stanford university global climate & energygy j project · pdf filestanford university...

33
Stanford University Global Climate & Energy Project Public Workshops on Carbon Capture and Sequestration Bloomberg National Headquarters, NY and Carbon Dioxide Capture and Sequestration in Rayburn House Office Bldg., Washington, DC March 5&6, 2009 Professor Sally M Benson Deep Geological Formations Professor Sally M. Benson Energy Resources Engineering Department Director, Global Climate and Energy Project Stanford University Science and technology for a low GHG emission world.

Upload: dinhnhan

Post on 27-Feb-2018

218 views

Category:

Documents


4 download

TRANSCRIPT

Page 1: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Stanford UniversityGlobal Climate & Energy Projectgy j

Public Workshops on Carbon Capture and SequestrationBloomberg National Headquarters, NY and

Carbon Dioxide Capture and Sequestration in

g q ,Rayburn House Office Bldg., Washington, DCMarch 5&6, 2009

Professor Sally M Benson

p qDeep Geological Formations

Professor Sally M. BensonEnergy Resources Engineering DepartmentDirector, Global Climate and Energy Project

Stanford Universityy

Science and technology for a low GHG emission world.

Page 2: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Carbon Dioxide Capture and Geologic Storage

CaptureCaptureUndergroundUnderground

InjectionInjectionPipelinePipeline

TransportTransportCompressionCompression

Page 3: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Options for CO2 Capture

• Post-combustion– Scrub CO2 after combustionScrub CO2 after combustion– Established technology

• Pre-combustion (IGCC)– Convert coal to a gas before

combustion– Established technology for

other applications– Not demonstrated for

power production

• Oxygen combustion (Oxy-fuel)– Use O2 instead of air for

combustioncombustion– Not demonstrated for power

production

Page 4: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

What Types of Rock Formations are Suitable for Geological Storage?g g

Rocks in deep sedimentary basins are suitable for CO2 storage.p y 2 g100 km

Northern California Sedimentary Basinhttp://www.glossary.oilfield.slb.com/

Map showing world-wide sedimentary basins

Example of a sedimentary basin with alternating layers of sandstone and shale.

1 inch

Sandstone

Page 5: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Options for Geological Storage

Page 6: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Oil and Gas Reservoirs

Page 7: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Coal Beds

Page 8: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Saline Aquifers

Page 9: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Expert Opinion about Storage Safety and Securityy y

“ Observations from engineered and natural analogues as well as models suggest that the fraction retained in appropriately selected and managed geological reservoirs is very likely* to exceed 99% over 100 years and is likely** to exceed 99% over 1,000 years.”

“ With appropriate site selection informed by available subsurface information, a monitoring gprogram to detect problems, a regulatory system, and the appropriate use of remediation methodsto stop or control CO2 releases if they arise, the local health, safety and environment risks of ygeological storage would be comparable to risks of current activities such as natural gas storage, EOR, and deep underground disposal of acid gas.”g

* "Very likely" is a probability between 90 and 99%.** Likely is a probability between 66 and 90%.

Page 10: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Evidence to Support these Conclusions

• Natural analogs– Oil and gas reservoirs

CO reservoirs– CO2 reservoirs• Performance of industrial analogs

– 30+ years experience with CO2 EOR– 100 years experience with natural gas 00 yea s e pe e ce t atu a gas

storage– Acid gas disposal

• 25+ years of cumulative performance of actual CO2 storage projectsactual CO2 storage projects

– Sleipner, off-shore Norway, 1996– Weyburn, Canada, 2000– In Salah, Algeria, 2004– Snovhit, Norway, 2008

~35 Mt/yr are injected for CO2-EOR

Page 11: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Natural Gas Storage

• Seasonal storage to meet winterto meet winter demands for natural gas

• Storage formations• Storage formations– Depleted oil and

gas reservoirsAquifers– Aquifers

– Caverns

Page 12: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Sleipner Project, North Sea

1996 to present1 Mt CO i j ti /1 Mt CO2 injection/yrSeismic monitoring

Courtesy Statoil

Page 13: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Weyburn CO2-EOR and Storage Project

• 2000 to present• 1-2 Mt/year CO2 injection• CO2 from the Dakota

G ifi ti Pl t i th U SGasification Plant in the U.S.

Photo’s and map courtesy of PTRC and Encana

Page 14: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

In Salah Gas Project

Gas Processing and CO2 Separation Facility

In Salah Gas Project- Krechba, Algeria

Gas Purification- Amine Extraction

1 Mt/year CO2 Injection1 Mt/year CO2 InjectionOperations Commence

- June, 2004 Courtesy of BP

Page 15: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Snohvit, Norway

• Snohvit Liquefied Natural Gas Project (LNG)– Barents Sea, Norway

• Gas Purification (removal of 5-8% CO2)– Amine Extraction

0 7 Mt/year CO Injection• 0.7 Mt/year CO2 Injection– Saline aquifer at a depth of 2,600 m (8530 ft) below sea-bed

• Sub-sea injectionj• Operations Commence

– April, 2008

Courtesy StatoilHydro

Page 16: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Key Elements of a Geological Storage Safety and Security Strategy

Financial

“ With appropriate site selectioninformed by available subsurface information, amonitoring program to detect

“… risks similar to existing activities such as natural gas storage and EOR.”

Regulatory Oversight

Responsibility “… the fraction retained is likely to exceed 99% over 1,000 years.”

g p gproblems, a regulatory system, and the appropriate use of remediation methods…”

IPCC, 2005

Remediation

Monitoringg

Safe Operations

Storage Engineering

Site Characterization and Selection

Fundamental Storage and Leakage Mechanisms

Page 17: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Density of Carbon Dioxide

Storage at Depths Greater p

than 800 m (2,600 ft)

Page 18: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Sequestration Mechanisms

• Injected at depths of 1 km or deeper into k ith tirocks with tiny pore spaces

• Primary trapping– Beneath seals of low permeability rocksBeneath seals of low permeability rocks

• Secondary trapping– CO2 dissolves in water

CO i t d b ill f– CO2 is trapped by capillary forces– CO2 converts to solid minerals– CO2 adsorbs to coal

Image courtesy of ISGS and MGSC

Page 19: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

X-ray Micro-tomography at theAdvanced Light Sourceg

Micro-tomography Beamline Image of Rock with CO2

WaterCO2

Mineralgrain

2 mm

Page 20: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Multi-Phase Flow Laboratory

Replicate in situ conditionsReplicate in situ conditions- Pressure- Temperature- Brine composition

Page 21: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Multiphase Flow of CO2 and Brine

Influence of Heterogeneity

Waare C Sandstone

Heterogeneity

Influence of Buoyancy

Berea Sandstone

Page 22: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Seal Rocks and Mechanisms

• Shale, clay, and 1 E 10

1.E-07

m2 )Shale, clay, and

carbonates• Permeability barriers 1.E-16

1.E-13

1.E-10

Perm

eabl

ity (m

yto CO2 migration

• Capillary barriers to

1.E-19Gravel Course

SandSilty

sandsClayeysands

Clay Shale

P

p yCO2 migration Cappilary Barrier Effectiveness

1000

s)

10

100

Entr

y Pr

essu

re (B

ars

1Delta Plain

ShalesChannel

AbandonmentSilts

Pro-DeltaShales

Delta FrontShales

ShelfCarbonates

E

Increasing Effectiveness

Page 23: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Secondary Trapping Mechanisms Increase Over Time

Page 24: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Seismic Monitoring Data from SleipnerMany Monitoring Methods are Available

3-D Seismic

Satellite land surface deformationRemote sensing of vegetative stress

Flux Accumulation ChamberFlux Tower

Walk Away VSP

Injection RateWellhead PressureAnnulus PressureCasing Logs

Cross-Well Seismic

Casing LogsCO2 Sensors

Active Source Thermal SensorsInjection

WellMonitoring

Well

Pressure Monitoring

Page 25: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Seismic Monitoring Data from Sleipnerp

F Ch d i k t l GHGT 9 2008From Chadwick et al., GHGT-9, 2008.

Page 26: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Surface Monitoring

Detection Verification Facility(Montana State University)

Flux Tower

80 m

Field Site

Horizontal

HyperspectralImaging ofVegetationHorizontal

Injection WellVegetation

Flow Controllers

Soil Gas

Flux accumulation chamber

Page 27: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Leak Detection Using Flux Accumulation Chambers

Page 28: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

What Could Go Wrong?

Potential Consequences1. Worker safety1. Worker safety

2. Groundwater quality degradation

3. Resource damage

4. Ecosystem degradation

5 Public safety5. Public safety

6. Structural damage

7. Release to atmosphere• Well leakage (injection and abandoned Potential Release Pathways

e ease to at osp e eg ( jwells)

• Poor site characterization (undetected faults)• Excessive pressure buildup damages seal

What about a catastrophic release, like what happened at , ppLake Nyos in Cameroon?

Page 29: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Risk Management

Financial Responsibility

Financial mechanisms and institutional approaches for long term stewardship (e.g. monitoring and remediation if needed)

Regulatory Oversight

R di ti

p y

Oversight for site characterization and selection, storage system operation, safety, monitoring and contingency plans

p ( g g )

Active and abandoned well repair, groundwater cleanup, and Remediation

Monitoring

p , g p,ecosystem restoration

Monitoring plume migration, pressure monitoring in the storage reservoir and above the seal, and surface releases

Safe Operations

Storage Engineering

Well maintenance, conduct of operations, well-field monitoring and controls

Number and location of injection wells, strategies to maximize capacity and accelerate trapping and well completion design

Site Characterization and Selection

Fundamental Storage M lti h fl t i h i h i l

capacity and accelerate trapping, and well completion design

Site specific assessment of storage capacity, seal integrity, injectivity and brine migration

Fundamental Storage and Leakage Mechanisms

Multi-phase flow, trapping mechanisms, geochemical interactions, geomechanics, and basin-scale hydrology

Page 30: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Storage Security: Long Term Risk Profile

Acceptable Risk

Sit l ti

ety

and

tal R

isk

Site selectionActive and abandoned well completionsStorage engineering

P

Hea

lth S

afe

nviro

nmen

t Pressure recoverySecondary trapping mechanismsConfidence in predictive models

Injectionb i

Injection t

2 x injection i d

3 x injection i d

n x injection i d

H E

begins stops period period period

Monitor Calibrate&

Calibrate&

ModelValidateModels

ValidateModels

Page 31: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Maturity of CCS Technology

• Are we ready for CCS?

Oil and gas reservoirsOil and gas reservoirs

Saline aquifers

C lb dCoalbeds

State-of-the-art is well developed, scientific understanding is excellent and engineering methods are mature

Sufficient knowledge is available but practical experience is lacking, economics may be sub-optimal, scientific understanding is goodmay be sub optimal, scientific understanding is good

Demonstration projects are needed to advance the state-of-the art for commercial scale projects, scientific understanding is limited

Pilot projects are needed to provide proof-of-concept, scientific understanding is immature

Page 32: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Institutional Issues

• Policy and regulations to limit carbon emissions• Regulations for storage: siting, monitoring, performance

specificationsspecifications• Long term liability for stored CO2• Legal framework for access to underground pore space• Carbon trading credits• Public acceptance

None is likely to be a show stopper, but all require effort to resolve.

Page 33: Stanford University Global Climate & Energygy j Project · PDF fileStanford University Global Climate & Energygy j Project Public Workshops on Carbon Capture and Sequestration

Concluding Remarks

• CCS is an important part of the portfolio of technologies for reducing greenhouse gas emissions

• Progress on CCS proceeding on all fronts– Industrial-scale projects– Demonstration plants– Research and development

• Technology is sufficiently mature for large scale demonstration projects and commercial projects with CO EORCO2-EOR

• Research is needed to support deployment at scale– Capture: Lower the cost and increase reliability

S i I fid i– Sequestration: Increase confidence in permanence• Institutional issues need to be resolved to support

widespread deployment