A «tidal» magnetic field?
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Abstract
t is shown that on the magnetization axis of a uniformly magnetized body of constant density the magnetic field intensity displays a «tidal» structure,i.e. the ratios among the differential magnetic field intensity in three orthogonal directions are the same as the ratios among the gravitational gradient tensor components pertaining to the same directions; it is also seen that the same characteristic ratios occur, both locally and non-locally, among the components of the magnetic field intensity and among the components of the gradient tensors of the two fields.
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How to Cite
Bocchio, F. (1997) “A «tidal» magnetic field?”, Annals of Geophysics, 40(5). doi: 10.4401/ag-3847.
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