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Spherical multipole moments
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Spherical multipole moments : ウィキペディア英語版
Spherical multipole moments

Spherical multipole moments are the coefficients in a series expansion
of a potential that varies inversely with the distance R to a source, ''i.e.'', as 1/''R''. Examples of such potentials are the electric potential, the magnetic potential and the gravitational potential.
For clarity, we illustrate the expansion for a point charge, then generalize to an arbitrary charge density \rho(\mathbf}
refer to the position of charge(s), whereas the unprimed coordinates such as \mathbf refer to the point at which the potential is being observed. We also use spherical coordinates throughout, e.g., the vector \mathbf, \theta^, \phi^) where r^ is the radius, \theta^ is the colatitude and \phi^ is the azimuthal angle.
==Spherical multipole moments of a point charge==

The electric potential due to a point charge located at \mathbf) =
\frac \frac =
\frac
\frac - 2 r^ r \cos \gamma}}.

where
R \ \stackrel\ \left|\mathbf - \mathbf and \mathbf of the charge,
we may factor out 1/''r'' and expand the square root in powers of (r^/r)<1 using Legendre polynomials
:
\Phi(\mathbf) =
\frac \sum_^
\left( \frac \right)^ P_(\cos \gamma )

This is exactly analogous to the axial
multipole expansion
.
We may express \cos \gamma in terms of the coordinates
of the observation point and charge position using the
spherical law of cosines (Fig. 2)
:
\cos \gamma =
\cos \theta \cos \theta^ +
\sin \theta \sin \theta^ \cos(\phi - \phi^)

Substituting this equation for \cos \gamma into
the Legendre polynomials and factoring the primed and unprimed
coordinates yields the important formula known as the spherical harmonic addition theorem
:
P_(\cos \gamma) = \frac \sum_^
Y_(\theta, \phi) Y_^(\theta^, \phi^)

where the Y_ functions are the spherical harmonics.
Substitution of this formula into the potential yields
:
\Phi(\mathbf) =
\frac \sum_^
\left( \frac \right)^
\left( \frac \right)
\sum_^
Y_(\theta, \phi) Y_^(\theta^, \phi^)

which can be written as
:
\Phi(\mathbf) =
\frac
\sum_^ \sum_^
\left( \frac} \right)
\sqrt} Y_(\theta, \phi)

where the multipole moments are defined
:
Q_ \ \stackrel\
q \left( r^ \right)^
\sqrt}
Y_^(\theta^, \phi^).
As with axial multipole moments, we may also consider
the case when
the radius r of the observation point is less
than the radius r^ of the charge.
In that case, we may write
:
\Phi(\mathbf) =
\frac^
\left( \frac
\left( \frac \right)
\sum_^
Y_(\theta, \phi) Y_^(\theta^, \phi^)

which can be written as
:
\Phi(\mathbf) =
\frac
\sum_^ \sum_^ I_ r^
\sqrt}
Y_(\theta, \phi)

where the interior spherical multipole moments are defined as the complex conjugate of irregular solid harmonics
:
I_ \ \stackrel\ \frac}
\sqrt}
Y_^(\theta^, \phi^)

The two cases can be subsumed in a single expression if
r_< and r_> are defined
to be the lesser and greater, respectively, of the two
radii r and r^; the
potential of a point charge then takes the form, which is sometimes referred to as Laplace expansion
:
\Phi(\mathbf) =
\frac \sum_^
\frac}
\left( \frac \right)
\sum_^
Y_(\theta, \phi) Y_^(\theta^, \phi^)


抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「Spherical multipole moments」の詳細全文を読む



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