The Wave Equation — Question 7

Section 16-7 · Physics pages 2524–2525

Question 7 A localized initial kick can leave a displaced plateau An infinite string starts flat: h(x) = 0. Its initial velocity is g(x) = U for |x| < a and zero elsewhere. Use y(x, t) = (2v)−1 ∫x+vt x−vt g(s)ds. Ideal sharp edges may be smoothed. x g(x) = U −a a Initial velocity is a top-hat profile; initial displacement is zero. (a) Find y(0, t) for t ≥0. (b) Explain how a stationary central plateau after the pulse fronts depart is compatible with wave propagation and finite energy.
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Question 7 - Solution A localized initial kick can leave a displaced plateau x g(x) = U −a a Method and mathematical working With zero initial displacement, only the integral of initial velocity remains. At the center, its integration interval overlaps a length that grows until it covers the entire nonzero interval. y(0, t) = U 2v 2 min(vt, a) = { Ut, vt < a, Ua/v, vt ≥a. vt > a : y(0, t) = Ua/v, yt(0, t) = 0, yx(0, t) = 0 ⇒u(0, t) = 0. (a) Calculation and conclusion For vt < a, the integration interval has length 2vt inside the kicked region, so y(0, t) = Ut. For vt ≥a, it contains all the initial kick, giving y(0, t) = Ua/v. The central displacement stops changing after a/v. (b) Interpretation and limits The advancing transition regions carry slope and velocity; a constant plateau has neither. Thus the ideal transverse-string energy density vanishes inside the plateau even though its displacement is nonzero. The disturbance propagates through moving fronts, not by every point oscillating forever. Physical check After the fronts pass, the central plateau has zero slope and zero velocity. Nonzero displacement alone does not require nonzero local elastic or kinetic energy.

Question 7

A localized initial kick can leave a displaced plateau

An infinite string starts flat: h(x)=0h(x)=0. Its initial velocity is g(x)=Ug(x)=U for |x|<a|x|<a and zero elsewhere. Use y(x,t)=(2v)−1∫x−vtx+vtg(s)dsy(x,t)=(2v)^{-1}\int_{x-vt}^{x+vt}g(s)ds. Ideal sharp edges may be smoothed.

Diagram shown in the original SVG worksheet.

  1. Find y(0,t)y(0,t) for t≥0t\ge0.

  2. Explain how a stationary central plateau after the pulse fronts depart is compatible with wave propagation and finite energy.

Question 7 - Solution

A localized initial kick can leave a displaced plateau

Diagram shown in the original SVG worksheet.

Method and mathematical working

With zero initial displacement, only the integral of initial velocity remains. At the center, its integration interval overlaps a length that grows until it covers the entire nonzero interval.y(0,t)=U2v2min⁡(vt,a)={Ut,vt<a,Ua/v,vt≥a.vt>a:y(0,t)=Ua/v,yt(0,t)=0,yx(0,t)=0⇒u(0,t)=0.\begin{aligned}y(0,t)&=\frac{U}{2v}\,2\min(vt,a)\\&=\begin{cases}Ut,&vt<a,\\Ua/v,&vt\ge a.\end{cases}\\[4pt]vt>a&:\quad y(0,t)=Ua/v,\quad y_t(0,t)=0,\quad y_x(0,t)=0\Rightarrow u(0,t)=0.\end{aligned}

(a) Calculation and conclusion

For vt<avt<a, the integration interval has length 2vt2vt inside the kicked region, so y(0,t)=Uty(0,t)=Ut. For vt≥avt\ge a, it contains all the initial kick, giving y(0,t)=Ua/vy(0,t)=Ua/v. The central displacement stops changing after a/va/v.

(b) Interpretation and limits

The advancing transition regions carry slope and velocity; a constant plateau has neither. Thus the ideal transverse-string energy density vanishes inside the plateau even though its displacement is nonzero. The disturbance propagates through moving fronts, not by every point oscillating forever.

Physical check

After the fronts pass, the central plateau has zero slope and zero velocity. Nonzero displacement alone does not require nonzero local elastic or kinetic energy.