| "Currents of electricity may be induced by the influence
of terrestrial magnetism, but in consequence of the feebleness of the action
it is not easy to render it by the aid of wire coils alone. Deflections
may, however, be obtained by connecting with a very delicate galvanometer
a helix of coarse wire. A very evident effect may be produced by employing
the instrument represented [below and to the right]. It consists of a small
rod of soft iron wound with wire, and fitted to revolve on a horizontal
axis, which is provided with a pole-changer. Upon the the segments of the
pole-changer press two wires. ... Now on causing the bar to revolve by
hand in one direction, each end of the iron will become alternately a north
and south pole... and a current of electricity, whose directions changes
twice in each revolution, will be induced in the surrounding wire. The
two currents are turned into one direction by the pole-changer, and the
needle of the galvanometer will be steadily deflected." (1841 Manual
of Magnetism, pg 197) |
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