University Experiments / Physics
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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