High fidelity vibratory source seismic method with source separation

• US 5,721,710 A
• Filed: 09/20/1996
• Issued: 02/24/1998
• Est. Priority Date: 09/29/1995
• Status: Expired due to Term

• Current Assignee: Atlantic Richfield Company (BP PLC), Mobil Oil Corporation (Exxon Mobil Corporation)
• Original Assignee: Atlantic Richfield Company (BP PLC), Mobil Oil Corporation (Exxon Mobil Corporation)
• Inventors: Sallas, John J., Allen, Kenneth Paul, Corrigan, Dennis
• Primary Examiner(s): Lobo, Ian J.
• Application Number:
  US08/717,176
• Time in Patent Office: 522 Days
• Field of Search: 364/421, 367/38, 367/41, 367/42, 367/43, 367/46
• US Class Current: 367/41
• CPC Class Codes: G01V 1/375 Correlating received seismic signals with the emitted source signal
• CPC Class Codes: G01V 2210/127 Cooperating multiple sources
• CPC Class Codes: G01V 2210/26 Modulation or demodulation, e.g. for continuous sources

Abstract

A method of separating the effects of the earth response on vibratory energy from individual ones of multiple vibrators to geophones, in generating a seismic survey, is disclosed. According to the disclosed method, measurements of the actual vibrations generated at the source are made, in addition to the geophone measurements of the refracted and reflected vibrations, both over a number of frequency sweeps. The source and geophone vibrations are first transformed into frequency domain representations, by way of Discrete Fourier Transforms. An inverse matrix of the recorded frequency-domain source vibrations is then generated for each frequency. When the number of sweeps equals the number of vibrators, the inverse matrix is merely the multiplicative inverse of the source measurements; if the number of sweeps exceeds the number of vibrators, the inverse matrix is the generalized inverse of the original matrix. The inverse matrix for the frequency is applied to the recorded geophone vibrations at that frequency, to derive the transfer function, corresponding to the earth response, for each vibrator-geophone path in the survey. A weighting factor may be used to discount the effects of poorly behaved sweeps, and may be based on the ratio of the maximum and minimum eigenvalues for the inverse matrix. Using these derived transfer functions, an earth reflectivity function may be derived for each vibrator-geophone path by applying a minimum phase filter to the separated vibrator-geophone transfer function over frequency; this filter removes the effects of a ##EQU1## term, and yields the earth reflectivity function for the path.

Claims

1. A method of performing a vibratory seismic survey, comprising the steps of:

energizing a plurality of vibrators at the surface of the earth to vibrate the earth over a plurality of frequency sweeps, the number of the plurality of frequency sweeps being at least the number of the plurality of vibrators;

during the energizing step, measuring source vibrations at or near the plurality of vibrators;

storing a representation of the measured source vibrations in computer memory;

detecting field vibrations at a plurality of detecting locations at the surface of the earth, the detecting locations being spaced apart from the location of the plurality of vibrators to define a plurality of vibrator-detector paths, each associated with one of the plurality of vibrators and one of the plurality of detecting locations;

storing a representation of the measured field vibrations in computer memory;

for each of the plurality of vibrator-detector paths, determining an earth response transfer function at a plurality of frequencies based upon a representation of the measured field vibrations at the detecting location associated with the vibrator-detector path as contributed by the vibrator associated with the vibrator-detector path and upon a representation of the measured source vibrations from the associated vibrator; and

determining an earth reflectivity function for each of the plurality of vibrator-detector paths by operating a computer to perform a plurality of operations comprising;

retrieving the earth response transfer function associated with the vibrator-detector path, over the plurality of frequencies; and

filtering the retrieved earth response transfer function with a minimum phase filter to yield the earth reflectivity function for the vibrator-detector path.

2. The method of claim 1, wherein the step of determining an earth response transfer function comprises:

retrieving, from computer memory, the stored representations of the measured source vibrations and measured field vibrations;

operating the computer to transform the stored representations of the measured source vibrations and measured field vibrations into frequency domain representations; and

operating the computer to perform, for each of the plurality of vibrator-detector paths, a plurality of operations comprising;

defining a first matrix of the frequency domain representation of the measured source vibrations at a frequency, and a second matrix of the frequency domain representation of the detected vibrations at the frequency;

determining an inverse of the first matrix;

multiplying the second matrix by the inverse of the first matrix to derive the earth response transfer functions at the frequency; and

repealing the defining, determining, and multiplying steps for a plurality of frequencies.

3. The method of claim 2, further comprising, at each of the plurality of frequencies:

determining the eigenvalues of the inverse of the first matrix; and

determining a weighting factor corresponding to the eigenvalues from the determining step.

4. The method of claim 3, wherein the weighting factor corresponds to a ratio of a maximum one of the eigenvalues to a minimum one of the eigenvalues from the determining step.

5. The method of claim 2, wherein the energizing step comprises:

energizing the plurality of vibrators over a plurality of frequency sweeps that equals the number of the plurality of vibrators;

and wherein the step of determining an inverse of the first matrix determines the multiplicative inverse of the first matrix.

6. The method of claim 2, wherein the energizing step comprises:

energizing the plurality of vibrators over a plurality of frequency sweeps that is greater than the number of the plurality of vibrators;

and wherein the step of determining an inverse of the first matrix determines the generalized inverse of the first matrix.

7. The method of claim 1, wherein the energizing step comprises:

simultaneously energizing each of the plurality of vibrators in a first phase relationship for a first frequency sweep; and

simultaneously energizing each of the plurality of vibrators in a second phase relationship, different from the first phase relationship, for a second frequency sweep.

8. The method of claim 1, wherein a selected one of the plurality of vibrators is not energized during each of the plurality of sweeps.

9. A method of generating a seismic survey based upon previously obtained vibratory seismic measurements including measurements of source vibrations from at or near vibrators located at the surface of the earth that are simultaneously energized over a plurality of sweeps, and measurements of detected vibrations from detector locations spaced away from the vibrators, the previously obtained vibratory seismic measurements being stored in digital form in a computer memory, comprising:

determining earth response transfer functions for each seismic path between one of the plurality of vibrators and one of the plurality of detecting locations, by operating a computer to perform the steps of;

retrieving, from computer memory, the stored representations of the measured source vibrations and measured field vibrations;

transforming the stored representations of the measured source vibrations and measured field vibrations into frequency domain representations;

defining a first matrix of the frequency domain representation of the measured source vibrations at a frequency, and a second matrix of the frequency domain representation of the detected vibrations at the frequency;

determining an inverse of the first matrix;

multiplying the second matrix by the inverse of the first matrix to derive the earth response transfer functions at the frequency to derive earth response transfer functions at the frequency; and

repeating the defining, determining, and multiplying steps for a plurality of frequencies; and

for a plurality of frequencies, filtering the earth response transfer function with a minimum phase filter.

10. The method of claim 9, further comprising:

for each pair of one of the plurality of vibrators and one of the plurality of detecting locations, at each of the plurality of frequencies;

determining the eigenvalues of the inverse of the first matrix; and

determining a weighting factor corresponding to the eigenvalues from the determining step.

11. The method of claim 10, wherein the weighting factor corresponds to a ratio of a maximum one of the eigenvalues to a minimum one of the eigenvalues from the determining step.

12. The method of claim 9, wherein the number of the plurality of frequency sweeps equals the number of the plurality of vibrators;

and wherein the step of determining an inverse of the first matrix determines the multiplicative inverse of the first matrix.

13. The method of claim 9, wherein the number of the plurality of frequency sweeps exceeds the number of the plurality of vibrators;

and wherein the step of determining an inverse of the first matrix determines the generalized inverse of the first matrix.

14. The method of claim 13, wherein the combining step is performed using frequency domain representations of the earth response transfer functions and measured source vibrations.

15. The method of claim 14, wherein the combining step is performed using time domain representations of the earth response transfer functions and measured source vibrations.

16. An apparatus for separating, from one another, the earth response to a plurality of sweeps of vibratory signals imparted from a plurality of vibrators simultaneously and received at a detecting location, comprising:

memory for storing representations of source vibrations as recorded at or near each of the plurality of vibrators;

memory for storing representations of vibrations detected at the detecting location;

a computer, coupled to the memories, and programmed in such a manner as to perform the steps of;

retrieving the stored representations of the measured source vibrations and measured field vibrations;

transforming the stored representations of the measured source vibrations and measured field vibrations into frequency domain representations;

defining a first matrix of the frequency domain representation of the measured source vibrations at a frequency, and a second matrix of the frequency domain representation of the detected vibrations at the frequency;

determining an inverse of the first matrix;

multiplying the second matrix by the inverse of the first matrix to derive the earth response transfer functions at the frequency;

repeating the defining, determining, and multiplying steps for a plurality of frequencies; and

applying a minimum phase filter to the result of the repeating step; and

an output device, coupled to the computer, for display of seismic survey information based on the earth response transfer functions.

17. The apparatus of claim 16, wherein the computer is also programmed to perform, at each of the plurality of frequencies, the steps of:

determining the eigenvalues of the inverse of the first matrix; and

determining a weighting factor corresponding to the eigenvalues from the determining step.

18. The apparatus of claim 17, wherein the weighting factor corresponds to a ratio of a maximum one of the eigenvalues to a minimum one of the eigenvalues from the determining step.

19. The apparatus of claim 17, wherein the number of the plurality of frequency sweeps equals the number of the plurality of vibrators;

and wherein the step of determining an inverse of the first matrix determines the multiplicative inverse of the first matrix.

20. The apparatus of claim 17, wherein the number of the plurality of frequency sweeps in the energizing step exceeds the number of the plurality of vibrators;

and wherein the step of determining an inverse of the first matrix determines the generalized inverse of the first matrix.