Page:Elementary Principles in Statistical Mechanics (1902).djvu/33

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DENSITY-IN-PHASE.
9

would alter the values of the 's as determined by equations (3), and thus disturb the relation expressed in the last equation.

If we write equation (19) in the form

(21)
it will be seen to express a theorem of remarkable simplicity. Since is a function of , , , its complete differential will consist of parts due to the variations of all these quantities. Now the first term of the equation represents the increment of due to an increment of (with constant values of the 's and 's), and the rest of the first member represents the increments of due to increments of the 's and 's, expressed by , , etc. But these are precisely the increments which the 's and 's receive in the movement of a system in the time . The whole expression represents the total increment of for the varying phase of a moving system. We have therefore the theorem:—

In an ensemble of mechanical systems identical in nature and subject to forces determined by identical laws, but distributed in phase in any continuous manner, the density-in-phase is constant in time for the varying phases of a moving system; provided, that the forces of a system are functions of its coördinates, either alone or with the time.[1]

This may be called the principle of conservation of density-in-phase. It may also be written

(22)
where represent the arbitrary constants of the integral equations of motion, and are suffixed to the differential co-
  1. The condition that the forces are functions of and , , etc., which last are functions of the time, is analytically equivalent to the condition that are functions of and the time. Explicit mention of the external coördinates, , , etc., has been made in the preceding pages, because our purpose will require us hereafter to consider these coördinates and the connected forces, , , etc., which represent the action of the systems on external bodies.