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COLLIE HUB
   Presentation
Groundwater Issues

     3 May 2011
THE CONCEPT
COLLIE HUB
•Integrated industrial CO2
geosequestration system
•Storage within an
identified area
• Red mud sequestration
300,000 + tpa (Alcoa)
• 2.4 mtpa Perdaman CO2
• Potential for up to 7 mtpa
for future power
generation
HOW IT WILL WORK
Target formations
 • The target injection formation is the Lesueur
   Sandstone with a top depth of approximately
   1300 metres.
 • The depths of injection will be approximately
   2000 and 2500 metres.
 • The Eneabba Formation will be the upper,
   “sealing” formation
 • Modelling shows the CO2 just reaching the
   base Eneabba
CO2 Injectivity and
Dynamic Capacity
                                                      OPTION 1              OPTION 2
• Injection rate range:                               Single well          Multiple well
                                                  w/ dual completion   w/ single completion
 • Base Myalup & top Wonnerup: 0.2 – 1
   Mt/a/completion
 • Mid Myalup: 0.3 – 1 Mt/a/completion
  • Total: 0.9 – 1.7 Mt/a/well
• CO2 contained volume (cumulative after
   40 yrs of injection) :
     • Base Myalup & top Wonnerup: 110 - 150 Mt
     • Mid Myalup: 90 – 150 Mt
     • Total injection range: 200 – 260 Mt
• Maximum pressure buildup of ~ 50 bar
  occurred across Darling fault, in Myalup
  and Wonnerup. Fault is still stable.
Dynamic Simulations

• Target injection (40 yrs): 6 injectors
• Completion consideration to optimize
  injection volume and manage
  containment risk:
 • Proximity to faults and well spacing
 • Rock quality distribution
 • Reservoir dip
• Two potential injection zones
  identified:
    • Base Myalup/Top Wonnerup with lower
      containment risk
    • Mid Myalup with higher injectivity
      potential and higher containment risk
      due to the proximity to Eneabba:
         • Smaller injection intervals away from
           the Base Eneabba
• Injection   constraints: frac-pressure
                                          Darling Fault
Injection Intervals
1000
                            yrs


                                   1000 yrs
Distance, m




                                   Distance, m
              Distance, m
CO2 Containment and Trapping
Mechanism
• CO2 reaches base of Eneabba at
  250 yrs
• After shut-in, up dip
• After 100 years shut-in:
        • mobile gas from 77% to 35%


• After 1000 years shut-in:
 • Mobile gas: 10%
 • Residual / immobile gas: 60%
 • Dissolved gas: 30%
                                       Trapping mechanism in Base
                                       Scenario
  • * residual saturation 10-40%
Fault Seal Analysis

                      •Fault Seal Analysis of
                       bounding faults in the
                       study area (Petrel):
                        • Darling Fault – main bounding fault
                          (considered sealing)
                        • 4NS
                        • 8EW

                      •Fault / Fracture
                       Reactivation
                      • faults stable up to 110 bar
                        overpressure


                                                                11
GSWA Harvey 1
Preparation Phase 2010 – 2012
 Pre-Competitive
• Further technical investigation of the
  Lesueur;
• Commenced a community & stakeholder
  consultation process
• Establishment of necessary legislative
  measures, approvals and easements; and
• Development of the proposed commercial
  structure and arrangements to facilitate the
  development.
Groundwater Analysis
 • The main Perth domestic water supply
   aquifer is the Yarragadee Formation.
 • The area chosen is on a structural high
   where the Yarragadee has been eroded off.
 • Main water supply from irrigation and
   superficial formations.
 • The Cockleshell Gully Fm is saline
 • The Leederville Fm mainly saline.
 • Lesueur Sst is a confined saline aquifer
This
section
eroded
off
New Seismic: note unconformity
COLLIE HUB AND WATER

Primary aim is not to isolate potential
  groundwater sources either above or
  below the injection depth
• How will we ensure aquifers above
  injection zone are protected?
• How will CO2 injection alter the water
  chemistry and rock chemistry?
Upper Aquifers
• Leederville Fm – 1.5km above injection formation

• Eneabba Fm consists of siltstones, mudstones and
  other “barrier” formations – need more data to prove
  this up in the area.

• Need to set up monitoring regime with tracers,
  monitoring bores etc

• Refine modelling with new data from seismic and
  GSWA Harvey 1 well.
Water Chemistry
• Sampling program
  using MDT (Modular
  formation Dynamics
  Tester)

• Core geochemistry
  XRD, SEM, Hylogger
  analyses
Conclusions

 • Collie Hub Project aware of resource conflict
   issues generally and groundwater
   specifically
 • Already taken steps to avoid Perth’s main
   groundwater source, the Yarragadee Fm
 • Data paucity means more acquisition
   necessary
 • Planning team for future work includes DoW
 • Monitoring essential
Thank you

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Collie Hub presentation groundwater issues

  • 1.
  • 2. COLLIE HUB Presentation Groundwater Issues 3 May 2011
  • 3. THE CONCEPT COLLIE HUB •Integrated industrial CO2 geosequestration system •Storage within an identified area • Red mud sequestration 300,000 + tpa (Alcoa) • 2.4 mtpa Perdaman CO2 • Potential for up to 7 mtpa for future power generation
  • 4. HOW IT WILL WORK
  • 5. Target formations • The target injection formation is the Lesueur Sandstone with a top depth of approximately 1300 metres. • The depths of injection will be approximately 2000 and 2500 metres. • The Eneabba Formation will be the upper, “sealing” formation • Modelling shows the CO2 just reaching the base Eneabba
  • 6. CO2 Injectivity and Dynamic Capacity OPTION 1 OPTION 2 • Injection rate range: Single well Multiple well w/ dual completion w/ single completion • Base Myalup & top Wonnerup: 0.2 – 1 Mt/a/completion • Mid Myalup: 0.3 – 1 Mt/a/completion • Total: 0.9 – 1.7 Mt/a/well • CO2 contained volume (cumulative after 40 yrs of injection) : • Base Myalup & top Wonnerup: 110 - 150 Mt • Mid Myalup: 90 – 150 Mt • Total injection range: 200 – 260 Mt • Maximum pressure buildup of ~ 50 bar occurred across Darling fault, in Myalup and Wonnerup. Fault is still stable.
  • 7. Dynamic Simulations • Target injection (40 yrs): 6 injectors • Completion consideration to optimize injection volume and manage containment risk: • Proximity to faults and well spacing • Rock quality distribution • Reservoir dip • Two potential injection zones identified: • Base Myalup/Top Wonnerup with lower containment risk • Mid Myalup with higher injectivity potential and higher containment risk due to the proximity to Eneabba: • Smaller injection intervals away from the Base Eneabba • Injection constraints: frac-pressure Darling Fault
  • 9. 1000 yrs 1000 yrs Distance, m Distance, m Distance, m
  • 10. CO2 Containment and Trapping Mechanism • CO2 reaches base of Eneabba at 250 yrs • After shut-in, up dip • After 100 years shut-in: • mobile gas from 77% to 35% • After 1000 years shut-in: • Mobile gas: 10% • Residual / immobile gas: 60% • Dissolved gas: 30% Trapping mechanism in Base Scenario • * residual saturation 10-40%
  • 11. Fault Seal Analysis •Fault Seal Analysis of bounding faults in the study area (Petrel): • Darling Fault – main bounding fault (considered sealing) • 4NS • 8EW •Fault / Fracture Reactivation • faults stable up to 110 bar overpressure 11
  • 13. Preparation Phase 2010 – 2012 Pre-Competitive • Further technical investigation of the Lesueur; • Commenced a community & stakeholder consultation process • Establishment of necessary legislative measures, approvals and easements; and • Development of the proposed commercial structure and arrangements to facilitate the development.
  • 14. Groundwater Analysis • The main Perth domestic water supply aquifer is the Yarragadee Formation. • The area chosen is on a structural high where the Yarragadee has been eroded off. • Main water supply from irrigation and superficial formations. • The Cockleshell Gully Fm is saline • The Leederville Fm mainly saline. • Lesueur Sst is a confined saline aquifer
  • 16. New Seismic: note unconformity
  • 17. COLLIE HUB AND WATER Primary aim is not to isolate potential groundwater sources either above or below the injection depth • How will we ensure aquifers above injection zone are protected? • How will CO2 injection alter the water chemistry and rock chemistry?
  • 18. Upper Aquifers • Leederville Fm – 1.5km above injection formation • Eneabba Fm consists of siltstones, mudstones and other “barrier” formations – need more data to prove this up in the area. • Need to set up monitoring regime with tracers, monitoring bores etc • Refine modelling with new data from seismic and GSWA Harvey 1 well.
  • 19. Water Chemistry • Sampling program using MDT (Modular formation Dynamics Tester) • Core geochemistry XRD, SEM, Hylogger analyses
  • 20. Conclusions • Collie Hub Project aware of resource conflict issues generally and groundwater specifically • Already taken steps to avoid Perth’s main groundwater source, the Yarragadee Fm • Data paucity means more acquisition necessary • Planning team for future work includes DoW • Monitoring essential