from the surface . The quantities and correspond to superficial densities, but at present we must consider them as defined by the above equations.
Green's Theorem is obtained by integrating by parts the expression
|
| (5)
|
throughout the space within the surface .
If we consider as a component of a force whose potential is , and as a component of a flux, the expression will give the work done by the force on the flux.
If we apply the method of integration by parts, we find
|
| |
|
;
| (6)
|
or
|
.
| (7)
|
In precisely the same manner by exchanging and , we should find
|
| (8)
|
The statement of Green's Theorem is that these three expressions for are identical, or that
|
| |
|
| (9)
|
Correction of Green's Theorem for Cyclosis.
There are cases in which the resultant force at any point of a certain region fulfils the ordinary condition of having a potential, while the potential itself is a many-valued function of the coordinates. For instance, if
we find , a many-valued function of and , the values of forming an arithmetical series whose common difference