Magneto-hydrodynamic seismic source and a method of marine seismic surveying

• US 10,001,572 B2
• Filed: 10/02/2015
• Issued: 06/19/2018
• Est. Priority Date: 04/05/2013
• Status: Active Grant

• Current Assignee: Woodside Energy Technologies Pty Ltd.
• Original Assignee: Woodside Energy Technologies Pty Ltd.
• Inventors: Lockwood, Andrew Maxwell
• Primary Examiner(s): Baghdasaryan, Hovhannes
• Application Number:
  US14/873,286
• Publication Number:
  US 20160077227A1
• Time in Patent Office: 991 Days
• CPC Class Codes: G01V 1/02 Generating seismic energy G01V1/003 takes precedence
• CPC Class Codes: G01V 1/04 Details
• CPC Class Codes: G01V 1/133 using fluidic driving means, e.g. highly pressurised fluids; using implosionG01V1/104 takes precedence
• CPC Class Codes: G01V 1/137 which fluid escapes from the generator in a pulsating manner, e.g. for generating bursts , airguns
• CPC Class Codes: G01V 1/38 specially adapted for water-covered areas G01V1/28 takes precedence
• CPC Class Codes: G01V 1/3808 Seismic data acquisition, e.g. survey design
• CPC Class Codes: G01V 1/3852 to the seabed

Abstract

A magneto-hydrodynamic seismic source includes a casing having a central longitudinal axis; a fluid flow channel, and a plurality of electromagnets arranged along the channel for generating a uniform magnetic field at right angles to the central longitudinal axis of the channel, a first electrode positioned on a first side of the fluid flow channel, the first electrode being positioned opposite a second electrode that is positioned on a second opposing side of the fluid flow channel, and a controllable power source in electrical communication with the first electrode and the second electrode for generating a continuously varying electric field between the first electrode and second electrodes to generate a continuously varying inflow of seawater into the first end of the fluid flow channel with a corresponding continuously varying outflow of seawater in the form of a seismic signal being produced from the second end of the fluid flow channel.

Claims

1. A magneto-hydrodynamic seismic source comprising:

a casing having a central longitudinal axis;

a fluid flow channel having a first end and a second end and a longitudinal axis extending from the first end of the fluid flow channel to the second end of the fluid flow channel;

a plurality of electromagnets arranged along the channel for generating a uniform magnetic field at right angles to the central longitudinal axis of the channel;

a first electrode positioned on a first side of the fluid flow channel, the first electrode being positioned opposite a second electrode that is positioned on a second opposing side of the fluid flow channel; and

a controllable power source in electrical communication with the first electrode and the second electrode for generating a continuously varying electric field between the first electrode and second electrodes to generate a continuously varying inflow of seawater into the first end of the fluid flow channel with a corresponding continuously varying outflow of seawater in the form of a seismic signal being produced from the second end of the fluid flow channel;

wherein each of the electromagnets has a polarity and the polarities of the plurality of electromagnets arranged along the casing are paired and opposed such that a first inflow of seawater enters at the first end of the fluid flow channel, a second inflow of water enters at the second end of the fluid flow channel, the fluid flow channel includes a discharge port for producing an outflow of seawater in the form of a seismic signal, and the discharge port is positioned a discharge location intermediate between the first end of the fluid flow channel and the second end of the fluid flow channel.

2. The magneto-hydrodynamic seismic source of claim 1 wherein the seismic signal has a frequency less than 5 Hz.

3. The magneto-hydrodynamic seismic source of claim 1 wherein the plurality of electromagnets includes a first electromagnet arranged along a first side of the channel and a second paired electromagnet arranged on a second opposing side of the channel, and each of the plurality of electromagnets is a saddle-type electromagnet.

4. The magneto-hydrodynamic seismic source of claim 1 wherein each of the plurality of electromagnets is a superconducting electromagnet.

5. The magneto-hydrodynamic seismic source of claim 1 wherein the discharge location is centrally located between the first end of the fluid flow channel and second end of the fluid flow channel.

6. The magneto-hydrodynamic seismic source of claim 1 wherein the discharge port takes the form of a plurality of spaced apart apertures such that the outflow of seawater is directed radially outwardly from the fluid flow channel.

7. The magneto-hydrodynamic seismic source of claim 1 wherein the casing has a central longitudinal axis and the longitudinal axis of the fluid flow channel is parallel to or coaxial with the central longitudinal axis of the casing.

8. The magneto-hydrodynamic seismic source of claim 1 wherein the seismic signal has a broadband waveform.

9. The magneto-hydrodynamic seismic source of claim 1 wherein the seismic signal has a variable waveform.

10. The magneto-hydrodynamic seismic source of claim 1 wherein the seismic signal has a waveform in the form of a spike, a narrow band signal, a coded wave form, or a monochromatic waveform.

11. The magneto-hydrodynamic seismic source of claim 1 wherein the magneto-hydrodynamic seismic source is one of a plurality of seismic sources arranged in an array.

12. The magneto-hydrodynamic seismic source of claim 11 wherein the array is a phased array.

13. The magneto-hydrodynamic seismic source of claim 11 wherein at least one of the seismic sources in the array is a magneto-hydrodynamic seismic source and at least one of the seismic sources in the array is an impulsive source.

14. The magneto-hydrodynamic seismic source of claim 11 wherein at least one of the seismic sources in the array is a magneto-hydrodynamic seismic source and at least one of the seismic sources in the array is a marine vibration seismic source.

15. The magneto-hydrodynamic seismic source of claim 1 wherein the fluid flow channel is one of a plurality of fluid flow channels, each fluid flow channel having a first end and a second end and a set of first and second electrodes.

16. The magneto-hydrodynamic seismic source of claim 15 wherein the casing has a central longitudinal axis and the longitudinal axis of each fluid flow channel is parallel to and radially offset from a central longitudinal axis of the casing so that the plurality of flow fluid channels is evenly spaced around the circumference of the casing.

17. The magneto-hydrodynamic seismic source of claim 1 wherein the plurality of electromagnets is provided in the form of a plurality of electromagnet segments.

18. The magneto-hydrodynamic seismic source of claim 17 wherein there is a corresponding number of the plurality of fluid flow channels and the plurality of electromagnet segments.

19. The magneto-hydrodynamic seismic source of claim 1 wherein the plurality of electromagnet segments is a plurality of toroidal or solenoidal magnet segments, arranged around the circumference of the casing.

20. The magneto-hydrodynamic seismic source of claim 1 wherein the casing is cylindrical and has a circumference, and, the plurality of fluid flow channels is arranged at radially evenly spaced intervals around the outside of the circumference of the casing.

21. The magneto-hydrodynamic seismic source of claim 15 wherein the plurality of fluid flow channels comprises a first subset of fluid flow channels and second subset of flow fluid channels and the power source is configured so that the direction of the inflow into the first subset of fluid flow channels is reversed relative to the direction of the inflow of seawater into the second subset of fluid flow channels.

22. The magneto-hydrodynamic seismic source of claim 15 wherein the electrical field being generated across each set of first and second electrodes is tuned to adjust the inflow and outflow of seawater through each of the plurality of channels to counteract an overall drag force experienced by the magneto-hydrodynamic source when towed behind a marine vessel in use.

23. The magneto-hydrodynamic seismic source of claim 15 wherein the electrical field being generated across each set of first and second electrodes is tuned to adjust the inflow and outflow of seawater through each of the plurality of channels so that the magneto-hydrodynamic source can be self-propelling.

24. The magneto-hydrodynamic seismic source of claim 1 wherein the power source is one of a plurality of power sources.

25. A method of acquiring marine seismic data comprising:

actuating a magneto-hydrodynamic seismic source to generate a seismic signal, a portion of said seismic signal being reflected at an interface associated with a subsea geological feature in the form of a reflected seismic signal; and

collecting the reflected seismic signal with a seismic signal receiver to generate a set of survey data,

wherein the magneto-hydrodynamic seismic source comprises;

a casing having a central longitudinal axis;

a fluid flow channel having a first end and a second end and a longitudinal axis extending from the first end of the fluid flow channel to the second end of the fluid flow channel;

a plurality of electromagnets arranged along the channel for generating a uniform magnetic field at right angles to the central longitudinal axis of the channel;

a first electrode positioned on a first side of the fluid flow channel, the first electrode being positioned opposite a second electrode that is positioned on a second opposing side of the fluid flow channel; and

a controllable power source in electrical communication with the first electrode and the second electrode for generating a continuously varying electric field between the first electrode and second electrodes to generate a continuously varying inflow of seawater into the first end of the fluid flow channel with a corresponding continuously varying outflow of seawater in the form of a seismic signal being produced from the second end of the fluid flow channel;

wherein each electromagnet has a polarity and the polarities of the plurality of electromagnets arranged along the casing are paired and opposed such that a first inflow of seawater enters at the first end of the fluid flow channel, a second inflow of water enters at the second end of the fluid flow channel, the fluid flow channel includes a discharge port for producing an outflow of seawater in the form of a seismic signal, and the discharge port is positioned a discharge location intermediate between the first end of the fluid flow channel and the second end of the fluid flow channel.

26. The method of claim 25 wherein the seismic signal has a frequency less than 5 Hz.

27. The method of claim 25 wherein the plurality of electromagnets includes a first electromagnet arranged along a first side of the channel and a second paired electromagnet arranged on a second opposing side of the channel, and each of the plurality of electromagnets is a saddle-type electromagnet.

28. The method of claim 25 wherein each of the plurality of electromagnets is a superconducting electromagnet.

29. The method of claim 25 wherein the discharge location is centrally located between the first end of the fluid flow channel and second end of the fluid flow channel.

30. The method of claim 25 wherein the discharge port takes the form of a plurality of spaced apart apertures such that the outflow of seawater is directed radially outwardly from the fluid flow channel.

31. The method of claim 25 wherein the casing has a central longitudinal axis and the longitudinal axis of the fluid flow channel is parallel to or coaxial with the central longitudinal axis of the casing.

32. The method of claim 25 wherein the seismic signal has a broadband waveform.

33. The method of claim 25 wherein the seismic signal has a variable waveform.

34. The method of claim 25 wherein the seismic signal has a waveform in the form of a spike, a narrow band signal, a coded wave form, or a monochromatic waveform.

35. The method of claim 25 wherein the magneto-hydrodynamic seismic source is one of a plurality of seismic sources arranged in an array.

36. The method of claim 35 wherein the array is a phased array.

37. The method of claim 35 wherein at least one of the seismic sources in the array is a magneto-hydrodynamic seismic source and at least one of the seismic sources in the array is an impulsive source.

38. The method of claim 35 wherein at least one of the seismic sources in the array is a magneto-hydrodynamic seismic source and at least one of the seismic sources in the array is a marine vibration seismic source.

39. The method of claim 25 wherein the fluid flow channel is one of a plurality of fluid flow channels, each fluid flow channel having a first end and a second end and a set of first and second electrodes.

40. The method of claim 39 wherein the casing has a central longitudinal axis and the longitudinal axis of each fluid flow channel is parallel to and radially offset from a central longitudinal axis of the casing so that the plurality of flow fluid channels is evenly spaced around the circumference of the casing.

41. The method of claim 25 wherein the plurality of electromagnets is provided in the form of a plurality of electromagnet segments.

42. The method of claim 41 wherein there is a corresponding number of the plurality of fluid flow channels and the plurality of electromagnet segments.

43. The method of claim 41 wherein the plurality of electromagnet segments is a plurality of toroidal or solenoidal magnet segments, arranged around the circumference of the casing.

44. The method of claim 39 wherein the casing is cylindrical and has a circumference, and, the plurality of fluid flow channels is arranged at radially evenly spaced intervals around the outside of the circumference of the casing.

45. The method of claim 39 wherein the plurality of fluid flow channels comprises a first subset of fluid flow channels and second subset of flow fluid channels and the power source is configured so that the direction of the inflow into the first subset of fluid flow channels is reversed relative to the direction of the inflow of seawater into the second subset of fluid flow channels.

46. The method of claim 39 the electrical field being generated across each set of first and second electrodes is tuned to adjust the inflow and outflow of seawater through each of the plurality of channels to counteract an overall drag force experienced by the magneto-hydrodynamic source when towed behind a marine vessel in use.

47. The method of claim 39 wherein the electrical field being generated across each set of first and second electrodes is tuned to adjust the inflow and outflow of seawater through each of the plurality of channels so that the magneto-hydrodynamic source can be self-propelling.

48. The method of claim 25 wherein the power source is one of a plurality of power sources.