SYSTEMS, DEVICES AND METHODS FOR BOREHOLE GRAVIMETRY

• US 20140083186A1
• Filed: 08/13/2013
• Published: 03/27/2014
• Est. Priority Date: 09/24/2012
• Status: Active Grant

• Current Assignee: Schlumberger Technology Corporation (Schlumberger NV)
• Original Assignee: Schlumberger Technology Corporation (Schlumberger NV)
• Inventors: LEVITT, BENJAMIN, POITZSCH, MARTIN E., ROSCOE, BRADLEY ALBERT
• Granted Patent: US 9,939,551 B2
• Time in Patent Office: Days
• US Class Current: 73/382.R
• CPC Class Codes: E21B 47/00 Survey of boreholes or wells monitoring pressure or flow of drilling fluid E21B21/08
• CPC Class Codes: G01D 5/30 the beams of light being detected by photocells
• CPC Class Codes: G01H 9/00 Measuring mechanical vibrations or ultrasonic, sonic or infrasonic waves by using radiation-sensitive means, e.g. optical means
• CPC Class Codes: G01V 7/00 Measuring gravitational fields or waves; Gravimetric prospecting or detecting
• CPC Class Codes: G01V 7/04 Electric, photoelectric, or magnetic indicating or recording means

Abstract

A gravimeter, a gravimeter system, and a method for measuring gravitational acceleration within a borehole are described herein. The gravimeter includes a proof mass that is constrained by springs and an optical interferometer for measuring displacement of the proof mass. The optical interferometer generates a light path from a light source to a reflective surface on the proof mass. Spatial displacement of the proof mass from a reference position to a position of gravitational equilibrium is determined by measuring a change in length of the light path. In turn, gravitational acceleration can be determined from the spatial displacement of the proof mass. A number of such gravimeters can be used in a gravimeter system to make measurements of gravitational acceleration in variety of different directions.

Claims

1. A method for measuring gravitational acceleration, the method comprising:

locating a gravimeter within a borehole, wherein the gravimeter includes a proof mass that is constrained by at least one spring;

generating a light path from a light source to a reflective surface on the proof mass; and

determining spatial displacement of the proof mass from a reference position to a position of gravitational equilibrium by measuring a change in length of the light path.

2. The method according to claim 1, further comprising:

determining gravitational acceleration based upon the spatial displacement.

3. The method according to claim 2, wherein the reference position is a position of gravitational equilibrium at a surface location.

4. The method according to claim 2, wherein measuring the change in length of the light path includes determining a number of interference fringes between the reference position and the position of gravitational equilibrium using an optical interferometer.

5. The method according to claim 2, wherein the reference position is a position of the proof mass at a limit of spatial displacement.

6. The method of claim 1, further comprising:

moving the proof mass to a first position, wherein the first position is displaced from a position of gravitational equilibrium of the proof mass;

moving the proof mass to a second position, wherein the second position is displaced from the position of gravitational equilibrium of the proof mass;

determining spatial displacement of the proof mass from the first position to the second position.

7. The method of claim 6, wherein the proof mass has a first limit of spatial displacement and a second limit of spatial displacement.

8. The method of claim 7, wherein the first position is at the first limit and the second position is at the second limit.

9. The method of claim 1, further comprising:

releasing the proof mass so that the proof mass moves from a reference position to a position of gravitational equilibrium.

10. A gravimeter comprising:

a proof mass that is constrained by at least one spring and that is displaceable in response to gravitational acceleration;

an optical interferometer for measuring displacement of the proof mass, wherein the optical interferometer comprises a light source and is configured to generate a light path from the light source to a reflective surface on the proof mass; and

a processor in electronic communication with the optical interferometer, wherein the processor is configured to determine spatial displacement of the proof mass from a reference position to a position of gravitational equilibrium by measuring a change in length of the light path.

11. The gravimeter according to claim 10, wherein the processor is further configured to determine gravitational acceleration based upon the spatial displacement.

12. The gravimeter according to claim 10, wherein the optical interferometer further comprises:

a light detector for detecting the light path.

13. The gravimeter according to claim 12, wherein the optical interferometer further comprises:

a light modulator configured to split the light path into two or more light components.

14. The gravimeter according to claim 13, wherein the light modulator is a beam splitter.

15. The gravimeter according to claim 13, wherein the light modulator is an optical grating.

16. A borehole tool comprising:

a first set of gravimeters, wherein the first set includes a plurality of gravimeters oriented to detect gravitational acceleration in at least two different directions;

a second set of gravimeters, wherein the second set includes a plurality of gravimeters oriented to detect gravitational acceleration in at least two different directions; and

wherein the first set of gravimeters and the second set of gravimeters are spaced apart from each other by a known distance.

17. The tool according to claim 16, wherein the first set of gravimeters includes at least three gravimeters oriented to detect gravitational acceleration in at least three different directions and the second set of gravimeters includes at least three gravimeters oriented to detect gravitational acceleration in at least three different directions.

18. The tool according to claim 17, wherein the at least three different directions are orthogonal directions.

19. The tool according to claim 16, further comprising:

a processor configured to determine a density at a location using a first gravitational acceleration measurement at the first set of gravimeters and a second gravitational acceleration measurement at the second set of gravimeters.

20. The tool according to claim 19, wherein the processor is configured to determine the density at the location within the formation using the known distance between the first set of gravimeters and the second set of gravimeters.

21. The tool according to claim 16, wherein the tool comprises greater than two sets of gravimeters.

22. The tools according to claim 16, wherein the tool includes a longitudinal axis and the first set of gravimeters and the second set of gravimeters are aligned with the longitudinal axis.

23. A method for determining a characteristic of a formation, the method comprising:

using a first set of gravimeters to perform a first set of measurements that includes gravitational acceleration in at least two different directions at a first position within a borehole;

using a second set of gravimeters to perform a second set of measurements that includes gravitational acceleration in at least two different directions at a second position within the borehole, wherein the first position and second position are spaced apart from each other by a known distance; and

determining a first density at a location within the formation using the first set of measurements and the second set of measurements.

24. The method according to claim 23, wherein the density is determined using the known distance between the first location and the second location.

25. The method according to claim 23, wherein the first set of measurements includes gravitational acceleration in at least three different directions at the first position within the borehole and the second set of measurements includes at least three different directions at the second position within the borehole.

26. The method according to claim 25, wherein the at least three different directions are orthogonal directions.

27. The method according to claim 23, further comprising:

using the first set of gravimeters and the second set of gravimeters to determine a second density at the location within the formation, wherein the first density and the second density are measures of density at different times within the location.

28. The method according to claim 27, further comprising:

comparing the first density to the second density to determine a density change within the location over time.

29. The method according to claim 28, further comprising:

using the density change within the location over time to monitor a flood front.