Gauss's law and multipole expansion
Separate exact flux constraints from symmetry arguments and estimate distant fields with controlled multipole approximations.
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The question for today
What you’ll understand
- Identify when Gauss's law determines a local field.
- Compute monopole and dipole contributions to a distant potential.
- Estimate the error and angular limitations of a multipole truncation.
A closed surface counts enclosed charge through electric flux, but it does not usually tell you the field at every point on that surface. Symmetry supplies the missing information in special cases. For a complicated localized source seen from far away, a different simplification becomes useful: organize its field by progressively finer features of the charge distribution.
Flux is an integral statement
Electric flux measures the normal field integrated over an oriented surface. A charge outside a closed surface can produce a large field on it while contributing zero net flux: field entering one side leaves another. Conversely, zero enclosed charge does not imply that every normal field component vanishes. Gauss's law constrains the sum, not each contribution separately.
For a spherically symmetric isolated charge distribution, rotations require the field to be radial and to have the same magnitude everywhere on a centered sphere. Only then may that magnitude be removed from the surface integral. Cylindrical and planar symmetry support other useful surfaces, but a rectangular charged object does not become symmetric merely because one draws a spherical surface around it.
A distant observer resolves moments
Let all source charges lie within a radius a of the chosen origin and observe at distance r greater than a. Expanding the Coulomb kernel in powers of source position divided by r gives a convergent exterior multipole series. The monopole depends only on total charge. The dipole records the first spatial moment, so its potential has angular structure and decreases one additional power of distance.
For a neutral source the dipole moment does not depend on a translation of origin; for a charged source it does. This is not a physical ambiguity because the whole expansion transforms together. Truncating after the dipole is controlled by , provided one compares nonvanishing terms. On a nodal direction where a leading term is zero, relative error can be large even when the absolute omitted field is small.
Differentiate before interpreting a zero
For a dipole along the vertical axis, potential is proportional to cosine of polar angle. Its equatorial potential vanishes, but its electric field does not: a spatial derivative of a function can be nonzero where the function itself is zero. Along the axis the field points with the dipole moment; in the equatorial plane it points opposite to it. A scalar contour and a vector field answer different questions.
An ideal point dipole is an exact mathematical source with a singular center. Two finite separated charges reproduce its leading distant field, with corrections near the pair. A dipole approximation is therefore a statement about observational scale, not a claim that the actual charges occupy the same point. Always compare the observation distance with the charge separation before using its inverse-cube field.
Work it through
How accurate is a small dipole?
Charges are separated by 1.0 cm. Find the potential 10 cm from their midpoint along the positive-charge axis, using .
The dipole moment magnitude is . The distance ratio is , making a distant approximation plausible but worth checking.
On the positive axis, . The dipole estimate is , and the axial field estimate is .
The exact potential is . The approximate potential is about 0.25% below the exact result; symmetry removes the next even-power charge moment for this pair.
The potential is approximately 18 V, with a directly checked 0.25% relative error in this geometry. A generic source need not share the pair's cancellation of its quadrupole moment.
The living notebook
Explore the model
Interactive lab · fields
Flux-like source structure and circulation
Adjust source strength q and rotation Ω in the softened two-dimensional field q r/(r²+ε) + Ω(−y,x). Setting Ω to zero exposes radial structure; adding rotation shows why flux and circulation differ. This is not a Coulomb dipole, a three-dimensional Gaussian surface, or a multipole solver.
- Fx at (1, 0)
- 0.833
- Fy at (1, 0)
- 0.5
- Field magnitude there
- 0.972
The softened illustration is q·r/(r² + 0.2) + Ω(−y, x). Moving markers indicate local direction, not integrated particle paths or a Maxwell solution. Parameter changes pause playback and recompute the model at the current elapsed time. Reset restores both parameters and returns time to zero. Playback starts paused. Adjust either parameter, then choose Play or Step.
Look forA picture of arrows must be interpreted with its actual dimensionality and source law.
Pause & reason
Check your understanding
Your turn
Try it yourself
For the pair in the worked example, estimate the electric field at a point 10 cm from the midpoint in the equatorial plane. State its direction and the status of the approximation.
Take a moment to make a prediction or work it out on paper. Open a hint when you need one.
Give me a hint
The dot product of the dipole moment with the equatorial radial unit vector vanishes.
Compare with the solution
The dipole formula becomes . Its magnitude is , directed opposite to the dipole moment, from the positive-charge side toward the negative-charge side. This is a far-field estimate for finite separated charges; its error must be checked separately rather than copied from the axial potential calculation.
Keep the idea
Take it with you
- Gauss's law becomes a pointwise shortcut only with sufficient symmetry.
- Multipoles organize source information by angular structure and distance scaling.
- A zero leading potential does not automatically imply a zero electric field.
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