geological sequestration of c carbon sequestration in sedimentary basins module 4: sleipner project...

27
ological Sequestration of C Carbon Sequestration Carbon Sequestration in Sedimentary Basins in Sedimentary Basins Module 4: Sleipner Module 4: Sleipner Project Project Maurice Dusseault Department of Earth Sciences University of Waterloo Most of these slides are from a presentation by: Tore A Torp , Dr.ing., Adviser CO 2 Storage, StatoilHydro ASA, Norway

Upload: mckayla-mangham

Post on 14-Dec-2015

218 views

Category:

Documents


2 download

TRANSCRIPT

Page 1: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C

Carbon SequestrationCarbon Sequestrationin Sedimentary Basinsin Sedimentary Basins

Module 4: Sleipner Module 4: Sleipner ProjectProject

Maurice DusseaultDepartment of Earth Sciences

University of WaterlooMost of these slides are from a presentation by:

Tore A Torp, Dr.ing., Adviser CO2 Storage, StatoilHydro ASA, Norway

Page 2: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C2

Time Magazine,Time Magazine,17. May 200417. May 2004

Sleipner COSleipner CO2 2

injection:injection:

- Decided in 1992- Decided in 1992- In operation since - In operation since 19961996- 1 million tonne - 1 million tonne COCO22/year/year

Tore A Torp

Page 3: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C

North Sea, Sleipner North Sea, Sleipner About 2,800 tonnes of carbon dioxide

are separated daily from Sleipner West's gas production and injected into the Utsira sandstone formation (aquifer), rather than released to the air.

Why? Purely economics from the gov’t…

But… Good Politics as well (Norway, EU, StatoilHydro, joint funding…)

Page 4: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C

SleipnerSleipner

9.5% CO2 in the produced gas They would …

Be penalized a bit by having less pure gas

Have to pipeline it at extra cost So…

It is better to separate on platform And re-inject the CO2 into a shallow

stratum, the Utsira Sandstone

Page 5: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C

Experience with COExperience with CO22 & & InjectionInjectionEnhanced Oil Recovery (Texas, Hungary, Turkey, Brazil, Croatia)

Natural gas cleaning Transport – Pipelines & ShipsNatural gas re-injectionNatural gas underground storageBut, SLEIPNER is the first project to massively inject CO2 without EOR

application - Sequestration

Page 6: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C6

COCO22-tankers, 1500 m-tankers, 1500 m3 3

capacitycapacity

Tore A Torp

Page 7: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C7

Sleipner Facility 2004Sleipner Facility 2004

Tore A Torp

Page 8: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C

Sleipner FacilitySleipner Facility

Page 9: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C

Injection into the Utsira Injection into the Utsira Fmn.Fmn.

CO2 Injection Well in "Utsira"

9

Sleipner A

Sleipner T

UtsiraFormation

Heimdal Formation

Sleipner ØstProduction and Injection

Wells

CO2

CO2 Injection Well1000m

2000m

2500m

0

500m

1500m

1000m

0 500m

1500m

Tore A Torp

Page 10: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C

The Utsira FormationThe Utsira Formation

10

Tore A Torp

Page 11: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C

The Utsira FormationThe Utsira Formation High porosity sandstone

~30% porosity Permeabilities > 1 D (up to +10 D) H2O saturated, no gas or oil… 200 m thick, with a modest central shale

zone that appears continuous Large volumes available

Regionally continuous 50-60 million m3 capacity per km2

Excellent lateral transmissivity!

Page 12: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C12

StatoilBPExxonMobilTotalNorsk HydroVattenfall

BGSBRGMGEUS

IFPNITG-TNO

SINTEF

IEA Greenhouse Gas R&D ProgrammeSchlumberger ResearchNO, DK, NL, FR & UK Authorities

SALINE AQUIFER CO2 STORAGE PROJECT

Page 13: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C

COCO22 Zone Growth Zone Growth

Page 14: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C14

Time-lapse seismic datasets of CO2 stored in Utsira Time-lapse seismic datasets of CO2 stored in Utsira formationformation

Tore A Torp

Page 15: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C15

1 km

Plume outline June 2006

Plume outline Oct 2001

8,4 million tonnes injected over 10 years Plume area: 2,8 km2 (1,3 km2 in 2001) Plume long axis: 3760 m Maximum distance from injection point:

2560m Maximum speed of front since 2004: 250

m/year, Distance from CO2 to wells:

Exploration well 15/9-13: 430m, decreasing about 12 m/year

D-template: about 2 km straight west of northern plume 15/9-19 wells: about 4,5 km north of plume

3,7

6 k

m

Plume extension & top Utsira time map

saddle

Amplitude maps of the uppermost horizon, in 2001 (left), 2004 (middle) and 2006 (right). Hot colours represent higher amplitudes and thicker CO2 accumulation.

15/9-13

430m

Injection point

Seismic section

COCO22 distribution June 2006 distribution June 2006

Tore A Torp

Page 16: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C16

Simulated picture of the distribution of CO2 after three years.

Radius of largest bubble 800 m and the total plume 200 m high.Ref: SINTEF Petroleum 2001

Tore A Torp

Page 17: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C17

Dissolution of CO2 in the Utsira Brine

Year 2021 Year 2412

Year 2621 Year 5019 Year 7018

Source: Gemini No. 1, 2004 (NTNU and Sintef)

Tore A Torp

Page 18: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C

SACS Project 1998-2002SACS Project 1998-2002

18

WHAT WAS ACHIEVED:

• 3D Seismic proven, Gravimetry tested • Reservoir simulation tools partly proven • Geology and Geochemistry of “Utsira” mapped• Reason to expect the CO2 to stay for thousands of years

DOCUMENTATION• “SACS Best Practice Manual, 1.version.”• Download from www.co2store.org, see page “SACS”.

Tore A Torp

Page 19: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C19

Demonstrations of CODemonstrations of CO22 storage storage

SLEIPNER SNØHVIT

WEYBURN

IN SALAH

GORGONK12B Source: IEA GHG

FRIO BRINE

KETZIN

Nagaoka

Page 20: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C20

Sleipner CO2 Sleipner CO2 InjectionInjection

Page 21: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C21

What is keeping the COWhat is keeping the CO22 there? there?

Trapping MechanismsClosure - from day one – faults?Micro-pore trapping - during injection - lasting

Dissolution in water - sinking to the bottom – centuries

Mineral binding - precipitating solids – centuries/millennia

Tore A Torp

Page 22: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C22

Possible Leakage?Possible Leakage?

Leakage paths?WELLS - Corrosion of cement & steelFaults/Cracks – Overpressure criticalUnderground fluid mobility – Site specific

PreventionDetectionRemediation

Tore A Torp

Page 23: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C

Monitoring: Safety Over TIME?Monitoring: Safety Over TIME?Before start: Site selection, Planning and Risk assessment =>licence

During injection: Monitoring – “Watch the barn doors” => report

Closure: Monitoring and long-term risk => agreement

Post-closure: Monitoring gradually less => hand-over Safety against leakage will be better over time!

23

Tore A Torp

Page 24: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C

COCO22 Capture and Storage (CCS) Capture and Storage (CCS)

24

Leg 2: COST of Capture Energy use Costs Better technologies

Leg 1: TRUST in Storage Methods from oil and gas industry Geology varies from place to place More demonstrations

Pace: CO2 Transport

• Pipeline

• Ship

Large projects

Tore A Torp

Page 25: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C25

Page 26: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C

Total Lacq Project (~60 MM Total Lacq Project (~60 MM €)€) Gas processing plant Steam needs, to be done with CH4 + O2

This results in almost pure CO2 + H2O So, they plan to inject the CO2 into the

Lacq natural gas reservoir, displace a little bit more gas

150,000 t in 2 yrs, starting in 2008 …the first integrated CO2 capture system

using oxy-fuel combustion combined with storage in a depleted hydrocarbon field.

Page 27: Geological Sequestration of C Carbon Sequestration in Sedimentary Basins Module 4: Sleipner Project Maurice Dusseault Department of Earth Sciences University

Geological Sequestration of C

SUMMARY…SUMMARY… First genuine sequestration project High permeability, high porosity

reservoir for the CO2, good seal, etc. Not fully driven by economics (gov’t

subsidy) A model for future sequestration

projects…