The Speed of a Traveling Wave — Question 9

Section 16-4 · Physics pages 2468–2469

Question 9 A moving phase need not translate at a uniform speed For x > 0, consider y = A cos(ax2 −ωt), with a, ω > 0. This is a prescribed field, not assumed to solve a uniform-string wave equation. x q At one instant, the oscillations become more closely spaced as position increases. (a) Find the local velocity of a fixed-phase feature. (b) Find the feature position as a function of time from x(0) = x0. Explain why writing one global wavelength is inappropriate.
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Question 9 - Solution A moving phase need not translate at a uniform speed x q Method and mathematical working Differentiate the full position-dependent phase along a trajectory. Integrate the resulting first-order equation using the given initial position. 2ax ˙x = ω, d(x2) dt = ω a , x2 = x2 0 + ωt a . x(t) = √ x2 0 + (ω/a)t, ¨x = −ω2 4a2x3 < 0. (a) Calculation and conclusion Constant phase gives 2ax dx/dt −ω = 0, so cphase(x) = ω/(2ax). The local spatial phase gradient is 2ax, not a constant wave number. (b) Interpretation and limits x(t) = √ x2 0 + (ω/a)t. The feature slows as x grows. Exact adjacent-phase locations satisfy a(x2 2 −x2 1) = 2π, so their spacing depends on position; 2π/(2ax) is a local phase-length scale, not a global repeat distance. Physical check Differentiating the resulting square-root trajectory returns ω/(2ax). The derivation is restricted to x > 0; it does not assign a finite uniform speed at the origin.

Question 9

A moving phase need not translate at a uniform speed

For x>0x>0, consider y=Acos⁡(ax2−ωt)y=A\cos(ax^2-\omega t), with a,ω>0a,\omega>0. This is a prescribed field, not assumed to solve a uniform-string wave equation.

Diagram shown in the original SVG worksheet.

  1. Find the local velocity of a fixed-phase feature.

  2. Find the feature position as a function of time from x(0)=x0x(0)=x_0. Explain why writing one global wavelength is inappropriate.

Question 9 - Solution

A moving phase need not translate at a uniform speed

Diagram shown in the original SVG worksheet.

Method and mathematical working

Differentiate the full position-dependent phase along a trajectory. Integrate the resulting first-order equation using the given initial position.2axẋ=ω,d(x2)dt=ωa,x2=x02+ωta.x(t)=x02+(ω/a)t,ẍ=−ω24a2x3<0.\begin{aligned}2ax\dot x&=\omega,\\\frac{d(x^2)}{dt}&=\frac{\omega}{a},\qquad x^2=x_0^2+\frac{\omega t}{a}.\\[4pt]x(t)&=\sqrt{x_0^2+(\omega/a)t},\qquad \ddot x=-\frac{\omega^2}{4a^2x^3}<0.\end{aligned}

(a) Calculation and conclusion

Constant phase gives 2axdx/dt−ω=02ax\,dx/dt-\omega=0, so cphase(x)=ω/(2ax)c_{\mathrm{phase}}(x)=\omega/(2ax). The local spatial phase gradient is 2ax2ax, not a constant wave number.

(b) Interpretation and limits

x(t)=x02+(ω/a)tx(t)=\sqrt{x_0^2+(\omega/a)t}. The feature slows as xx grows. Exact adjacent-phase locations satisfy a(x22−x12)=2πa(x_2^2-x_1^2)=2\pi, so their spacing depends on position; 2π/(2ax)2\pi/(2ax) is a local phase-length scale, not a global repeat distance.

Physical check

Differentiating the resulting square-root trajectory returns ω/(2ax)\omega/(2ax). The derivation is restricted to x>0x>0; it does not assign a finite uniform speed at the origin.