![Page 1: An acoustic wave equation for pure P wave in 2D TTI media Sept. 21, 2011 Ge Zhan, Reynam C. Pestana and Paul L. Stoffa](https://reader036.vdocuments.us/reader036/viewer/2022062422/56649f1c5503460f94c31cb8/html5/thumbnails/1.jpg)
An acoustic wave equation for pure P wave in 2D TTI media
Sept. 21, 2011
Ge Zhan, Reynam C. Pestana and Paul L. Stoffa
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Outline
1. Motivation
2. Introduction
3. Theory• TTI coupled equations (coupled P and SV wavefield)
• TTI decoupled equations (pure P and pure SV wavefield)
• Numerical implementation
4. Numerical Results• Impulse response result
• Wedge model result
• BP TTI model result
5. Conclusions
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Outline
1. Motivation
2. Introduction
3. Theory• TTI coupled equations (coupled P and SV wavefield)
• TTI decoupled equations (pure P and pure SV wavefield)
• Numerical implementation
4. Numerical Results• Impulse response result
• Wedge model result
• BP TTI model result
5. Conclusions
Vs0=0
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Motivation
1. Why go TTI (Tilted Transversely Isotropy)?
• Isotropic assumption is not always appropriate (this fact has been recognized in North Sea, Canadian Foothills and GOM).
• Conventional isotropic/VTI methods result in low resolution and misplaced images of subsurface structures.
• To obtain a significant improvement in image quality, clarity and positioning.
2. Pure P wave equation VS. TTI coupled equations
• TTI coupled equations are not free of SV wave.
• SV wave component leads to instability problem.
• To model clean and stable P wave propagation.TTI RTMVTI RTMModel
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Outline
1. Motivation
2. Introduction
3. Theory• TTI coupled equations (coupled P and SV wavefield)
• TTI decoupled equations (pure P and pure SV wavefield)
• Numerical implementation
4. Numerical Results• Impulse response result
• Wedge model result
• BP TTI model result
5. Conclusions
Vs0=0
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Introduction
Coupled equations (suffer from shear-wave artifacts, unstable)
• 4th-order equation: Alkhalifah, 2000;
• 2nd-order equations: Zhou et al., 2006; Du et al., 2008; Duveneck et al., 2008; Fletcher et al., 2008; Zhang and Zhang, 2008.
Coupled equations (combined with shear-wave removal)
Setting ε=δ around source: Duveneck, 2008;
• Model smoothing: Zhang and Zhang, 2010; Yoon et al., 2010
Decoupled equations (free from shear-wave artifacts)
• Muir-Dellinger approximation (Dellinger and Muir, 1985; Dellinger et al., 1993; later reinvented by Stopin, 2001)
• Approximated VTI dispersion relation: Harlan, 1990&1995; Fowler, 2003; Etgen and Brandsberg-Dahl, 2009; Liu et al., 2009; Pestana et al., 2011
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Outline
1. Motivation
2. Introduction
3. Theory• TTI coupled equations (coupled P and SV wavefield)
• TTI decoupled equations (pure P and pure SV wavefield)
• Numerical implementation
4. Numerical Results• Impulse response result
• Wedge model result
• BP TTI model result
5. Conclusions
Vs0=0
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North
Φ
Tilted Axis
θTilted Axis
Vertical
TTI Coupled Equations
Start with the P-SV dispersion relation for TTI media, set Vs0=0 along the symmetry axis (” pseudo-acoustic”
approximation)TTI Coupled Equations(Zhou, 2006; Du et al., 2008; Fletcther et al., 2008; Zhang and Zhang, 2008)
Vp0=3000 m/s, epsilon=0.24delta=0.1, theta=45 degree
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Vp0=3000 m/s, epsilon=0.24delta=0.1, theta=45 degree
Vs0=Vp0/2Vs0=0
TTI Coupled Equations
Re-introduce non-zero Vs0 (Fletcher et al., 2009),
the above equations become
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Outline
1. Motivation
2. Introduction
3. Theory• TTI coupled equations (coupled P and SV wavefield)
• TTI decoupled equations (pure P and pure SV wavefield)
• Numerical implementation
4. Numerical Results• Impulse response result
• Wedge model result
• BP TTI model result
5. Conclusions
Vs0=0
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Square-root Approximation
Exact phase velocity expression for VTI media (Tsvankin, 1996)
expand the square root to 1st-order
where
_ _
(Muir-Dellinger approximation)
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VTI Decoupled Equations
P wave and SV wave dispersion relations for VTI media
P wave and SV wave phase velocity for VTI media
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VTI Decoupled Equations
P wave and SV wave dispersion relations for VTI media
pure-P pure-SV coupled P & SV
Vp0=3000 m/s epsilon=0.24 delta=0.1
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Replace ( , , ) by ( , , ), and
Dispersion relations for TTI media
TTI Decoupled Equations
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P-wave and SV-wave equations in 2D time-wavenumber domain
TTI Decoupled Equations
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Outline
1. Motivation
2. Introduction
3. Theory• TTI coupled equations (coupled P and SV wavefield)
• TTI decoupled equations (pure P and pure SV wavefield)
• Numerical implementation
4. Numerical Results• Impulse response result
• Wedge model result
• BP TTI model result
5. Conclusions
Vs0=0
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Pseudospectral in space coupled with REM in time.
Numerical Implementation
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Outline
1. Motivation
2. Introduction
3. Theory• TTI coupled equations (coupled P and SV wavefield)
• TTI decoupled equations (pure P and pure SV wavefield)
• Numerical implementation
4. Numerical Results• Impulse response result
• Wedge model result
• BP TTI model result
5. Conclusions
Vs0=0
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2D Impulse Responses ( epsilon > delta )
Vp0=3000 m/sepsilon=0.24delta=0.1theta=45 degree
Coupled Equations
Decoupled Equations
Vs0=0 Vs0≠0
pure-P pure-SV
Vs0=0 Vs0≠0
pure-P pure-SV
θ
Tilted AxisVertical
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2D Impulse Responses ( epsilon < delta )
Vs0=0 Vs0≠0
pure-P pure-SV
NaN NaN
Vs0=0 Vs0≠0
pure-P pure-SV
Coupled Equations
Decoupled Equations
Vp0=3000 m/sepsilon=0.1delta=0.24theta=45 degree
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Outline
1. Motivation
2. Introduction
3. Theory• TTI coupled equations (coupled P and SV wavefield)
• TTI decoupled equations (pure P and pure SV wavefield)
• Numerical implementation
4. Numerical Results• Impulse response result
• Wedge model result
• BP TTI model result
5. Conclusions
Vs0=0
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Wedge Model (coutesy of Duveneck and Bakker, 2011)
Vp (km/s) theta (degree)
epsilon delta
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Wavefield Snapshots ( t =1 s)
Vs0=0
Vs0≠0 pure-P
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Wavefield Snapshots ( t =1.5 s)
Vs0=0
Vs0≠0 pure-P
instability
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Wavefield Snapshots ( t =4 s)
Vs0=0
Vs0≠0 pure-P
unstable
unstable stable
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Outline
1. Motivation
2. Introduction
3. Theory• TTI coupled equations (coupled P and SV wavefield)
• TTI decoupled equations (pure P and pure SV wavefield)
• Numerical implementation
4. Numerical Results• Impulse response result
• Wedge model result
• BP TTI model result
5. Conclusions
Vs0=0
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BP TTI Model
Vp theta
epsilon delta
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Wavefield Snapshots ( t=4 s)
Vs0=0
Vs0≠0 pure-P
insitibility
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RTM Image
VTI RTM
TTI RTM
VTI RTM
TTI RTM
Model
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Outline
1. Motivation
2. Introduction
3. Theory• TTI coupled equations (coupled P and SV wavefield)
• TTI decoupled equations (pure P and pure SV wavefield)
• Numerical implementation
4. Numerical Results• Impulse response result
• Wedge model result
• BP TTI model result
5. Conclusions
Vs0=0
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Conclusions
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TTI coupled and decoupled equations have long history with many contributors and derivations and methods of implementation.
We have shown that the numerical implementation using pseudospectral in space coupled with REM in time provides stable, near-analytically-accurate and numerical clean results.
Due to many FFTs (7 terms for 2D, 21 terms for 3D) per time step in the implementation, large clusters are needed for practical applications.
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Acknowledgments
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The authors wish to thank King Abdullah University of Science and Technology (KAUST) for providing research funding to this project.
We would like to thank BP for making the TTI model and dataset available.
We are also grateful to Faqi Liu, Hongbo Zhou, John Etgen and Paul Fowler for many useful suggestions on this work.
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Thank you for your attention!
Questions?