Time and Clocks: A Description of Ancient and Modern Methods of Measuring TimeCunynghame, Henry H. (Henry Hardinge), Sir
Philosophy
Time and Clocks: A Description of Ancient and Modern Methods of Measuring Time
Cunynghame, Henry H. (Henry Hardinge), Sir
Clocks and watches; Time
This interesting curve is called a parabola. With a ball simply hit by
a bat, the motion is so very fast that we cannot see it well. Cannot
we make it go slowly? Let us remember what Galileo did. He used an
inclined plane to water down his force of gravity. Let us do the same.
Let us take an inclined plane and throw on it a ball horizontally.
It will go in a curve. Its speed is uniform horizontally, but is
accelerated downwards. If we desire to trace the curve it is easy to
do. We coat the ball with cloth and then dip it in the inkpot. It will
then describe a visible parabola. If I tilt up the plane and make the
force of gravity big, the parabola is long and thin; if I weaken down
the force of gravity by making the plane nearly horizontal, then it is
wide and flat.
One can also show this by a stream of peas or shot. The little bullets
go each with a uniform velocity horizontally, and an accelerated force
downwards.
Instead of peas we can use water. A stream of it rushing horizontally
out of an orifice will soon bend down into a parabola.
Thus then I have tried to show what force is and how it is measured. I
repeat again, when a body is free to move, then, if no further force
acts on it, it will go on in a straight line at a uniform speed, but
if a force continues to act on it in any direction, then that force
produces in each unit of time a unit of acceleration in the direction
in which the force acts, and the result is that the body goes on moving
towards the direction of acceleration at a constantly increasing speed,
and hence passing over spaces that are greater and greater as the speed
increases. This is the notion of a “force.” In all that has been said
above it has been assumed that the attraction of gravity on a body
does not increase as that body gets nearer to the earth. This is not
strictly true; in reality the attractive force of gravity increases as
the earth’s centre is approached. But small distances through which
the weights in Attwood’s machine fall make no appreciable difference,
being as nothing compared to the radius of earth. For practical
purposes, therefore, the force may be considered uniform on bodies that
are being moved within a few feet of the earth’s surface. It is only
when we have to consider the motions of the planets that considerations
of the change of attractive force due to distance have to be considered.
I am glad to say that the most tiresome, or rather the most difficult,
part of our inquiry is now over. With the help of the notions already
acquired, we are now ready to get to the pendulum, and to show how it
came about that a boy who once in church amused himself by watching the
swinging of the great lamps instead of attending to the service laid
the foundation of our modern methods of measuring time.
CHAPTER III.
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