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Ødegaard
FORWARD MODELLING FROM THE SIMULATOR
4D.inversion
Analysis and workflow
Ødegaard
FEASABLE TECHNOLOGY PUT INTO PLAY
AT THE RIGHT TIME
Well log
analysis
Rock physics
diagnostics
Seismic
modelling
Field studies Exploitation
Feasibility
studies
Lithology &
fluid prediction
4D timelapse
Reservoir
characterisation
Reservoir
simulation
SEISMIC
INVERSION
Acoustic
impedance
Poisson’s
Ratio
Density
ATTRIBUTE
CALCULATION
NEURAL
NETWORK
3 WEEKS 6 WEEKS 1 YEAR
Ødegaard
Simulation Seismic
AI
PR
r
AI
PR
r
4D ISIS
MODELLED OBSERVED
Seismic data
Reservoir
Simulator
Production
data
Seismic
inversion
Static Model
Base Elastic Time/Depth Information
Ødegaard
Ødegaard
4D Loop Seismic-2-Simulation-2-Seismic
3D Seismic
Geological
Model
Reservoir
Model
Seismic
Acquisition
Time
4D Body
Identification
New Data
Difference
Cube
Baseline
Time-lapse
Depth
Geological
Model
Geological
Model
Geological
Model
Geological
Model
Reservoir
Model
Reservoir
Model
Reservoir
Model
Reservoir
Model
Predictions
Wells
Wells
Ødegaard
Understand acoustic vs physical properties
in inverted seismic data.
Apply rock physics in 4D modelling
Reservoir engineering aspects
Multiple wells with sonic and shear logs
3 vintages of 3D seismic data (near and far offset)
AVO inversion and lithology prediction
NELSON
4D AVO seismic
Ødegaard
The location of the Nelson Field
Ødegaard
Comparison of the conventional far-offset difference data
to the inverted far offset difference data. In the lower section bright
colours indicate a positive impedance change. The difference signal
is restricted to the lower Z3 reservoir interval.
Top Forties
Top Z3
Top Z2
Ødegaard
Oil sand prediction 1990 1997 2000Oil sand prediction 1990 1997 2000Oil sand prediction 1990 1997 2000
Ødegaard
Oil sand prediction 1990 1997 2000Oil sand prediction 1990 1997 2000Oil sand prediction 1990 1997 2000
Ødegaard
Crossplot of Poisson’s ratio versus acoustic impedance for well log data
from the Nelson reservoir interval. Oil and water filled sands as well as
shale fields can be clearly defined.
Ødegaard
Combined pressure and saturation response for a typical Nelson
sandstone (Boyd–Gorst pers.comm.).
Ødegaard
Oil sand Brine sand
Oil sand Brine sand
1990
1997
4D Rock physics Diagnostics
Defining lithology and fluid fields from inversion data to carry
out a probabilistic prediction of fluid and lithology volumes.
Ødegaard
A perspective view to the northeast of the Oil sand volume
prediction from the 1990 baseline acoustic impedance and Poisson’s
ratio data.
Ødegaard
Isometric perspective to view to the north of a volume detection of
high oil sand probability (bright colours) masked by a detection of
positive impedance change (2000-1990) in grey. Bright colours
indicate potential unswept oil at the top of the reservoir at mid-2000.
Ødegaard
Oil Sand Probability Volume
Far Offset Impedance Difference
Positive impedance change (red) indicating sweep (2000)
SW NE
Oil Sands in Red (1990)
Cone around production well
Edge Drive
Basal Rise
4D Target
500m
Oil sand probability and far-offset impedance difference sections
through the N30 target, between two nearby production wells. It can
be seen from the sweep pattern on the far-offset impedance section
that oil is not being swept effectively from the Z4 section between the
two producers, in an area which the oil sand probability shows to be
good reservoir.
Ødegaard
SIMULATOR PREDICTION – converted into AI
changes including S/N filter
Ødegaard
Far offset impedance difference section intersecting the N30y production well.
Bright colours show a high positive impedance contrast (sweep).
The pilot hole for the well encountered an 25 meters oil column before penetrating the moved
OWC as prognosed by 4D.
Simulation had indicated that the area would be almost completely swept (orange horizon).
OWC from 4D
Seismic (FO Inv Diff) OWC from SimulatorTop Forties
Ødegaard
ABSTRACT:
Integrated analysis of 4D seismic data and petrophysical data is used
to produce probabilistic fluid and lithology volumes for monitoring
reservoir performance on the Nelson Field.
Petrophysical analysis of log data shows distinct fields for oil sand, water
sand, shale and heterolithic ‘lithologies’ in acoustic impedance - Poisson’s ratio
space.
Elastic inversion techniques applied to conventional 4D AVO datasets convert
the reflectivity data to acoustic impedance, shear impedance, Poisson’s ratio
and angle impedances. The elastic inversion datasets are used to quantify oil
water contact movements through volume sculpting techniques.
Well derived relationships are used to predict 3D volumes of oil sand probability
from three different seismic survey vintages, 1990, 1997 and 2000. Changes in
oil sand probability due to production are verified by comparison with repeat
production logs.
Integrated volume interpretation of 4D far offset inversion difference
(oil water contact movement) and oil sand probability show areas of
unswept oil, highlighting infill opportunities. Early results from infill
drilling have validated the method realising the potential economic
benefits of 4D seismic technologies.
Ødegaard
TERN
4D full stack seismic
Reservoir Engineering aspects
Physical properties linked to acoustic properties
Ødegaard
Gamma
Sonic
Quartz matrix
0 % 100
Bulk volume water
100 % 0
Porosity
100 % 0
Clay volume
0 % 100
Neutron
Density
Acoustic Impedance
Depth(m)
WELL LOG FLUID SUBSTITUTION: 1980-1995
Ødegaard
4D DIFFERENCE VOLUME IN AI: 1995-1980
red = hardening
Ødegaard
4D INVERSION RESULTS
Acoustic impedance 1980
Acoustic impedance 1995
Acoustic impedance 2000
Ødegaard
SIMULATOR MODELING: WATER SATURATION
5 days
1307 days
Ødegaard
From change in Sw From change in pressure
From combined effect of
change in Sw and pressure
ROCK PROPERTIES FROM SIMULATOR: 1980 - 1995
Changes in acoustic impedance
Ødegaard
AI 1983-1995 with alternative realistion of noise – Top Etive
Ødegaard
HUDSON
4D full stack seismic
QC of 4D potential in data
Re-processing required
Ødegaard
FLUID REPLACEMENT MODELLING
Ødegaard
1999 1990
ACOUSTIC IMPEDANCE
Ødegaard
SIMULATOR RESULTS 1999-1993
Relative change in Poisson’s ratioRelative change in Zp
Ødegaard
PRESSURE CHANGE 1999-1993
Ødegaard
Timelapse acoustic impedance Timelapse Poisson’s ratio
TIMELAPSE HORIZON 1999-1993
Ødegaard
KIMMERIDGE REPEATABILITY 1999 DATA
Ødegaard
4D - KIMMERIDGE REPEATABILITY
Ødegaard
NINIAN
4D seismic
Generated from 2D baseline and 3D time-lapse
Ødegaard
MAP OF SEISMIC
- 1981 origional 3D survey
- 1995 three 2D seismic sections
Ødegaard
1981 ACOUSTIC IMPEDANCE
Ødegaard
1995 ACOUSTIC IMPEDANCE
Ødegaard
LINE 1: ACOUSTIC IMPEDANCE DIFFERENCE
Ødegaard
LINE 2: ACOUSTIC IMPEDANCE DIFFERENCE
Ødegaard
LINE 3: ACOUSTIC IMPEDANCE DIFFERENCE
Ødegaard
NINIAN CONCLUSION
Ødegaard
GULLFAKS
4D amplitude vs inverted seismic
3 vintages of 3D seismic
Interaction rock Physics and reservoir model
Ødegaard
Elastic properties of Brent group sand (6 wells)
AI-PR-SWAI-PR-PHI
PHIT evaluation
AI-PR (for sandflag data only)
Active Zone : 4:34/10-B-8 Z:2 Top Tarbert
3.
4.
5.
6.
7.
8.
9.
AI10^6(kg/m2s)
0.1 0.2 0.3 0.4 0.5
PR
0.2
0.4
PHIT
8730 points plotted out of 12340
Well Zone Depths
34/10-B-8 (2) Top Tarbert 2616.M - 2768.M
34/10-B-8 (3) Top Ness 2768.M - 2919.M
34/10-B-8 (4) Top NER 2919.M - 3094.M
34/10-C-33 (2) Top Ness 2095.M - 2116.M
34/10-C-33 (3) Top NER 2116.M - 2231.5M
34/10-B-15 T2 (1) Top Tarbert 2476.M - 2579.M
PHIT evaluation
AI-PR (for sandflag data only)
Active Zones : W:4 Z:2, 3, 4 W:6 Z:3, 2 W:1 Z:2, 3 W:2 Z:2, 3, 1 W:3
3.
4.
5.
6.
7.
8.
9.
AI10^6(kg/m2s)
0.1 0.2 0.3 0.4 0.5
PR
0.
1.
SW
8230 points plotted out of 11663
Well Zone Depths
34/10-B-8 (2) Top Tarbert 2616.M - 2768.M
34/10-B-8 (3) Top Ness 2768.M - 2919.M
34/10-B-8 (4) Top NER 2919.M - 3094.M
34/10-C-33 (2) Top Ness 2095.M - 2116.M
34/10-C-33 (3) Top NER 2116.M - 2231.5M
34/10-B-15 T2 (2) Top Ness 2579.M - 2670.M
•PP and Sw of four generations are extracted from the reservoir model.
•The RP model transform changes in SW and PP into changes in elastic rock properties.
Ødegaard
Seismic data vintage 1- near and far
Significant AVO effect
Significant 4D effect on both stacks
Ødegaard
Vintage 1 - AI around well A
Ødegaard
Vintage 3- AI around well A
Ødegaard
OFFSHORE UK
MULTI ATTRIBUTE ANALYSIS
Integration of physical attributes in wells with acoustic attributes in seismic
Ødegaard
1. Generate suite of attributes
from the seismic
2. Extract attributes at well
locations
3. Investigate methods of
relating well log rock
properties to volume
derived data.
4. Apply derived relationships
to input volumes
5. Interpret the resultant
volumes
WORKFLOW
Ødegaard
Absolute acoustic impedance (AI):
• Real rock physics property
• Contains low frequency
information not present in
seismic
• Good ties with well log derived
acoustic impedance
• Hydrocarbon identification not
possible on AI alone.
ACOUSTIC IMPEDANCE
Ødegaard
ATTRIBUTE CROSSPLOT – NEURAL ANALYSIS
Synth.seis Zp Attenuation Inst.amp Inst.freq Inst.phase Coherence Mean.freq
Snth.seisZpAtten.Inst.ampInst.freqInst.phasCoheMean.freq
Hydrocarbons
Ødegaard
• All the well data loaded into a GEOVIEW database.
• All the original and generated attribute volumes loaded.
• A target log specified – water saturation
• Attributes extracted along the well path
WELL LOG/ATTRIBUTE RELATIONSHIP
Sw synth Vp f fm Ia If phase dIa/dt filtseis IntIa
Ødegaard
• Neural networks used to generate non-linear transform between
attributes and target logs
• Transform applied to the inputs at the well locations produces very
good results
WELL LOG PREDICTIONS
WATER SATURATION
Well Prediction
Ødegaard
Comparison of actual and predicted water saturation
WATER SATURATION PREDICTION AND FORECASTING
Ødegaard
HIGH HYDROCARBON POTENTIAL BODIES
Ødegaard
We would like to thank the following contributors to the
presentation:
STATOIL
NORSK HYDRO
CONCOPHILLIPS
AMERADA HESS
SHELL
Ødegaard
• Experience with this type of datasets
 25 major 4D projects ‘under the belt’
 Variety of PE Objectives Realised
 Number of Different Geological Settings
 Large group, Varied Disciplines
• Proprietary Technology
 Simultaneous Inversion
 4D ISIS
• Fast Project Start-up and Turnaround
• Cost Effective, High Quality
WHY USE INVERSION DATA 4D CAPABILITIES
Ødegaard
RA Geophysical Well Log Analysis
IP Rock Properties Modeling
OSIRIS Precise Seismic Modeling
EMERGE Neural Net
4D*ISIS Global Seismic Inversion
MAAT Seismic Attributes

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ods-moscow2003

  • 1. Ødegaard FORWARD MODELLING FROM THE SIMULATOR 4D.inversion Analysis and workflow
  • 2. Ødegaard FEASABLE TECHNOLOGY PUT INTO PLAY AT THE RIGHT TIME Well log analysis Rock physics diagnostics Seismic modelling Field studies Exploitation Feasibility studies Lithology & fluid prediction 4D timelapse Reservoir characterisation Reservoir simulation SEISMIC INVERSION Acoustic impedance Poisson’s Ratio Density ATTRIBUTE CALCULATION NEURAL NETWORK 3 WEEKS 6 WEEKS 1 YEAR
  • 5. Ødegaard 4D Loop Seismic-2-Simulation-2-Seismic 3D Seismic Geological Model Reservoir Model Seismic Acquisition Time 4D Body Identification New Data Difference Cube Baseline Time-lapse Depth Geological Model Geological Model Geological Model Geological Model Reservoir Model Reservoir Model Reservoir Model Reservoir Model Predictions Wells Wells
  • 6. Ødegaard Understand acoustic vs physical properties in inverted seismic data. Apply rock physics in 4D modelling Reservoir engineering aspects Multiple wells with sonic and shear logs 3 vintages of 3D seismic data (near and far offset) AVO inversion and lithology prediction NELSON 4D AVO seismic
  • 7. Ødegaard The location of the Nelson Field
  • 8. Ødegaard Comparison of the conventional far-offset difference data to the inverted far offset difference data. In the lower section bright colours indicate a positive impedance change. The difference signal is restricted to the lower Z3 reservoir interval. Top Forties Top Z3 Top Z2
  • 9. Ødegaard Oil sand prediction 1990 1997 2000Oil sand prediction 1990 1997 2000Oil sand prediction 1990 1997 2000
  • 10. Ødegaard Oil sand prediction 1990 1997 2000Oil sand prediction 1990 1997 2000Oil sand prediction 1990 1997 2000
  • 11. Ødegaard Crossplot of Poisson’s ratio versus acoustic impedance for well log data from the Nelson reservoir interval. Oil and water filled sands as well as shale fields can be clearly defined.
  • 12. Ødegaard Combined pressure and saturation response for a typical Nelson sandstone (Boyd–Gorst pers.comm.).
  • 13. Ødegaard Oil sand Brine sand Oil sand Brine sand 1990 1997 4D Rock physics Diagnostics Defining lithology and fluid fields from inversion data to carry out a probabilistic prediction of fluid and lithology volumes.
  • 14. Ødegaard A perspective view to the northeast of the Oil sand volume prediction from the 1990 baseline acoustic impedance and Poisson’s ratio data.
  • 15. Ødegaard Isometric perspective to view to the north of a volume detection of high oil sand probability (bright colours) masked by a detection of positive impedance change (2000-1990) in grey. Bright colours indicate potential unswept oil at the top of the reservoir at mid-2000.
  • 16. Ødegaard Oil Sand Probability Volume Far Offset Impedance Difference Positive impedance change (red) indicating sweep (2000) SW NE Oil Sands in Red (1990) Cone around production well Edge Drive Basal Rise 4D Target 500m Oil sand probability and far-offset impedance difference sections through the N30 target, between two nearby production wells. It can be seen from the sweep pattern on the far-offset impedance section that oil is not being swept effectively from the Z4 section between the two producers, in an area which the oil sand probability shows to be good reservoir.
  • 17. Ødegaard SIMULATOR PREDICTION – converted into AI changes including S/N filter
  • 18. Ødegaard Far offset impedance difference section intersecting the N30y production well. Bright colours show a high positive impedance contrast (sweep). The pilot hole for the well encountered an 25 meters oil column before penetrating the moved OWC as prognosed by 4D. Simulation had indicated that the area would be almost completely swept (orange horizon). OWC from 4D Seismic (FO Inv Diff) OWC from SimulatorTop Forties
  • 19. Ødegaard ABSTRACT: Integrated analysis of 4D seismic data and petrophysical data is used to produce probabilistic fluid and lithology volumes for monitoring reservoir performance on the Nelson Field. Petrophysical analysis of log data shows distinct fields for oil sand, water sand, shale and heterolithic ‘lithologies’ in acoustic impedance - Poisson’s ratio space. Elastic inversion techniques applied to conventional 4D AVO datasets convert the reflectivity data to acoustic impedance, shear impedance, Poisson’s ratio and angle impedances. The elastic inversion datasets are used to quantify oil water contact movements through volume sculpting techniques. Well derived relationships are used to predict 3D volumes of oil sand probability from three different seismic survey vintages, 1990, 1997 and 2000. Changes in oil sand probability due to production are verified by comparison with repeat production logs. Integrated volume interpretation of 4D far offset inversion difference (oil water contact movement) and oil sand probability show areas of unswept oil, highlighting infill opportunities. Early results from infill drilling have validated the method realising the potential economic benefits of 4D seismic technologies.
  • 20. Ødegaard TERN 4D full stack seismic Reservoir Engineering aspects Physical properties linked to acoustic properties
  • 21. Ødegaard Gamma Sonic Quartz matrix 0 % 100 Bulk volume water 100 % 0 Porosity 100 % 0 Clay volume 0 % 100 Neutron Density Acoustic Impedance Depth(m) WELL LOG FLUID SUBSTITUTION: 1980-1995
  • 22. Ødegaard 4D DIFFERENCE VOLUME IN AI: 1995-1980 red = hardening
  • 23. Ødegaard 4D INVERSION RESULTS Acoustic impedance 1980 Acoustic impedance 1995 Acoustic impedance 2000
  • 24. Ødegaard SIMULATOR MODELING: WATER SATURATION 5 days 1307 days
  • 25. Ødegaard From change in Sw From change in pressure From combined effect of change in Sw and pressure ROCK PROPERTIES FROM SIMULATOR: 1980 - 1995 Changes in acoustic impedance
  • 26. Ødegaard AI 1983-1995 with alternative realistion of noise – Top Etive
  • 27. Ødegaard HUDSON 4D full stack seismic QC of 4D potential in data Re-processing required
  • 30. Ødegaard SIMULATOR RESULTS 1999-1993 Relative change in Poisson’s ratioRelative change in Zp
  • 32. Ødegaard Timelapse acoustic impedance Timelapse Poisson’s ratio TIMELAPSE HORIZON 1999-1993
  • 34. Ødegaard 4D - KIMMERIDGE REPEATABILITY
  • 35. Ødegaard NINIAN 4D seismic Generated from 2D baseline and 3D time-lapse
  • 36. Ødegaard MAP OF SEISMIC - 1981 origional 3D survey - 1995 three 2D seismic sections
  • 39. Ødegaard LINE 1: ACOUSTIC IMPEDANCE DIFFERENCE
  • 40. Ødegaard LINE 2: ACOUSTIC IMPEDANCE DIFFERENCE
  • 41. Ødegaard LINE 3: ACOUSTIC IMPEDANCE DIFFERENCE
  • 43. Ødegaard GULLFAKS 4D amplitude vs inverted seismic 3 vintages of 3D seismic Interaction rock Physics and reservoir model
  • 44. Ødegaard Elastic properties of Brent group sand (6 wells) AI-PR-SWAI-PR-PHI PHIT evaluation AI-PR (for sandflag data only) Active Zone : 4:34/10-B-8 Z:2 Top Tarbert 3. 4. 5. 6. 7. 8. 9. AI10^6(kg/m2s) 0.1 0.2 0.3 0.4 0.5 PR 0.2 0.4 PHIT 8730 points plotted out of 12340 Well Zone Depths 34/10-B-8 (2) Top Tarbert 2616.M - 2768.M 34/10-B-8 (3) Top Ness 2768.M - 2919.M 34/10-B-8 (4) Top NER 2919.M - 3094.M 34/10-C-33 (2) Top Ness 2095.M - 2116.M 34/10-C-33 (3) Top NER 2116.M - 2231.5M 34/10-B-15 T2 (1) Top Tarbert 2476.M - 2579.M PHIT evaluation AI-PR (for sandflag data only) Active Zones : W:4 Z:2, 3, 4 W:6 Z:3, 2 W:1 Z:2, 3 W:2 Z:2, 3, 1 W:3 3. 4. 5. 6. 7. 8. 9. AI10^6(kg/m2s) 0.1 0.2 0.3 0.4 0.5 PR 0. 1. SW 8230 points plotted out of 11663 Well Zone Depths 34/10-B-8 (2) Top Tarbert 2616.M - 2768.M 34/10-B-8 (3) Top Ness 2768.M - 2919.M 34/10-B-8 (4) Top NER 2919.M - 3094.M 34/10-C-33 (2) Top Ness 2095.M - 2116.M 34/10-C-33 (3) Top NER 2116.M - 2231.5M 34/10-B-15 T2 (2) Top Ness 2579.M - 2670.M •PP and Sw of four generations are extracted from the reservoir model. •The RP model transform changes in SW and PP into changes in elastic rock properties.
  • 45. Ødegaard Seismic data vintage 1- near and far Significant AVO effect Significant 4D effect on both stacks
  • 46. Ødegaard Vintage 1 - AI around well A
  • 47. Ødegaard Vintage 3- AI around well A
  • 48. Ødegaard OFFSHORE UK MULTI ATTRIBUTE ANALYSIS Integration of physical attributes in wells with acoustic attributes in seismic
  • 49. Ødegaard 1. Generate suite of attributes from the seismic 2. Extract attributes at well locations 3. Investigate methods of relating well log rock properties to volume derived data. 4. Apply derived relationships to input volumes 5. Interpret the resultant volumes WORKFLOW
  • 50. Ødegaard Absolute acoustic impedance (AI): • Real rock physics property • Contains low frequency information not present in seismic • Good ties with well log derived acoustic impedance • Hydrocarbon identification not possible on AI alone. ACOUSTIC IMPEDANCE
  • 51. Ødegaard ATTRIBUTE CROSSPLOT – NEURAL ANALYSIS Synth.seis Zp Attenuation Inst.amp Inst.freq Inst.phase Coherence Mean.freq Snth.seisZpAtten.Inst.ampInst.freqInst.phasCoheMean.freq Hydrocarbons
  • 52. Ødegaard • All the well data loaded into a GEOVIEW database. • All the original and generated attribute volumes loaded. • A target log specified – water saturation • Attributes extracted along the well path WELL LOG/ATTRIBUTE RELATIONSHIP Sw synth Vp f fm Ia If phase dIa/dt filtseis IntIa
  • 53. Ødegaard • Neural networks used to generate non-linear transform between attributes and target logs • Transform applied to the inputs at the well locations produces very good results WELL LOG PREDICTIONS WATER SATURATION Well Prediction
  • 54. Ødegaard Comparison of actual and predicted water saturation WATER SATURATION PREDICTION AND FORECASTING
  • 56. Ødegaard We would like to thank the following contributors to the presentation: STATOIL NORSK HYDRO CONCOPHILLIPS AMERADA HESS SHELL
  • 57. Ødegaard • Experience with this type of datasets  25 major 4D projects ‘under the belt’  Variety of PE Objectives Realised  Number of Different Geological Settings  Large group, Varied Disciplines • Proprietary Technology  Simultaneous Inversion  4D ISIS • Fast Project Start-up and Turnaround • Cost Effective, High Quality WHY USE INVERSION DATA 4D CAPABILITIES
  • 58. Ødegaard RA Geophysical Well Log Analysis IP Rock Properties Modeling OSIRIS Precise Seismic Modeling EMERGE Neural Net 4D*ISIS Global Seismic Inversion MAAT Seismic Attributes