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Polar Coordinates from the Rim

Irodov 3.34DifficultyDifficulty 3 of 5UniquenessUniqueness 4 of 5

Problem Irodov 3.34

A thin disc of radius RR carries charge spread uniformly over it with surface density σ\sigma. Find the electric potential φ\varphi at a point on the disc’s edge.

The uniformly charged disc of radius R seen face-on, and the point A on its edge where the potential is wanted.

The uniformly charged disc of radius RR seen face-on, and the point AA on its edge where the potential is wanted.

Given
  • radius RR
  • uniform surface density σ\sigma
Find
the potential φ\varphi at a point AA of the edge

Solution

Step 1Coordinates centred on the edge point

The potential at AA is the sum of σ dS/(4πε0r)\sigma\,dS/(4\pi\varepsilon_0 r) over the disc, where rr is the distance from AA. The 1/r1/r suggests polar coordinates centred on AA itself: the area element is then dS=r dr dθdS = r\,dr\,d\theta, and the rr in it cancels the 1/r1/r.

Polar coordinates about the edge point A, with θ measured from the diameter through A. The chord at angle θ has length 2Rθ, and the element dS lies on it at distance r from A.

Polar coordinates about the edge point AA, with θ\theta measured from the diameter through AA. The chord at angle θ\theta has length 2Rcos⁡θ2R\cos\theta, and the element dSdS lies on it at distance rr from AA.

The chord from AA at angle θ\theta to the diameter, together with the diameter, makes a triangle whose angle at the chord’s far end is a right angle (an angle in a semicircle), so its length is

ℓ(θ)=2Rcos⁡θ,−π2≤θ≤π2(1) \ell(\theta) = 2R\cos\theta, \qquad -\frac{\pi}{2} \leq \theta \leq \frac{\pi}{2} \tag{1}
Step 2The integral

Writing the sum with dS=r dr dθdS = r\,dr\,d\theta, integrating rr along each chord from 00 to (1), then θ\theta across the disc:

φ=σ4πε0∫−π/2π/2∫02Rcos⁡θr drr dθ=σ4πε0∫−π/2π/22Rcos⁡θ dθ=σ4πε0⋅2R[sin⁡θ]−π/2π/2=σ4πε0⋅4R\begin{aligned} \varphi &= \frac{\sigma}{4\pi\varepsilon_0}\int_{-\pi/2}^{\pi/2}\int_0^{2R\cos\theta}\frac{r\,dr}{r}\,d\theta\\ &= \frac{\sigma}{4\pi\varepsilon_0}\int_{-\pi/2}^{\pi/2}2R\cos\theta\,d\theta\\ &= \frac{\sigma}{4\pi\varepsilon_0}\cdot 2R\Big[\sin\theta\Big]_{-\pi/2}^{\pi/2} = \frac{\sigma}{4\pi\varepsilon_0}\cdot 4R \end{aligned}
φ=σRπε0\varphi = \frac{\sigma R}{\pi\varepsilon_0}
(2)
Check

Compare with the centre, where every ring of radius rr and width drdr is at distance rr:

φcentre=σ4πε0∫0R2πr drr=σR2ε0\varphi_{\text{centre}} = \frac{\sigma}{4\pi\varepsilon_0}\int_0^R\frac{2\pi r\,dr}{r} = \frac{\sigma R}{2\varepsilon_0}

The ratio of edge to centre is (1/π)/(1/2)=2/π≈0.64(1/\pi)/(1/2) = 2/\pi \approx 0.64: lower at the edge, as it must be, since the charge lies on average farther from a point of the edge than from the centre. Units: σR/ε0\sigma R/\varepsilon_0 is charge per length over ε0\varepsilon_0, a potential.

Remark

The potential of a uniformly charged disc is not the same over its surface, so a uniformly charged disc is not a conductor’s charge distribution: on a conducting disc the charge would flow outward until the potential evened out, piling up toward the rim (the conducting disc’s density grows as 1/R2−r21/\sqrt{R^2 - r^2} near the edge). For a field point in the plane of any uniformly charged flat region, the same trick of centring the coordinates on the point turns the potential into a sum of chord lengths.