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The IUP Journal of Earth Sciences :
Behavior of a Magnetic Dipole Freely Floating on Water Surface
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In this paper, the authors have detected a new effect in the area of geomagnetism, related to the behavior of a magnetic dipole freely floating on water surface. An experiment is described in the present paper in which a magnetic dipole fixed upon a float placed on non-magnetized water surface undergoes displacement along with reorientation caused by fine structure of the earth's magnetic field. This fact can probably be explained by secular decrease of the earth's major dipole moment. Further, a detailed study of the phenomenon may create interesting premises for its practical use, particularly for the analysis of fine structure of geomagnetic field and its time-dependent anomalies. A strange behavior of some sea fish species prior to strong earthquakes may be explained if the fish are assumed as `live magnetic dipoles'.

The history of human familiarity with the magnetic field of the earth goes down to such ancient times that one is even unable to determine the epoch when the people learned to use the magnetic needle properties for orientation. However, the birth of geomagnetism as the earth science is assumed to occur in the year 1600, when William Gilbert published his book, De Magnete. Although the magnetic inclination phenomenon was discovered by Robert Norman 20 years before that book appeared, it was Gilbert who generalized all the effects related with magnetic needle known by that time and explained them by the presence of the earth's magnetic field, in which case the earth appeared as a `big magnet'.

Norman invented a needle which could turn in a vertical plane, and thus discovered the magnetic inclination phenomenon. He also suggested that the earth's action on the needle represents a rotation moment, rather than an attraction force. His second idea on that special point should exist on the earth's surface around which the compass needle turns, however, was rejected by Gilbert who represented the earth as a magnet having two opposite polarities. But the Norman's first concept is preserved until now. Particularly, Borgman wrote (Borgman 1914-1916): "A magnet attached to a float freely swimming on water surface, away from iron masses or other magnets, does not undergo any displacement. Thus, only directional force acts on the magnet, as a result of which its magnetic axis assumes a certain orientation in space".

 
 
 

Magnetic Dipole Freely Floating on Water Surface, geomagnetism, time-dependent anomalies, live magnetic dipoles, magnetic inclination phenomenon, geomagnetism development, magnetic anomalies, geomagnetic field, earth's magnetic field.