Waves and ripples in water, air, and æther : $b Being a course of Christmas lectures delivered at the Royal Institution of Great BritainFleming, J. A. (John Ambrose), Sir
Science
Waves and ripples in water, air, and æther : $b Being a course of Christmas lectures delivered at the Royal Institution of Great Britain
Fleming, J. A. (John Ambrose), Sir
Electric waves; Sound; Waves
Since the date of these pioneer inventions many different forms of
wave detector have been discovered, and wireless telegraphy has shown
itself to be of the greatest utility in effecting communication between
ship and ship, and ship and shore. Its value in enabling intelligence
to be transmitted from lightships or lighthouses to coast stations
cannot be over estimated. One very remarkable feature of the apparatus
as arranged by Mr. Marconi is the small space it occupies. It is in
this respect most admirably adapted for use on board ship. It only
requires a long, insulated, vertical wire which can easily be suspended
from a mast, and the whole receiving and transmitting apparatus can be
placed on board ship in a small cabin. Employing the sensitive tube and
Marconi receiving arrangements, messages can easily be sent 150 miles
over the sea-surface by means of an aerial 150 feet high and a 10-inch
induction coil.
It is a curious fact that better results are obtained over a
water-surface than over land. Two similar stations with the same
appliances can communicate at two or three times greater distance if
they are separated by sea than if they are on land and have no water
between. This is connected with the fact that electric waves are not
able to pass through sea-water, but can diffuse through dry earth.
The sea-surface acts somewhat like an optical reflector or mirror,
and the electric waves glide along its surface. The rotundity of the
earth within certain limits hardly makes any perceptible effect upon
the ease of communication. The waves sent out by the transmitter of
a long-distance wireless station are from 3000 to 20,000 feet in
length, and there is, therefore, a considerable amount of bending
or diffraction. It is a familiar fact, as already explained, that a
wave-motion, whether on water or in air, spreads round an obstacle to
a certain extent. Thus an interposing rock or wall does not form a
sharply marked _sound-shadow_, but there is some deflection of the air
waves by the edge of the obstacle. The amount of bending which takes
place depends on the length of the wave.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account