Science for the School and Family, Part I. Natural PhilosophyHooker, Worthington
Science
Science for the School and Family, Part I. Natural Philosophy
Hooker, Worthington
Physics; Science
214. =Illustrations of Centrifugal Force.=--When a wet mop is
whirled the water flies off in every direction by its centrifugal
force. On the same principle a dog, coming out of the water,
shakes off the water by a semi-rotary motion.--When a suspended
bucket of water is turned swiftly around the water rises high on
its sides, and leaves a hollow in the middle. It is the tendency
to fly away from the centre of motion that causes this.--Large
wheels, revolving with great velocity, have been broken by the
centrifugal force of its particles, and hence the necessity of
having such wheels made very strong. The immense grindstones used
in gun-factories have sometimes been broken through in the middle,
or have flown into pieces from the same cause.--A man riding
horseback on turning a sharp corner inclines his body toward the
corner, to avoid being thrown off by the centrifugal force. So, in
the feats of the circus, a man standing on a horse running at full
speed around the ring inclines his body strongly inward, as you
see in Fig. 148 (p. 167). The horse also instinctively inclines in
the same direction for the same reason. If the rider finds himself
in danger of falling, by making the horse go a little faster, thus
adding to the centrifugal force, the difficulty is relieved.--The
centrifugal force is made use of in milling. The grain is admitted
between two circular stones by a hole in the centre of the upper
one, and as the stone revolves it constantly moves toward the
circumference, and there escapes as flour.
[Illustration: Fig. 149.]
215. =Bends in Rivers.=--We see the operation of the centrifugal
force in the bends of rivers. When a bend has once commenced in
a river it is apt to increase, for as the water sweeps along the
outer bank of the bend it presses strongly against it, just as the
water in the whirled bucket, § 214, presses against its sides,
by its centrifugal tendency, or, in other words, its tendency to
assume a straight motion. Of course the result is a wearing away of
this outer bank, and in proportion to the looseness of the material
of which it is composed and the velocity of the river's current.
And when one bend is formed another is apt to form below, but in an
opposite direction. The water, by sweeping along the bend _a_, Fig.
149, is directed by it toward the opposite bank at _b_, and makes a
bend there also.
[Illustration: Fig, 150.]
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