Flux of an Electric Field — Question 4

Section 23-2 · Physics pages 3658–3659

Question 4 An angularly varying normal field separates hemisphere fluxes On a sphere of radius R, the outward normal field is En(θ) = E0(1 + η cos θ), with polar angle 0 ≤θ ≤π, E0 > 0 and |η| < 1. R N S Cross-section of concentric spherical surfaces; labels specify radii. (a) Find the total outward flux by direct surface integration. (b) Find the northern and southern hemisphere fluxes and recover η from their difference divided by their sum.
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Question 4 - Solution An angularly varying normal field separates hemisphere fluxes R N S (a) Method and calculation Φ = 2πR2E0 ∫π 0 (1 + η cos θ) sin θ dθ. Φ = 4πR2E0. (b) Interpretation and further calculation ΦN = 2πR2E0(1 + η/2), ΦS = 2πR2E0(1 −η/2). ΦN −ΦS ΦN + ΦS = η 2. Total flux alone cannot reveal this north-south asymmetry. Physical check The term odd in cos θ cancels over the whole sphere but not over a single hemisphere.

Question 4

An angularly varying normal field separates hemisphere fluxes

On a sphere of radius R, the outward normal field is En(θ)=E0(1+ηcos⁡θ)E_n(\theta)=E_0(1+\eta\cos\theta), with polar angle 0≤θ≤π0\le\theta\le\pi, E0>0E_0>0 and |η|<1|\eta|<1.

Diagram shown in the original SVG worksheet.

  1. Find the total outward flux by direct surface integration.

  2. Find the northern and southern hemisphere fluxes and recover η\eta from their difference divided by their sum.

Question 4 - Solution

An angularly varying normal field separates hemisphere fluxes

Diagram shown in the original SVG worksheet.

(a) Method and calculation

Φ=2πR2E0∫0π(1+ηcos⁡θ)sin⁡θdθ.\Phi=2\pi R^2E_0\int_0^\pi(1+\eta\cos\theta)\sin\theta\,d\theta.Φ=4πR2E0.\Phi=4\pi R^2E_0.

(b) Interpretation and further calculation

ΦN=2πR2E0(1+η/2),ΦS=2πR2E0(1−η/2).\Phi_N=2\pi R^2E_0(1+\eta/2),\quad\Phi_S=2\pi R^2E_0(1-\eta/2).ΦN−ΦSΦN+ΦS=η2.\frac{\Phi_N-\Phi_S}{\Phi_N+\Phi_S}=\frac\eta2.Total flux alone cannot reveal this north-south asymmetry.

Physical check

The term odd in cos⁡θ\cos\theta cancels over the whole sphere but not over a single hemisphere.