Applying Gauss' Law: Planar Symmetry — Question 10

Section 23-7 · Physics pages 3770–3771

Question 10 A neutral three-sheet trap produces oscillations with an amplitude-dependent period Three infinite, ideal permeable charge sheets at x = 0, d, 2d carry +σ, −2σ, +σ, with σ > 0. A weak particle of charge q > 0 and mass m starts at rest at x = d −A, with 0 < A < d. Ignore collisions with the ideal sheets and all other forces. +σ −2σ +σ x = d Schematic; labels, not drawing lengths, specify the data. (a) Find the field in the two interior gaps and show that the particle accelerates toward x = d on either side. (b) Find the oscillation period and its dependence on A. Compare with amplitude-independent harmonic motion.
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Question 10 - Solution A neutral three-sheet trap produces oscillations with an amplitude-dependent period +σ −2σ +σ x = d (a) Method and calculation Ex = +σ/ϵ0 (0 < x < d), Ex = −σ/ϵ0 (d < x < 2d). a0 = qσ mϵ0 , ¨x = −a0 sgn(x −d). (b) Interpretation and further calculation A = 1 2a0t2 q ⇒tq = √ 2A/a0. T = 4tq = 4 √ 2Amϵ0 qσ ∝ √ A. The speed is continuous when acceleration reverses at the central ideal sheet; the particle turns at d + A and returns symmetrically. Physical check The acceleration is piecewise constant rather than proportional to displacement, so this motion is periodic but not simple harmonic.

Question 10

A neutral three-sheet trap produces oscillations with an amplitude-dependent period

Three infinite, ideal permeable charge sheets at x=0,d,2dx=0,d,2d carry +σ,−2σ,+σ+\sigma,-2\sigma,+\sigma, with σ>0\sigma>0. A weak particle of charge q>0q>0 and mass m starts at rest at x=d−Ax=d-A, with 0<A<d0<A<d. Ignore collisions with the ideal sheets and all other forces.

Diagram shown in the original SVG worksheet.

  1. Find the field in the two interior gaps and show that the particle accelerates toward x=dx=d on either side.

  2. Find the oscillation period and its dependence on A. Compare with amplitude-independent harmonic motion.

Question 10 - Solution

A neutral three-sheet trap produces oscillations with an amplitude-dependent period

Diagram shown in the original SVG worksheet.

(a) Method and calculation

Ex=+σ/ϵ0(0<x<d),Ex=−σ/ϵ0(d<x<2d).E_x=+\sigma/\epsilon_0\quad(0<x<d),\qquad E_x=-\sigma/\epsilon_0\quad(d<x<2d).a0=qσmϵ0,ẍ=−a0sgn⁡(x−d).a_0=\frac{q\sigma}{m\epsilon_0},\quad\ddot x=-a_0\operatorname{sgn}(x-d).

(b) Interpretation and further calculation

A=12a0tq2⇒tq=2A/a0.A=\tfrac12a_0t_q^2\Rightarrow t_q=\sqrt{2A/a_0}.T=4tq=42Amϵ0qσ∝A.T=4t_q=4\sqrt{\frac{2Am\epsilon_0}{q\sigma}}\propto\sqrt A.The speed is continuous when acceleration reverses at the central ideal sheet; the particle turns at d+Ad+A and returns symmetrically.

Physical check

The acceleration is piecewise constant rather than proportional to displacement, so this motion is periodic but not simple harmonic.