Let us imagine an ensemble of systems distributed in phase according to the index of probability
|
|
where
is any constant which is a possible value of the energy, except only the least value which is consistent with the values of the external coördinates, and
and
are other constants. We have therefore
|
(403)
|
or
|
(404)
|
or again
|
(405)
|
From (404) we have
|
(406)
|
where
denotes the average value of
in those systems of the ensemble which have any same energy
. (This is the same thing as the average value of
in a microcanonical ensemble of energy
.) The validity of the transformation is evident, if we consider separately the part of each integral which lies between two infinitesimally differing limits of energy. Integrating by parts, we get