Method Of Borehole Seismic Surveying Using An Optical Fiber

• US 20140347957A1
• Filed: 05/22/2013
• Published: 11/27/2014
• Est. Priority Date: 05/22/2013
• Status: Active Grant

• Current Assignee: Schlumberger Technology Corporation (Schlumberger NV)
• Original Assignee: Schlumberger Technology Corporation (Schlumberger NV)
• Inventors: Hartog, Arthur H., Mackie, Duncan, Frignet, Bernard, Clark, Michael
• Granted Patent: US 9,377,551 B2
• Time in Patent Office: Days
• US Class Current: 367/33
• CPC Class Codes: G01H 9/004 using fibre optic sensors light guides per se G02B6/00, acousto-optical devices specially adapted for gating or modulating in optical wave guides G02F1/125
• CPC Class Codes: G01V 1/20 Arrangements of receiving elements, e.g. geophone pattern
• CPC Class Codes: G01V 1/40 specially adapted for well-logging
• CPC Class Codes: G01V 1/42 using generators in one well and receivers elsewhere or vice versa G01V1/52 takes precedence
• CPC Class Codes: G01V 1/44 using generators and receivers in the same well G01V1/52 takes precedence
• CPC Class Codes: G01V 2210/1429 Subsurface, e.g. in borehole or below weathering layer or mud line

Abstract

A method of detecting seismic waves traveling through a subsurface formation includes lowering a cable into a borehole in the subsurface formation, the cable having at least one optical fiber associated therewith, and causing descent of a remote end of the cable to be arrested. The method further includes feeding a further length of the cable into the borehole such that the cable is slack and in contact with at least part of a wall of the borehole, and using an interrogator coupled to the at least one optical fiber to detect seismic waves traveling through the subsurface formation and into the cable.

Claims

1. A method of detecting seismic waves traveling through a subsurface formation comprising:

lowering a cable into a borehole in the subsurface formation, the cable having at least one optical fiber associated therewith;

causing descent of a remote end of the cable to be arrested;

feeding a further length of the cable into the borehole such that the cable is slack and in contact with at least part of a wall of the borehole; and

using an interrogator coupled to the at least one optical fiber to detect seismic waves traveling through the subsurface formation and into the cable.

2. The method of claim 1, wherein the seismic waves are generated by activating a seismic source at the surface.

3. The method of claim 1, wherein the seismic waves are generated by activating a seismic source in the borehole.

4. The method of claim 1, wherein the seismic waves are generated by activating a seismic source in another borehole.

5. The method of claim 1, wherein the seismic waves are generated by a microseismic event.

6. The method of claim 1, wherein the descent of the remote end of the cable is arrested by a bottom of the borehole.

7. The method of claim 1, wherein the descent of the remote end of the cable is arrested by a restriction in the borehole.

8. The method of claim 1, wherein the descent of the remote end of the cable is arrested by an anchoring system.

9. The method of claim 1, wherein an exterior surface of the cable is textured so as to increase friction between the cable and the wall of the borehole.

10. The method of claim 1, wherein a hardness of an exterior surface of the cable is selected so as to increase friction between the cable and the wall of the borehole.

11. The method of claim 1, wherein the cable has the at least one optical cable embedded therein.

12. The method of claim 1, wherein the cable has the at least one optical cable affixed thereto.

13. The method of claim 1, wherein the cable comprises a plurality of strands with the at least one optical cable helically wound therethrough.

14. The method of claim 1, wherein the cable comprises a plurality of strands wound helically around the at least one optical fiber.

15. The method of claim 1, further comprising determining at least one formation property from the detected seismic waves, using a computer coupled to the interrogator.

16. The method of claim 15, wherein determining the at least one formation property includes correlating the detected seismic waves to a true depth of a given portion of the at least one optical fiber in the borehole.

17. The method of claim 16, wherein correlating the detected seismic waves to the true depth of the given portion of the at least one optical fiber in the borehole comprises:

making a first distributed strain measurement of the at least one optical fiber before the descent of the remote end of the cable is arrested;

making a second distributed strain measurement of the at least one optical fiber after the descent of the remote end of the cable is arrested;

determining a strain profile along the at least one optical fiber based upon the first distributed strain measurement and the second distributed strain measurement;

using the strain profile to correlate the detected seismic waves to the true depth of the given portion of the at least one optical fiber in the borehole.

18. The method of claim 17, wherein the first distributed strain measurement is a first Brillouin backscatter measurement;

and wherein the second distributed strain measurement is a second Brillouin backscatter measurement.

19. The method of claim 17, wherein the first distributed strain measurement is a first Rayleigh backscatter measurement;

and wherein the second distributed strain measurement is a second Rayleigh backscatter measurement.

20. The method of claim 16, wherein correlating the detected seismic waves to the true depth of the given portion of the at least one optical fiber in the borehole comprises:

waiting a first period of time to allow a temperature of the cable to stabilize after descent of the remote end of the cable has been arrested but before the further length of the cable has been fed into the borehole;

using a distributed temperature sensing technique to measure a first temperature profile of the at least one optical fiber;

waiting a second period of time to allow the temperature of the cable to further stabilize after the further length of the cable has been fed into the borehole;

using the distributed temperature sensing technique to measure a second temperature profile of the at least one optical fiber after waiting the second period of time;

using the first temperature profile and the second temperature profile to correlate the detected seismic waves to the true depth of the given portion of the at least one optical fiber in the borehole.

21. The method of claim 16, wherein the at least one optical fiber comprises a vibration sensing optical fiber and a temperature sensing optical fiber;

and wherein correlating the detected seismic waves to the true depth of the given portion of the at least one optical fiber in the borehole comprises;

waiting a first period of time to allow a temperature of the cable to stabilize after descent of the remote end of the cable has been arrested but before the further length of the cable has been fed into the borehole;

using a distributed temperature sensing technique to measure a first temperature profile of the temperature sensing optical fiber;

waiting a second period of time to allow the temperature of the cable to further stabilize after the further length of the cable has been fed into the borehole;

using the distributed temperature sensing technique to measure a second temperature profile of the temperature sensing after waiting the second period of time;

using the first temperature profile and the second temperature profile to correlate the detected seismic waves to the true depth of the given portion of the vibration sensing optical fiber in the borehole.

28. The method of claim 21, wherein the cable comprises a plurality of strands wound helically around the at least one optical fiber.

29. The method of claim 21, wherein determining the at least one formation property includes correlating the detected seismic waves to a true depth of a given portion of the at least one optical fiber in the borehole.

22. A method of detecting seismic waves traveling through a subsurface formation comprising:

lowering a cable into a borehole in the subsurface formation, the cable having at least one optical fiber associated therewith;

deploying a seismic sensing tool associated with the cable;

causing descent of a remote end of the cable to be arrested;

feeding a further length of the cable into the borehole such that the cable is slack and in contact with at least part of a wall of the borehole;

detecting seismic waves traveling through the subsurface formation and into the seismic sensing tool;

using an interrogator coupled to the at least one optical fiber to detect seismic waves traveling through the subsurface formation and into the cable; and

determining at least one formation property from the detected seismic waves, using a computer coupled to the seismic sensing tool and to the interrogator.

23. The method of claim 22, wherein the descent of the remote end of the cable is arrested by an anchoring mechanism of the seismic sensing tool.

24. The method of claim 22, wherein the seismic waves are generated by activating a seismic source at the surface.

25. The method of claim 22, wherein the seismic waves are generated by activating a seismic source in the borehole.

26. The method of claim 22, wherein the seismic waves are generated by a microseismic event.

27. The method of claim 22, wherein the cable comprises a plurality of strands with the at least one optical cable helically wound therethrough.