The Rotational Variables — Question 4

Section 10-1 · Physics pages 1378–1379

Question 4 Average acceleration does not require constant acceleration A rotor has ω(t) = 2 + t2 rad/s for SI numerical t between 0 and 3 s. t ω 3 The dashed endpoint chord lies above the curved angular-velocity trace. (a) Find average angular acceleration and the time when instantaneous acceleration equals that average. (b) Find angular displacement and compare with the trapezoidal average of endpoint angular velocities.
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Question 4 - Solution Average acceleration does not require constant acceleration t ω 3 (a) Derivation and calculation Use the endpoint difference for the average and the derivative for the instantaneous value: ¯α = ω(3) −ω(0) 3 = 11 −2 3 = 3 rad/s2 . α(t) = 2t, 2t = 3 =⇒ t = 1.5 s . (b) Result and interpretation The exact angular displacement is the area under the curve: ∆θ = ∫3 0 (2 + t2) dt = [ 2t + t3 3 ]3 0 = 15 rad . ∆θtrap = 2 + 11 2 (3) = 19.5 rad, ∆θtrap −∆θ = 4.5 rad. Endpoint averaging requires a linear velocity history; this curve is quadratic. Physical check The convex velocity curve lies below its endpoint chord, so the trapezoidal estimate is too large.

Question 4

Average acceleration does not require constant acceleration

A rotor has ω(t)=2+t2rad/s\omega(t)=2+t^2\,\mathrm{rad/s} for SI numerical tt between 00 and 3s3\,\mathrm s.

Diagram shown in the original SVG worksheet.

  1. Find average angular acceleration and the time when instantaneous acceleration equals that average.

  2. Find angular displacement and compare with the trapezoidal average of endpoint angular velocities.

Question 4 - Solution

Average acceleration does not require constant acceleration

Diagram shown in the original SVG worksheet.

(a) Derivation and calculation

Use the endpoint difference for the average and the derivative for the instantaneous value: α‾=ω(3)−ω(0)3=11−23=3rad/s2.\bar\alpha=\frac{\omega(3)-\omega(0)}{3} =\frac{11-2}{3}=\boxed{3\ \mathrm{rad/s^2}}. α(t)=2t,2t=3⇒t=1.5s.\alpha(t)=2t,\qquad 2t=3\quad\Longrightarrow\quad\boxed{t=1.5\ \mathrm s}.

(b) Result and interpretation

The exact angular displacement is the area under the curve: Δθ=∫03(2+t2)dt=[2t+t33]03=15rad.\Delta\theta=\int_0^3(2+t^2)\,dt =\left[2t+\frac{t^3}{3}\right]_0^3=\boxed{15\ \mathrm{rad}}. Δθtrap=2+112(3)=19.5rad,Δθtrap−Δθ=4.5rad.\Delta\theta_{\mathrm{trap}}=\frac{2+11}{2}(3)=19.5\ \mathrm{rad},\qquad \Delta\theta_{\mathrm{trap}}-\Delta\theta=4.5\ \mathrm{rad}. Endpoint averaging requires a linear velocity history; this curve is quadratic.

Physical check

The convex velocity curve lies below its endpoint chord, so the trapezoidal estimate is too large.