Near-Surface Monitoring at Geologic CO2 Storage...
Transcript of Near-Surface Monitoring at Geologic CO2 Storage...
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Near-Surface Monitoring at Geologic CO2 Storage Sites
IEAGHG Summer School Austin, Texas, USA, 6-11 July 2014
Katherine Romanak,
The University of Texas at Austin
Bureau of Economic Geology
Gulf Coast Carbon Center/STORE
Photo by Striker TM
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One Geologist’s Story
National Museum of Natural History
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One Geologist’s Story
*
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Work in CCS
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Presentation Outline
• Near-surface versus deep monitoring
• Challenges of near-surface monitoring
• Strategies and tools for near-surface leak detection
• Proving a negative
• Real life example
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Potential CO2 Migration Pathways
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• Brine leakage through faults/wells to the shallow subsurface
• Along-dip water displacement
Brine Migration Pathways
Nicot et. al, 2008, GCCC Digital Publication Series #08-03g
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Developing a Monitoring Plan
1. Site Characterization-Primary means of protection. High level of assurance required for permitting
4. Monitoring Plan
Verification Monitoring
Does what happened
conform to predictions?
Assurance Monitoring
No unwanted outcomes
3. Project Design-Design injection to further minimize perceived risk
2. Risk Assessment-Aided by modeling, identifies potential unwanted outcomes
Deep subsurface Near-surface
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• Deep (verification)– Verify containment
– Track movement of CO2
and brine
– Test models
• Near-Surface (assurance) – Detect a leak
– Quantify any release to
atmosphere
– Assess environmental impacts
– Address public concerns
Deep versus Near-Surface Monitoring
courtesy of Becky Smyth
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Aquifer and USDW
Atmosphere
Biosphere
Vadose zone
Seal
Seal
Deep
Monitoring
Zone
CO2 plume
Deep versus Near-Surface Monitoring
Near-Surface
Monitoring
ZoneShallow groundwater
Static, quiet environment,
variability is from CO2
injection, CO2/brine migration
Minimal variability, early detection, small signals
Moderate background variability, assurance of no damage to drinking water, easy access
Strong variability, dynamic, many challenges, release to atmosphere, biosphere impacts
Figure courtesy of Sue Hovorka
Reservoir
Above Zone Interval
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Near-Surface Monitoring
CHALLENGES
• Locating an anomaly
– Need wide coverage over large areas
• Attributing source of anomaly
– natural variation
– leakage
ADVANTAGES
• Inexpensive and accessible
• Monitors area near “release to atmosphere”
• Direct observation of resources
• Groundwater
• Biosphere
• Aids in assessing impacts to the environment
• Useful for responding to public concerns
• Important for quantification/accounting
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Where To Look?
• Sampling Grids– Good spatial coverage
– Expensive and time consuming
– Still doesn’t cover all area
• Targeted– Heavily based on risk
– Small spatial coverage
– More economic than grids
– Less likely to find a leak
• Remote Sensing– Excellent spatial coverage
– No land access issues.
– Interferences/vegetation
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Near-Surface Leakage Assessment
Leakage Migration Mechanism
Leakage Flux
Locate Anomaly
Attribute Source
Determine the origin
Exogenous
ReservoirNo Leakage
Generated In-situ
Intermediate Zone
No Leakage
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Leak
Soil moisture
Soil carbonate
Organics → CO2
Plant activity
Leak
Natural CO2 sources and sinks
Weather and seasons
Attribution: Signal over Noise
Mimic signal
Dampen signal
Produce CO2
Consume CO2
Background
“noise”
Leak Signal
Leak
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Popular MethodsBackground Measurements Isotopes
• Different isotopic signatures can indicate the source of CO2 whether natural or injected.
• Measure “background” CO2 for 1-3 years before project start to understand seasonal variability.
• Monitor CO2 during project and compare to background.
• Significant increase from background during a project could signal a leak
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Popular Methods-Challenges
• Natural CO2 variability can mask a moderate leakage signal
• Requires long lead time
• “Baseline” will be dynamic – climate, land use, and
ecosystem variations during a project
• Background CO2 cannot be measured across all potential leak points
• Not always definitive
Background Measurements Isotopes
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Where To Look?
Complex migration pathways and
transport mechanisms
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Available Monitoring Tools
20 subsurface12 near-surface5 atmospheric
Description,
Benefits
Challenges
http://www.netl.doe.gov/technologies/carbon_seq/refshelf/MVA_
Document.pdf
January 2009
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Atmospheric Methods
DOE/NETL-311/081508, January 2009
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Near-Surface Methods
DOE/NETL-311/081508, January 2009
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ZERT Controlled Release Site
• Zero Emissions Research and Technology Center
• Montana State University, Bozeman
• Controlled CO2 release
• Leakage scenario for near surface monitoring research
• 98-m-long horizontal pipe
• 2 meters below surface in groundwater
• 6 zones of CO2 release
Spangler et al., 2009 Energy Procedia,
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• LIDAR
• Soil gas geochemistry
• Water chemistry
• Plant stress
• CO2 flux chambers
• Eddy covariance
• Tracers
• Shallow geophysical
Monitoring Tools Tested At ZERT
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LIDAR: Light Detection and Ranging
• Optical remote sensing
technology using light
(sometimes generated by
a laser)
• Can determine CO2
concentrations or detect
plant stress.
• Can indicate plant stress
before it is visible to the
eye.
Male et al.,
Environ Earth
Science (2010)
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Eddy Covariance • Uses statistical analysis of
atmospheric data to calculate
vertical turbulent fluxes.
• Complex, uses many
assumptions, much data
• Proven technology in
atmospheric monitoring
• At ZERT showed limits on
detection sensitivity.
– No detection of Release 1
( 0.1 t CO2/day)
– Detection of Release 2
(0.3 t CO2/day)
Lewicki et al., Energy Procedia 1 (2009)
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CO2 Flux Chambers
• Measures the leakage of
CO2 to atmosphere
• Accurate
• Small measurement area so
time intensive
• Flux does not always
represent CO2
concentrations in the soil
• Does not distinguish signal
from noise without extensive
background measurements
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Groundwater Chemistry• Measures CO2 input indirectly
– Results of CO2 input (e.g. mineral dissolution), not CO2
itself
– Tracers
• Noble gases, stable isotopes
• Depends on aquifer sediments
• Measures brine directly
• Needs background
• At ZERT found fluctuating geochemistry
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Introduced Tracers - PFT• Perfluorocarbon Tracers
(PFTs)
• Low natural background
levels – (don’t need
background measurements)
• Excellent detection limits
• Assumed inert and stable
• Powerful greenhouse gases
• Many false positives
• Cannot quantify CO 2
Fig. 10. Contour plots representing soil–gas tracer concentrations at 1 m
depth measured at the points marked by black dots. Colors display relative
tracer concentration within each set with pinks and reds the highest, orange
and yellow medium and green and blues are the lowest amounts of tracer.
Strazisar et al., 2009, International Journal of Greenhouse Gas Control
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Shallow Geophysical
• Resistivity and
electromagnetic
induction survey
• Shows high permeability
layers and migration
pathways
• Can detect CO2
Resistivity/depth profiles acquired along an east/west line
through the vertical injection well before (upper) and after
(lower) CO2 injection. Area made more
conductive (less resistive) by the injection of CO2 is
depicted by dashed red line. Strazisar et al., 2009,
International Journal of Greenhouse Gas Control
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Soil GasGeochemistry
• Two approaches
– Concentration-based
• Measure CO2 in soils and
compare to background
– Process-based
• Use ratios among major gases
(CO2, CH4, N2, O2) to identify near
surface processes
• Successfully identified signal from
noise at ZERT without using
background measurements
• Can potentially quantify a leak
• Still a very new method
Romanak et al, 2012
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Challenge: Proving A Negative
Example:
SACROC Oilfield, West Texas
40 years CO2 injection for
enhanced oil recovery
150 Mt CO2 injected
75 Mt recovered and
recycled
No indication of impact to
groundwater quality
Where is the rest?
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Real Example:
Allegation of a Leaknear the
Weyburn-Midale Monitoring and Storage Project
Saskatchewan Canada
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IEAGHG Weyburn-Midale CO2
Monitoring and Storage Project• Largest geologic CO2
monitoring and storage
project
• Since 2000 > 24 M tonnes of
CO2 injected
• CO2-EOR operated by
Cenovus Energy
• Studied by an international
team of CO2 storage experts
• Managed by Petroleum
Technology Research Centre
(PTRC)
www.PTRC.ca
Rostron and Whittaker, Energy Procedia 4 (2011)
3636–3643
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News of a “Leak” at the Kerr FarmJanuary 11, 2011
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Alleged Land Disturbances
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Petro-Find Conclusion
“The...source of the high
concentrations of CO2 in
soils of the Kerr property is
clearly the anthropogenic
CO2 injected into the
Weyburn reservoir.”
Source: Lafleur, P. 2010. Geochemical Soil Gas
Survey: A Site Investigation of SW30-5-13-W2M
Weyburn Field, Saskatchewan. Saskatoon, SK:
Petro-Find Geochem Ltd.)
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Petroleum Technology Research
Centre Response
“Researchers, engineers, geologists and
geophysicists involved in the IEAGHG
project have reviewed the Petro-Find
report and concluded that it does not
support its claim.”PTRC Response to Petro-Find report
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Why the Confusion?
• Vadose zone CO2 is
naturally variable
• Injected (anthropogenic)
CO2 is isotopically similar
to natural CO2
• Comparison with
background data
imprecise
– Kerr Farm not in
Weyburn monitoring
areas
Background Area
Monitoring
Grid
Kerr Quarter
Section
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Investigations in Response to
Allegation
Third PartyThe OperatorEuropean Research Team
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Third PartyThe OperatorEuropean
Research Team
CONCLUSION: NO LEAKAGE
Investigations in Response to Allegation
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Validating the Allegation
PetroFind study used
as reconnaissance
survey
Targeted approach
• 10 sampling
locations
• Minimal number of
analytes
• Process-based soil
gas method
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Results
CO2 is from
biologic
respiration with
some dissolution
of CO2 into
groundwater. No input of
exogenous gas
from depth
Methane oxidation
is negligible
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Need protocol for allegation response that is:
Lessons From Kerr Farm Incident
Different studies,
Different approaches
Different tools
Same conclusion
NO LEAK!
• Effective
• Economical
• Efficient
• High level of certainty
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Summary of Near Surface Monitoring
• Near- surface monitoring is for assurance; including leak detection, assessing environmental impacts, quantifying leakage, and addressing public concerns.
• The biggest challenge is separating leakage signal from background noise.
• Most approaches require at least one year of background monitoring.
• Background monitoring may not capture full variability over the life of a project, requires a lead time, and cannot be done everywhere within a project' boundaries.
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Summary of Near Surface Monitoring
• In some ways, monitoring attempts to prove a negative
• There are many tools and approaches that can be used.
All have benefits and challenges. A site specific
combination of approaches may be required.
• There is a need for integrated, cost effective, efficient,
economical monitoring plans for industry.
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Contact InformationKatherine Romanak
Gulf Coast Carbon Center
Bureau of Economic Geology
The University of Texas at Austin
http://www.beg.utexas.edu/gccc/
http://www.storeco2now.com/