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Society of Petroleum Engineers
Distinguished Lecturer Program
www.spe.org/dl
1
Dr. Isabela Falk
Schlumberger
IMPROVING RESERVOIR SIMULATION
MODELING WITH SEISMIC ATTRIBUTES
AGENDA
 Seismic attributes description
 Horizon and fault interpretation
 Geological modeling
 Facies modeling
 Property modeling
 Conclusions
2
OUTLINE
 Seismic interpretation is an integrated part of
the reservoir modeling process.
 Besides standard structural interpretation of
horizons and faults, seismic attributes make a
major contribution to geological modeling.
 Seismic attributes provide very useful
information regarding stratigraphy, facies
distribution, and reservoir properties.
3
INTEGRATED RESERVOIR MODELING
Seismic
interpretation
Well
correlation
Facies
modeling
Property
modeling
Simulation
Data analysis
Well design
4
HOW CAN SEISMIC HELP?
 The sound waves are reflected and refracted by
different rock layers and they are captured on the
surface by sensors.
 The analysis of the time the waves take to return to
surface and the changes in their properties, provides
important information about the rock types, their
properties and possible fluid content.
 Different types of seismic processing, computation and
interpretation can generate several surface and
volume attributes that can be used to better
understand and characterize the hydrocarbon
reservoirs. 5
SEISMIC ACQUISITION AND
INTERPRETATION
6
Land seismic acquisition Offshore acquisition
Processed seismic trace Seismic attributes extraction
SEISMIC ATTRIBUTES APPLICABILITY
 The seismic attributes are most often used in
siliciclastic reservoirs (sandstones).
 Compared with sandstones, the carbonates present
many challenges, such as: stronger lateral variations
in rock properties, facies changes, velocity dispersion
due to permeability heterogeneity, etc.
 All of these characteristics make quantitative analysis
in carbonate reservoirs more difficult.
7
J. Wang, D. Dopkin – Visualization, Analysis, and Interpretation of Seismic Attributes
for Characterizing a Carbonate Reservoir. 7th International Conference & Exposition
on Petroleum Geophysics, Hyderabad, India, 2008. P-375
WORKFLOW
 Seismic interpretation: horizons and faults
 Volume and surface attributes extraction
 Correlation with petrophysical properties from
wells
 Use of seismic attributes for facies and
property modeling
8
VOLUME ATTRIBUTES
 Structural attributes – for horizons and faults
interpretation
 Stratigraphic attributes – for lithology and facies
interpretation
 AVO attributes – for fluid and lithology
interpretation
9
 Volume attributes are extracted inside a 3D
seismic cube, based on various properties of the
analytical signal.
HORIZON INTERPRETATION
10
 Sometimes the seismic signal is poor and horizon
interpretation can be difficult.
? ? ? ?
SEISMIC ATTRIBUTES FOR
STRUCTURAL INTERPRETATION
11
 Volume attributes can be used to help with the horizon
interpretation when the seismic signal is poor.
Cosine of phase Relative Acoustic Impedance
HORIZON INTERPRETATION
12
 Improved seismic interpretation based on 3D attributes
AUTO-TRACKING & MANUAL
EDITING
13
When the seismic signal shows good lateral continuity,
the interpretation can be done by auto-tracking
FAULT INTERPRETATION: MANUAL
INTERPRETATION AND AUTO-TRACKING
14
Auto-trackingManual interpretation
MANUAL FAULTS INTERPRETATION
15
FAULTS INTERPRETATION
16
AUTO-TRACKING RESULTS
17
GEOLOGICAL MODELING
18
 Time surfaces are
converted to depth
using a velocity
model.
 These surfaces are
used to create the
geological grid.
 The geological
model is vertically
divided into
zones/layers.
WELL CORRELATION
 Well correlation is the first step in the
geological modeling.
 Complex stratigraphy (channels, sand lenses,
etc.), can make the correlation challenging.
 Seismic makes a major contribution in
understanding the large scale facies
distribution.
19
WELL CORRELATION SHOWING
LITHOLOGY VARIATIONS
20
Channels observed in some of the wells are difficult to
correlate laterally with other wells. Seismic attributes can
show the direction of channels and their connectivity.
SEISMIC ATTRIBUTES BY LAYERS
 Volume attributes can be
extracted between two
horizons and flattened.
 This way we can create
stratigraphic slices parallel
with sedimentation layers.
 This is very useful for
understanding the
depositional processes.
21
SEISMIC EXTRACTION AND FLATTENING
BETWEEN TWO HORIZONS
22
3D seismic with two interpreted horizons Seismic slice extracted between horizons
3D seismic slice extracted 3D seismic slice flattened
VARIANCE ATTRIBUTE
23
 Variance attribute is calculated from 3D seismic and it represents
trace-to-trace variability of seismic signal (discontinuities)
 Helps identifying channels and faults
ENVELOPE ATTRIBUTE
 Is defined as total energy of the seismic trace
 Shows lithological changes that might not be apparent on the
seismic data, caused by strong energy reflections and
sequence boundaries
24
SURFACE ATTRIBUTES
 Amplitude attributes
 Statistical attributes
 Signal shape attributes
 Measurable interval
 These attributes can be used for facies and
property distribution inside reservoir layers
25
 Surface attributes are extracted from a seismic
volume across a surface, within an interval near
the surface.
EXAMPLES OF SURFACE ATTRIBUTES
26
 The attributes were extracted from the same
reservoir, but different depths.
STRATIGRAPHIC FEATURES
FROM SEISMIC ATTRIBUTES
27
NEURAL NETWORK MODEL
USING SEISMIC ATTRIBUTES
28
 Neural Network can be used to predict and estimate
reservoir properties by correlating log or core properties
with surface or volume attributes
 One or more seismic attributes can be used as input, and
different log types can be used for supervising the data
training process
 Based on the input data, the output can be a 2D or 3D
probability distribution
 The resulted probability can be then used in the facies or
property modeling process, as a 2D or 3D distribution
trend
NEURAL NETWORK WORKFLOW
29
Well log property
Probability of sand distributionSeismic attributes
FACIES MODELING BASED ON
SEISMIC ATTRIBUTES
30
 Facies modeling is based on facies logs defined from
petrophysical interpretation (VCL, GR, etc.).
 Surface or volume seismic attributes can be used in the
modeling process as probability trends.
 2D trends help with lateral distribution only.
 3D trends help also with vertical distribution of
lithology, which is very useful in case of channels.
FACIES MODEL BASED ON
SEISMIC ATRIBUTES
31
 A 3D AVO gradient attribute was used as probability
trend to distribute lithology between wells and in areas
without wells.
AVO gradient rescaled Facies model
FACIES MODEL COMPARISON
32
From wells only Using seismic attribute as a
3D probability trend
PROPERTY MODELS
 Porosity distribution can be conditioned to the
facies models.
 Acoustic Impedance (AI) shows a good
correlation with porosity in sandstone
reservoirs and can be used as a 3D probability
trend for porosity modeling.
 Surface attributes can also be used as horizontal
trends, if AI not available.
33
SEISMIC INVERSION RESULTS
CONVERTED TO POROSITY MODEL
34
Acoustic Impedance inversion results
Acoustic Impedance vs. Total
Porosity function from log data
Porosity from Acoustic Impedance
POROSITY MODELING WITH 2D
TRENDS
35
2D seismic trend Porosity model
 The 2D probability trend was created from a seismic
attribute and used as a secondary variable for porosity
distribution.
PERMEABILITY MODELING
36
Porosity model Permeability model
 The permeability model is created after the porosity
model, using cokriging with porosity.
SATURATION MODELING
37
 Fluids distribution can be interpreted from AVO
attributes.
CONCLUSIONS
 Seismic attributes can significantly improve the
facies and property modeling.
 They are very useful for the lateral distribution
of the reservoir properties between the wells
and in areas without wells.
 As a result, dynamic reservoir models,
simulation processes and production forecasts
are improved.
 More reliable hydrocarbon volume estimations
and well planning are achieved. 38
Thank You For Attending!
Question & Answer Session
39
Society of Petroleum Engineers
Distinguished Lecturer Program
www.spe.org/dl 40
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Enter your section in the DL Evaluation Contest by
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Improving Reservoir Simulation Modeling with Seismic Attributes

  • 1. Society of Petroleum Engineers Distinguished Lecturer Program www.spe.org/dl 1 Dr. Isabela Falk Schlumberger IMPROVING RESERVOIR SIMULATION MODELING WITH SEISMIC ATTRIBUTES
  • 2. AGENDA  Seismic attributes description  Horizon and fault interpretation  Geological modeling  Facies modeling  Property modeling  Conclusions 2
  • 3. OUTLINE  Seismic interpretation is an integrated part of the reservoir modeling process.  Besides standard structural interpretation of horizons and faults, seismic attributes make a major contribution to geological modeling.  Seismic attributes provide very useful information regarding stratigraphy, facies distribution, and reservoir properties. 3
  • 5. HOW CAN SEISMIC HELP?  The sound waves are reflected and refracted by different rock layers and they are captured on the surface by sensors.  The analysis of the time the waves take to return to surface and the changes in their properties, provides important information about the rock types, their properties and possible fluid content.  Different types of seismic processing, computation and interpretation can generate several surface and volume attributes that can be used to better understand and characterize the hydrocarbon reservoirs. 5
  • 6. SEISMIC ACQUISITION AND INTERPRETATION 6 Land seismic acquisition Offshore acquisition Processed seismic trace Seismic attributes extraction
  • 7. SEISMIC ATTRIBUTES APPLICABILITY  The seismic attributes are most often used in siliciclastic reservoirs (sandstones).  Compared with sandstones, the carbonates present many challenges, such as: stronger lateral variations in rock properties, facies changes, velocity dispersion due to permeability heterogeneity, etc.  All of these characteristics make quantitative analysis in carbonate reservoirs more difficult. 7 J. Wang, D. Dopkin – Visualization, Analysis, and Interpretation of Seismic Attributes for Characterizing a Carbonate Reservoir. 7th International Conference & Exposition on Petroleum Geophysics, Hyderabad, India, 2008. P-375
  • 8. WORKFLOW  Seismic interpretation: horizons and faults  Volume and surface attributes extraction  Correlation with petrophysical properties from wells  Use of seismic attributes for facies and property modeling 8
  • 9. VOLUME ATTRIBUTES  Structural attributes – for horizons and faults interpretation  Stratigraphic attributes – for lithology and facies interpretation  AVO attributes – for fluid and lithology interpretation 9  Volume attributes are extracted inside a 3D seismic cube, based on various properties of the analytical signal.
  • 10. HORIZON INTERPRETATION 10  Sometimes the seismic signal is poor and horizon interpretation can be difficult. ? ? ? ?
  • 11. SEISMIC ATTRIBUTES FOR STRUCTURAL INTERPRETATION 11  Volume attributes can be used to help with the horizon interpretation when the seismic signal is poor. Cosine of phase Relative Acoustic Impedance
  • 12. HORIZON INTERPRETATION 12  Improved seismic interpretation based on 3D attributes
  • 13. AUTO-TRACKING & MANUAL EDITING 13 When the seismic signal shows good lateral continuity, the interpretation can be done by auto-tracking
  • 14. FAULT INTERPRETATION: MANUAL INTERPRETATION AND AUTO-TRACKING 14 Auto-trackingManual interpretation
  • 18. GEOLOGICAL MODELING 18  Time surfaces are converted to depth using a velocity model.  These surfaces are used to create the geological grid.  The geological model is vertically divided into zones/layers.
  • 19. WELL CORRELATION  Well correlation is the first step in the geological modeling.  Complex stratigraphy (channels, sand lenses, etc.), can make the correlation challenging.  Seismic makes a major contribution in understanding the large scale facies distribution. 19
  • 20. WELL CORRELATION SHOWING LITHOLOGY VARIATIONS 20 Channels observed in some of the wells are difficult to correlate laterally with other wells. Seismic attributes can show the direction of channels and their connectivity.
  • 21. SEISMIC ATTRIBUTES BY LAYERS  Volume attributes can be extracted between two horizons and flattened.  This way we can create stratigraphic slices parallel with sedimentation layers.  This is very useful for understanding the depositional processes. 21
  • 22. SEISMIC EXTRACTION AND FLATTENING BETWEEN TWO HORIZONS 22 3D seismic with two interpreted horizons Seismic slice extracted between horizons 3D seismic slice extracted 3D seismic slice flattened
  • 23. VARIANCE ATTRIBUTE 23  Variance attribute is calculated from 3D seismic and it represents trace-to-trace variability of seismic signal (discontinuities)  Helps identifying channels and faults
  • 24. ENVELOPE ATTRIBUTE  Is defined as total energy of the seismic trace  Shows lithological changes that might not be apparent on the seismic data, caused by strong energy reflections and sequence boundaries 24
  • 25. SURFACE ATTRIBUTES  Amplitude attributes  Statistical attributes  Signal shape attributes  Measurable interval  These attributes can be used for facies and property distribution inside reservoir layers 25  Surface attributes are extracted from a seismic volume across a surface, within an interval near the surface.
  • 26. EXAMPLES OF SURFACE ATTRIBUTES 26  The attributes were extracted from the same reservoir, but different depths.
  • 28. NEURAL NETWORK MODEL USING SEISMIC ATTRIBUTES 28  Neural Network can be used to predict and estimate reservoir properties by correlating log or core properties with surface or volume attributes  One or more seismic attributes can be used as input, and different log types can be used for supervising the data training process  Based on the input data, the output can be a 2D or 3D probability distribution  The resulted probability can be then used in the facies or property modeling process, as a 2D or 3D distribution trend
  • 29. NEURAL NETWORK WORKFLOW 29 Well log property Probability of sand distributionSeismic attributes
  • 30. FACIES MODELING BASED ON SEISMIC ATTRIBUTES 30  Facies modeling is based on facies logs defined from petrophysical interpretation (VCL, GR, etc.).  Surface or volume seismic attributes can be used in the modeling process as probability trends.  2D trends help with lateral distribution only.  3D trends help also with vertical distribution of lithology, which is very useful in case of channels.
  • 31. FACIES MODEL BASED ON SEISMIC ATRIBUTES 31  A 3D AVO gradient attribute was used as probability trend to distribute lithology between wells and in areas without wells. AVO gradient rescaled Facies model
  • 32. FACIES MODEL COMPARISON 32 From wells only Using seismic attribute as a 3D probability trend
  • 33. PROPERTY MODELS  Porosity distribution can be conditioned to the facies models.  Acoustic Impedance (AI) shows a good correlation with porosity in sandstone reservoirs and can be used as a 3D probability trend for porosity modeling.  Surface attributes can also be used as horizontal trends, if AI not available. 33
  • 34. SEISMIC INVERSION RESULTS CONVERTED TO POROSITY MODEL 34 Acoustic Impedance inversion results Acoustic Impedance vs. Total Porosity function from log data Porosity from Acoustic Impedance
  • 35. POROSITY MODELING WITH 2D TRENDS 35 2D seismic trend Porosity model  The 2D probability trend was created from a seismic attribute and used as a secondary variable for porosity distribution.
  • 36. PERMEABILITY MODELING 36 Porosity model Permeability model  The permeability model is created after the porosity model, using cokriging with porosity.
  • 37. SATURATION MODELING 37  Fluids distribution can be interpreted from AVO attributes.
  • 38. CONCLUSIONS  Seismic attributes can significantly improve the facies and property modeling.  They are very useful for the lateral distribution of the reservoir properties between the wells and in areas without wells.  As a result, dynamic reservoir models, simulation processes and production forecasts are improved.  More reliable hydrocarbon volume estimations and well planning are achieved. 38
  • 39. Thank You For Attending! Question & Answer Session 39
  • 40. Society of Petroleum Engineers Distinguished Lecturer Program www.spe.org/dl 40 Your Feedback is Important Enter your section in the DL Evaluation Contest by completing the evaluation form for this presentation Visit SPE.org/dl

Editor's Notes

  1. We encourage feedback to the static model during history matching so any changes are verified as geologically realistic. Also static and dynamic models are consistent.
  2. Cosine of phase improves reflectors continuity – commonly used for guiding interpretation in areas of poor amplitude Variance highlights the discontinuities in horizons – very good stratigraphic attribute Dip deviation indicates rapid changes in the orientation of the seismic horizons Envelope (reflection strength) is important for detecting bright spots and major lithology changes Instantaneous frequency is useful in indicating lateral changes in lithology Instantaneous phase is a good indicator of continuities, faults, pinch-outs, sequence boundaries, on-lap patterns RAI indicates sequence boundaries, unconformity surfaces and discontinuities
  3. Cosine of phase improves reflectors continuity – commonly used for guiding interpretation in areas of poor amplitude RAI indicates sequence boundaries, unconformity surfaces and discontinuities
  4. Ant tracking is a method of edge enhancement for the identification of faults, fractures and other linear anomalies
  5. Commonly used today is to depth the whole cube or have a pre depth migrated cube for interpretation.
  6. Can be done both in time and depth domains.
  7. AKA Reflection strength – shows subtle lithological changes that might not be apparent on the seismic data
  8. This should show wells ideally with log motifs showing net.
  9. Probability or co-krigged.
  10. Well locations need to be added as it says from logs.
  11. As long as there is a correlation coefficient greater than 0.85. If not use Cloud transform.