Borehole surveying

• US 6,021,577 A
• Filed: 03/16/1998
• Issued: 02/08/2000
• Est. Priority Date: 09/16/1995
• Status: Expired due to Term

• Current Assignee: Halliburton Energy Services Incorporated (Halliburton Company), Natural Environment Research Council
• Original Assignee: Baroid Technology Incorporated
• Inventors: Shiells, Gordon Malcolm, Kerridge, David John
• Primary Examiner(s): Fulton, Christopher W.
• Assistant Examiner(s): DOAN, QUYEN M
• Application Number:
  US09/043,338
• Time in Patent Office: 694 Days
• Field of Search: 33/304, 33/302, 33/303, 33/310, 33/313, 175/45, 175/61
• US Class Current: 33/304
• CPC Class Codes: E21B 47/022 of the borehole, e.g. using geomagnetism

Abstract

A borehole survey is conducted at a drilling site S by a so-called Interpolated In-Field Referencing (IIFR) method in which: (a) absolute local geomagnetic field data is obtained by spot measurement of the earth'"'"'s magnetic field at a local measurement site R which is sufficiently close to the drilling site S that the measurement data is indicative of the earth'"'"'s magnetic field at the drilling site S but which is sufficiently remote from the drilling site S that the measurement data is unaffected by magnetic interference from the drilling site and other man-made installations; (b) time-varying geomagnetic field data is obtained by combining the absolute local geomagnetic field data with data indicative of variation of the geomagnetic field with respect to time obtained by monitoring variation of the earth'"'"'s magnetic field with respect to time at a remote monitoring site P1, P2; (c) downhole magnetic field data is obtained by monitoring by means of a surveying instrument the magnetic field in the vicinity of the borehole at a series of locations along the borehole; and (d) the orientation of the borehole is determined from the downhole magnetic field data and the time-varying geomagnetic field data. Such a survey method takes into account short-term variations in the geomagnetic field caused by electrical currents in the ionosphere and is therefore more accurate than known survey methods.

Claims

1. A method of surveying a borehole at a drilling site comprising:

(a) obtaining local geomagnetic field data by spot measurement of the earth'"'"'s magnetic field at a local measurement site which is sufficiently close to the drilling site that the measurement data is indicative of the earth'"'"'s magnetic field at the drilling site but which is sufficiently remote from the drilling site that the measurement data is unaffected by magnetic interference from the drilling site and other man-made installations;

(b) obtaining time-varying geomagnetic field data by combining said local geomagnetic field data with data indicative of variation of the geomagnetic field with respect to time obtained by monitoring variation of the earth'"'"'s magnetic field with respect to time at a remote monitoring site;

(c) obtaining downhole magnetic field data by monitoring by means of a surveying instrument the magnetic field in the vicinity of the borehole at a series of locations along the borehole; and

(d) determining the orientation of the borehole from said downhole magnetic field data and said time-varying geomagnetic field data.

2. A method according to claim 1, wherein said time-varying geomagnetic field data is obtained by transforming said monitored data indicative of variation of the geomagnetic field with respect to time in order to take account of the longitude difference between the remote monitoring site and the local measurement site so as to obtain transformed time-varying data for combining with said absolute local geomagnetic field data.

3. A method according to claim 2, wherein the transformed time-varying data E_R^var (t₁) at time t₁ is obtained from the data E_Pn^var from N remote monitoring sites using the general expression:

##EQU5## where the first term on the right hand side is to account for the regular daily variation which occurs with a fundamental period of 24 hours and is dependent on local time, Λ

(E_Pn^var) represents a low pass filter, Φ

(λ

_Pn -λ

_R) represents a function (which may actually be incorporated in Λ

) which introduces a phase shift as a function of the longitude (λ

) difference between Pn and R, the second term on the right hand side, in which II(E_Pn^var) represents a high pass filter, is to account for the irregular variations which typically occur on time scales of a few hours or less, and w and μ

represent weight functions for combining the filtered variations from the N remote monitoring sites.

4. A method according to claim 1, wherein, in determining the orientation of the borehole from said downhole magnetic field data, a geomagnetic field value is used which is obtained by adding to said time-varying geomagnetic field data a site difference correction value which is indicative of the fact that the local measurement site is located at a distance from the drilling site and which is substantially constant with respect to time.

5. A method claim 1, wherein the step of determining the orientation of the borehole comprises determining the true azimuth angle of the borehole with respect to the earth'"'"'s magnetic field from the magnetic azimuth angle determined from said downhole magnetic field data and from a value indicative of the declination of the geomagnetic field obtained from said time-varying geomagnetic field data.

6. A method claim 1, wherein the step of determining the orientation of the borehole comprises determining an initial value for the azimuth angle of the borehole with respect to the earth'"'"'s magnetic field from said downhole magnetic field data and a value indicative of the vertical component of the geomagnetic field obtained from said time-varying geomagnetic field data, and carrying out a series of iterations in order to obtain successively more accurate values for the azimuth angle of the borehole.

7. A method according to claim 6, wherein each of the iterations comprises determining a value for the downhole magnetic field component in the direction of the borehole utilizing a previously determined value for the azimuth angle, and determining a further value for the azimuth angle utilizing the previously determined value for the downhole magnetic field component in the direction of the borehole.

8. A method claim 1, wherein said data indicative of variation of the geomagnetic field with respect to time comprises total intensity, declination and inclination values of the geomagnetic field.

9. A system for surveying a borehole at a drilling site comprising:

(a) a surveying instrument for monitoring the magnetic field in the vicinity of the borehole at a series of locations along the borehole in order to obtain downhole magnetic field data;

(b) means for recording local geomagnetic field data obtained by spot measurement of the earth'"'"'s magnetic field at a local measurement site which is sufficiently close to the drilling site that the measurement data is indicative of the earth'"'"'s magnetic field at the drilling site but which is sufficiently remote from the drilling site that the measurement data is unaffected by magnetic interference from the drilling site and other man-made installations;

(c) means for determining time-varying geomagnetic field data by combining said local geomagnetic field data with data indicative of variation of the geomagnetic field with respect to time obtained by monitoring variation of the earth'"'"'s magnetic field with respect to time at a remote monitoring site; and

(d) means for determining the orientation of the borehole from said downhole magnetic field data and said time-varying geomagnetic field data.