
particular law of motion which has been confirmed with great precision in recent years.
The theory of relativity leads to the same law of motion, without requiring any special hypothesis
whatsoever as to the structure and the behaviour of the electron. We arrived at a similar conclusion
in Section 13 in connection with the experiment of Fizeau, the result of which is foretold by the
theory of relativity without the necessity of drawing on hypotheses as to the physical nature of the
liquid.
The second class of facts to which we have alluded has reference to the question whether or not
the motion of the earth in space can be made perceptible in terrestrial experiments. We have
already remarked in Section 5 that all attempts of this nature led to a negative result. Before the
theory of relativity was put forward, it was difficult to become reconciled to this negative result, for
reasons now to be discussed. The inherited prejudices about time and space did not allow any
doubt to arise as to the prime importance of the Galileian transformation for changing over from
one body of reference to another. Now assuming that the Maxwell−Lorentz equations hold for a
reference−body K, we then find that they do not hold for a reference−body K
1
moving uniformly with
respect to K, if we assume that the relations of the Galileian transformstion exist between the
co−ordinates of K and K
1
. It thus appears that, of all Galileian co−ordinate systems, one (K)
corresponding to a particular state of motion is physically unique. This result was interpreted
physically by regarding K as at rest with respect to a hypothetical æther of space. On the other
hand, all coordinate systems K
1
moving relatively to K were to be regarded as in motion with
respect to the æther. To this motion of K
1
against the æther ("æther−drift " relative to K
1
) were
attributed the more complicated laws which were supposed to hold relative to K
1
. Strictly speaking,
such an æther−drift ought also to be assumed relative to the earth, and for a long time the efforts of
physicists were devoted to attempts to detect the existence of an æther−drift at the earth's surface.
In one of the most notable of these attempts Michelson devised a method which appears as though
it must be decisive. Imagine two mirrors so arranged on a rigid body that the reflecting surfaces
face each other. A ray of light requires a perfectly definite time T to pass from one mirror to the
other and back again, if the whole system be at rest with respect to the æther. It is found by
calculation, however, that a slightly different time T
1
is required for this process, if the body,
together with the mirrors, be moving relatively to the æther. And yet another point: it is shown by
calculation that for a given velocity v with reference to the æther, this time T
1
is different when the
body is moving perpendicularly to the planes of the mirrors from that resulting when the motion is
parallel to these planes. Although the estimated difference between these two times is exceedingly
small, Michelson and Morley performed an experiment involving interference in which this
difference should have been clearly detectable. But the experiment gave a negative result — a fact
very perplexing to physicists. Lorentz and FitzGerald rescued the theory from this difficulty by
assuming that the motion of the body relative to the æther produces a contraction of the body in the
direction of motion, the amount of contraction being just sufficient to compensate for the differeace
in time mentioned above. Comparison with the discussion in Section 11 shows that also from the
standpoint of the theory of relativity this solution of the difficulty was the right one. But on the basis
of the theory of relativity the method of interpretation is incomparably more satisfactory. According
to this theory there is no such thing as a " specially favoured " (unique) co−ordinate system to
occasion the introduction of the æther−idea, and hence there can be no æther−drift, nor any
experiment with which to demonstrate it. Here the contraction of moving bodies follows from the
two fundamental principles of the theory, without the introduction of particular hypotheses ; and as
the prime factor involved in this contraction we find, not the motion in itself, to which we cannot
attach any meaning, but the motion with respect to the body of reference chosen in the particular
case in point. Thus for a co−ordinate system moving with the earth the mirror system of Michelson
and Morley is not shortened, but it is shortened for a co−ordinate system which is at rest relatively
to the sun.
Relativity: The Special and General Theory
35