IP Library › Granted Patent US 7,986,586
Granted Patent B2
US 7,986,586 · App. 12/082,006 · Granted Jul 26, 2011

Method for deghosting marine seismic streamer data with irregular receiver positions

Assignee: PGS Geophysical AS
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Quick Facts
Patent No.
US 7,986,586
App. No.
12/082,006
Granted
Jul 26, 2011
Kind
B2
Abstract

Seismic data are obtained for each seismic source activation in a marine streamer and for each frequency, after being transformed to a spectral domain. An iterative conjugate gradient scheme, using a physically-based preconditioner, is applied to the transformed seismic data, to provide a least squares solution to a normal set of equations for a deghosting system of equations. The solution is inverse-transformed back to a space-time domain to provide deghosted seismic data.

Claims (1140)

1. A method for deghosting seismic data recorded from marine streamers with irregular receiver positions, comprising:

obtaining seismic data for a seismic source activation and for a frequency after being transformed to a spectral domain;

applying an iterative conjugate gradient scheme, using a preconditioner constructed according to a physical problem of deghosting seismic data from marine streamers, to the transformed seismic data, to provide a least squares solution to a normal set of equations for a deghosting system of equations; and

inverse-transforming the solution back to a space-time domain to provide deghosted seismic data.

2. The method of claim 1 , wherein the obtaining seismic data comprises:

obtaining seismic data recorded with a marine streamer;

obtaining recorded seismic data for a seismic source activation;

transforming the recorded seismic data for a seismic source activation from the space-time domain to the space-frequency domain;

obtaining transformed seismic data for a frequency; and

transforming the transformed seismic data for a frequency from the space-frequency domain to the spectral domain.

3. The method of claim 2 , wherein the transforming the recorded seismic data comprises:

transforming the scattered acoustic wavefield from the space-time (x 1 R ,x 2 R ,x 3 R ,t) domain to the space-frequency (x 1 R ,x 2 R ,x 3 R ,s) domain using a Fourier transform, so:

p sct =p sct ( x 1,q R ,x 2,r R ,x 3 R ;s )

where

s=jω=j 2 πf,

and p sct is the scattered acoustic wavefield in the space-frequency domain, x 1,q R is an in-line receiver coordinate, q is an in-line receiver number, x 2,r R is a cross-line receiver coordinate, r is a cross-line receiver number, x 3 R is receiver depth as a function of x 1,q R and x 2,r R , s is a complex Laplace transform parameter, j is imaginary unit √{square root over (−1)}, ω is circular frequency, and f is frequency.

4. The method of claim 3 , wherein the transforming the transformed seismic data comprises:

transforming the scattered wave field p sct from the space-frequency domain (x 1 R ,x 2 R ,x 3 R ,s) to the spectral domain (sα n ,sβ m ,x 3 R ,s) by:

P

n

,

m

sct

=

Δ

⁢

⁢

x

1

R

⁢

Δ

⁢

⁢

x

2

R

⁢

∑

q

=

-

1

2

⁢

N

+

1

1

2

⁢

N

⁢

∑

r

=

-

1

2

⁢

M

+

1

1

2

⁢

M

⁢

exp

⁡

(

j

⁢

⁢

s

⁢

⁢

α

n

⁢

x

1

,

q

R

+

j

⁢

⁢

s

⁢

⁢

β

m

⁢

x

2

,

r

R

)

⁢

p

sct

,

⁢

where

⁢

:

s

⁢

⁢

α

n

=

n

⁢

⁢

Δ

⁡

(

s

⁢

⁢

α

)

,

s

⁢

⁢

β

m

=

m

⁢

⁢

Δ

⁡

(

s

⁢

⁢

β

)

,

⁢

and

⁢

:

Δ

⁡

(

s

⁢

⁢

α

)

=

2

⁢

π

N

⁢

⁢

Δ

⁢

⁢

x

1

R

,

Δ

⁡

(

s

⁢

⁢

β

)

=

2

⁢

π

M

⁢

⁢

Δ

⁢

⁢

x

2

R

⁢

,

and P n,m sct is the scattered acoustic wavefield in the spectral domain, n is an in-line spectral number, m is a cross-line spectral number, Δx 1 R is in-line receiver sampling distance, Δx 2 R is cross-line receiver sampling distance, jsα n is an in-line spectral Fourier parameter, Δ(sα) is in-line spectral sampling distance, jsβ m is a cross-line spectral Fourier parameter, Δ(sβ) is cross-line spectral sampling distance, N is total number of in-line receivers, and M is total number of cross-line receivers.

5. The method of claim 4 , further comprising:

determining a system of equations for deghosting the transformed seismic data for a frequency;

determining a normal set of equations for the deghosting system of equations; and

applying the constructed preconditioner to the normal set of equations.

6. The method of claim 5 , wherein the determining a system of equations for deghosting comprises applying the following equation:

∑

n

=

-

1

2

⁢

N

+

1

1

2

⁢

N

⁢

∑

m

=

-

1

2

⁢

M

+

1

1

2

⁢

M

⁢

K

q

,

r

;

n

,

m

⁢

P

n

,

m

dgh

=

p

q

,

r

sct

,

⁢

q

=

-

1

2

⁢

N

+

1

,

…

⁢

,

1

2

⁢

N

,

⁢

r

=

-

1

2

⁢

M

+

1

,

…

⁢

,

1

2

⁢

M

,

in which the system matrix K q,r;n,m is given by

K

q

,

r

;

n

,

m

=

Δ

⁢

⁢

(

s

⁢

⁢

α

)

⁢

Δ

⁡

(

s

⁢

⁢

β

)

4

⁢

π

2

⁢

∑

n

=

-

1

2

⁢

N

+

1

1

2

⁢

N

⁢

∑

m

=

-

1

2

⁢

M

+

1

1

2

⁢

M

⁢

exp

⁡

(

-

j

⁢

⁢

s

⁢

⁢

α

n

⁢

x

1

,

q

R

-

j

⁢

⁢

s

⁢

⁢

β

m

⁢

x

2

,

r

R

)

⁢

2

⁢

⁢

sinh

⁡

(

s

⁢

⁢

Γ

n

,

m

⁢

x

3

R

)

.

7. The method of claim 6 , wherein the determining a normal set of equations comprises applying the following equation:

∑

n

=

-

1

2

⁢

N

+

1

1

2

⁢

N

⁢

∑

m

=

-

1

2

⁢

M

+

1

1

2

⁢

M

⁢

A

n

′

,

m

′

;

n

,

m

⁢

P

n

,

m

dgh

=

B

n

′

,

m

′

,

⁢

n

′

=

-

1

2

⁢

N

+

1

,

…

⁢

,

1

2

⁢

N

,

m

′

=

-

1

2

⁢

M

+

1

,

…

⁢

,

1

2

⁢

M

,

where, the matrix A n′,m;n,m is given by

A

n

′

,

m

′

;

n

,

m

=

∑

q

=

-

1

2

⁢

N

+

1

1

2

⁢

N

⁢

∑

r

=

-

1

2

⁢

M

+

1

1

2

⁢

M

⁢

K

q

,

r

;

n

′

,

m

′

_

⁢

K

q

,

r

;

n

,

m

,

the known vector B n′,m′ is given by

B

n

′

,

m

′

=

∑

q

=

-

1

2

⁢

N

+

1

1

2

⁢

N

⁢

∑

r

=

-

1

2

⁢

M

+

1

1

2

⁢

M

⁢

K

q

,

r

;

n

′

,

m

′

_

⁢

p

q

,

r

sct

,

and n and n′ are in-line spectral numbers, m and m′ are cross-line spectral numbers, and the overline designates complex conjugation.

8. The method of claim 6 , wherein the preconditioner comprises an inverse of the system matrix for a horizontal streamer.

9. The method of claim 8 , wherein the applying a preconditioner comprises applying the following equation:

P

~

n

,

m

=

[

A

n

,

m

;

n

,

m

]

-

1

2

=

(

∑

q

=

-

1

2

⁢

N

+

1

1

2

⁢

N

⁢

∑

r

=

-

1

2

⁢

M

+

1

1

2

⁢

M

⁢

K

q

,

r

;

n

,

m

2

)

-

1

2

.

10. The method of claim 1 , wherein the applying an iterative conjugate gradient scheme comprises:

selecting an initial estimate for iteration counter k=0, as follows:

P n dgh(0) =0, r q (0) =p q sct ,

calculating estimates for iteration counter k=1, as follows:

g

n

(

1

)

=

P

~

n

⁢

∑

q

⁢

K

q

,

n

_

⁢

r

q

(

0

)

,

v

n

(

1

)

=

P

~

n

⁢

g

n

(

1

)

,

K

⁢

⁢

v

n

(

1

)

=

∑

n

⁢

K

q

,

n

⁢

v

n

(

1

)

,

α

(

1

)

=

∑

n

⁢

g

n

(

1

)

2

∑

q

⁢

Kv

n

(

1

)

2

,

P

n

dgh

⁡

(

1

)

=

P

n

dgh

⁡

(

0

)

+

α

(

1

)

⁢

v

n

(

1

)

,

r

q

(

1

)

=

r

q

(

0

)

-

α

(

1

)

⁢

Kv

n

(

1

)

,

performing the following until an error criterion is met:

increasing the iteration counter by k=k+1; and

calculating estimates for iteration counter k, using previous estimates calculated for k−1, as follows:

g

n

(

k

)

=

P

~

n

⁢

∑

q

⁢

K

q

,

n

_

⁢

r

q

(

k

-

1

)

,

v

n

(

k

)

=

P

~

n

⁢

g

n

(

k

)

+

∑

n

⁢

g

n

(

k

)

2

∑

n

⁢

g

n

(

k

-

1

)

2

⁢

v

n

(

k

)

,

K

⁢

⁢

v

n

(

k

)

=

∑

n

⁢

K

q

,

n

⁢

v

n

(

k

)

,

α

(

k

)

=

∑

n

⁢

g

n

(

k

)

2

∑

q

⁢

Kv

n

(

k

)

2

,

P

n

dgh

⁡

(

k

)

=

P

n

dgh

⁡

(

k

-

1

)

+

α

(

k

)

⁢

v

n

(

k

)

,

r

q

(

k

)

=

r

q

(

k

-

1

)

-

α

(

k

)

⁢

Kv

n

(

k

)

.

11. The method of claim 5 , wherein the error criterion is given by:

∑

q

⁢

r

q

(

k

)

2

∑

q

⁢

p

q

sct

2

<

10

-

3

.

12. The method of claim 4 , wherein the inverse-transforming the solution comprises applying the following equation:

p

dgh

=

Δ

⁡

(

s

⁢

⁢

α

)

⁢

Δ

⁡

(

s

⁢

⁢

β

)

4

⁢

π

2

⁢

∑

n

=

-

1

2

⁢

N

+

1

1

2

⁢

N

⁢

∑

m

=

-

1

2

⁢

M

+

1

1

2

⁢

M

⁢

exp

⁡

(

-

j

⁢

⁢

s

⁢

⁢

α

n

⁢

x

1

,

q

R

-

j

⁢

⁢

s

⁢

⁢

β

m

⁢

x

2

,

r

R

)

⁢

P

n

,

m

dgh

.

Assignments (2)
ASSIGNMENT OF ASSIGNOR'S INTEREST Recorded Jul 16, 2008
From: VAN BORELEN, ROALD G.; BERG, PETER M. VAN DEN; FOKKEMA, JACOB T.
To: PGS GEOPHYSICAL AS
Reel/Frame 021249/0556 →
ASSIGNMENT OF ASSIGNOR'S INTEREST Recorded Dec 8, 2006
From: SILVERBROOK, KIA
To: SILVERBROOK RESEARCH PTY LTD
Reel/Frame 018659/0907 →
Continuity (1)
Related Publication 20090251992A1 · Oct 8, 2009