Method and system for determining the depth of an electrically conductive body in a medium having a known conductivity and a known permeability by measuring phase difference between a primary and secondary magnetic field

• US 5,119,028 A
• Filed: 04/26/1990
• Issued: 06/02/1992
• Est. Priority Date: 04/26/1990
• Status: Expired due to Fees

• Current Assignee: Grumman Aerospace Corporation (Northrop Grumman Corporation)
• Original Assignee: Grumman Aerospace Corporation (Northrop Grumman Corporation)
• Inventors: Mooney, John J., Witt, Christopher J., Mohr, Michael T.
• Primary Examiner(s): Strecker, Gerard R.
• Application Number:
  US07/514,618
• Time in Patent Office: 768 Days
• Field of Search: 324/326, 324/329, 324/330, 324/334, 324/335, 324/233, 324/207.17, 324/207.26, 342/459
• US Class Current: 324/326
• CPC Class Codes: G01V 3/165 operating with magnetic or electric fields produced or modified by the object or by the detecting device with electromagnetic waves G01V3/17

Abstract

A method and system for determining the depth of an electrically conductive body in a medium having a known conductivity and a known permeability. The method comprises the steps of generating a primary magnetic field having a time-varying field strength, and transmitting that primary magnetic field into the medium. The primary magnetic field induces an electric current in the conductive body, and this electric current generates a secondary magnetic field that also has a time-varying field strength and that propagates outward from the conductive body and through the medium. The method of this invention further includes the steps of sensing the strength of that secondary magnetic field, comparing the primary and secondary magnetic fields to measure the phase difference therebetween, and then calculating the depth of the conductive body in the medium from the detected phase difference.

Claims

1. A method of determining the depth of an electrically conductive body in a medium having a known conductivity and a known permeability, comprising the steps of:

generating a primary magnetic field from an electromagnetic wave transmitting means located a distance apart from said conductive body, said primary magnetic field having a time-varying field strength;

generating a first signal representing the time-varying field strength of said primary magnetic field;

transmitting the primary magnetic field from said transmitting means into the medium, wherein the primary magnetic field induces an electric current in the conductive body, and the electric current generates a secondary magnetic field having a time-varying field strength and propagating outward from the conductive body and through the medium;

sensing the strength of the secondary magnetic field by a receiving means, said receiving means generating a second signal representing the time-varying field strength of said secondary magnetic field;

conducting said first and second signals to a comparator means;

the comparator means,

processing said first and second signals to obtain a third signal having a value indicating the magnitude of a phase difference between said primary and secondary magnetic fields caused by the primary magnetic field propagating through the medium to the conductive body, and by the secondary magnetic field propagating outward from the conductive body and through the medium; and

transmitting the third signal to a processor means, the processor means

calculating the depth of the conductive body in the medium from the third signal and the conductivity and permeability of the medium.

2. A method according to claim 1, wherein the medium has a conductivity of less than 10⁴ siemens/m.

3. A method according to claim 2, wherein the medium is water.

4. A method according to claim 1, wherein:

the field strength of the primary magnetic field varies at a given frequency;

the field strength of the secondary magnetic field also varies at the given frequency; and

the given frequency is less than about 10⁶ Hz.

5. A method according to claim 4, wherein:

the given frequency is less than 10 Hz;

the conductivity of the medium at said given frequency is approximately 4 siemens/meter;

the permeability of the medium at said given frequency is approximately 4π

×

10^-7 Telsa-m/amp.

6. A method according to claim 5, wherein the conductive body has a magnetic moment in a known range.

7. A method according to claim 1

further comprising the step of locating the transmitting means and the receiving means on a common platform supported for movement over the medium.

8. A method according to claim 7, further comprising the steps of:

maintaining the platform at a fixed height above the medium; and

locating the platform at a position where the sensed strength of the secondary magnetic field is a maximum.

9. A method according to claim 1 further comprising the steps of

i) locating the transmitting means on a first platform supported for movement over the medium, and

ii) locating the receiving means on a second platform supported for movement over the medium.

10. A method according to claim 9, wherein each of the first and second platforms are supported for movement independent of the other platform over the medium.

11. A method according to claim 9, further comprising the steps of:

maintaining both the first and second platforms at a common, fixed height above the medium; and

moving the first and second platforms to positions where the sensed strength of the secondary magnetic field is a maximum to help identify the location of the conductive body.

27. A method according to claim 1, wherein said processor means includes a look-up table of depth values that correspond to a respective value of said third signal, and wherein said calculating step includes the step of looking for the value of said third signal in said table and obtaining therefrom its corresponding depth value.

28. A method according to claim 1, wherein the calculating step includes the step of solving an equation to determine a depth value from the third signal and the conductivity and permeability of the medium.

12. A method of determining the depth of an electrically conductive body in a medium having a known conductivity and a known permeability, comprising the steps of:

generating in a second medium a primary magnetic field from an electromagnetic wave transmitting means located a distance apart from said first medium, said primary magnetic field having a time-varying field strength;

generating a first signal representing the time-varying field strength of said primary magnetic field;

transmitting the primary magnetic field from said transmitting means into the first medium, wherein the primary magnetic field induces an electric current in the conductive body, and the electric current generates a secondary magnetic field having a time-varying field strength and propagating outward from the conductive body, through the first medium and into the second medium;

sensing the strength of the secondary magnetic field by a receiving means located in the second medium, said receiving means generating a second signal representing the time-varying field strength of said secondary magnetic field;

conducting said first and second electric signals to a comparator means;

the comparator means,

processing said first and second electrical signals to obtain a third signal having a value indicating the magnitude of a phase difference between said primary and secondary magnetic fields that is caused by the first medium as (i) the primary magnetic field is transmitted therethrough to the conductive body, and (ii) the secondary magnetic field propagates outward from the conductive body and through the first medium; and

transmitting the third signal to a processor means, the processor means

calculating the depth of the conductive body in the first medium from the third signal and the conductivity and permeability of the medium.

13. A method according to claim 12, wherein the first medium has a conductivity of less than 10⁴ siemens/m.

14. A method according to claim 13, wherein the second medium is air.

15. A method according to claim 13, wherein the first medium is water.

16. A method according to claim 13, wherein the field strengths of both the primary and secondary fields vary at a frequency less than about 10⁶ Hz.

17. A method according to claim 12, wherein:

the processor means includes a table having

i) values for the third signal, and

ii) associated depth values for the conductive body; and

the calculating step includes the step of obtaining a depth value for the conductive body from the table.

18. A method according to claim 12, wherein the calculating step includes the step of solving an equation to determine the depth of the conductive body in the medium from the third signal and the conductivity and permeability of the medium.

19. Apparatus for determining the depth of an electrically conductive body in a medium having a known conductivity and a known permeability, comprising:

transmitting means located a distance apart from said conductive body to generate a primary magnetic field having a time-varying field strength, and to transmit the magnetic field into the medium, wherein the magnetic field induces an electric current in the conductive body, and the electric current generates a secondary magnetic field having a time-varying field strength and propagating outward from the conductive body and through the medium, said transmitting means further including a means for generating a first signal representing the time-varying field strength of said primary magnetic field;

receiving means to sense the secondary magnetic field and to generate a second signal proportional to the strength thereof;

phase shift detecting means connected to the receiving means to receive said second signal therefrom, and further adapted to receive said first signal from said transmitting means, wherein said phase shift detecting means further includes comparator means for processing said first and second signals and to generate therefrom a third signal having a value indicating the magnitude of a phase difference between said primary and secondary magnetic fields caused by the medium as the primary magnetic filed is transmitted through the medium to the conductive body, and as the secondary magnetic field propagates outward from the conductive body and through the medium; and

depth determining means connected to the phase shift detecting means to receive said third signal therefrom and to calculate the depth of the conductive body from the third signal and the conductivity and permeability of the medium.

20. Apparatus according to claim 19, wherein the transmitting means includes means to generate the primary magnetic moment with a maximum strength of about 31 Tesla-m³, and to vary the primary magnetic field strength at a frequency of about 1 Hz.

21. Apparatus according to claim 20, wherein the receiving means includes means to sense the secondary magnetic field having a strength of about 10^-6 nanoTesla, and where the field strength of the secondary magnetic field varies at a frequency of about 1 Hz.

22. Apparatus according to claim 20, wherein the receiving means includes means to sense the secondary magnetic field having a strength of about 10^-4 nanoTesla, and where the field strength of the secondary magnetic field varies at a frequency of about 1 Hz.

23. Apparatus according to claim 19, wherein said depth determining means includes:

a look-up table of depth values that correspond to a respective value of said third signal; and

means for looking up the value of said third signal in said table and obtaining therefrom its corresponding depth value.

29. Apparatus according to claim 19, wherein the transmitting means varies the field strength of the primary magnetic field at a frequency less than 10 Hz.

24. A method of determining the depth of an electrically conductive body in a medium having a known conductivity and a known permeability, comprising the steps of:

generating a primary magnetic field from a transmitting means located a distance apart from said conductive body, said primary magnetic field having a time-varying field strength;

generating a first signal representing the time-varying field strength of said primary magnetic field;

transmitting the primary magnetic field from said transmitting means into the medium, wherein the primary magnetic field induces an electric current in the conductive body, and the electric current generates a target secondary magnetic field having a time-varying field strength and propagating outward from the conductive body and through the medium;

sensing the strength of the secondary magnetic field by a receiving means and generating therefrom a second signal representing the time-varying field strength of said secondary magnetic field;

conducting said first and second electrical signals to a comparator means;

the comparator means,

processing said first and second signals to obtain a third signal having a value indicating the magnitude of a phase shifted target returns in the primary and secondary magnetic fields that is caused by the medium as (i) the primary magnetic field is transmitted through the medium to the conductive body, and (ii) the secondary magnetic field propagates outward from the conductive body and through the medium;

transmitting the third signal to a processor means, the processor means

calculating the depth of the conductive body in the first medium from the third signal and the conductivity and permeability of the medium.

25. A method according to claim 24, wherein the medium is water and has a conductivity of less than 10⁴ siemens/m.

26. A method according to claim 25, wherein the field strengths of both the primary and secondary fields vary at a frequency less than about 10⁶ Hz.