Lord Kelvin: An account of his scientific life and workGray, Andrew
Science
Lord Kelvin: An account of his scientific life and work
Gray, Andrew
Kelvin, William Thomson, Baron, 1824-1907
Further, if q be distributed over an element dS of a surface, the
inverse charge aq⧸f will be distributed over the corresponding element
dS' of the inverse surface. But dS'⧸dS = a⁴⧸f⁴ = f'⁴⧸a⁴ where f, f'
are the distances of O from dS and dS'. Thus if s be the density on dS
and s' the inverse density on dS' we have s'⧸s = a³⧸f'³ = f³⧸a³.
When V is constant over the direct surface, while r has different
values for different directions of OQ, the different points of the
inverse surface may be brought to zero potential by placing at O a
charge -aV. For this will produce at Q' a potential -aV⧸r' which
with V' will give at Q' a potential zero. This shows that V' is the
potential of the induced distribution on S' due to a charge -aV at O,
or that -V' is the potential due to the induced charge on S' produced
by the charge aV at O.
Thus we have the conclusion that by the process of inversion we get from
a distribution in equilibrium, on a conductor of any form, an induced
distribution on the inverse surface supposed insulated and conducting;
and conversely we obtain from a given induced distribution on an
insulated conducting surface, a natural equilibrium distribution on the
inverse surface. In each case the inducing charge is situated at the
centre of inversion. The charges on the conductor (or conductors) after
inversion are always obtainable at once from the fact that they are the
inverses of the charges on the conductor (or conductors) in the direct
case, and the surface-densities or volume-densities can be found from
the relations stated above.
[Illustration: FIG. 7.]
Now take the case of two concentric spheres insulated and influenced by
a point-charge q placed at a point P between them as shown in Fig. 7. We
have seen at p. 49 how the induced distribution, and the amount of the
charge, on each sphere is obtained from the two convergent series of
images, one outside the outer sphere, the other inside the inner sphere.
We do not here calculate the density of distribution at any point, as
our object is only to explain the method; but the quantities on the
spheres S₁ and S₂, are respectively -q.OA.PB⧸(OP.AB), -q.OB.AP⧸(OP.AB).
It may be noticed that the sum of the induced charges is -q, and that
as the radii of the spheres are both made indefinitely great, while
the distance AB is kept finite, the ratios OA⧸OP, OB⧸OP approximate
to unity, and the charges to -q.PB⧸AB, -q.AP⧸AB, that is, the
charges are inversely as the distances of P from the nearest points of
the two surfaces. But when the radii are made indefinitely great we have
the case of two infinite plane conducting surfaces with a point-charge
between them, which we have described above.
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