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Seismic monitoring of a unique CO2 injection site at Sleipner

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CO2 is injected into a thick sandstone layer at 800-1100 m depth below sealevel ... of Denmark and Greenland, Institut Francais du P trole, Netherlands Institute of ... – PowerPoint PPT presentation

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Title: Seismic monitoring of a unique CO2 injection site at Sleipner


1
Seismic monitoring of a unique CO2 injection site
at Sleipner
  • Ola Eiken, Statoil

2
Increasing atmospheric CO2 causes global warming.
The Kyoto agreement put limits on emissions.A
CO2 free vision
3
CO2 physical properties
Measured at HARC 2000
4
Sleipner A
5
CO2 injection well in Utsira Fm.
6
Sleipner CO2 injection
  • CO2 is injected into a thick sandstone layer at
    800-1100 m depth below sealevel
  • 97.5-98 of the injected gas is CO2
  • The sandstones have porosities of 35-40 and 1-8
    D permeability

seismic survey
7
Seismic data acquisition and processing
  • Reprocessing of base survey together with
    processing of monitor survey.
  • Comprehensive processing sequence with aim of
    maximum repeatability
  • Deterministic zero-phasing using supplied
    far-field signatures from 1994 and 1999.
  • Tidal correction based on model
  • Swath consistent static correction
  • Global frequency-amplitude match between surveys
  • New velocity analyses in CO2 injection area

8
difference
1994
october 1999
after injecting 2 mill. tons CO2 since 1996
no change above this level
top Utsira Fm.
100 ms
injection point
1000 m
9
200 m
crossline 1122
east
east
west
west
horizon A0
horizon A
100 ms
horizon A1
horizon B
horizon C
horizon D
B
D
C
.
A
A1
1994 vintage
1999 - 1994 difference
10
southwest
northeast
500 m
100 ms
B
C
D
A
.
A1
1994 vintage
11
amplitude Horizon B time
500 m
.
.
16000 8000 0 amplitude
929 949 969 ms
12
Model of reflection from top and bottom of a thin
CO2-filled layer (with velocity 1450 m/s).
Bottom of layer is at constant depth.
Maximum amplitude
Pulse 0 1 2 3 4 5 6 7 8
9 10 11 12 13 14
Layer thickness in meters
13
Estimated mass based on seismic time-delay
Time delay Gas column height
Uncertainty distribution assessed in each
factor. Monte Carlo simulation.
14
Possible causes of discrepancies in mass
calculations
  • CO2 is partly accumulated in thin layers and
    partly distributed at low saturations between the
    layers.
  • The reservoir is warmer and CO2 less dense than
    assumed ?
  • The Gassman theory is not valid ?

15
Fundamental limitations on seismically based mass
estimates
  • The non-linear relation between Vp and Sg.
  • Causes gas saturations between 0.1 and 1.0 to be
    unresolvable
  • Lack of information in the 2-10 Hz frequency
    band.
  • Saturation gradients are not discernible

16
Conclusions
  • Injected CO2 is well imaged by time-lapse seismic
    data.
  • The geometry of the CO2 bubble is well defined.
  • There is no evidence of leakage through the seal.
  • A portion of the injected CO2 is trapped at high
    saturations beneath thin shales.
  • The observed time-delays is not sufficiently
    explained by high-saturation CO2 layers.
  • There is a basic limitation in time-lapse seismic
    data on resolving long-wavelength variations and
    on quantifying CO2 saturations.

17
Acknowledgement
  • Rob Arts from TNO, Andy Chadwick from BGS and
    Erik Lindeberg from SINTEF, who all have
    contributed a lot in the multi-diciplinary SACS
    team.
  • Statoil and the Sleipner field partners Exxon,
    Norsk Hydro and TotalFinaElf.
  • Statoils SACS partners BP-Amoco, Norsk Hydro,
    Exxon, TotalFinaElf, Vattenfall, British
    Geological Survey, Bureau de Recherches
    Gèologiques et Minières, Geological Survey of
    Denmark and Greenland, Institut Francais du
    Pètrole, Netherlands Institute of Applied
    Geoscience, Sintef Petroleum Research.
  • WesternGeco, who acquired and processed the
    seismic data.
  • The European Union RD programme Thermie.
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