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CO2 Sequestration in Hydrates with Associated Methane Gas Production - - PowerPoint PPT Presentation

Energy for the Future CO2 Sequestration in Hydrates with Associated Methane Gas Production by Prof. Arne Graue Dept. of Physics and Technology University of Bergen, NORWAY Whole Value Chain CCUS Student Week, Oct. 15 th - 19 th , 2018,


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Energy for the Future – CO2 Sequestration in Hydrates with Associated Methane Gas Production

by

  • Prof. Arne Graue
  • Dept. of Physics and Technology

University of Bergen, NORWAY

Whole Value Chain CCUS Student Week, Oct. 15th - 19th, 2018, Golden, CO, USA.

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Normal text - click to edit GAS HYDRATES

  • Solid state of gas and water where the water

molecules form a cavity that encapsulates the guest molecule.

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What is natural gas hydrate?

  • Methane and other

small non-polar (or slightly polar) molecules immersed in water will induce

  • rganisation of the

water structure that maximizes the entropy.

  • Above certain

pressures, and below certain temperatures , this results in a phase transition over to a solid like structure. The glass to the right contains water at 0 C The pipe to the left contains hydrate at 5 C

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Why are hydrates of interest?

  • Initial interest as a curiosity
  • Plugging of production and transportation pipelines

Department of Physics and Technology

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Renewed interest

– Significant amount of energy

  • Permafrost regions
  • Marine environments (high water column)

Hester and Brewer, 2009

Department of Physics and Technology

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University of Bergen - Department of Physics and Technology

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Hydrate as Energy Resource

Gas Hydrates Resource Pyramid (left). To the right is an example gas resources pyramid for all non-gas-hydrate resources.

Ref.: Fire in the Ice, U.S. Department of Energy • Office of Fossil Energy • National Energy Technology Laboratory

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Modified from "GAS HYDRATES OF NORTHERN ALASKA", January 2005 Evaluation of Alaska North Slope Gas Hydrate Energy Resources: A Cooperative Energy Resource Assessment Project US Bureau of Land Management, US Geological Survey, & State of Alaska Division of Geological and Geophysical Surveys Bob Fisk, USBLM, Anchorage, Alaska, Tim Collett, USGS, Denver, Colorado & Jim Clough, DGGS, Fairbanks, Alaska

Gas Hydrate Production Methods

  • CO2 Flood
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Normal text - click to edit Depressurization: PROS AND CONS

  • Pros

– All of the methane is accessible for production by depressurization; at sufficient low pressures

  • Cons

– Large pressure drop may be needed to initiate hydrate dissociation – Water production may represent an economic challenge and an environmental issue – Hydrate melts; causing possible unstable formation

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GAS HYDRATE PRODUCTION METHODS

  • Move the gas hydrate outside its

stability region – Depressurization – Thermal stimulation – Hydrate inhibitors

  • CO2 exchange

Hydrate stable region Pressure Temperature Hydrate Reservoir Condition Unstable region

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  • The amount of energy bound in hydrates may be more than

twice the world’s total energy resources in conventional hydrocarbon reservoirs; i.e. oil-, gas- and coal reserves

  • Simultaneous CO2 Sequestration
  • Win-win situation for gas production
  • Need no hydrate melting or heat stimulation
  • Spontaneous process
  • No associated water production
  • Formation integrity

CO2 Exchange: Project Motivation

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CO2 storage in hydrates with associated methane gas production

Challenge:

Determine exchange mechanisms during potential sequestration of CO2 to produce methane from hydrates

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Three component Phase Field Theory

 

 

                                    

  

  i i ci i i i L S bulk bulk j i i j j i j i

c F c c c M c c c F M T c c c f p T c c c f p wTg f T c c c f c c c c T T r d F              

 

) , , ( 1 ) , , , ( ) ( ) , , , ( )] ( 1 [ ) ( ) , , , , ( 4 2

3 2 1 3 1 3 2 1 3 2 1 3 2 1 3 1 , 2 2 , 2 2

 

Parameters ε and w can be fixed from the interface thickness and interface free energy. ε ij set equal to ε

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CH4 PRODUCTION INDUCED BY CO2 INJECTION

  • Provides thermodynamically more stable gas hydrate than CH4

Husebø, 2008 Experimental Conditions

Department of Physics and Technology

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Experimental Setup

CO2 & CH4 Pumps Temperature & Confining Pressure Controls High Pressure Cell Inside Bore of Magnet Insulated Lines & Heat Exchanger

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Normal text - click to edit Experimental Setup

Ou t In

P

Ou t In

CH4 CO2 Cooling Bath Insulated Lines Confining Pressure Pump Reciprocatin g Pump Pore Pressure Pumps High Pressure Cell Core Plug Confining Pressure Pore Pressure

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Normal text - click to edit Experimental Setup

Ou t In

P

Ou t In

CH4 CO2 Cooling Bath Insulated Lines Confining Pressure Pump Reciprocatin g Pump Pore Pressure Pumps MRI High Pressure Cell Core Plug Confining Pressure Pore Pressure MRI Magnet

Monitor P-V-T and MRI Intensity During Hydrate Formation

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Normal text - click to edit Volumetrics and MRI Results

MRI Intensity in Core and CH4 Volume Consumption

0.2 0.4 0.6 0.8 1 20 40 60 80 100 120 140 160 Time [hours] MRI Intensity (Inverted and normalized) Methane Consumption (normalized)

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CONDITIONS OF A HYDRATE RESERVOIR

  • Hydrate reservoirs are often found in porous media

– Sedimentary rock

Mineralogy: mainly quartz Porosity: 22-23% Permeability: 1.1 D Pore diameter: 125 microns Department of Physics and Technology

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Conditions for Methane Hydrate Formation/Dissociation

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Core Sample Design

Bentheim Sandstone

20-25% porosity, ~1.1 D Perm

  • Whole Core
  • Longitudinal Cut With

Machined Spacer to Simulate Open Fracture.

1 cm

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Sample – BH-01

Sample halves saturated With methane and water Middle space saturated With methane

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Sample – BH-01

Run – 17-39 Time – 0min Started cooling sample To 4

0 C

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Sample – BH-01

Run – 18-01 Time – 55min

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Sample – BH-01

Run – 18-03 Time – 2hr 45min

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Sample – BH-01

Run – 18-05 Time – 4hr 35min

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Sample – BH-01

Run – 18-06 Time – 5hr 30min

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Sample – BH-01

Run – 18-07 Time – 6hr 25min Methane Hydrate forming

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Sample – BH-01

Run – 18-08 Time – 7hr 20min Methane Hydrate forming

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Sample – BH-01

Run – 18-09 Time – 8hr 15min Methane Hydrate forming

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Sample – BH-01

Run – 18-10 Time – 9hr 10min Methane Hydrate forming

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Sample – BH-01

Run – 18-11 Time – 10hr 05min Methane Hydrate forming

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Sample – BH-01

Run – 18-12 Time – 11hr 00min

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Sample – BH-01

Run – 18-14 Time – 12hr 50min Methane in spacer

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Sample – BH-01

Run – 18-16 Time – 14hr 40min Methane in spacer

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Sample – BH-01

Run – 18-17 Time – 15hr 35min Methane in spacer

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Sample – BH-01

Run – 18-19 Time – 17hr 25min

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Sample – BH-01

Run – 18-37 Time – 31hr 05min

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Sample – BH-01

Run – 18-42 Time – 36hr 20min

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Sample – BH-01

Run – 18-43 Time – 37hr 15min

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Sample – BH-01

Run – 18-43 Time – 37hr 15min

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Sample – BH-01

Run – 18-57 Time – 54hr 10min

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Run – 18-59

Sample – BH-01

Time – 56hr 00min

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Progress of Hydrate Front

  • Longitudinal Profile

in Core – 5 mm from Fracture.

  • Approximately 35

Hours, ~ Equal Time Increments.

  • Hydrate Growth

Slows with Time.

0.1 0.2 0.3 0.4 0.5

  • 2

2 4 6 8 10 Distance along plug (cm) MRI Intensity

Time

Water-Filled Pores

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33-03 0.0 hrs Methane in Spacer

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33-07 0.0 hrs Sw=0.5 + Methane

5 10 15 20 25 30 5 10 15 20 25 30 Time (hrs) Volume (cm3) 0.01 0.02 0.03 0.04 0.05 0.06 0.07

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33a-01 5.0 hrs Cooling Starts

5 10 15 20 25 30 5 10 15 20 25 30 Time (hrs) Volume (cm3) 0.01 0.02 0.03 0.04 0.05 0.06 0.07

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33c-01 7.2 hrs

5 10 15 20 25 30 5 10 15 20 25 30 Time (hrs) Volume (cm3) 0.01 0.02 0.03 0.04 0.05 0.06 0.07

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33c-02 9.4 hrs

5 10 15 20 25 30 5 10 15 20 25 30 Time (hrs) Volume (cm3) 0.01 0.02 0.03 0.04 0.05 0.06 0.07

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33c-03 12.0 hrs

5 10 15 20 25 30 5 10 15 20 25 30 Time (hrs) Volume (cm3) 0.01 0.02 0.03 0.04 0.05 0.06 0.07

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33c-04 14.0 hrs

5 10 15 20 25 30 5 10 15 20 25 30 Time (hrs) Volume (cm3) 0.01 0.02 0.03 0.04 0.05 0.06 0.07

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33c-05 16.3 hrs

5 10 15 20 25 30 5 10 15 20 25 30 Time (hrs) Volume (cm3) 0.01 0.02 0.03 0.04 0.05 0.06 0.07

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33c-06 18.6 hrs

5 10 15 20 25 30 5 10 15 20 25 30 Time (hrs) Volume (cm3) 0.01 0.02 0.03 0.04 0.05 0.06 0.07

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33c-07 20.9 hrs

5 10 15 20 25 30 5 10 15 20 25 30 Time (hrs) Volume (cm3) 0.01 0.02 0.03 0.04 0.05 0.06 0.07

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33c-08 23.2 hrs

5 10 15 20 25 30 5 10 15 20 25 30 Time (hrs) Volume (cm3) 0.01 0.02 0.03 0.04 0.05 0.06 0.07

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33c-09 25.5 hrs

5 10 15 20 25 30 5 10 15 20 25 30 Time (hrs) Volume (cm3) 0.01 0.02 0.03 0.04 0.05 0.06 0.07

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33c-10 27.7 hrs

5 10 15 20 25 30 5 10 15 20 25 30 Time (hrs) Volume (cm3) 0.01 0.02 0.03 0.04 0.05 0.06 0.07

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33c-11 30.0 hrs

5 10 15 20 25 30 5 10 15 20 25 30 Time (hrs) Volume (cm3) 0.01 0.02 0.03 0.04 0.05 0.06 0.07

Core Halves Saturated with hydrate

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0.0 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34a-01 9.1 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-01 20.6 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-02 32.0 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-03 43.4 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-04 54.9 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-05 66.3 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-06 77.8 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-07 89.2 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-08 100.6 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-09 112.1 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-10 123.5 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-11 135.0 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-12 146.4 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-13 157.8 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-14 169.3 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-15 180.7 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-20 237.9 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-25 295.1 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-30 352.3 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-35 409.5 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-40 501.0 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-45 523.8 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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34b-52 603.9 hrs

0.004 0.008 0.012 0.016 100 200 300 400 500 600 Time (Hours) Intensity

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Scientific Conclusions

  • MRI Provides Unique Dynamic Data of Hydrate

Formation and Production Consistent with Conventional Results.

  • CO2 Exchange for CH4 in Hydrates Is Rapid and

Efficient.

  • No Free Water Observed During Exchange

Process.

  • Sufficient Permeability Remains During Hydrate

Formation and Subsequent Production.

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CO2 Storage in Hydrate Reservoirs with Associated Spontaneous Natural Gas Production

In-Situ imaging (MRI) of hydrate formation Methane production by CO2 injection in field test in Alaska 2012

Objectives: Experimentally and theorethically determine spontaneous methane production when hydrate is exposed to CO2; with the purpose of CO2 sequestration.

Methane hydrate reservoirs Arne Graue and Bjørn Kvamme, Dept. of Physics, University of Bergen, NORWAY Funding: ConocoPhillips, Statoil and The Research Council of Norway

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  • ConocoPhillips, USDOE and JOGMEC
  • US$ 11.6 mill funding from US DOE, total cost ca. US$30mill
  • CO2 injection

Alaska Field Injection Test 2011-2012

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Summary of Field Test (Injection Test)

Schedule:

  • Apr. 2011:

Drilling test well (Complete)

  • Nov. 2011:

Finalizing parameters for the field test Jan.-Apr. 2012: Field test Location: Prudhoe Bay operating unit in Alaska, USA Operator: ConocoPhillips Company (COP), through its wholly owned subsidiary, ConocoPhillips Alaska, Inc. Investors: The United States Department of Energy(DOE) JOGMEC; Japan Oil, Gas and Metals National Corp.

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Students and Staff :

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Iġnik Sikumi #1 Flowback/Drawdown: Gas composition

Gas Production from the Field Test

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Conclusions on Industry Collaboration

  • Mutually beneficial
  • Students exposed to experienced senior

petroleum experts

  • Access to advanced and expensive

equipment

  • Leveraged research
  • Provides qualified candidates for Norway and

the oil industry

  • Recruitment of national students
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Energy for the Future Gas Production WITH CO2 Storage in Hydrates

Department of Physics and Technology

“While this is just the beginning, this research could potentially

yield significant new supplies of natural gas.”

U.S. Energy Secretary Steven Chu, May 2nd 2012

Methane hydrates are ice-like structures with natural gas trapped inside, and are found both onshore and offshore along nearly every continental shelf in the world.

What are Methane Hydrates? Energy bound in hydrates is more than combined energy in conventional oil, gas and coal reserves

DOE, ConocoPhillips and JOGMEC at the Iġnik Sikumi test site, Alaska

Excerpt from U.S. Energy Secretary Steven Chu’s statement

…to conduct a test of natural gas extraction from methane hydrate using a unique

production technology, developed through laboratory collaboration between the University of Bergen, Norway… [D]emonstrated that this mixture

could promote the production of natural gas. Ongoing analyses of the extensive datasets acquired at the field site will be needed to determine the efficiency of simultaneous CO2 storage in the reservoirs.

UiB Laboratory Verification of Technology Field Verification of UiB Technology

< 10 year US $30 mill

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Summary

Department of Physics and Technology

Use of CO2 as a commodity: Business Case for CO2 Storage:

  • CO2 EOR
  • Integrated EOR (IEOR) with Foam: Carbon Negative Oil Production
  • Exploitation of Hydrate Energy: Carbon Neutral Gas Production

New technologies ready for industrial scale implementation:

  • Onshore in Permian Basin, USA (80% CO2EOR, EOR target 137Bbbl)
  • Offshore Opportunities: NCS, Middle East, Asia, Africa and Brazil
  • International Whole Value Chain CCUS Collaboration Offshore

Way Forward

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Thank you!