                           steel
     200 ppm Petrosource
     10,000 ppm Weyburn
     As much as 70% H2S transported
     and injected in Canada
  Pipeline water content                                           Columbia River Basalt
  specifications vary widely and are                              90°C, 41 days, 10.2 MPa
  related to H2S content in CO2                                      11,935 ppmw H2S
  stream
     Dry CO2 and CO2-H2S streams are
     unreactive with pipeline steels
     Knowledge gap for CO2 streams
     containing intermediate water content
     Water saturated CO2 phase in               pyrite
     geologic reservoir
  Lack of industry experience and
  even basic science studies with
  CO2-SO2-H2O systems
Principal Legal “Hurdles” in CCS Projects
                “Hurdles”
 Mineral rights
    Complex law and varies state to state
    Severed ownership issues
    CO2 Storage Deed
 Landowner cooperation required over much larger area than traditional
 power plant
 Liability issues remain unresolved except for specific instances
    Texas and Illinois passed liability legislation specific to the FutureGen
    project
    States that have passed CCS legislation (i.e. WA and WY) have not
    addressed liability
    Establishment of Trust Funds (State administered) seem to be an often
    cited approach
    Industry stepping into market (Zurich Financial Services Group, AIG)




                                                                                20
Example of Land Ownership Issues
on a Small CCS Project
MVA Tool Suite
 Atmospheric Monitoring
     Eddy covariance
     Accumulation chambers
     LIDAR
 Remote Sensing
     Color infrared orthoimagery
     Aerial photography/spectroscopy
     Tiltmeter
     Gravimetric interferometry
 Vadose Zone
     Infrared Gas Analyzers
     Laser Induced Breakdown Spectroscopy
     (LIBS)
     Isotope Mass Spectrometry
     GC/MS
 Geophysical Methods
     Electromagnetic Induction
     High Resolution Electrical Resistivity
     Dedicated Seismic Array Network
     Mobile Seismic Surveys
 Groundwater Monitoring
     Shallow and Deep Monitoring Wells
     Water chemistry analysis by ICP-MS and a
     variety of other methods
Big Sky Carbon Sequestration Partnership




                                           23
Pilot Project Partners
       Research Institutions (universities, labs, others)
          MSU, UI, Columbia University, INL, Oregon State University
       Department of Natural Resources
       International Collaborators
          Institut de Physique du Globe (France)
          National Geophysical Research Institute (India)
          Vernadsky Institute of Geochemistry and Analytical Chemistry (Russia)
       Industry
          Boise White Paper L.L.C.
          Shell Oil Company
          Portland General Electric
          Others




24
Layered Basalt Flows




      Interflow zones have properties that
      allow fluids to move in and out
      Overlying flow interiors have
      extremely low permeability and act
      as caprock seals
25
Lab Experiments with Columbia River Basalt

         Indirect: Rock-Water-CO2
                                             Direct: Rock-CO2-solvated water




                  What happens with impurities in the CO2 stream?




     Some basalts (like CRB) react even          Other basalts form armoring coatings
     faster                                      that reduce carbonate formation
          Basalt Reacts with Supercritical CO2 in both the Aqueous and Gas Phase
          to Form Carbonates

26
Why this Area?
                                                                 

        Hanford Site



                                                                                                      License area
                                        Snake River

                                                                                                +
                                              Field Test Site
                                                                                                    Well location




        Washington     Columbia River




                                          Oregon

                                                                    Located where some of the deepest and
                                                                    thickest basalt exists in the region
                                                                    Located on an active industrial site that
                                                                    has been extensively disturbed during
                                                                    original plant construction
                                                                    Data collected will assist plant owner with
                                                                    commercial operations after pilot study is
                                                                    complete

27
Basalt Pilot Project Summary
      Pre-Injection Site Characterization
          Soil gas and shallow well water geochemistry
          Seismic survey
          Well logging and geochemical sampling during borehole drilling phase
          Hydrologic tests
      Injection Facts
          Water is non-potable at target depth
          1000 MT of CO2 total (1/2 Olympic-sized pool)
          Injection would occur over a 2 to 4 week period
          Initial radius of CO2 bubble is only about 100 ft. Maximum spread radius is about 250 ft
          The CO2 will dissolve in the formation water and eventually become mineralized over a period
          of a couple of years
      Monitoring Program
          An extensive monitoring program is planned that includes air, shallow subsurface, and deep
          monitoring components
          Water samples will be obtained periodically to monitor geochemical changes
          Core sample extraction (1-2 years post-injection)
      Closure
          Wells would be plugged and abandoned according to state regulations
          Site would be restored to pre-test condition
          Closure option will depend on possible future use by landowner


28
Seismic Survey
       Seismic survey completed 12/07/2007
       Field tests immediately prior to
       initiation of the seismic acquisition
       showed that ground roll could be
       suppressed by eliminating frequencies
       below 12 Hz, and by using (for each
       seismic source station) four vibroseis
       sweeps
       Optimized sweep resulted in longer
       production of high frequency source
       energy and a desirable flattened
       frequency spectrum
       The swath design of five receiver lines
       flanked by two source lines, together
       with the use of the optimized sweep
       design, results in a dominant
       frequency of 80 HZ at the target
       interval of 3,000-4,000 feet, and a fold
       of 200.
       Raw field records of the 2D data
       acquired confirm acquisition of P-wave
       and converted wave data
       Initial data processing complete. No
       faulting or fracture zones are indicated
       at the site
29
Current Stack Overlapped by the Current RMS Velocity
     Model: Noise Attenuated, Deconvoluted, Spectral
     Balanced, Residual Statics




30
31
Seismic swath




                                North
     Basalt Test Well




32
Top Water Table 35’
                                        2450
                                                                                                                                        Wallula P ilot
                                                                                                                                     Hydrogeologic Model
                                                     Umtanum Basalt
                                                     Flow-Interior Section
                                                                                                                                                Top of Basalt 44’
                                                     (Secondary Caprock)
     Depth, feet below ground surface   2550                                                                                             Umtanum Basalt




                                        2650
                                                    Slack Canyon Basalt
                                                    Flow-Interior Section
                                                                                                                                       Slack Canyon Basalt
                                                    (Primary Caprock )
                                                                                                     Test Zone 8B
                                        2750                                                         (Injection R eservoir)




                                        2850                                                                  Test Zone 8A

                                                                                                                                             Ortley Basalt
                                                    Ortley Ba salt
                                                    Flow Interior Section
                                                    Lower Hydrogeologic Confining Unit

                                        2950
                                               10                                        100                                  1000                           10000
                                                                                               Deep Resistivity, ohm-m

                                                Selected injection zone transects three interconnected
                                                basalt flows that offer significant potential for scientific
                                                study of CO2 migration and mineralization processes in
                                                a unique geological setting

33
Packer Tool Assembly Deployment




                                                                                      Shut-In Tool Valve
                                                                                         Assembly




                                                          Inflatable Packer




                                                                              Bottom Well Screen
                                 Pressure Probe Housing



                           Packer Expansion
                               Chamber




34
35
Cores and Image Log From Test Zone




36
Conclusions
      Sequestration systems need to be integrated from plant
      gate to sequestration site to operate effectively and
      efficiently
      Design tools are being developed to make the task easier
      but maintain robust design
      CCS is a completely new paradigm for power plant
      developers and their financial backers
      Achilles heel of CCS systems appears to rest on financial,
      legal, liability, and public acceptance issues
      The Pacific Northwest is making unique contributions
      towards advancing CCS opportunities both regionally and
      worldwide



37
Acknowledgements


The work discussed in this presentation was sponsored by
               Office of Fossil Energy and
        National Energy Technology Laboratory
                  Department of Energy
            with special acknowledgement to
Sequestration System Design Considerations

  Plant operations
     Unscheduled and scheduled plant shutdowns result in periodic flow interruptions
     Infrastructure sized to accept full rate of CO2 output when the plant is operating
  Pipeline
     Specify diameter large enough to handle peak flow rate without excessive
     pressure drop and wall thickness sufficient to accommodate pressure
     requirements
     Cost-benefit analysis may be needed to determine specifications for delivered
     CO2 (purity requirements)
  Wellbore
     Injection tubing string of sufficient diameter to prevent excessive pressure drop at
     peak CO2 injection rate
     Account for impacts of seasonal temperature variations on operating parameters
  Target Formation(s)
     Utilize reservoir simulations to estimate required injection pressure to support
     range of injection rates
     Maintain operating pressures below fracture gradient limit
     Assess impacts of CO2 delivery temperature on operating parameters and
     reservoir stresses*
Components of a CCS Program
  Subsurface
Characterization

                  Permitting

                                     Subsurface
                                    Infrastructure
                                      & Pipeline

          Pro                                        Operations &
              jec                                    Maintenance
                  t   Tim
                         e   line
                                                                    Monitoring


                                                                                 Closure

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CO2 Sequestration Technologies in the Pacific Northwest

  • 1. CO2 Sequestration and Climate: Forefront Technologies in the Pacific Northwest B. Peter McGrail, Ph.D Laboratory Fellow Energy & Environment Directorate Washington Society of Professional Engineer’s Conference Seattle, Washington May 15, 2009
  • 2. Historical Record of Atmospheric CO2 Concentrations 400 CO2 Concentration (ppmv) 350 300 250 200 150 50000 40000 30000 20000 10000 0 Time (yr BP)
  • 3. Climate change is a long-term strategic problem with implications for today 20 Global Fossil Fuel Carbon Emissions Gigatons per Year Historical Emissions Stabilizing atmospheric concentrations of GTSP_750 GTSP_650 greenhouse gases and not their annual 15 GTSP_550 GTSP_450 emissions levels should be the strategic GTSP Reference Case goal of climate policy 10 A fixed and finite amount of CO2 can be 5 released to the atmosphere over the course of this century - 1850 1900 1950 2000 2050 2100 2150 2200 2250 2300 Every ton of emissions released to the atmosphere reduces the budget left for Stabilization of CO2 at 550 ppm 1600 future generations History Future Oil 1400 As we move forward in time and the Natural Gas . Coal planetary emissions budget is drawn Global Primary Energy 1850-2100 (Exajoules) 1200 Biomass Energy down, the remaining allowable emissions Non-Biomass Renewable Energy 1000 will become more valuable Oil + CCS Natural Gas + CCS CO2 capture and storage (CCS) plays a 800 Coal + CCS Nuclear Energy large role but… 600 End-use Energy Government and industry must make adequate provision for its use 400 CCS is not a silver bullet 200 0 1850 1900 1950 2000 2050 2100 3
  • 4. Coal Gasification Integrated with CO2 Capture Conventional Gas Cleanup PRODUCT CO2 ABSORBER VENT Sulfur Coal ASU DEMIN WATER MAKEUP CW CW CW H2 CO2 to LP Sequestration LP WGS STEAM STEAM Reactor Gas Separator FLUE GAS FEED WASTE TO EXCESS DISPOSAL CW WATER SODA ASH MAKEUP SOLVENT
  • 5. Metal-Organic Solid Sorbent Technology Several classes of organic solids (including clathrates) are stable at high temperatures (250°C+) Cage/pore properties can be tailored to targeted guest Molecular engineered selectivity for CO2 (or other gases) Can be produced in engineered structures, i.e. thin films, membranes, microporous materials No covalent/ionic chemical bonds involved – gas separation and retrieval cycles performed without degradation of the host
  • 6. New Technologies Offer Breakthroughs in CO2 Capture Economics Coordination solid based on hydroxytetephalic acid and various metals Porous tubular network 25 wt% CO2 uptake at 1 bar and RT (4X amine solvents) No uptake of N2 at 1 bar Absorbs SO2 without degradation of material Heat of regeneration <140 BTU/lb-CO2 versus 710 BTU/lb-CO2 for MEA
  • 7. Worldwide Portfolio of CCS Projects 7
  • 8. Generic Sequestration System CO2 Phase Diagram 8
  • 9. Reservoir Simulation of CO2 Injection
  • 10. The Sequestration System Design “Pentagon” Capture system Pipeline ity Le Wellbore bil ga l Lia & Lia Reservoir(s) l& Monitoring ga Verification bil ity Le Accounting Systems Control and Delivery Data Infrastructure Acquisition Systems ity Le iabil gal & L gal & Liabil Cost Le Permitting Estimation ity Legal & Liability
  • 11. The CCS and Power Plant Developer Nexus CCS introduces a new and unfamiliar paradigm Outline of Incised Valley (>50 ft Muddy thickness) Thins may indicate areas with for power plant preserved Rozet remnants developers Traditional siting factors (water, transmission lines, Rozet Member, largely fuel cost) no longer solely continuous to the east; variable porosity determine project viability should offer the possibility of multiple, segregated aquifers. Suitable geology for sequestration or buyer for Gas - Red Oil - Green CO2 required Water - Blue Production ratios tend to distinguish Springen Ranch vs 400 to 700 acre plant Ute Members. No Rozet production this immediate area. boundary expands to 5000 to 10,000 acre AOI
  • 12. Integrated Sequestration System Design Wellbore Design Po Pipeline Design Reservoir Simulation Pb To Po & m m& To m& TCO2 TCO2 Pipeline design Geological data specifications Hydrologic data Heat transfer Geochemical data parameters Initial and boundary Well design parameters conditions Soil temperature Heat transfer parameters CO2 EOS Boundary conditions CO2 EOS • Plant specifications 12
  • 13. Coupled Thermohydraulic Modeling One dimensional finite-difference flow model CO2 properties computed from equation of state (Span and Wagner, 1996) Heat transfer from soil (pipeline) and surrounding rock (wellbore) ⎡ 64 744 6447448 64 744 ⎤ 4 frictional loss 8 gravity head 4 8 flow acceleration j +1 ⎢ fG (Vi + Vi −1 ) (ρi + ρi −1 ) sin α + G (V − V ) ⎥ p j = p1 − ΔL ∑ ⎢ −g i −1 ⎥ ΔL i i =2 ⎢ 4D 2 ⎥ ⎢ ⎣ ⎥ ⎦ ⎡ heat transfer 64 energy 64748 gravitational energy ⎤ } potential 74 8 kinetic energy j +1 ⎢ 6 74 ⎥ 4 8 Qi ⎛ pi pi −1 ⎞ 1 2 u j = u1 + ∑ ⎢ ΔL − ⎜ − ⎟ − (Vi − Vi −1 ) + g ΔL sin α ⎥ 2 i =2 ⎢ m ⎝ ρi ρi −1 ⎠ 2 ⎥ ⎢ ⎣ ⎥ ⎦ 13
  • 14. Major Features at Each Candidate Site Jewett Odessa Mattoon Tuscola Woodbine Delaware Sands Mt. Simon Mt. Simon • 5K to 6K ft plus Queen • 6K to 7K ft • 6K to 7K ft • 1 injection well • 3K to 5K ft • 1 injection well • 1 injection well • 10 vertical • Injection on plant • Install ~10-miles of Travis Peak injection wells site new pipeline • R&D Potential • Use all or part of • No nearby wells • No nearby wells • 10K to 12K ft existing pipeline penetrate penetrate primary • 5 Wells (1 injector/4 (56 miles total) production primary seal seal • Near-by wells • Install ~30-miles of new pipeline • Near-by wells
  • 15. Depth In Feet 1000 Major Features: Comparison of Sites by 5000 Depth 5600’ 7750’ 8350’ Seal Injection 10000 11,500’
  • 16. Design Data Comparison By Site (130 MMscfd) Parameter Units Illinois Illinois Texas Texas Odessa Mattoon Tuscola Jewett Pipeline miles 0 11.0 52.5 86 Well Connector Pipe miles 0.5 2 1 8 #Wells 1 1 1 10 Injection Tubing OD inches 5.5 5.5 5.5 2.88 Injection Tubing ID (Drift) inches 4.55 4.55 4.55 2.17 Depth to Reservoir feet 6950 6150 4800 2900 Pipeline Inlet Pressure psi 2140-2160 1720-2030 1800-2160 1410-1630 Wellhead Pressure psi 2140-2160 1690-2010 1740-2100 1320-1520 Required BHP psi 3096 2790 2760 2190 In situ Temperature °F 138 130 153 107 Predicted Temp °F 117-118 90-114 69-109 62-101 Pipe Diameter inches 16 16 18 18 Operating at lower pressure in winter can save $300K to $400K per year in compression costs 16
  • 17. Nonisothermal Simulations with STOMP-CO2 • Woodbine formation, Brazos, Texas • Field temperature of 68° C with a geothermal gradient • Injection temperature between 21° C and 43° C • 50 MMT Injection for 27.34 years with two 28-day plant shutdowns per year • 50-year simulation period Temperature, 20° C (blue) - 70° C (red) 17
  • 18. Nonisothermal Simulations with STOMP-CO2e • Woodbine formation, Brazos, Texas • Field temperature of 68° C with a geothermal gradient • Injection temperature between 21° C and 43° C • 50 MMT Injection for 27.34 years with two 28-day plant shutdowns per year • 50-year simulation period Dissolved CO2 Concentration, 0.0 (blue) - 0.07 gm/cm3 (red) 18
  • 19. Liquid CO2 (~2500 ppmw H2O, 298 ppmw H2S) CO2 Purity Effects Pipeline regulations vary widely for H2S Pipeline 20 ppm K-M Central Basin system steel 200 ppm Petrosource 10,000 ppm Weyburn As much as 70% H2S transported and injected in Canada Pipeline water content Columbia River Basalt specifications vary widely and are 90°C, 41 days, 10.2 MPa related to H2S content in CO2 11,935 ppmw H2S stream Dry CO2 and CO2-H2S streams are unreactive with pipeline steels Knowledge gap for CO2 streams containing intermediate water content Water saturated CO2 phase in pyrite geologic reservoir Lack of industry experience and even basic science studies with CO2-SO2-H2O systems
  • 20. Principal Legal “Hurdles” in CCS Projects “Hurdles” Mineral rights Complex law and varies state to state Severed ownership issues CO2 Storage Deed Landowner cooperation required over much larger area than traditional power plant Liability issues remain unresolved except for specific instances Texas and Illinois passed liability legislation specific to the FutureGen project States that have passed CCS legislation (i.e. WA and WY) have not addressed liability Establishment of Trust Funds (State administered) seem to be an often cited approach Industry stepping into market (Zurich Financial Services Group, AIG) 20
  • 21. Example of Land Ownership Issues on a Small CCS Project
  • 22. MVA Tool Suite Atmospheric Monitoring Eddy covariance Accumulation chambers LIDAR Remote Sensing Color infrared orthoimagery Aerial photography/spectroscopy Tiltmeter Gravimetric interferometry Vadose Zone Infrared Gas Analyzers Laser Induced Breakdown Spectroscopy (LIBS) Isotope Mass Spectrometry GC/MS Geophysical Methods Electromagnetic Induction High Resolution Electrical Resistivity Dedicated Seismic Array Network Mobile Seismic Surveys Groundwater Monitoring Shallow and Deep Monitoring Wells Water chemistry analysis by ICP-MS and a variety of other methods
  • 23. Big Sky Carbon Sequestration Partnership 23
  • 24. Pilot Project Partners Research Institutions (universities, labs, others) MSU, UI, Columbia University, INL, Oregon State University Department of Natural Resources International Collaborators Institut de Physique du Globe (France) National Geophysical Research Institute (India) Vernadsky Institute of Geochemistry and Analytical Chemistry (Russia) Industry Boise White Paper L.L.C. Shell Oil Company Portland General Electric Others 24
  • 25. Layered Basalt Flows Interflow zones have properties that allow fluids to move in and out Overlying flow interiors have extremely low permeability and act as caprock seals 25
  • 26. Lab Experiments with Columbia River Basalt Indirect: Rock-Water-CO2 Direct: Rock-CO2-solvated water What happens with impurities in the CO2 stream? Some basalts (like CRB) react even Other basalts form armoring coatings faster that reduce carbonate formation Basalt Reacts with Supercritical CO2 in both the Aqueous and Gas Phase to Form Carbonates 26
  • 27. Why this Area?   Hanford Site License area Snake River + Field Test Site Well location Washington Columbia River Oregon Located where some of the deepest and thickest basalt exists in the region Located on an active industrial site that has been extensively disturbed during original plant construction Data collected will assist plant owner with commercial operations after pilot study is complete 27
  • 28. Basalt Pilot Project Summary Pre-Injection Site Characterization Soil gas and shallow well water geochemistry Seismic survey Well logging and geochemical sampling during borehole drilling phase Hydrologic tests Injection Facts Water is non-potable at target depth 1000 MT of CO2 total (1/2 Olympic-sized pool) Injection would occur over a 2 to 4 week period Initial radius of CO2 bubble is only about 100 ft. Maximum spread radius is about 250 ft The CO2 will dissolve in the formation water and eventually become mineralized over a period of a couple of years Monitoring Program An extensive monitoring program is planned that includes air, shallow subsurface, and deep monitoring components Water samples will be obtained periodically to monitor geochemical changes Core sample extraction (1-2 years post-injection) Closure Wells would be plugged and abandoned according to state regulations Site would be restored to pre-test condition Closure option will depend on possible future use by landowner 28
  • 29. Seismic Survey Seismic survey completed 12/07/2007 Field tests immediately prior to initiation of the seismic acquisition showed that ground roll could be suppressed by eliminating frequencies below 12 Hz, and by using (for each seismic source station) four vibroseis sweeps Optimized sweep resulted in longer production of high frequency source energy and a desirable flattened frequency spectrum The swath design of five receiver lines flanked by two source lines, together with the use of the optimized sweep design, results in a dominant frequency of 80 HZ at the target interval of 3,000-4,000 feet, and a fold of 200. Raw field records of the 2D data acquired confirm acquisition of P-wave and converted wave data Initial data processing complete. No faulting or fracture zones are indicated at the site 29
  • 30. Current Stack Overlapped by the Current RMS Velocity Model: Noise Attenuated, Deconvoluted, Spectral Balanced, Residual Statics 30
  • 31. 31
  • 32. Seismic swath North Basalt Test Well 32
  • 33. Top Water Table 35’ 2450 Wallula P ilot Hydrogeologic Model Umtanum Basalt Flow-Interior Section Top of Basalt 44’ (Secondary Caprock) Depth, feet below ground surface 2550 Umtanum Basalt 2650 Slack Canyon Basalt Flow-Interior Section Slack Canyon Basalt (Primary Caprock ) Test Zone 8B 2750 (Injection R eservoir) 2850 Test Zone 8A Ortley Basalt Ortley Ba salt Flow Interior Section Lower Hydrogeologic Confining Unit 2950 10 100 1000 10000 Deep Resistivity, ohm-m Selected injection zone transects three interconnected basalt flows that offer significant potential for scientific study of CO2 migration and mineralization processes in a unique geological setting 33
  • 34. Packer Tool Assembly Deployment Shut-In Tool Valve Assembly Inflatable Packer Bottom Well Screen Pressure Probe Housing Packer Expansion Chamber 34
  • 35. 35
  • 36. Cores and Image Log From Test Zone 36
  • 37. Conclusions Sequestration systems need to be integrated from plant gate to sequestration site to operate effectively and efficiently Design tools are being developed to make the task easier but maintain robust design CCS is a completely new paradigm for power plant developers and their financial backers Achilles heel of CCS systems appears to rest on financial, legal, liability, and public acceptance issues The Pacific Northwest is making unique contributions towards advancing CCS opportunities both regionally and worldwide 37
  • 38. Acknowledgements The work discussed in this presentation was sponsored by Office of Fossil Energy and National Energy Technology Laboratory Department of Energy with special acknowledgement to
  • 39. Sequestration System Design Considerations Plant operations Unscheduled and scheduled plant shutdowns result in periodic flow interruptions Infrastructure sized to accept full rate of CO2 output when the plant is operating Pipeline Specify diameter large enough to handle peak flow rate without excessive pressure drop and wall thickness sufficient to accommodate pressure requirements Cost-benefit analysis may be needed to determine specifications for delivered CO2 (purity requirements) Wellbore Injection tubing string of sufficient diameter to prevent excessive pressure drop at peak CO2 injection rate Account for impacts of seasonal temperature variations on operating parameters Target Formation(s) Utilize reservoir simulations to estimate required injection pressure to support range of injection rates Maintain operating pressures below fracture gradient limit Assess impacts of CO2 delivery temperature on operating parameters and reservoir stresses*
  • 40. Components of a CCS Program Subsurface Characterization Permitting Subsurface Infrastructure & Pipeline Pro Operations & jec Maintenance t Tim e line Monitoring Closure