Science and the modern worldWhitehead, Alfred North
Religion
Science and the modern world
Whitehead, Alfred North
Science
Michelson’s experiment could not have been made earlier than it was. It
required the general advance in technology, and Michelson’s experimental
genius. It concerns the determination of the earth’s motion through the
ether, and it assumes that light consists of waves of vibration
advancing at a fixed rate through the ether in any direction. Also, of
course, the earth is moving through the ether, and Michelson’s apparatus
is moving with the earth. In the centre of the apparatus a ray of light
is divided so that one half-ray goes in one direction _along_ the
apparatus through a given distance, and is reflected back to the centre
by a mirror in the apparatus. The other half-ray goes the same distance
_across_ the apparatus in a direction at right angles to the former ray,
and it also is reflected back to the centre. These reunited rays are
then reflected onto a screen in the apparatus. If precautions are taken,
you will see interference bands; namely bands of blackness where the
crests of the waves of one ray have filled up the troughs of the other
rays, owing to a minute difference in the lengths of paths of the two
half-rays, up to certain parts of the screens. These differences in
length will be affected by the motion of the earth. For it is the
lengths of the paths in the ether which count. Thus, since the apparatus
is moving with the earth, the path of one half-ray will be disturbed by
the motion in a different manner from the path of the other half-ray.
Think of yourself as moving in a railway carriage, first along the train
and then across the train; and mark out your paths on the railway track
which in this analogy corresponds to the ether. Now the motion of the
earth is very slow compared to that of light. Thus in the analogy you
must think of the train almost at a standstill, and of yourself as
moving very quickly.
In the experiment this effect of the earth’s motion would affect the
positions on the screen of the interference bands. Also if you turn the
apparatus round, through a right-angle, the effect of the earth’s motion
on the two half-rays will be interchanged, and the positions of the
interference bands would be shifted. We can calculate the small shift
which should result owing to the earth’s motion round the sun. Also to
this effect, we have to add that due to the sun’s motion through the
ether. The delicacy of the instrument can be tested, and it can be
proved that these effects of shifting are large enough to be observed by
it. Now the point is, that nothing was observed. There was no shifting
as you turned the instrument round.
Public-domain text, read in full here on John Shaqi.
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