Determination of the earth's magnetic field

Article No: P2430100

A constant magnetic field, its magnitude and direction known, is superimposed on the unknown earth magnetic field. The earth-magnetic field can then be calculated from the magnitude and direction of the resulting flux density.

Key Features

Particularly homogeneous magnetic field and high flux density due to large Helmholtz coil diameter
Setup with precalibrated teslameter does not require additional magnets and coils for calibration

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