System and method for locating an underground probe having orthogonally oriented magnetometers

• US 4,875,014 A
• Filed: 07/20/1988
• Issued: 10/17/1989
• Est. Priority Date: 07/20/1988
• Status: Expired due to Term

• Current Assignee: Reuter-Stokes, Inc. (General Electric Company)
• Original Assignee: Tensor, Inc. (GE Aerospace)
• Inventors: Roberts, George F., Walters, Philip H.
• Primary Examiner(s): STRECKER, GERARD R
• Application Number:
  US07/221,730
• Time in Patent Office: 454 Days
• Field of Search: 324/207, 324/208, 324/67, 324/326, 324/345, 324/346, 73/151, 340/551, 340/989, 175/26, 175/45, 175/61, 33/304, 33/312, 33/313, 364/424.02, 364/449, 342/459
• US Class Current: 324/326
• CPC Class Codes: E21B 47/0232 at least one of the energy sources or one of the detectors being located on or above the ground surface
• CPC Class Codes: E21B 47/024 of devices in the borehole determining slope or direction of the borehole E21B47/022
• CPC Class Codes: E21B 47/13 by electromagnetic energy, e.g. radio frequency
• CPC Class Codes: G01V 3/08 operating with magnetic or electric fields produced or modified by objects or geological structures or by detecting devices with electromagnetic waves G01V3/12

Abstract

A method and system for tracking a borehole by means of a probe and an externally produced magnetic field. The magnetic field is produced by a current configuration which facilitates the calculation of the magnitude and direction of the magnetic field at any point in space. In order to locate the probe, magnetometers within the probe are used to measure the magnetic field. Accelerometers within the probe allow the determination of the probe'"'"'s orientation which enables the measured field vector to be compared to the calculated field vector and the probe'"'"'s location thereby ascertained.

Claims

1. A method for tracking the progress of a borehole made by a drilling assembly, comprising the steps of:

generating a magnetic field by flowing a constant current through a conductive loop made up of straight segments placed on the surface of the ground above the proposed path of the borehole;

measuring the magnetic field by means of a probe fixed to the drilling assembly with three orthogonally oriented magnetometers;

iteratively calculating the theoretical magnetic field vector produced by the current flowing through the conductive loop at discrete points below the conductive loop until the calculated field vector is approximately equal to the measured magnetic field vector;

determining the location of the probe as being that point below the ground surface where the measured magnetic field vector most nearly matches the theoretically calculated magnetic field vector.

2. The method as set forth in claim 1 comprising the additional steps of:

measuring the inclination and roll angles of the probe with respect to a normal coordinate system by means of three orthogonally oriented accelerometers;

mapping the measured magnetic field vector from a probe coordinate system to the normal coordinate system before comparing the measured and calculated magnetic field vectors.

3. The method as set forth in claim 1 wherein the measured magnetic field vector is that resulting from the vectorial subtration of the field vector measured when current is made to flow through the loop in one direction from the field vector measured when an equal amount of current is made to flow through the loop in the opposite direction.

4. A system for tracking the progress of a borehole made by a drilling assembly, comprising:

a conductive loop made up of straight segments to be placed on the surface of the ground above the proposed path of the borehole;

means for applying constant current to the loop;

a probe fixed to the drilling assembly having three orthogonally oriented magnetometers for measuring the magnetic field vector at the probe'"'"'s location and three orthogonally oriented accelerometers for determining the orientation of the magnetometers; and

means for iteratively calculating the magnetic field vector existing at discrete points below the conductive loop produced by the constant current flowing through the conductive loop until an approximate match between the measured and calculated magnetic field vectors is found.

5. A method for locating the position of an underground probe having three orthogonally oriented magnetometers and three orthogonally oriented accelerometers mounted within with respect to a normal coordinate system, comprising the steps of:

generating a magnetic field by flowing a constant current through a conductive loop made up of straight segments located on the surface of the ground above the probe;

measuring the resulting magnetic field vector with respect to a probe coordinate system at the location of the probe by means of three orthogonally oriented magnetometers;

measuring the inclination and roll angles of the probe with respect to the normal coordinate system by means of three orthogonally oriented accelerometers;

mapping the measured magnetic field vector from the probe coordinate system to the normal coordinate system by performing a rotation of axes transformation according to the measured inclination and roll angles;

calculating the theoretical magnetic field vector produced by the same constant current flowing through the conductive loop for discrete points below the conductive loop in the normal coordinate system until an approximate match between the measured and calculated field vectors is found; and

determining the location of the probe as that point in the normal coordinate system where the calculated theoretical magnetic field vector most nearly matches the measured magnetic field vector mapped to the normal coordinate system.

6. The method as set forth in claim 5 wherein the measured magnetic field vector is that resulting from applying current to the conductive loop in one direction to generate a first magnetic field vector at the probe, applying current to the conductive loop in the opposite direction to generate a second magnetic field vector at the probe, and vectorially subtracting the second field vector from the first field vector, and further wherein the current value used to calculate the theoretical magnetic field vectors is the sum of the current magnitudes used to generate the first and second magnetic field vectors.

7. The method as set forth in claim 5 wherein the calculated theoretical magnetic field vector at each point is the vector summation of the magnetic field vector of point P resulting from each corner at point N of the conductive loop according to the formula:

##EQU21## where H is the magnetic field vector, R is the distance from point P to N, U is a unit vector in the direction from P to N, I is a unit vector in the direction of the current in the conductor segment, and j is the magnitude of the current which is positive or negative according to whether the corner is considered a current source or a current sink.