SURVEY SYSTEM FOR LOCATING GEOPHYSICAL ANOMALIES

• US 20110066379A1
• Filed: 05/15/2009
• Published: 03/17/2011
• Est. Priority Date: 05/26/2008
• Status: Abandoned Application

• Current Assignee: Norwegian Technology AS
• Original Assignee: Norwegian Technology AS
• Inventors: Mes, Marius J.
• Application Number:
  US12/994,358
• Publication Number:
  US 20110066379A1
• Time in Patent Office: Days
• US Class Current: 702/6
• 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 survey system is described for locating and classifying geophysical anomalies. It includes a moving platform equipped with a recording unit for recording the position of the platform. The system also comprises three first measuring units or sensors, adapted to record a varying electric field strength and a varying magnetic field strength at chosen intervals and thus positions, said first measuring units being adapted to measure said field strengths in three independent and mutually orthogonal directions at frequencies in a chosen range. The system includes a calculation unit for combining the measurements from each of said first sensors and calculating and recording as well as comparing the field strength vectors of the varying measured fields at each position, to find anomalies.

Claims

1. A survey system for locating geophysical anomalies, including a moving platform equipped with a recording unit for recording the position of the platform, the system also comprising three first measuring units, adapted to record a varying electric field strength and a varying magnetic field strength for frequencies in a chosen range at chosen intervals and thus positions, said first measuring units being adapted to measure each said field strength in three directions, the system including a calculation unit for combining the measurements from each of said first sensors and calculating the field strength vectors and recording at least one parameter based on said field strength vectors at each position, the system also being adapted to compare the recorded parameters at different positions and detect positions wherein said parameters differ significantly from the surrounding parameters at other positions.

2. System according to claim 1, wherein the measuring units are adapted to measure each said field strength in three independent mutually orthogonal directions.

3. System according to claim 1, wherein the magnetic sensor has a resolution in the pico Tesla range in each of the three independent mutually orthogonal directions combined with the ability to sample the magnetic field strength with a frequency of several thousand Hertz.

4. System according to claim 1, including an electronic filter adapted to remove signals outside the chosen frequency range.

5. System according to claim 1, wherein said calculation unit is positioned outside the platform, e.g. on a remote base reference station.

6. System according to claim 1, also including a temperature measuring means on said platform and wherein the calculation unit is adapted to modify the measurements for ambient temperature and ambient temperature changes.

7. System according to claim 1, also including a still picture camera that records photographic digital data at regular time intervals and wherein the image recording unit is adapted to store these images together with a time and geographical position tag for the purpose of confirming that no objects are present that could invalidate the interpretation.

8. System according to claim 1, also including means to supply calibration signals to the electronic system to confirm the calibration of the electronic system and if necessary provide the means to update the measurements for a different calibration.

9. System according to claim 1, wherein said parameters also include the frequency spectrum of the varying measured field strength vectors for frequencies in the chosen range.

10. System according to claim 1, wherein said at least one parameter includes both electric and the magnetic field strength measuring units suitable for frequencies in the chosen range, and wherein said calculation unit is adapted to calculate and record magnitudes of both said electric and magnetic field strength vectors for frequencies in that range.

11. System according to claim 1, wherein said at least one parameter also includes the relative directions of both electric and magnetic field strength vectors for frequencies in the chosen range.

12. System according to claim 1, wherein said at least one parameter includes the angle between the electric and magnetic field strength vectors derived from said measurements at each representative position for frequencies in the chosen range.

13. Method for locating geophysical anomalies, including the steps of moving a platform and recording the positions of the platform, and at each position measuring at least one of the magnetic or electric field strengths at said position in three dimensions and calculating and recording at least one parameter derived from the magnitude of said field strengths, and comparing the recorded field strength parameters to detect positions with parameters differing from the compatible surrounding parameters by a certain value at different frequencies in the chosen range.

14. Method according to claim 13, wherein said at least one parameter includes the frequency spectrum of the varying measured field strengths for frequencies in the chosen range at each representative position, said comparison also comparing said frequency spectra.

15. Method according to claim 13, wherein said at least one parameter includes the varying phase and angle between the measured field strength vectors being calculated and recorded at each representative position for frequencies in the chosen range, said comparison also comparing said angles.

16. Method according to claim 13, wherein said at least one parameter includes both calculated magnitudes of the measured electric and magnetic field strength vectors being calculated and recorded at each representative position for frequencies in the chosen range and compared in said comparison for frequencies in the chosen range.

17. Method according to claim 16, wherein said at least one parameter includes the angle between both said field strength vectors being recorded at each representative position and compared in said comparison for frequencies in the chosen range.

18. Method according to claim 16, wherein said at least one parameter includes other rational mathematical functions of both electric and magnetic field strength vector magnitudes calculated at each representative position and compared in said comparison for frequencies in the chosen range.

19. Method according to claim 16, wherein said at least one parameter includes differences in rates of signal attenuation at different frequencies calculated at each representative position and compared in said comparison for frequencies in the chosen range.

20. Method according to claim 16, wherein differences in rates of signal attenuation at different frequencies calculated at each representative position for frequencies in the chosen range are used to compute the depth of the anomalous volume.

21. Method according to claim 15, wherein differences in phases and angles between the E- and B-type vectors at different frequencies calculated at each representative position for frequencies in the chosen range are used to compute the type of the anomalous volume.