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Anderson function

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Overview

Anderson Functions describe the projection of a magnetic field in a given direction at points along a line passing a single magnetic dipole. They are useful in the study of magnetic anomaly detection, with historical applications in submarine hunting and underwater mine detection[1]. They approximately describe the signal detected by a total field sensor as the sensor passes by a target (assuming the targets signature is small compared to the Earth's magnetic field).

Definition

The magnetic field from a magnetic dipole along a given line, and in any given direction can be described by the following basis functions:

which are known as Anderson functions[1].

Definitions:

  • is the dipole's strength and direction
  • is the projected direction (often the earth's magnetic field in a region)
  • is the position along the line
  • points in the direction of the line
  • is a vector from the dipole to the point of closest approach (CPA) of the line
  • , a dimensionless quantity for simplification

The total magnetic field along the line is given by

where is the magnetic constant, and are the Anderson coefficients, which depend on the geometry of the system. These are[2]

where and are unit vectors (given by and , respectively).

Note, the antisymmetric portion of the function is represented by the second function. Correspondingly, the sign of depends on how is defined (e.g. direction is 'forward').

Also note, some sources do not have the minus sign between terms for .

References

  1. ^ a b Loane, Edward P. (12 October 1976). "Speed and Depth Effects in Magnetic Anomaly Detection". EPL ANALYSIS OLNEY MD. {{cite journal}}: Cite journal requires |journal= (help)
  2. ^ Baum, Carl E. (1998). Detection And Identification Of Visually Obscured Targets. CRC Press. p. 345. ISBN 9781560325338.