closely together that the most probable division may fairly represent the whole. This is in general the case, to a very close approximation, when
is enormously great; it entirely fails when
is small.
If we regard
as corresponding to the reciprocal of temperature, or, in other words,
as corresponding to temperature,
will correspond to entropy. It has been defined as
. In the considerations on which its definition is founded, it is therefore very similar to
. We have seen that
approaches the value unity when
is very great.[1]
To form a differential equation on the model of the thermodynamic equation (482), in which
shall take the place of temperature, and
of entropy, we may write
|
(489)
|
or
|
(490)
|
With respect to the differential coefficients in the last equation, which corresponds exactly to (482) solved with respect to

, we have seen that their average values in a canonical ensemble are equal to

, and the averages of

,

, etc.
[2] We have also seen that

(or

) has relations to the most probable values of energy in parts of a microcanonical ensemble. That

, etc., have properties somewhat analogous, may be shown as follows.
In a physical experiment, we measure a force by balancing it against another. If we should ask what force applied to increase or diminish
would balance the action of the systems, it would be one which varies with the different systems. But we may ask what single force will make a given value of
the most probable, and we shall find that under certain conditions
, a represents that force.
- ↑ See Chapter X, pages 120, 121.
- ↑ See Chapter IX, equations (321), (327).