A Charged Isolated Conductor — Question 7

Section 23-5 · Physics pages 3724–3725

Question 7 Surface pressure requires removing a patch from its own field A small patch on a conductor in electrostatic equilibrium has surface density σ. Locally the field just outside is σˆn/ϵ0. Model the patch self-field as σˆn/(2ϵ0) just outside; the remaining field is due to the other charges. Upper conducting hemisphere; arrows show outward electrostatic pressure. (a) Derive the outward electric force per unit area on the patch and show that its direction is independent of the sign of σ. (b) For an isolated spherical conductor of radius R and charge Q, integrate the z component of this pressure over its upper hemisphere to find the separating force on that hemisphere.
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Question 7 - Solution Surface pressure requires removing a patch from its own field (a) Method and calculation Eother = σ ϵ0 ˆn −σ 2ϵ0 ˆn = σ 2ϵ0 ˆn. dF dA = σEother = σ2 2ϵ0 ˆn, Pe = ϵ0E2 s 2 . (b) Interpretation and further calculation Fz = Pe ∫ hemisphere cos θ dA = PeπR2. σ = Q 4πR2 ⇒Fz = Q2 32πϵ0R2 . The vector force integral uses projected area, not the full hemisphere area. Physical check A charge patch cannot exert a net force on itself; using the full exterior field would give twice the correct local pressure.

Question 7

Surface pressure requires removing a patch from its own field

A small patch on a conductor in electrostatic equilibrium has surface density σ\sigma. Locally the field just outside is σ𝒏̂/ϵ0\sigma\hat{\mathbf n}/\epsilon_0. Model the patch self-field as σ𝒏̂/(2ϵ0)\sigma\hat{\mathbf n}/(2\epsilon_0) just outside; the remaining field is due to the other charges.

Diagram shown in the original SVG worksheet.

  1. Derive the outward electric force per unit area on the patch and show that its direction is independent of the sign of σ\sigma.

  2. For an isolated spherical conductor of radius R and charge Q, integrate the z component of this pressure over its upper hemisphere to find the separating force on that hemisphere.

Question 7 - Solution

Surface pressure requires removing a patch from its own field

Diagram shown in the original SVG worksheet.

(a) Method and calculation

𝑬other=σϵ0𝒏̂−σ2ϵ0𝒏̂=σ2ϵ0𝒏̂.\mathbf E_{\mathrm{other}}=\frac{\sigma}{\epsilon_0}\hat{\mathbf n}-\frac{\sigma}{2\epsilon_0}\hat{\mathbf n}=\frac{\sigma}{2\epsilon_0}\hat{\mathbf n}.d𝑭dA=σ𝑬other=σ22ϵ0𝒏̂,Pe=ϵ0Es22.\frac{d\mathbf F}{dA}=\sigma\mathbf E_{\mathrm{other}}=\frac{\sigma^2}{2\epsilon_0}\hat{\mathbf n},\quad P_e=\frac{\epsilon_0E_s^2}{2}.

(b) Interpretation and further calculation

Fz=Pe∫hemispherecos⁡θdA=PeπR2.F_z=P_e\int_{\mathrm{hemisphere}}\cos\theta\,dA=P_e\pi R^2.σ=Q4πR2⇒Fz=Q232πϵ0R2.\sigma=\frac Q{4\pi R^2}\Rightarrow F_z=\frac{Q^2}{32\pi\epsilon_0R^2}.The vector force integral uses projected area, not the full hemisphere area.

Physical check

A charge patch cannot exert a net force on itself; using the full exterior field would give twice the correct local pressure.