Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

33
Theory of Multisource Crosstalk Theory of Multisource Crosstalk Reduction by Phase-Encoded Static Reduction by Phase-Encoded Statics G. Schuster, X. Wang, Y. Huang, C. Boonyasiriwat G. Schuster, X. Wang, Y. Huang, C. Boonyasiriwat King Abdullah University Science & Technology King Abdullah University Science & Technology

description

Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics. G. Schuster, X. Wang, Y. Huang, C. Boonyasiriwat King Abdullah University Science & Technology. Outline. Seismic Experiment:. L m = d. 1. 1. L m = d. 2. 2. L m = d. N. N. - PowerPoint PPT Presentation

Transcript of Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Page 1: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Theory of Multisource CrosstalkTheory of Multisource Crosstalk

Reduction by Phase-Encoded StaticsReduction by Phase-Encoded Statics

G. Schuster, X. Wang, Y. Huang, C. BoonyasiriwatG. Schuster, X. Wang, Y. Huang, C. BoonyasiriwatKing Abdullah University Science & TechnologyKing Abdullah University Science & Technology

Page 2: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

OutlineOutline1.1. Seismic Experiment:Seismic Experiment:

L m = d

L m = d1 1

L m = d2 2...N N

2. Standard vs Phase Encoded Least Squares Soln.2. Standard vs Phase Encoded Least Squares Soln.

LL11

LL22

dd 11

dd 22m =m = vs N L + N LN L + N L11 2211 22[ ]mm = [N = [N dd + N + N dd ] ]11 2211 22

3. Theory Noise Reduction3. Theory Noise Reduction 4. Summmary and Road Ahead4. Summmary and Road Ahead

Page 3: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Gulf of Mexico Seismic SurveyGulf of Mexico Seismic Survey

mm

L m = d

L m = d1 1

L m = d2 2...N N

Time (s)

6 X (km)

4

0

d

Goal:Goal: Solve overdetermined Solve overdeterminedSystem of equations for mSystem of equations for m

Predicted data Observed data

Problem:Problem: Expensive, one Expensive, one migration/shot gathermigration/shot gather

Solution:Solution: Supergather Supergather migrationmigration

Page 4: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Brief History Multisource Brief History Multisource Phase Encoded ImagingPhase Encoded Imaging

Romero, Ghiglia, Ober, & Morton, Geophysics, (2000)

Krebs, Anderson, Hinkley, Neelamani, Lee, Baumstein, Lacasse, SEG, (2009)

Virieux and Operto, EAGE, (2009)

Dai and Schuster, SEG, (2009)

Migration

Waveform Inversion and Least Squares Migration

Biondi et al., SEG, (2009)

Page 5: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

OutlineOutline1.1. Seismic Experiment:Seismic Experiment:

L m = d

L m = d1 1

L m = d2 2...N N

2. Standard vs Phase Encoded Least Squares Soln.2. Standard vs Phase Encoded Least Squares Soln.

LL11

LL22

dd 11

dd 22m =m = vs N L + N LN L + N L11 2211 22[ ]mm = [N = [N dd + N + N dd ] ]11 2211 22

3. Theory Noise Reduction3. Theory Noise Reduction 4. Summmary and Road Ahead4. Summmary and Road Ahead

Page 6: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

(k)(k)

Conventional Least Squares Conventional Least Squares Solution: Solution: L=L= & & d = d =

GivenGiven: : LLm=dm=d

FindFind: m : m s.t.s.t. min|| min||LLm-d||m-d||22

SolutionSolution: m = [: m = [L LL L] ] LL d d TT TT-1-1

m = m – m = m – LL ( (LLm - d) m - d) TT(k+1)(k+1) (k)(k) (k)(k)(k)(k)

or if or if LL is too big is too big

ProblemProblem::

LL11

LL22

dd 11

dd 22

= m – = m – LL ( (L L m - d ) m - d ) (k)(k)

+ L+ L ( (L L m - d ) m - d ) 11 11 22 22 2211

TTTT[ ]

In general, hugedimension matrix

Note: subscripts agree

Page 7: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Conventional Least Squares Conventional Least Squares Solution: Solution: L=L= & & d = d =

GivenGiven: : LLm=dm=d

FindFind: m : m s.t.s.t. min|| min||LLm-d||m-d||22

SolutionSolution: m = [: m = [L LL L] ] LL d d TT TT-1-1

m = m – m = m – LL ( (LLm - d) m - d) TT(k+1)(k+1) (k)(k) (k)(k)(k)(k)

ProblemProblem::

LL11

LL22

dd 11

dd 22

= m – = m – LL ( (L L m - d ) m - d ) (k)(k)

+ L+ L ( (L L m - d ) m - d ) 11 11 22 22 2211

TTTT[ ]

In general, hugedimension matrix

Problem: Expensive, FD solve/CSGSolution: Blend+encode Data

(k)(k)

Page 8: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Blending+Phase EncodingBlending+Phase Encoding

22 dd = = N d + N d + N dN d + N d + N d221111 3333

PhasePhasePhasePhaseBlendingBlending

Encoding MatrixEncodedsupergather

LL = = NN L + L + NN L L + + NN L L33 3322 2211 11m [ ]m

dd 11LL mm==11

Encoded supergather modeler

dd 33LL mm==33dd 22LL mm==22

BlendingBlending11

e i in in domain domain

Page 9: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

(k)(k)(k)(k)(k) (k) (k) (k)

++

Blended Phase-Encoded Least Squares Solution Blended Phase-Encoded Least Squares Solution

LL = = && dd = = N d + N dN d + N d

GivenGiven: : LLm=m=ddFindFind: m s.t. min||: m s.t. min||LLm-m-dd||||22

SolutionSolution: m = [: m = [LL LL] ] LL dd TT TT-1-1

TT(k+1)(k+1) (k)(k) (k)(k)(k)(k)

or if or if LL is too big is too big

11N L + N LN L + N L22 11

= m – = m – LL ( (L L m - d ) m - d ) (k)(k)

+ L+ L ( (L L m - d ) m - d ) 11 11 22 22 2211

TTTT[ ]

11 22 11 22 22

+ Crosstalk+ L+ L N N ( N N (L L m - d ) m - d ) 22

TT

11 L L N N (N N (L L m - d ) m - d ) 11

TT

11 2222 11 11 22 22

** **

(k)(k)

In general, SMALLdimension matrix

(k)(k) (k)(k)

Iterations are proxyFor ensemble averaging

(k+1)(k+1) (k)(k) (k)(k)

(k)(k) (k)(k)

(k)(k)(k)(k)(k)(k)(k)(k) (k)(k) (k)(k)

(k)(k) (k)(k)

m = m – m = m – LL ( (LLm - m - dd) )

Page 10: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

OutlineOutline1.1. Seismic Experiment:Seismic Experiment:

L m = d

L m = d1 1

L m = d2 2...N N

2. Standard vs Phase Encoded Least Squares Soln.2. Standard vs Phase Encoded Least Squares Soln.

LL11

LL22

dd 11

dd 22m =m = vs N L + N LN L + N L11 2211 22[ ]mm = [N = [N dd + N + N dd ] ]11 2211 22

3. Theory Noise Reduction3. Theory Noise Reduction

4. Summary 4. Summary

Page 11: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Ensemble Average of Crosstalk TermEnsemble Average of Crosstalk Term

With Random Time ShiftsWith Random Time Shifts

++Crosstalk: LL N N ( N N (L L m - d ) m - d ) 22

TT

1111 L L N N (N N (L L m - d ) m - d ) 11

TT

11 2222 11 11 22 22

** **

N NN N1122

** = e e -i 2i 1 e i

1 2< > < > >= <

e i1 2= e

1 2

-2

dd1 2

~ e 2 2

e -i 2

Gaussian PDF

Noise

Crosstalk term decreaseswith increasing and

<Noise>:

Page 12: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Crosstalk Prediction FormulaLL ( (L L m - d ) m - d ) 22

TT

1111 + L+ L ( (L L m - d ) m - d ) 11

TT

2222 e-2 2

O( )~X =

Pt. Scatt. Stand. Mig. Pt. Scatt.. Mig. of Supergathers.

Pt. Scatt.. Mig. of Supergathers.Pt. Scatt.. Mig. of Supergathers.

= .05 s = .1 s

= .01 s

X Offset

Page 13: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Ensemble Average of Crosstalk TermEnsemble Average of Crosstalk Term

With Random PolarityWith Random Polarity

++Crosstalk: LL N N ( N N (L L m - d ) m - d ) 22

TT

1111 L L N N (N N (L L m - d ) m - d ) 11

TT

11 2222 11 11 22 22

** **

N NN N1122

** 1 2<Noise>: < > = < > = 0

sgn(

Noise

sgn(sgn(

Conclusion: Conclusion: Random polarity better than Random polarity better than random time shiftsrandom time shifts

Further Analysis: Further Analysis: Variance of the crosstalk noise Variance of the crosstalk noise

says that random polarity & random time shifts says that random polarity & random time shifts can be almost twice better than polarity alone can be almost twice better than polarity alone

< >N NN N1122

**( )22

Page 14: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

0 6.75X (km)

a) Standard migration (320 CSG) b) Time static σ = 0.1 s

f) SNR

c) Noise

0 6.75X (km) 0 6.75X (km)

0 6.75X (km) 0 6.75X (km)

e) Noise

0.01 0.1Time static σ (s)

polarity

Time static

Polarity and time static

Polarity+Time Statics+Location StaticsPolarity+Time StaticsPolarity

< < +/-+/- < < +/-+/-, , < < xx Time Statics

a) Polarity b) Noise d) Source polarity & static

Key Theory+Num. Results for 320 CSG SupergatherKey Theory+Num. Results for 320 CSG Supergather(Xin Wang, Yunsong Huang)(Xin Wang, Yunsong Huang)

Page 15: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Key Results Theory of Multisource Imaging Key Results Theory of Multisource Imaging of Encoded Supergathers of Encoded Supergathers (Xin Wang)(Xin Wang)

Sig/Noise = GI < GINSig/Noise = GI < GIN

# geophones/supergather

# subsupergatherss

0 6.7X (km)

a) Image of 1 stack

Iteration Number

c) Image of 50 stacks

0 6.75

X (km)

0 6.7X (km)

b) Image of 5 stacks

1 115

d) SNR vs Iterations

Observed

Prediction

# iterations

Bulk shift

Page 16: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Standard Migration SNR

GS# geophones/CSG# geophones/CSG

# CSGs# CSGs

SNR= ...

migrate

SNR=

d(t) =d(t) =Zero-mean white noise

[s(t) +n(t) ][s(t) +n(t) ] Neglect geometric spreading

Standard Migration SNR

Standard Migration SNR

Assume:

migrate+++

stack

S1

SGS G~~

iterate

GI

Iterative Multisrc. Mig. SNR

# iterations# iterations

SNR=

Cost ~ O(S)

Cost ~ O(I)

Page 17: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

OutlineOutline1.1. Seismic Experiment:Seismic Experiment:

L m = d

L m = d1 1

L m = d2 2...N N

2. Standard vs Phase Encoded Least Squares Soln.2. Standard vs Phase Encoded Least Squares Soln.

LL11

LL22

dd 11

dd 22m =m = vs N L + N LN L + N L11 2211 22[ ]mm = [N = [N dd + N + N dd ] ]11 2211 22

3. Theory Noise Reduction3. Theory Noise Reduction

4. Summary 4. Summary

Page 18: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

SNR: VS3. 3. GS GI

2. 2.

11. .

Polarity+Time Statics+Location StaticsPolarity+Time StaticsPolarity

< < +/- +/- < < +/-+/-, , < < xx Time Statics

LL11

LL22

dd 11

dd 22m =m = N L + N LN L + N L

11 2211 22[ ]mm = [N = [N dd + N + N dd ] ]

11 2211 22

Summary

vs

LL ( (L L m - d ) m - d ) 22

TT

1111 + L+ L ( (L L m - d ) m - d ) 11

TT

2222 e-2 2

O( )~< >

4. Passive Seismic Interferometry = Multisrc4. Passive Seismic Interferometry = Multisrc Imaging Imaging

Page 19: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

IO 1 1/320

Cost ~

Resolution dx 1 1

SNR~

Stnd. Mig Multsrc. LSMStnd. Mig Multsrc. LSM

Less 1

1 <1/10

Cost vs QualityCost vs Quality

Summary

1

LL11

LL22

dd 11

dd 22m =m = N L + N LN L + N L

11 2211 22[ ]mm = [N = [N dd + N + N dd ] ]

11 2211 22

Page 20: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

SN

R0

1 Number of Iterations 300

7The SNR of MLSM image grows as the square root of the number of iterations.

SNR = GI

Page 21: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

0 6.75X (km)

a) Standard migration (320 CSG) b) Time static σ = 0.1 s

f) SNR

c) Noise

0 6.75X (km) 0 6.75X (km)

0 6.75X (km) 0 6.75X (km)

e) Noise

0.01 0.1Time static σ (s)

polarity

Time static

Polarity and time static

Polarity+Time Statics+Location StaticsPolarity+Time StaticsPolarity

< +/- < +/-, < +/- < +/-, < < xx Time Statics

a) Polarity b) Noise d) Source polarity & static

Key Theory+Num. Results for 320 CSG SupergatherKey Theory+Num. Results for 320 CSG Supergather(Xin Wang, Yunsong Huang)(Xin Wang, Yunsong Huang)

Page 22: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Key Results Theory of Multisource Imaging Key Results Theory of Multisource Imaging of Encoded Supergathers of Encoded Supergathers (Xin Wang)(Xin Wang)

Sig/Noise = GI < GINSig/Noise = GI < GIN

# geophones/supergather

# subsupergatherss

0 6.7X (km)

a) Image of 1 stack

Iteration Number

c) Image of 50 stacks

0 6.75

X (km)

0 6.7X (km)

b) Image of 5 stacks

1 115

d) SNR vs Iterations

Observed

Prediction

# iterations

Page 23: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Key Results Theory of Multisource Imaging Key Results Theory of Multisource Imaging of Encoded Supergathers of Encoded Supergathers (Boonyasiriwat)(Boonyasiriwat)

Sig/Noise = GI < GINSig/Noise = GI < GIN

3.5 km

Dynamic QMC TomogramDynamic QMC Tomogram (99 CSGs/supergather)(99 CSGs/supergather)

Dynamic Polarity TomogramDynamic Polarity Tomogram(1089 CSGs/supergather)(1089 CSGs/supergather)

1/1000 1/300

# geophones/supergather

# iterations

# subsupergatherss

Page 24: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Multisource Migration:Multisource Migration: mmmigmig=L=LTTdd

Forward Model:Forward Model:

Multisource Phase Encoded ImagingMultisource Phase Encoded Imaging

d +d +dd =[ =[L +L +LL ]m ]m11 222211

LL{dd{

=[=[L +L +LL ]( ](dd + + dd ) ) 11 222211

TT TT

= = L d +L d +L dL d + + 11 222211

TT TT

LL dd + +L L dd22 112211

Crosstalk noiseCrosstalk noiseStandard migrationStandard migration

TT TT

m = m +(k+1) (k)

Page 25: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Polarity+Time Statics+Location StaticsPolarity+Time StaticsPolarity

Relative Merits of 4 Encoding StrategiesRelative Merits of 4 Encoding Strategies < < +/- +/- < < +/-+/-, , < < xx

dd 11LL mm==11 dd 33LL mm==33dd 22LL mm==22

Time Statics

supergather

Supergather #2

Supergather #3

Supergather #4

Supergather #1

< < +/- +/- < < +/-+/-, , < < xx

Page 26: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Multisource Migration:Multisource Migration: mmmigmig=L=LTTdd

Forward Model:Forward Model:

Phase Encoded Multisource Migration Phase Encoded Multisource Migration

d +d +dd =[ =[L +L +LL ]m ]m11 222211

LL{dd{

=[=[L +L +LL ]( ](dd + + dd ) ) 11 222211

TT TT

= = L d +L d +L dL d + + 11 222211

TT TT

LL dd + +L L dd22 112211

Crosstalk noiseCrosstalk noiseStandard migrationStandard migration

TT TTmmmigmig

= = L d +L d +L dL d + + 11 222211

TT TT

LL dd + +LL dd22 112211

TT TTmmmigmig

mmmigmig

= = L d +L d +L dL d11 222211

mmmigmig

+ +

Page 27: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Multisource Migration:Multisource Migration: mmmigmig=L=LTTdd

Forward Model:Forward Model:

Phase Encoded Multisrce Phase Encoded Multisrce Least Squares Least Squares Migration Migration

d +d +dd =[ =[L +L +LL ]m ]m11 222211

LL{dd{

=[=[L +L +LL ]( ](dd + + dd ) ) 11 222211

TT TTmmmigmig

= = L d +L d +L dL d + + 11 222211

TT TT

LL dd + +L L dd22 112211

Crosstalk noiseCrosstalk noiseStandard migrationStandard migration

TT TT

m = m +(k+1) (k)

Page 28: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

OutlineOutline1.1. Seismic Experiment:Seismic Experiment:

L m = d

L m = d1 1

L m = d2 2...N N

2. Standard vs Phase Encoded Least Squares Soln.2. Standard vs Phase Encoded Least Squares Soln.

LL11

LL22

dd 11

dd 22m =m = vs N L + N LN L + N L11 2211 22[ ]mm = [N = [N dd + N + N dd ] ]11 2211 22

3. Theory Noise Reduction3. Theory Noise Reduction

4. Numerical 4. Numerical

TestsTests

Page 29: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

RTM & FWI Problem & Possible Soln.RTM & FWI Problem & Possible Soln.

• ProblemProblem:: RTM & FWI computationally costly RTM & FWI computationally costly

• Solution:Solution: Multisource LSM & FWI Multisource LSM & FWI

Preconditioning speeds up by factor 2-3Preconditioning speeds up by factor 2-3

LSM reduces crosstalkLSM reduces crosstalk

Page 30: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Multisource Migration:Multisource Migration: mmmigmig=L=LTTdd

Forward Model:Forward Model:

Multisource Least Squares Migration Multisource Least Squares Migration

d +d =[d +d =[L +L ]mL +L ]m11 222211

LL{dd{Standard migration

Crosstalk term

Phase encodingPhase encoding

Kirchhoff kernelKirchhoff kernel

Page 31: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Multisource Least Squares Migration Multisource Least Squares Migration Crosstalk term

Page 32: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Conventional Least Squares Conventional Least Squares Solution: Solution: L=L= & & d = d =

GivenGiven: : LLm=dm=d

FindFind: m s.t. min||: m s.t. min||LLm-d||m-d|| 22

SolutionSolution: m = [: m = [L LL L] ] LL d d TT TT-1-1

m = m – m = m – LL ( (LLm - d) m - d) TT(k+1)(k+1) (k)(k) (k)(k)(k)(k)

or if or if LL is too big is too big

ProblemProblem::

LL11

LL22

dd 11

dd 22

= m – = m – LL ( (L L m - d ) m - d ) (k)(k)

+ L+ L ( (L L m - d ) m - d ) 11 11 22 22 2211

TTTT[ ]

In general, hugedimension matrix

Note: subscripts agree

Page 33: Theory of Multisource Crosstalk Reduction by Phase-Encoded Statics

Key Results Theory of Multisource Imaging Key Results Theory of Multisource Imaging of Encoded Supergathers of Encoded Supergathers (Boonyasiriwat)(Boonyasiriwat)

Sig/Noise = GI < GINSig/Noise = GI < GIN

3.5 km

Dynamic QMC TomogramDynamic QMC Tomogram (99 CSGs/supergather)(99 CSGs/supergather)

Dynamic Polarity TomogramDynamic Polarity Tomogram(1089 CSGs/supergather)(1089 CSGs/supergather)

1/1000 1/300

# geophones/supergather

# iterations

# subsupergatherss