Since is a homogeneous function of the degree in and ,
,
or
,
and
.
Since and are constant during the surface-integration,
.
But if is the potential due to a sheet of imaginary matter of surface-density ,
,
and , the magnetic potential of the current-sheet, may he expressed in terms of in the form
.
671.] We may determine , the -component of the vector-potential, from the expression given in Art. 416,
,
where , , are the coordinates of the element , and , , are the direction-cosines of the normal.
Since the sheet is a sphere, the direction-cosines of the normal are
,,.
But
,
and
,
so that
,
,
;
multiplying by , and integrating over the surface of the sphere, we find