Elastic and Acoustic Wave Phenomena

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Elastic and Acoustic Wave Phenomena by Phil Bording Memorial University of Newfoundland Swastika Sharma and Steve Butt Dalhousie University SIAM GEOSCIENCES - 2007

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Elastic and Acoustic Wave Phenomena. by Phil Bording Memorial University of Newfoundland Swastika Sharma and Steve Butt Dalhousie University SIAM GEOSCIENCES - 2007. Acoustic Wave Equations. 1D 2D 3D 2.5D. Source – Causality ?. Uniform Grid. Nyquist Criteria. - PowerPoint PPT Presentation

Transcript of Elastic and Acoustic Wave Phenomena

Page 1: Elastic and Acoustic Wave Phenomena

Elastic and Acoustic Wave Phenomena

by

Phil BordingMemorial University of Newfoundland

Swastika Sharma and Steve ButtDalhousie University

SIAM GEOSCIENCES - 2007

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Acoustic Wave Equations1D

2D

3D

2.5D

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Source – Causality ?

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Uniform Grid

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Nyquist Criteria

• Two grid points – support wave without aliasing

• Dominate frequency at source

• Does the earth act as a filter?• Yes, deeper has higher velocities and lower

frequencies

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Stability Limit

Courant – Nifty Mathematical Fellow– had a condition!

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Grid points per Wave length

• Wave length = Velocity/Frequency• Nyquist requires 2 points to support ..

– Using at least two points we can reconstruct the waves without aliasing

– Modeling requires more than 2 to reduce the error in dispersion, numerical error

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Kirchhoff PSDM 100% Velocity - inline 300

(Lazarevic, 2004)

Horizons approximated by stair steps!

Faults

0

1

2

3

4

Marfurt, 2004

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So just how many Grid Points per Wavelength

do we really need???

Nyquist says………. 2

We can image to…. ¼ Lambda 4

Dispersion error requires too many…. 10+

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So just how many Grid Points per Wavelength

do we really need???

The difference operators control everything!

Error = D(spatial) – D(time)

Taylor Series -- Weights(T=0)Optimal Weights – Weights(T=t)Spectral Methods -- D(spatial) = 0Frequency Domain -- D(time) = 0

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Complexity – how long will it run??

n(x,y,z) are the spatial grid sizesn(t) is the number of time stepsw(s) is the work per stepn(s) is the number of shots

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Realistic Models

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Early Elastic Modeling

• Amoco Group -- Kelly, Alford, and Treitel

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Elastic Staggered Grid

Alan Levander – Rice

P-Sv waves with higher Poisson’s ratio

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Elastic P-S Modeling

Levander

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Elastic - Continued

Levander

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Elastic Wave Equation

Levander, 1988

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Elastic today

• 4th order staggered grid - Veiiux• Topography Surface - Hestholm

• Slow shear waves dominate the grid sizing (spacing is small)

• 3D is at least 10X more computing• Visco-elastic schemes in development –

another 10X more? -- Aldridge at Sandia

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Imaging Machine

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Wave Machine

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Acknowledgements

• ACOA – AIF• Husky• IBM

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