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satisfactorily for them. M. De la Rive compares them to the
deviations of the galvanometer, under like circumstances. For
instance, while Faraday was making experiments to determine
the velocity of galvanic electricity, he obtained the use of several
hundred coils of large telegraph wire, covered with gutta percha,
and intended for subterranean or submarine lines, which were
half a mile in length each. He suspended these to a series of
barges, in a canal, so that each coil was plunged entirely under
water its whole length, with the exception of a very short bit at
each end. These he connected metallically end to end, so as to
constitute a single wire of some two hundred miles in length.
Then he attached to one end of this long, insulated wire a com-
pound galvanic battery composed of three hundred and sixty
cups, and hence as many pairs of zinc and copper plates, in
acidulated water, including in the circuit also a very sensitive
galvanometer. Then, after the current had thus been traversing
this long wire for a time, at the moment when communication
was cut off between the battery and the long wire, a very strong
shock was felt, by merely touching for an instant either end of
the long wire. This he found could be repeated some forty times
in succession, with the same residt, but less and less in degree.
Again: instead of thus touching the long wire and so leading off
the accumulated electricity so immediately after taking away the
battery from it, if one pole or end is placed in connection with
the galvanometer, while the other end or pole connects witli the
ground, then the needle of the instrument was quickly and
powerfully deflected; and this was still sensible, if the trial was
not made again with it, for some half hour.
Faraday explains this as the result of the thus formed unique
Leyden jar of enormous length; consisting of the long wire,
the envelope by which it was insulated, and the liquid which
surrounded it. The wire plays the inner coat of the Leyden
jar, which is charged. The gutta percha, being a non-conductor,
is the jar itself; while the water, or the moist earth, is the con-
ductor for its negative electricity, like the outside of a positively
charged Leyden jar. Volta early showed that a Leyden jar
might be charged by connecting its inner coating of foil with