Faraday, Michael, 1791-1867; Physicists -- Great Britain -- Biography
It required long subsequent effort to subdue the complications of
magne-crystallic action, and to bring under the dominion of elementary
principles the vast mass of facts which the experiments of Faraday and
Plucker had brought to light. It was proved by Reich, Edmond Becquerel,
and myself, that the condition of diamagnetic bodies, in virtue of which
they were repelled by the poles of a magnet, was excited in them by
those poles; that the strength of this condition rose and fell with, and
was proportional to, the strength of the acting magnet. It was not then
any property possessed permanently by the bismuth, and which merely
required the development of magnetism to act upon it, that caused the
repulsion; for then the repulsion would have been simply proportional to
the strength of the influencing magnet, whereas experiment proved it to
augment as the square of the strength. The capacity to be repelled was
therefore not inherent in the bismuth, but induced. So far an identity
of action was established between magnetic and diamagnetic bodies.
After this the deportment of magnetic bodies, 'normal' and 'abnormal';
crystalline, amorphous, and compressed, was compared with that of
crystalline, amorphous, and compressed diamagnetic bodies; and by a
series of experiments, executed in the laboratory of this Institution,
the most complete antithesis was established between magnetism and
diamagnetism. This antithesis embraced the quality of polarity,--the
theory of reversed polarity, first propounded by Faraday, being proved
to be true. The discussion of the question was very brisk. On the
Continent Professor Wilhelm Weber was the ablest and most successful
supporter of the doctrine of diamagnetic polarity; and it was with an
apparatus, devised by him and constructed under his own superintendence,
by Leyser of Leipzig, that the last demands of the opponents of
diamagnetic polarity were satisfied. The establishment of this point was
absolutely necessary to the explanation of magne-crystallic action.
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