System and method for estimating seismic material properties

• US 6,903,999 B2
• Filed: 01/19/2001
• Issued: 06/07/2005
• Est. Priority Date: 01/21/2000
• Status: Expired due to Term

• Current Assignee: Schlumberger Technology Corporation (SLB)
• Original Assignee: Schlumberger Technology Corporation (SLB)
• Inventors: Curtis, Andrew, Robertsson, Johan Olof Anders, Muijs, Remco
• Primary Examiner(s): Lobo, Ian J.
• Application Number:
  US10/181,234
• Publication Number:
  US 20030117894A1
• Time in Patent Office: 1,600 Days
• Field of Search: 367/21, 367/25, 367/38, 367/54, 367/58, 367/59, 367/60, 367/73, 702/6, 702/11, 702/14
• US Class Current: 367/38
• CPC Class Codes: G01V 1/20 Arrangements of receiving elements, e.g. geophone pattern
• CPC Class Codes: G01V 1/286 Mode conversion
• CPC Class Codes: G01V 1/30 Analysis G01V1/50 takes precedence
• CPC Class Codes: G01V 1/32 Transforming one recording into another or one representation into another
• CPC Class Codes: G01V 1/364 Seismic filtering G01V1/37 takes precedence
• CPC Class Codes: G01V 2210/42 Waveform, i.e. using raw or pre-filtered trace data

Abstract

A method for estimating near-surface material properties in the vicinity of a locally dense group of seismic receivers is disclosed. The method includes receiving seismic data that has been measured by a locally dense group of seismic receivers. Local derivatives of the wavefield are estimated such that the derivatives are centered at a single location preferably using the Lax-Wendroff correction. Physical relationships between the estimated derivatives including the free surface condition and wave equations are used to estimate near-surface material properties in the vicinity of the receiver group. Another embodiment of the invention is disclosed wherein the physical relationships used to estimate material properties are derived from the physics of plane waves arriving at the receiver group, and the group of receivers does not include any buried receivers.

Claims

1. A method of estimating near-surface material properties in the vicinity of a locally dense group of seismic receivers comprising the steps of:

receiving data measured by the locally dense group of seismic receivers, the data representing earth motion caused by a seismic wavefield;

estimating local derivatives of the wavefield such that the derivatives are centered at a single location in the vicinity of the receiver group; and

using physical relationships between the estimated derivatives to estimate near-surface material properties in the vicinity of the receiver group.

2. The method of claim 1 wherein the step of estimating the local derivatives includes centering the derivatives using a technique substantially similar to the Lax-Wendroff correction.

3. The method of claim 1 wherein the physical relationships used to estimate material properties include the free surface condition.

4. The method of claim 1 wherein the physical relationships used to estimate material properties include wave equations.

5. The method of claim 1 wherein at least one of the receivers in the receiver group is buried below the earth surface such that the receiver group encloses a volume.

6. The method of claim 1 wherein the receivers in the locally dense group are spaced around 1 meter or less from each other.

7. The method of claim 6 wherein the receivers in the group are spaced around 0.5 meters or less from each other.

8. The method of claim 7 wherein the receivers in the group are spaced around 0.25 meters or less form each other.

9. The method of claim 1 wherein the receivers in the group are spaced apart by a distance approximately equal to or less than one-fifth of the shortest wavelength of interest.

10. The method of claim 1 wherein the material properties estimated include those experienced by the incoming wavefield that are frequency and wave type dependent.

11. The method of claim 1 wherein the receivers are located at or near the sea bottom, and wherein the physical relationships used to estimate material properties include fluid-solid boundary conditions.

12. The method of claim 1 wherein the receivers are located in a borehole.

13. The method of claim 1 wherein the physical relationships used to estimate material properties are derived from the physics of plane waves arriving at the receiver group.

14. The method of claim 13 wherein the group of receivers does not include any buried receivers.

15. An apparatus for estimating near-surface material properties in the vicinity of a locally dense group of seismic receivers comprising:

a storage configured to store data measured by the locally dense group of seismic receivers, the stored data representing earth motion caused by a seismic wavefield;

a derivative estimator adapted to process the stored data and estimate local derivatives of the wavefield such that the derivatives are centered at a single location in the vicinity of the receiver group; and

a material property estimator adapted to estimate physical relationships between the estimated derivatives to estimate near-surface material properties in the vicinity of the receiver group.

16. The apparatus of claim 15 wherein the derivative estimator centers the derivatives using a technique substantially similar to the Lax-Wendroff correction, and the physical relationships used to estimate material properties include the free surface condition.

17. The apparatus of claim 16 wherein the receivers in the locally dense group are spaced around 1 meter or less from each other.

18. The apparatus of claim 15 wherein the receivers are located at or near the sea bottom, and wherein the physical relationships used to estimate material properties include fluid-solid boundary conditions.

19. The apparatus of claim 15 wherein the physical relationships used to estimate material properties are derived from the physics of plane waves arriving at the receiver group.