Multipole Expansion

An intuitive derivation of the far-field multipole expansion for a localized charge distribution, including monopole, dipole, quadrupole, origin dependence, and the ideal-dipole field.

What is a multipole expansion?

I had just encountered it when I wrote the original post, and the basic idea is surprisingly intuitive. A localized charge distribution viewed from far away can often be described by a sequence of progressively finer terms: monopole, dipole, quadrupole, and so on. If the total charge is nonzero, the monopole term usually dominates the far field. If it vanishes, the first nonzero higher moment takes over.

Starting with a finite dipole

Consider two charges, \(+q\) and \(-q\), separated by a displacement of magnitude \(d\).

Two opposite charges, plus q and minus q, separated by distance d

Place the charges at \(\pm (d/2)\hat{\mathbf z}\), and let the observation point be \(\mathbf r\), with \(r=|\mathbf r|\) and polar angle \(\theta\).

Far-field geometry for a centered electric dipole, showing r, d, theta, and source distances

The exact potential is the sum of the two point-charge potentials:

Exact potential of the two-charge dipole in terms of the two source distances

The exact source-to-field-point distances are

\[ R_+=\sqrt{r^2+\frac{d^2}{4}-rd\cos\theta}, \qquad R_-=\sqrt{r^2+\frac{d^2}{4}+rd\cos\theta}. \]

For \(r\gg d\), their first-order projected-distance approximations are

First-order far-field approximations for the two source distances

or \(R_+\approx r-(d/2)\cos\theta\) and \(R_-\approx r+(d/2)\cos\theta\). Substituting these approximations gives

\[ \begin{aligned} V(r,\theta) &\approx \frac{q}{4\pi\epsilon_0} \left[ \frac{1}{r-(d/2)\cos\theta} -\frac{1}{r+(d/2)\cos\theta} \right] \\ &=\frac{1}{4\pi\epsilon_0} \frac{qd\cos\theta}{r^2-(d^2/4)\cos^2\theta} \\ &\approx \frac{1}{4\pi\epsilon_0}\frac{p\cos\theta}{r^2}, \qquad p=qd, \end{aligned} \]

where the last line keeps the leading term for \(r\gg d\).

Source correction. The source image at this point prints a plus sign in the projected-distance denominator. The corrected denominator is \(r^2-(d^2/4)\cos^2\theta\), as shown above.

The pattern is now visible. A monopole contribution scales as \(r^{-1}\), a dipole contribution as \(r^{-2}\), a quadrupole contribution as \(r^{-3}\), and an octupole contribution as \(r^{-4}\). These statements describe the radial order at a fixed direction where the relevant angular factor is nonzero. An angular node of the potential does not mean that the whole multipole moment—or even the electric field—vanishes there.

Alternating-charge quadrupole and octupole arrangements

For the centered \(+q,-q\) pair above, inversion symmetry makes the charge distribution odd. Its even-\(\ell\) contributions cancel, but odd orders beyond the dipole, such as \(\ell=3,5,\ldots\), can still remain. Calling it a “dipole” identifies its leading nonzero moment, not the only term in the exact finite-separation potential.

A general localized charge distribution

Now consider a continuous charge distribution confined to a finite region.

Localized continuous charge distribution

Let \(\mathbf r\) be the observation point and \(\mathbf r'\) a source point. Define

\[ \mathbf R=\mathbf r-\mathbf r',\qquad R=|\mathbf R|,\qquad r=|\mathbf r|,\qquad r'=|\mathbf r'|, \]

and let \(\alpha\) be the angle between \(\mathbf r\) and \(\mathbf r'\), so that \(\cos\alpha=\hat{\mathbf r}\cdot\hat{\mathbf r}'\).

Source point and observation point geometry for a continuous charge distribution

The electrostatic potential is

Coulomb-potential integral for a continuous charge density

and the geometry gives

Law-of-cosines expression for the source-to-field-point distance

that is,

\[ R^2=r^2+r'^2-2rr'\cos\alpha. \]

Set \(t=r'/r\). The Legendre generating function gives

\[ \frac{1}{R} =\frac{1}{r}\left(1-2t\cos\alpha+t^2\right)^{-1/2} =\frac{1}{r}\sum_{\ell=0}^{\infty}t^\ell P_\ell(\cos\alpha), \qquad r'\lt r. \]

For a source contained inside \(r'\le a\), this exterior expansion applies for \(r>a\). On any region \(r\ge r_0>a\), the series converges uniformly enough to justify term-by-term integration.

If one reaches the result through the binomial series, it is important not to stop too soon. With \(u=t^2-2t\cos\alpha\), a derivation through \(P_3\) needs the \(-5u^3/16\) term; the displayed \(u^0\), \(u^1\), and \(u^2\) terms alone do not produce the full cubic coefficient. The Legendre generating function is also the clean way to state the full domain \(|t|<1\); the intermediate condition \(|u|<1\) can be unnecessarily restrictive.

Legendre generating series for the inverse source-to-field-point distance

The first few terms are

Collected expansion through the first four Legendre polynomials

so the coefficient of \(t^\ell\) is \(P_\ell(\cos\alpha)\). Substituting the series into the potential produces

\[ V(\mathbf r) =\frac{1}{4\pi\epsilon_0} \sum_{\ell=0}^{\infty}\frac{1}{r^{\ell+1}} \int r'^\ell P_\ell(\cos\alpha)\rho(\mathbf r')\,d\tau'. \]

The first three orders are

\[ V(\mathbf r)=\frac{1}{4\pi\epsilon_0} \left[ \frac{Q}{r} +\frac{1}{r^2}\int r'\cos\alpha\,\rho(\mathbf r')\,d\tau' +\frac{1}{r^3}\int \frac{r'^2}{2}\left(3\cos^2\alpha-1\right) \rho(\mathbf r')\,d\tau' +\cdots \right], \]

with \(Q=\int\rho(\mathbf r')\,d\tau'\).

Source correction. The source image uses \(r'^2\) in the general \(\ell\) term and gives an incorrect power and angular factor in the quadrupole term. The equations above restore \(r'^\ell\) generally and \(r'^2(3\cos^2\alpha-1)/2\) at \(\ell=2\).

For a fixed source distribution and a fixed origin, the multipole moments are fixed. Moving the observer changes \(r\) and the angular factors at which the expansion is evaluated; it does not change the source moments themselves. If the \(z\)-axis is chosen along \(\mathbf r\), then \(\alpha\) is the source point’s polar angle \(\theta'\). Later, when the \(z\)-axis is chosen along \(\mathbf p\), the \(\theta\) in \(p\cos\theta\) is the observation angle. Those are different coordinate choices.

The far-field hierarchy is controlled by the lowest nonzero moment, but only away from its angular nodes. When \(Q\ne0\), the monopole term is normally leading. When \(Q=0\), the dipole term leads only if the dipole moment is nonzero.

The dipole moment

The dipole term can be written using

\[ \mathbf p=\int \mathbf r'\rho(\mathbf r')\,d\tau', \qquad V_{\mathrm{dip}}(\mathbf r) =\frac{1}{4\pi\epsilon_0}\frac{\mathbf p\cdot\hat{\mathbf r}}{r^2}. \]

Source correction. The corresponding source image omits the explicit scalar-product dot in its last expression. It is restored here because the potential is a scalar.

For discrete point charges,

Electric dipole moment of discrete point charges

or \(\mathbf p=\sum_i q_i\mathbf r_i'\).

Return to a pair of charges \(-q\) and \(+q\).

Two opposite point charges in Cartesian coordinates

Let \(\mathbf r_1'\) point from the origin to \(-q\), and \(\mathbf r_2'\) point from the origin to \(+q\). Define the displacement from the negative charge to the positive charge by

\[ \mathbf d=\mathbf r_2'-\mathbf r_1'. \]

Dipole displacement vector from minus q to plus q

Then

Derivation of p equals q times d for two opposite charges

so \(\mathbf p=q\mathbf d\).

When the dipole moment also vanishes

A neutral distribution need not have a nonzero dipole moment. With equal-magnitude charges at centered symmetric positions, an alternating-charge square has \(Q=0\) and \(\mathbf p=0\), while a quadrupole component remains. Likewise, the centered alternating cube shown below cancels all orders below \(\ell=3\), leaving an octupole as its leading moment. Finite arrangements can still contain higher moments beyond the leading one.

Centered alternating-charge quadrupole and octupole examples

This is why “the first nonzero multipole” is the useful phrase: symmetry may eliminate one or several lower orders.

Dependence on the choice of origin

There is one more important detail: multipole moments are coordinates of a source relative to a chosen origin.

Single point charge located at the coordinate origin

For a point charge at the origin, the discrete definition

Discrete dipole-moment definition applied at the origin

gives zero dipole moment.

Single point charge displaced from the coordinate origin

If the origin is shifted by a vector \(\mathbf a\), so that \(\mathbf r'_{\mathrm{new}}=\mathbf r'_{\mathrm{old}}-\mathbf a\), then

\[ \mathbf p_{\mathrm{new}}=\mathbf p_{\mathrm{old}}-Q\mathbf a. \]

Therefore the dipole moment is origin-independent when \(Q=0\), but not in general. This coordinate dependence of individual moments does not change the physical potential or electric field when the whole expansion and coordinates are transformed consistently.

Electric field of an ideal dipole

Choose the \(z\)-axis along \(\mathbf p=p\hat{\mathbf z}\), and use spherical coordinates for an observation point away from the source.

Spherical coordinates for an observation point relative to the dipole axis

For \(r>0\), the ideal-dipole potential is

\[ V_{\mathrm{dip}}(r,\theta) =\frac{1}{4\pi\epsilon_0} \frac{\mathbf p\cdot\hat{\mathbf r}}{r^2} =\frac{1}{4\pi\epsilon_0}\frac{p\cos\theta}{r^2}. \]

It is independent of the azimuthal angle \(\phi\). Taking \(\mathbf E=-\nabla V\) gives

\[ \mathbf E(r,\theta) =\frac{p}{4\pi\epsilon_0 r^3} \left(2\cos\theta\,\hat{\mathbf r} +\sin\theta\,\hat{\boldsymbol\theta}\right), \qquad E_\phi=0, \qquad r>0. \]

Source correction. The source image omits \(p\) from its first displayed radial component. The corrected field above includes it. The ideal-dipole expression is not defined at \(r=0\).

That completes the basic picture: expand the inverse distance in Legendre polynomials, integrate each angular order against the source, and let the first nonzero moment describe the leading far field.

References

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