Search coil magnetometer explained

The search coil magnetometer or induction magnetometer, based on an inductive sensor (also known as inductive loop and inductive coil), is a magnetometer which measures the varying magnetic flux. An inductive sensor connected to a conditioning electronic circuit constitutes a search coil magnetometer. It is a vector magnetometer which can measure one or more components of the magnetic field. A classical configuration uses three orthogonal inductive sensors. The search-coil magnetometer can measure magnetic field from mHz up to hundreds of MHz.

Principle

\Phi

through a N turns circuit will induce a voltage

e

which follows

e=-N

d\Phi
dt
which can be expressed in a simpler way

e=-NS

dB
dt
by assuming that the induced magnetic field B is homogeneous over a surface S (the magnetic flux will be expressed

\Phi=B x S

).

The induced voltage (

e

) may be increased several ways:

Search coil using a ferromagnetic core

When a coil is wound around a ferromagnetic core, that increases the sensitivity of the sensor thanks to the apparent permeability of the ferromagnetic core.

Apparent permeability

The magnetic amplification, known as apparent permeability

\muapp

, is the result of the magnetization of the ferromagnetic core response to an external magnetic field. The magnetization is reduced by the demagnetizing field.

\muapp=

\mur
1+Nz(\mur-1)

where

\mur

is the relative permeability,

Nz

is the demagnetizing coefficient in the z direction.

The induced voltage will be written

-Ne=NS\muapp

NdB
dt

The demagnetizing coefficient can easily be computed in the case of simple shapes (spheres and ellipsoids).

Applications

References

See also