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Square-Root Speed, Quadratic Position

Irodov 1.22DifficultyDifficulty 3 of 5UniquenessUniqueness 3 of 5

Problem Irodov 1.22

A particle moves along the positive xx axis with its speed set by its own position, v=αxv=\alpha\sqrt{x}, where α\alpha is a positive constant. At t=0t=0 the particle sits at x=0x=0. Find:

  1. the velocity v(t)v(t) and the acceleration w(t)w(t) as functions of time

  2. the mean velocity ⟨v⟩\langle v\rangle, averaged over the time taken to cover the first ss meters of the path

Given
  • v=αxv=\alpha\sqrt{x}
  • x(0)=0x(0)=0 at t=0t=0
Find
(a) v(t)v(t), w(t)w(t); (b) ⟨v⟩\langle v\rangle over the first ss meters

Solution

Step 1Separate variables and integrate to find x(t)x(t)

The velocity dx/dtdx/dt is given only as a function of xx, so the equation separates directly into xx and tt; integrating both sides from the start, x=0x=0 at t=0t=0, to a general instant fixes x(t)x(t).

dxdt=αx  ⟹  ∫0xdx′x′=∫0tα dt′\frac{dx}{dt} = \alpha\sqrt{x} \;\Longrightarrow\; \int_0^{x} \frac{dx'}{\sqrt{x'}} = \int_0^{t} \alpha\,dt'
2x=αtx=α2t24\begin{align*}2\sqrt{x} &= \alpha t \\ x &= \frac{\alpha^2 t^2}{4}\end{align*}
x(t)=α2t24x(t) = \dfrac{\alpha^2 t^2}{4}
(1)
Step 2Differentiate for the velocity and the acceleration

With x(t)x(t) in hand (1), the velocity and acceleration follow by straightforward differentiation.

v(t)=dxdt=ddt(α2t24)v(t) = \frac{dx}{dt} = \frac{d}{dt}\left(\frac{\alpha^2 t^2}{4}\right)
v(t)=α2t2v(t) = \dfrac{\alpha^2 t}{2}
(2)
w(t)=dvdt=ddt(α2t2)w(t) = \frac{dv}{dt} = \frac{d}{dt}\left(\frac{\alpha^2 t}{2}\right)
w(t)=α22w(t) = \dfrac{\alpha^2}{2}
(3)

so the particle moves with constant acceleration even though its speed was only ever given as a function of position, never of time.

Step 3Mean velocity over the first ss meters

Setting x(ts)=sx(t_s)=s in (1) and solving for tst_s,

s=α2ts24  ⟹  ts=2sα.s = \frac{\alpha^2 t_s^2}{4} \;\Longrightarrow\; t_s = \frac{2\sqrt{s}}{\alpha}.

The mean velocity is the distance ss divided by this time,

⟨v⟩=sts=s2s/α\begin{align*}\langle v\rangle &= \frac{s}{t_s} \\ &= \frac{s}{2\sqrt{s}/\alpha}\end{align*}
⟨v⟩=αs2\langle v\rangle = \dfrac{\alpha\sqrt{s}}{2}
(4)

the slope of the chord OPOP drawn below.

The position x(t) of , a parabola through the origin. The point P is where the particle has covered the distance s, at t_s=2 s/α; the chord OP has slope s/t_s, the mean velocity.

The position x(t)x(t) of (1), a parabola through the origin. The point PP is where the particle has covered the distance ss, at ts=2s/αt_s=2\sqrt s/\alpha; the chord OPOP has slope s/tss/t_s, the mean velocity.

Check

Substituting x(t)x(t) from (1) back into αx\alpha\sqrt{x} reproduces v(t)v(t) exactly: αα2t2/4=α⋅(αt/2)=α2t/2\alpha\sqrt{\alpha^2t^2/4} = \alpha\cdot(\alpha t/2) = \alpha^2 t/2, matching Step 2, since t≥0t\geq0 keeps the square root’s sign consistent. And ⟨v⟩→0\langle v\rangle\to0 as s→0s\to0, as it must for a particle starting from rest.

Remark

A speed proportional to x\sqrt{x}, starting from rest at x=0x=0, always integrates to uniformly accelerated motion: this is the same x∝t2x\propto t^2 law a body dropped from rest obeys, with w=α2/2w=\alpha^2/2 standing in for gg. The unusual part of the problem, a velocity law given in xx rather than tt, was really just uniform acceleration wearing a disguise.