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Groundwater and CO2CRC- Insights from
the Otway Project and Monitoring Activities




Allison Hortle
Senior Researcher, Petroleum Hydrogeology
Cooperative Research Centre       Presenting to: GCCSI
for Greenhouse Gas                Groundwater Thematic Working Group
Technologies (CO2CRC)             Initial Workshop                     © CO2CRC
                                  Canberra, 3 May, 2011                All rights reserved
M&V Goals
• To monitor the freshwater aquifers to demonstrate that they are
  unaffected by the injection and storage of CO2


• To set-up a long term sentinel monitoring system



• To combine the hydrogeology and the geochemistry with the
  atmospheric and soil gas program to develop a methodology for
  an integrated surface and sub-surface monitoring system

• Create public confidence in “decarbonisation” technology and
  demonstrate that this technology can co-exist with existing
  exploitable resources
Concept of the CO2CRC Otway Project
                               Fluid Sampling
                                  Field Lab.




    Supercritical CO2 from
         Buttress-1
     80% CO2 : 20% CH4
Monitoring at the CO2CRC Otway site


                                δ
Schematic Stratigraphic Column of Otway
    Basin
    Port Campbell Limestone Aq.
•   Unconfined to semi-confined
• Major local freshwater source; dairy,
irrigation, domestic, etc

    Dilwyn Formation Aquifer
•   Confined, freshwater
•   Future urban water resource
•   Limited current use



     Waarre Aq.
Groundwater Monitoring Stations
                             • 24 Port Campbell
                               Limestone
                             • 3 Dilwyn Aquifer
                             • 5 Pre-injection
                               sampling trips
                             • 4 Post-injection
                               sampling trips
Monitoring groundwater levels
                                     Cap
• Install downhole pressure and                   Cable permanently
  temperature sensors                             installed
                                    Steel Cable



• Provide real-time measurements
  of fluctuations in water levels
                                                  Waterlevel


                                    5-10m
• Bi-annual downloads                              Datalogger




                                                   Screen
Field Sampling
•   At each site, pumped water was monitored
    for:
     –pH, Eh, EC, DO and temperature
     through a flow cell until stable readings were
     acquired


•   A set of samples were field titrated for
    alkalinity


•   A set of samples were analysed for reduced
    Fe2+ through the portable mass
    spectrophotometer


•   Sets were obtained for comparison of field and
    lab results to determine if field processing is
    necessary
Pt Campbell Groundwater Composition
Water levels in the Dilwyn Confined Aquifer
Outcomes to date
• Groundwater composition has not changed between pre- and
  post- injection


• No evidence of any changes in water level or temperature
  associated with CO2CRC activities


• All data has been given to landowners, consequently they are
  still very supportive


• We have demonstrated that no change has occurred at any of
  the monitoring stations – this is not the same as evidence of
  containment
What is a monitoring network?
• Monitor pre-existing wells, both groundwater and petroleum


• Under what circumstances will these installations “see”
  changes related to CO2?


• What volume, how far away from leak, what impacts?


• How do you define an acceptable detection limit? pH,
  pressure, HCO3?
Groundwater Monitoring
                                             Cap
• Standard practice, inexpensive, off-the                 Cable permanently
  shelf tools                                             installed
                                            Steel Cable



• Provide real-time measurements of
  fluctuations in water levels and
                                                          Waterlevel
  temperature and conductivity
                                            5-10m
                                                           Datalogger
• Still produce large amounts of data




                                                           Screen
Permanent Downhole Monitoring
• Becoming more standard in
  oil & gas industry
• Real-time monitoring of
  pressure, temperature and
  possibly fluids
• Much better reservoir
  management
• Drawbacks are costs and
  longevity
• Large amounts of data are
  produced, requiring complex
  and time-consuming analyses



     Schmidt, H.S., Nordtvedt, J-E., Nygaard, O. and Erskine, S., 2002, Reservoir management of gas
     fields using permanent sensors, World Oil, April, 2002, Vol. 223, No. 4, http://www.worldoil.com/April-
     2002-Reservoir-management-of-gas-fields-using-permanent-sensors.html
Cranfield, EOR, USA (SEACARB)
• PDS in injection interval, PT,
  and
• AMZI: 120m above injection
  zone, changes in pressure in
  injection zone are not
  apparent in AZMI
• Groundwater: geochemical
  sampling of aquifers at 70-
  100m; Ag, Al, As, Ba, Ca, Cd,
  Cr, Cu, Fe, K, Mg, Mn, Mo, Na,
  Pb, Se, Zn (Cations), F-, Cl-,
  SO42-, Br-, NO3-, PO43-
  (Anions), TOC, TIC, pH,
  Alkalinity, VOC, dC13.
                         http://bittooth.blogspot.com/2010/03/carbon-sequestration-sites-and-their.html
Ketzin, Germany (CO2SINK)
• Atmospheric monitoring:
  tunable diode laser system
  for CO2 and methane
• Gas monitoring: surface
  soil flux (20 stations),
  methane @ 2 m (10 wells)
• Groundwater: 2
  multisensor monitoring
  wells

                               Wuerdemann, et al., 2010
Summary
• Groundwater can be monitoring using geochemistry or
  pressure; pressure propagates further than CO2 plume
• Tools for monitoring groundwater pressures (heads) are
  off-the-shelf, cheap, long-lived and effective for
  monitoring changes in pressure, temperature and
  activity
• Tools for monitoring reservoir interval pressures are
  also off-the-shelf, but more expensive and longevity is
  less than 10 years
• Continuous monitoring is possible, but expensive and
  requires complex analysis combined with a very good
  geological model and field history
CO2CRC Participants




Supporting Partners: The Global CCS Institute | The University of Queensland | Process Group | Lawrence Berkeley National Laboratory | Government of South Australia | CANSYD Australia



            Established & supported under the Australian Government’s Cooperative Research Centres Program
Naylor area Pre-production potentiometric surface
Onshore Otway Basin: declining pressure with time




                                      Naylor-1   Croft-1
Hydrographs from the Unconfined Aquifer
                                              Date
                 1/10/00       13/02/02   28/06/03   9/11/04       24/03/06
                  0



                  2    ~3.5m


                  4
Depth (metres)




                  6                                            BORE 141239
                                                               BORE 141240
                                                               BORE 141241
                  8



                 10



                 12
Long-term Monitoring of Deep Aquifer
                                          Reduced Water Levels in Deep Bores (relative to AHD)
                                                                                    Date
                 14/11/84   23/01/87   2/04/89   11/06/91   19/08/93     28/10/95          5/01/98   15/03/00   24/05/02   1/08/04     10/10/06   18/12/08
                  0


                                                                       Pump test
                  5

                                                                                                                                     BORE 84288
                                                                                                                                     BORE 84290
                 10                                                                                                                  BORE 84291
                                                                                                                                     BORE 85937
                                                             Test impacts                                                            BORE 85942

                 15
Depth (metres)




                 20




                 25




                 30




                 35
Groundwater Resources in Victoria

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Groundwater and CO2CRC - insights from the Otway project and monitoring activities

  • 1. Groundwater and CO2CRC- Insights from the Otway Project and Monitoring Activities Allison Hortle Senior Researcher, Petroleum Hydrogeology Cooperative Research Centre Presenting to: GCCSI for Greenhouse Gas Groundwater Thematic Working Group Technologies (CO2CRC) Initial Workshop © CO2CRC Canberra, 3 May, 2011 All rights reserved
  • 2. M&V Goals • To monitor the freshwater aquifers to demonstrate that they are unaffected by the injection and storage of CO2 • To set-up a long term sentinel monitoring system • To combine the hydrogeology and the geochemistry with the atmospheric and soil gas program to develop a methodology for an integrated surface and sub-surface monitoring system • Create public confidence in “decarbonisation” technology and demonstrate that this technology can co-exist with existing exploitable resources
  • 3. Concept of the CO2CRC Otway Project Fluid Sampling Field Lab. Supercritical CO2 from Buttress-1 80% CO2 : 20% CH4
  • 4. Monitoring at the CO2CRC Otway site δ
  • 5. Schematic Stratigraphic Column of Otway Basin Port Campbell Limestone Aq. • Unconfined to semi-confined • Major local freshwater source; dairy, irrigation, domestic, etc Dilwyn Formation Aquifer • Confined, freshwater • Future urban water resource • Limited current use Waarre Aq.
  • 6. Groundwater Monitoring Stations • 24 Port Campbell Limestone • 3 Dilwyn Aquifer • 5 Pre-injection sampling trips • 4 Post-injection sampling trips
  • 7. Monitoring groundwater levels Cap • Install downhole pressure and Cable permanently temperature sensors installed Steel Cable • Provide real-time measurements of fluctuations in water levels Waterlevel 5-10m • Bi-annual downloads Datalogger Screen
  • 8. Field Sampling • At each site, pumped water was monitored for: –pH, Eh, EC, DO and temperature through a flow cell until stable readings were acquired • A set of samples were field titrated for alkalinity • A set of samples were analysed for reduced Fe2+ through the portable mass spectrophotometer • Sets were obtained for comparison of field and lab results to determine if field processing is necessary
  • 10. Water levels in the Dilwyn Confined Aquifer
  • 11. Outcomes to date • Groundwater composition has not changed between pre- and post- injection • No evidence of any changes in water level or temperature associated with CO2CRC activities • All data has been given to landowners, consequently they are still very supportive • We have demonstrated that no change has occurred at any of the monitoring stations – this is not the same as evidence of containment
  • 12. What is a monitoring network? • Monitor pre-existing wells, both groundwater and petroleum • Under what circumstances will these installations “see” changes related to CO2? • What volume, how far away from leak, what impacts? • How do you define an acceptable detection limit? pH, pressure, HCO3?
  • 13. Groundwater Monitoring Cap • Standard practice, inexpensive, off-the Cable permanently shelf tools installed Steel Cable • Provide real-time measurements of fluctuations in water levels and Waterlevel temperature and conductivity 5-10m Datalogger • Still produce large amounts of data Screen
  • 14. Permanent Downhole Monitoring • Becoming more standard in oil & gas industry • Real-time monitoring of pressure, temperature and possibly fluids • Much better reservoir management • Drawbacks are costs and longevity • Large amounts of data are produced, requiring complex and time-consuming analyses Schmidt, H.S., Nordtvedt, J-E., Nygaard, O. and Erskine, S., 2002, Reservoir management of gas fields using permanent sensors, World Oil, April, 2002, Vol. 223, No. 4, http://www.worldoil.com/April- 2002-Reservoir-management-of-gas-fields-using-permanent-sensors.html
  • 15. Cranfield, EOR, USA (SEACARB) • PDS in injection interval, PT, and • AMZI: 120m above injection zone, changes in pressure in injection zone are not apparent in AZMI • Groundwater: geochemical sampling of aquifers at 70- 100m; Ag, Al, As, Ba, Ca, Cd, Cr, Cu, Fe, K, Mg, Mn, Mo, Na, Pb, Se, Zn (Cations), F-, Cl-, SO42-, Br-, NO3-, PO43- (Anions), TOC, TIC, pH, Alkalinity, VOC, dC13. http://bittooth.blogspot.com/2010/03/carbon-sequestration-sites-and-their.html
  • 16. Ketzin, Germany (CO2SINK) • Atmospheric monitoring: tunable diode laser system for CO2 and methane • Gas monitoring: surface soil flux (20 stations), methane @ 2 m (10 wells) • Groundwater: 2 multisensor monitoring wells Wuerdemann, et al., 2010
  • 17. Summary • Groundwater can be monitoring using geochemistry or pressure; pressure propagates further than CO2 plume • Tools for monitoring groundwater pressures (heads) are off-the-shelf, cheap, long-lived and effective for monitoring changes in pressure, temperature and activity • Tools for monitoring reservoir interval pressures are also off-the-shelf, but more expensive and longevity is less than 10 years • Continuous monitoring is possible, but expensive and requires complex analysis combined with a very good geological model and field history
  • 18. CO2CRC Participants Supporting Partners: The Global CCS Institute | The University of Queensland | Process Group | Lawrence Berkeley National Laboratory | Government of South Australia | CANSYD Australia Established & supported under the Australian Government’s Cooperative Research Centres Program
  • 19. Naylor area Pre-production potentiometric surface
  • 20. Onshore Otway Basin: declining pressure with time Naylor-1 Croft-1
  • 21.
  • 22. Hydrographs from the Unconfined Aquifer Date 1/10/00 13/02/02 28/06/03 9/11/04 24/03/06 0 2 ~3.5m 4 Depth (metres) 6 BORE 141239 BORE 141240 BORE 141241 8 10 12
  • 23. Long-term Monitoring of Deep Aquifer Reduced Water Levels in Deep Bores (relative to AHD) Date 14/11/84 23/01/87 2/04/89 11/06/91 19/08/93 28/10/95 5/01/98 15/03/00 24/05/02 1/08/04 10/10/06 18/12/08 0 Pump test 5 BORE 84288 BORE 84290 10 BORE 84291 BORE 85937 Test impacts BORE 85942 15 Depth (metres) 20 25 30 35