Hertzian Wave Wireless TelegraphyFleming, J. A. (John Ambrose), Sir
Science
Hertzian Wave Wireless Telegraphy
Fleming, J. A. (John Ambrose), Sir
Electric waves; Telegraph, Wireless
We can represent the amplitude of the current and potential values
along the aerial by the ordinates of a dotted line so drawn that its
distance from the aerial represents the potential oscillation or
current oscillation at that point (see Fig. 6).
This distribution of potential and current along the wire does not
necessarily imply that any one electron moves far from its normal
position. The actual movement of any particular air molecule in the
case of a sound wave is probably very small, and reckoned in
millionths of an inch. So also we must suppose that any one electron
may have a small individual amplitude of movement, but the
displacement is transferred from one to another. Conduction in a solid
may be effected by the movement of free electrons intermingled with
the chemical atoms, but any one electron may be continually passing
from a condition of freedom to one of combination.
[Illustration: FIG. 6.--(_a_) DISTRIBUTION OF ELECTRIC PRESSURE IN A
MARCONI AERIAL, A, (_b_) DISTRIBUTION OF ELECTRIC CURRENT IN A MARCONI
AERIAL, AS SHOWN BY THE ORDINATES OF THE DOTTED LINE _xy_.]
So much for the events inside the wire, but now outside the wire its
electric charge is represented by lines of electric strain springing
from the aerial to the earth. It must be remembered that every line of
strain terminates on an electron or a co-electron. Hence, when the
discharge or spark takes place between the spark balls, the rapid
movement of the electrons in the wire is accompanied by a
redistribution and movement of the lines of strain outside. As the
negative charge flows out of the aerial the ends of the strain lines
abutting on to it run down the wire and are transferred to the earth,
and at the next instant this semi-loop of electric or ether strain,
with its ends on the earth, is pushed out sideways from the wire by
the growth of a new set of lines of ether strain in an opposite
direction. The process is best understood by consulting a series of
diagrams which represent the distribution and approximate form of a
few of the strain lines at successive instants (see Fig. 7). In
between the lines of formation of the successive strain lines between
the aerial and the earth, corresponding to the successive alternate
electric charges of the aerial with opposite sign, there are a set of
concentric rings of magnetic flux formed round it which are
alternately in opposite directions, and these expand out, keeping step
with the progress of the detached strain loops and having their planes
at right angles to the latter. As the semi-loops of electric strain
march outwards with their feet on the ground, these strain lines must
always be supposed to terminate on electrons, but not continually on
the same electrons. Since the earth is a conductor, we must suppose
that there is a continual migration of the electrons forming the atoms
of the earth, and that when one electron enters an atom, another
leaves it. Hence, corresponding to the electric wave in the space
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