Detection of seismic signals using fiber optic distributed sensors

• US 9,470,807 B2
• Filed: 11/06/2013
• Issued: 10/18/2016
• Est. Priority Date: 05/26/2010
• Status: Active Grant

• Current Assignee: Schlumberger Technology Corporation (SLB)
• Original Assignee: Schlumberger Technology Corporation (SLB)
• Inventors: Coates, Richard T., Miller, Douglas E., Hartog, Arthur H., Wilson, Colin A., Brady, Dominic, Menkiti, Henry, Auzerais, Francois M., Bradford, Ian David Richard
• Primary Examiner(s): Pihulic, Daniel
• Application Number:
  US14/073,475
• Publication Number:
  US 20140064028A1
• Time in Patent Office: 1,077 Days
• US Class Current: 1/1
• CPC Class Codes: E21B 47/01 Devices for supporting measuring instruments on drill bits, pipes, rods or wirelines; Protecting measuring instruments in boreholes against heat, shock, pressure or the like
• CPC Class Codes: G01D 5/35361 using elastic backscattering to detect the measured quantity, e.g. using Rayleigh backscattering
• 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: G01L 1/242 the material being an optical fibre
• CPC Class Codes: G01L 1/246 using integrated gratings, e.g. Bragg gratings
• CPC Class Codes: G01V 1/18 Receiving elements, e.g. seismometer, geophone or torque detectors, for localised single point measurements
• CPC Class Codes: G01V 1/208 having a continuous structure detecting traffic G08G, transducers in general G10K
• CPC Class Codes: G01V 1/226 Optoseismic systems
• 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 1/52 Structural details

Abstract

A fiber optic distributed vibration system for detecting seismic signals in an earth formation is provided. The system includes a fiber optic cable deployed in a borehole that extends into the earth formation and which is configured to react along its length to a seismic wave incident on the fiber optic cable from outside the borehole. An optical source launches an optical signal into the fiber optic cable while the seismic wave is incident thereon. A receiver detects coherent Rayleigh noise (CRN) produced in response to the optical signal. A processing circuit processes the detected CRN signal to determine characteristics of the earth formation.

Claims

1. A seismic event detection system, comprising:

a first fiber optic cable disposed in a borehole extending from an earth surface into a formation, the first fiber optic cable configured to react along its length to incident seismic signals originating inside the borehole and propagating through the formation and the borehole;

an optical source to launch optical pulses into the first fiber optic cable while the seismic signals are incident on the first fiber optic cable; and

a data acquisition system coupled to the first fiber optic cable to detect coherent Rayleigh noise (CRN) generated in response to the optical pulses to determine characteristics of the formation based on the detected CRN.

2. The system as recited in claim 1, further comprising:

a second fiber optic cable disposed in the borehole and coupled to the optical source, the second fiber optic cable configured to react along its length to incident seismic signals,

wherein the first fiber optic cable is disposed at a first location within a transverse cross-section of the borehole and the second fiber optic cable is disposed at a second location within the transverse cross-section of the borehole that is spaced apart from the first location, and

wherein the data acquisition system detects a phase difference between seismic signals incident on the first and second fiber optic cables at each of a plurality of locations along a length of the borehole to determine characteristics of the formation.

3. The system as recited in claim 1, further comprising:

a second fiber optic cable disposed in a second borehole, the second fiber optic cable configured to react along its length to incident seismic signals originating inside the second borehole and propagating through the formation and the borehole;

a second optical source to launch optical pulses into the second fiber optic cable while the seismic signals are incident on the second fiber optic cable; and

a data acquisition system coupled to the second fiber optic cable to detect CRN generated in response to the optical pulses,

wherein the CRN generated by the first fiber optic cable is correlated with the CRN generated by the second fiber optic cable to determine characteristics of the formation.

4. The system as recited in claim 1, wherein a hypocenter of a microseismic event is determined based on the detected CRN.

5. The system as recited in claim 1, wherein the first fiber optic cable comprises a plurality of discrete optical sensors.

6. The system as recited in claim 5, wherein the discrete optical sensors comprise fiber Bragg gratings spaced apart along the length of the first fiber optic cable.

7. The system as recited in claim 2, wherein the first fiber optic cable generates a first CRN response to pressure, velocity, acceleration and/or strain and the second fiber optic cable generates a second CRN response to the same pressure, velocity, acceleration and/or strain, and wherein the data acquisition system determines characteristics of the formation based on a difference between the first CRN response and the second CRN response.

8. The system as recited in claim 2, wherein the first and second fiber optic cables are installed in a first control line.

9. The system as recited in claim 1, wherein the first fiber optic cable comprises a pressure-sensitive material disposed along its length.

10. A method of detecting seismic signals, comprising:

deploying a first fiber optic cable in a first borehole extending from a surface into an earth formation, the first fiber optic cable configured to react along its length to incident seismic signals;

deploying a second fiber optic cable in a second borehole extending from the surface into the earth formation, the second fiber optic cable configured to react along its length to incident seismic signals;

launching optical pulses into the first and second fiber optic cables during occurrence of a seismic event in either the first or second borehole; and

detecting backscattered optical signals generated by the first and second fiber optic cables in response to the optical pulses to determine characteristics of the seismic event wherein the detecting backscattered optical signals comprises detecting coherent Rayleigh noise (CRN).

11. The method as recited in claim 10, wherein the second fiber optic cable is deployed in the same borehole as the first fiber optic, the second fiber optic cable being disposed at a location within the transverse cross-section of the same borehole that is spaced apart from a location of the first fiber optic cable.

12. The method as recited in claim 11, wherein detecting the backscattered optical signals comprises detecting a phase difference between seismic signals incident on the first and second fiber optic cables.

13. A method for conducting a seismic survey of an earth formation, comprising:

launching a first optical signal into a first fiber optic cable disposed in a borehole extending from an earth surface into the earth formation;

generating a seismic wave that propagates through the earth formation and the borehole from inside of the borehole; and

analyzing coherent Rayleigh noise (CRN) produced in response to the first optical signal while the seismic wave is incident along a length of the first fiber optic cable to determine characteristics of the earth formation.

14. The method as recited in claim 13, further comprising:

launching a second optical signal into a second fiber optic cable disposed in a borehole; and

analyzing CRN produced in response to the second optical signal while the seismic wave is incident along the length of the second fiber optic cable,

wherein characteristics of the earth formation are determined based on the CRN produced in response to the first optical signal and the CRN produced in response to the second optical signal.

15. The method as recited in claim 14, wherein the first fiber optic cable and the second fiber optic cable have a substantially identical construction and are disposed at different locations within a transverse cross-section of the same borehole, and wherein characteristics of the earth formation are determined based on a phase difference in the seismic wave incident on the first and second fiber optic cables at each of a plurality of locations along a length of the same borehole.

16. The method as recited in claim 14, wherein the first fiber optic cable is configured to react differently to pressure, velocity, acceleration and/or strain than the second fiber optic cable reacts to pressure, velocity, acceleration and/or strain.

17. A system comprising:

a first optical fiber disposed in a borehole that extends from an earth surface into an earth formation, the first optical fiber configured to react to a seismic wave incident on the first optical fiber at any of a plurality of locations along its length;

a seismic source to generate a seismic wave that originates inside the borehole;

an optical source to launch an optical signal into the first optical fiber to produce a backscattered optical signal while the seismic wave is incident on the first optical fiber;

a receiver to detect coherent Rayleigh noise (CRN) in the backscattered signal; and

a processing circuit to process the CRN to determine characteristics of the earth formation.

18. The system as recited in claim 17, further comprising a second optical fiber disposed in a borehole extending from the earth surface into the earth formation and configured to produce a second CRN signal while the seismic wave is incident at any of a plurality of locations along a length of the second optical fiber, and wherein the processing circuit further processes the second CRN signal to determine characteristics of the earth formation.

19. The system as recited in claim 18, wherein the first optical fiber and the second optical fiber are disposed in the same borehole.

20. The system as recited in claim 19, wherein the first optical fiber and the second optical fiber have a substantially identical construction and are disposed at different locations within a transverse cross-section of the same borehole, and wherein characteristics of the earth formation are determined based on a phase difference in the seismic wave incident on the first and second fiber optic cables at each of a plurality of locations along a length of the borehole.

21. The system as recited in claim 19, wherein the first optical fiber is configured to react differently to pressure, velocity, acceleration and/or strain than the second optical fiber reacts to pressure, velocity, acceleration and/or strain, and wherein characteristics of the earth formation are determined based on a difference in the reactions.

22. The system as recited in claim 17, wherein the seismic source is located in a second borehole that extends from the earth surface into the earth formation, wherein the second borehole is different than the borehole in which the first optical fiber is disposed.