30
THERMODYNAMICS OF RADIATION
Entropy.
24 . Quantitatively energy is conserved; qualitatively there is a con
tinuous unidirectional change in the character of the energy of the
universe.
In the ultimate analysis this change appears to be in all cases a change
from a more organised to a more chaotic condition. For example, a train
of plane waves may by irregular reflection or scattering be converted into
radiation moving in all directions at random. We cannot invert this
process or discover an appliance which will automatically convert dis
organised radiation into plane waves. Spherical waves can be converted
into plane waves by a parabolic mirror and back again to spherical waves
by another mirror. But spherical waves are in their way as highly or
ganised as plane waves ; no chance disturbances of regularity have befallen
them. When once the random element has been introduced it cannot be
eliminated by any natural process. If we construct a machine which
receives chaotic radiation and sends it out again as trains of plane waves
we must infer that the organisation has been given to the waves at the
expense of other energy put through the machine; and this energy is
drained of organisation and ejected from the machine in a more chaotic
state than it was originally. Such a machine continually requires fresh
supplies of energy not because it uses up energy but because it uses up
organisation of energy.
Thus in the vicissitudes of things energy is liable to take a step down
in rank which it cannot recover by any natural process. The potentiality
inherent in organisation—which is of immense importance for the practical
utilisation of energy—is lost to the universe, irrecoverably so far as we
can see.
25 . We introduce a numerical measure of the disorganisation caused
by these irreversible steps. Such a measure should evidently be propor
tional to the quantity of energy disorganised ; the other factor measuring
the degree of disorganisation will consist of the difference of two terms
dependent respectively on the initial and final states of the energy and
therefore functions of the physical variables used to specify those states.
The measure of disorganisation is thus expressed by a quantity S such
that
dS = dQ (6 2 — dj) (25-1),
where dQ is the quantity of energy passing from state 1 to state 2 and 9
is a function of the physical variables describing the states.
When several such transfers are contemplated it is convenient to express
the result in terms of the additions to the energy in the respective states.
Thus, in the above example, energy in state 1 receives an addition