Satellite-based measurements of surface deformation reveal fluid flow associated with the geological storage of carbon dioxide

Interferometric Synthetic Aperture Radar (InSAR) data, gathered over the In Salah CO2 storage project in Algeria, provide an early indication that satellite‐based geodetic methods can be effective in monitoring the geological storage of carbon dioxide. An injected mass of 3 million tons of carbon di...

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Published inGeophysical research letters Vol. 37; no. 3; pp. np - n/a
Main Authors Vasco, D. W., Rucci, A., Ferretti, A., Novali, F., Bissell, R. C., Ringrose, P. S., Mathieson, A. S., Wright, I. W.
Format Journal Article
LanguageEnglish
Published Washington, DC Blackwell Publishing Ltd 01.02.2010
American Geophysical Union
John Wiley & Sons, Inc
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Abstract Interferometric Synthetic Aperture Radar (InSAR) data, gathered over the In Salah CO2 storage project in Algeria, provide an early indication that satellite‐based geodetic methods can be effective in monitoring the geological storage of carbon dioxide. An injected mass of 3 million tons of carbon dioxide from one of the first large‐scale carbon sequestration efforts, produces a measurable surface displacement of approximately 5 mm/year. Using geophysical inverse techniques, we are able to infer flow within the reservoir layer and within a seismically detected fracture/fault zone intersecting the reservoir. We find that, if we use the best available elastic Earth model, the fluid flow need only occur in the vicinity of the reservoir layer. However, flow associated with the injection of the carbon dioxide does appear to extend several kilometers laterally within the reservoir, following the fracture/fault zone.
AbstractList Interferometric Synthetic Aperture Radar (InSAR) data, gathered over the In Salah CO2 storage project in Algeria, provide an early indication that satellite-based geodetic methods can be effective in monitoring the geological storage of carbon dioxide. An injected mass of 3 million tons of carbon dioxide from one of the first large-scale carbon sequestration efforts, produces a measurable surface displacement of approximately 5 mm/year. Using geophysical inverse techniques, we are able to infer flow within the reservoir layer and within a seismically detected fracture/fault zone intersecting the reservoir. We find that, if we use the best available elastic Earth model, the fluid flow need only occur in the vicinity of the reservoir layer. However, flow associated with the injection of the carbon dioxide does appear to extend several kilometers laterally within the reservoir, following the fracture/fault zone.
Interferometric Synthetic Aperture Radar (InSAR) data, gathered over the In Salah CO 2 storage project in Algeria, provide an early indication that satellite‐based geodetic methods can be effective in monitoring the geological storage of carbon dioxide. An injected mass of 3 million tons of carbon dioxide from one of the first large‐scale carbon sequestration efforts, produces a measurable surface displacement of approximately 5 mm/year. Using geophysical inverse techniques, we are able to infer flow within the reservoir layer and within a seismically detected fracture/fault zone intersecting the reservoir. We find that, if we use the best available elastic Earth model, the fluid flow need only occur in the vicinity of the reservoir layer. However, flow associated with the injection of the carbon dioxide does appear to extend several kilometers laterally within the reservoir, following the fracture/fault zone.
Interferometric Synthetic Aperture Radar (InSAR) data, gathered over the In Salah CO sub(2) storage project in Algeria, provide an early indication that satellite-based geodetic methods can be effective in monitoring the geological storage of carbon dioxide. An injected mass of 3 million tons of carbon dioxide from one of the first large-scale carbon sequestration efforts, produces a measurable surface displacement of approximately 5 mm/year. Using geophysical inverse techniques, we are able to infer flow within the reservoir layer and within a seismically detected fracture/fault zone intersecting the reservoir. We find that, if we use the best available elastic Earth model, the fluid flow need only occur in the vicinity of the reservoir layer. However, flow associated with the injection of the carbon dioxide does appear to extend several kilometers laterally within the reservoir, following the fracture/fault zone.
Author Wright, I. W.
Ferretti, A.
Vasco, D. W.
Mathieson, A. S.
Rucci, A.
Novali, F.
Ringrose, P. S.
Bissell, R. C.
Author_xml – sequence: 1
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  surname: Vasco
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– sequence: 2
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  organization: Tele-Rilevamento Europa, Milan, Italy
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  surname: Novali
  fullname: Novali, F.
  organization: Tele-Rilevamento Europa, Milan, Italy
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  surname: Bissell
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  fullname: Mathieson, A. S.
  organization: BP Alternative Energy, Middlesex, UK
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  surname: Wright
  fullname: Wright, I. W.
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Issue 3
Keywords satellites
carbon dioxide
models
projects
interferometry
reservoirs
storage
monitoring
Carbon sequestration
greenhouse gas
Flow(fluid)
displacements
fault zones
deformation
Elastic Earth
injection
fractures
Synthetic aperture radar
Language English
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American Geophysical Union
John Wiley & Sons, Inc
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Snippet Interferometric Synthetic Aperture Radar (InSAR) data, gathered over the In Salah CO2 storage project in Algeria, provide an early indication that...
Interferometric Synthetic Aperture Radar (InSAR) data, gathered over the In Salah CO 2 storage project in Algeria, provide an early indication that...
Interferometric Synthetic Aperture Radar (InSAR) data, gathered over the In Salah CO sub(2) storage project in Algeria, provide an early indication that...
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SubjectTerms Carbon capture and storage
Carbon dioxide
Carbon sequestration
Climate change
deformation
Earth
Earth sciences
Earth, ocean, space
Exact sciences and technology
Fluid flow
Fluids
Fracture mechanics
Geodetics
geological storage
Geology
Geophysics
Hydrology
InSAR
Remote sensing
Reservoirs
Rock deformation
Satellites
Title Satellite-based measurements of surface deformation reveal fluid flow associated with the geological storage of carbon dioxide
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