A Ball on a String, Seen Edge-On

You already have the equation of simple harmonic motion, x(t)=Acos(ωt+ϕ)x(t) = A\cos(\omega t + \phi). This section gives you a picture of it — and the picture is worth having, because a whole family of questions that are ugly with a calculator become one line of geometry once you can draw it.

Here is the experiment. Tie a small ball to a string and whirl it in a horizontal circle at a steady rate, so it is in uniform circular motion. Now crouch down until your eye is level with the plane of the circle, and look at the ball edge-on. You no longer see a circle at all: you see the ball sliding to and fro along a straight line, fastest in the middle, slowing to a stop at each end, then coming back. Shine a light on it from the side instead and its shadow on the wall does exactly the same thing.

What you are watching is the ball's projection onto one diameter of the circle. And that projection is not merely "something like" an oscillation. It is simple harmonic motion, exactly.

The mathematics behind the shadow

Let a particle PP move anticlockwise round a circle of radius AA centred at the origin, with a constant angular speed ω\omega. At t=0t = 0 let the radius OPOP make an angle ϕ\phi with the positive xx-axis.

In a time tt the radius sweeps through a further angle ωt\omega t, because the angular speed is constant. So at time tt the radius makes an angle ωt+ϕ\omega t + \phi with the positive xx-axis. Drop a perpendicular from PP onto the xx-axis and call its foot PP^{\prime}. Straight from the definition of the cosine, the xx-coordinate of PP — which is the position of PP^{\prime} — is x(t)=Acos(ωt+ϕ)x(t) = A\cos(\omega t + \phi)

That is the defining equation of SHM, arrived at with no calculus and no dynamics, purely by dropping a perpendicular.

Key Point — the reference circle: If a particle PP moves uniformly on a circle of radius AA with angular speed ω\omega, then its projection PP^{\prime} on any diameter of that circle performs simple harmonic motion of amplitude AA and angular frequency ω\omega. PP is called the reference particle and its circular path the reference circle.

Reference circle with phase constant, swept angle and the projection on the x-axis

The other diameter gives a sine

Nothing forced us to project onto the xx-axis. Project the same motion onto the yy-axis and the yy-coordinate of PP is y(t)=Asin(ωt+ϕ)y(t) = A\sin(\omega t + \phi) which is simple harmonic too, with the same amplitude and the same angular frequency, differing from the first only by a phase of π2\dfrac{\pi}{2}. One circular motion therefore contains two simple harmonic motions at right angles, a quarter cycle apart — a fact this section returns to at the end.

One warning, and it is examined

Key Point: Uniform circular motion is not simple harmonic motion. SHM is a to-and-fro motion along a straight line; the reference particle goes round and round and never reverses. What is simple harmonic is the projection, the shadow, not the particle itself.

The forces are different too. Keeping PP on the circle needs a centripetal force of constant magnitude, always pointing at the centre. Driving PP^{\prime} along the diameter needs a force that reverses direction every half cycle and vanishes at the middle. Two very different physical situations that share one piece of geometry.

[Board Important] "Show that the projection of a uniform circular motion on a diameter is simple harmonic" is a standard three-marker. The full answer is the four lines above: draw the circle, state that the angle at time tt is ωt+ϕ\omega t + \phi, project, and quote x=Acos(ωt+ϕ)x = A\cos(\omega t + \phi) as the definition of SHM.

Everything Read Off the Picture

The reference circle is useful because every symbol in x=Acos(ωt+ϕ)x = A\cos(\omega t + \phi) is something you can point at on the diagram. Learn this dictionary and half the section is done.

In the equation On the reference circle
amplitude AA the radius of the circle
angular frequency ω\omega the angular speed of the reference particle, in rad/s
phase (ωt+ϕ)(\omega t + \phi) the angle the radius OPOP makes with the +x+x axis at time tt
phase constant ϕ\phi the starting angle, the angle OPOP made at t=0t = 0
displacement xx the foot of the perpendicular from PP to the xx-axis
period TT the time for one complete revolution
one full oscillation one full trip round the circle, worth 2π2\pi of angle

The third row is the one to hold on to.

Key Point: The angle swept is the phase. Not something proportional to it, not something like it — the angle the radius vector makes with the +x+x axis, measured in radians, is the phase (ωt+ϕ)(\omega t + \phi). The starting angle is the phase constant ϕ\phi.

Because one revolution is one oscillation, the circle and the oscillation share their timing exactly: ω=2πT=2πν\omega = \frac{2\pi}{T} = 2\pi\nu with ω\omega in radians per second and the frequency ν\nu in hertz. The reference particle goes round ν\nu times a second, and the shadow completes ν\nu oscillations a second — the same number.

Circle positions connected by horizontal lines to the matching points of a cosine curve

Steady round the circle, anything but steady along the line

Look at the picture again. The reference particle covers equal angles in equal times — it never speeds up or slows down. Its shadow does nothing of the sort. Near the middle of the diameter the shadow races across; near either end it barely moves, stops, and turns.

The reason is pure geometry: when PP is near the top or bottom of the circle it is moving almost horizontally, so its shadow moves fast; when PP is near the left or right edge it is moving almost vertically, so the shadow hardly moves at all. That single observation is the engine behind everything in the rest of this section.

Two visits per revolution

Every value of xx strictly between A-A and +A+A corresponds to two points on the circle — one above the xx-axis, one below, at angles θ\theta and θ-\theta. So the shadow passes through each displacement twice per cycle, and the two visits are distinguished by the direction of travel:

  • PP in the upper half of the circle \Longrightarrow PP is moving leftwards \Longrightarrow the shadow is moving in the x-x direction
  • PP in the lower half \Longrightarrow the shadow is moving in the +x+x direction

(with the anticlockwise sense assumed throughout). Only x=+Ax = +A and x=Ax = -A are visited once, at the two ends of the horizontal diameter, and those are precisely the instants when the shadow is momentarily at rest.

Where the velocity and acceleration come from

The reference particle has a speed ωA\omega A along the tangent and a centripetal acceleration ω2A\omega^2 A pointing at the centre. Project each of those two vectors on the xx-axis and you get exactly the velocity and the acceleration of the shadow — the same vv and aa that the next section obtains by differentiating x=Acos(ωt+ϕ)x = A\cos(\omega t + \phi) twice. It is worth knowing that the two routes agree; the differentiation itself, and everything that follows from it, belongs to that section.

[NEET Important] A question that says "a particle moves on a circle of radius rr with angular speed ω\omega; find the amplitude and period of the motion of its projection" is asking for nothing more than A=rA = r and T=2πωT = \dfrac{2\pi}{\omega}. Read the radius, read the angular speed, and you are finished.

Drawing the Circle Both Ways

Two skills, and exam questions come in both directions.

Given the SHM, draw the circle

You are handed x=Acos(ωt+ϕ)x = A\cos(\omega t + \phi) and asked to draw its reference circle.

  1. Draw a circle of radius AA centred on the mean position, with the xx-axis along the direction of the actual oscillation.
  2. Mark the starting radius at the angle ϕ\phi, measured anticlockwise from the +x+x axis. (A negative ϕ\phi therefore lands below the axis.)
  3. Put an anticlockwise arrow on the circle, with the particle going round at ω\omega radians per second.
  4. Drop the perpendicular from the starting point to the xx-axis. Where it lands is x(0)=Acosϕx(0) = A\cos\phi, the displacement at the moment the clock started.

For x=4cos(2t+π3)x = 4\cos\left(2t + \dfrac{\pi}{3}\right) centimetres, that is a circle of radius 4 cm, the reference particle starting at 60°60° above the +x+x axis and going anticlockwise at 2 rad/s, with the shadow starting at 4cos60°=24\cos 60° = 2 cm.

Given the circle, write the SHM

Now the reverse. You are shown a circle with a radius, a period, a starting position and — crucially — an arrow showing the sense of rotation. Four steps:

  1. Amplitude: AA is the radius.
  2. Angular frequency: ω=2πT\omega = \dfrac{2\pi}{T}, in rad/s, from the period marked on the figure.
  3. Starting angle: measure the angle θ0\theta_0 that the initial radius makes with the +x+x axis, taking anticlockwise as positive.
  4. Sense of rotation: this fixes the sign, and it is where marks are lost.

Key Point — the sign of ϕ\phi from the sense of rotation:

  • Anticlockwise: the angle increases, so at time tt it is θ0+ωt\theta_0 + \omega t, and x=Acos(ωt+θ0)ϕ=+θ0x = A\cos(\omega t + \theta_0) \qquad \Longrightarrow \qquad \phi = +\theta_0
  • Clockwise: the angle decreases, so at time tt it is θ0ωt\theta_0 - \omega t, and x=Acos(θ0ωt)=Acos(ωtθ0)ϕ=θ0x = A\cos(\theta_0 - \omega t) = A\cos(\omega t - \theta_0) \qquad \Longrightarrow \qquad \phi = -\theta_0 The second step uses cos(α)=cosα\cos(-\alpha) = \cos\alpha, which is why a clockwise diagram can still be written in the standard form with nothing worse than a sign change.

The four starting positions everybody should recognise instantly, all anticlockwise:

Reference particle starts at θ0\theta_0 ϕ\phi The SHM
the +x+x axis 00 00 x=Acosωtx = A\cos\omega t
the +y+y axis (top) π2\dfrac{\pi}{2} +π2+\dfrac{\pi}{2} x=Asinωtx = -A\sin\omega t
the x-x axis π\pi π\pi x=Acosωtx = -A\cos\omega t
the y-y axis (bottom) π2-\dfrac{\pi}{2} π2-\dfrac{\pi}{2} x=Asinωtx = A\sin\omega t

The direction check, done on the picture

The circle also settles the sign of ϕ\phi when you are told where the particle is and which way it is going, rather than being shown a diagram:

  • shadow starting at the mean position and heading towards +A+A \Longrightarrow the reference particle starts at the bottom of the circle \Longrightarrow ϕ=π2\phi = -\dfrac{\pi}{2}
  • shadow starting at the mean position and heading towards A-A \Longrightarrow it starts at the top \Longrightarrow ϕ=+π2\phi = +\dfrac{\pi}{2}
  • shadow starting at x=+Ax = +A, momentarily at rest \Longrightarrow it starts on the +x+x axis \Longrightarrow ϕ=0\phi = 0

[JEE Tip] A clockwise figure is not a different kind of problem. Read off θ0\theta_0 exactly as you would for an anticlockwise one, then write ϕ=θ0\phi = -\theta_0 and carry on. Every other quantity — amplitude, period, frequency, the displacement at any instant — is unaffected by the sense of rotation.

The Time Between Two Displacements

This is what the reference circle is really for.

The question. A particle in SHM of amplitude AA and period TT moves from displacement x1x_1 to displacement x2x_2. How long does it take?

The algebraic route is to solve Acos(ωt1+ϕ)=x1A\cos(\omega t_1 + \phi) = x_1 and Acos(ωt2+ϕ)=x2A\cos(\omega t_2 + \phi) = x_2, worry about which of the two solutions of each inverse cosine you want, and subtract. It is slow and it invites sign errors.

The circle route is one line, because of a single fact: the reference particle covers equal angles in equal times. So the time taken is just the fraction of a revolution that the radius vector turns through.

Key Point — time from angle: t=angle sweptω=angle swept in degrees360°Tt = \frac{\text{angle swept}}{\omega} = \frac{\text{angle swept in degrees}}{360°}\,T and the angle belonging to a displacement xx is the angle its radius makes with the +x+x axis, θ=cos1 ⁣(xA)\theta = \cos^{-1}\!\left(\frac{x}{A}\right) measured from 00 at x=+Ax = +A, through 90°90° at the mean position, to 180°180° at x=Ax = -A.

The method, in four steps

  1. Draw the circle of radius AA and mark the two displacements x1x_1 and x2x_2 on the horizontal diameter.
  2. Draw the vertical lines through them; where each cuts the circle is the reference particle's position.
  3. Find the angle between the two radii, using θ=cos1(xA)\theta = \cos^{-1}\left(\dfrac{x}{A}\right) for each.
  4. Divide by ω\omega, or take that fraction of 360°360° and multiply by TT.

Circle wedges of sixty and thirty degrees beside the same intervals under a cosine

The standard results, worth memorising

Every one of these is for a particle moving directly between the two displacements, with no reversal in between.

Journey Angles swept Time
0A20 \to \dfrac{A}{2} 90°60°90° \to 60°, i.e. 30°30° T12\dfrac{T}{12}
A2A\dfrac{A}{2} \to A 60°0°60° \to 0°, i.e. 60°60° T6\dfrac{T}{6}
0A20 \to \dfrac{A}{\sqrt{2}} 90°45°90° \to 45°, i.e. 45°45° T8\dfrac{T}{8}
03A20 \to \dfrac{\sqrt{3}A}{2} 90°30°90° \to 30°, i.e. 60°60° T6\dfrac{T}{6}
3A2A\dfrac{\sqrt{3}A}{2} \to A 30°0°30° \to 0°, i.e. 30°30° T12\dfrac{T}{12}
A2+A2-\dfrac{A}{2} \to +\dfrac{A}{2} 120°60°120° \to 60°, i.e. 60°60° T6\dfrac{T}{6}
mean position \to either extreme 90°90° T4\dfrac{T}{4}
extreme \to extreme 180°180° T2\dfrac{T}{2}

Two consistency checks you can do in your head: T12+T6=T4\dfrac{T}{12} + \dfrac{T}{6} = \dfrac{T}{4}, which is the mean position to the extreme; and T8+T8=T4\dfrac{T}{8} + \dfrac{T}{8} = \dfrac{T}{4} as well, going by way of A2\dfrac{A}{\sqrt{2}}.

The trap this table exists to defeat

Key Point: Equal distances are not equal times. The inner half of the journey, from the mean position out to A2\dfrac{A}{2}, takes T12\dfrac{T}{12}. The outer half, from A2\dfrac{A}{2} to AA, takes T6\dfrac{T}{6}twice as long, over exactly the same distance. The particle is slowing down as it approaches the extreme.

Anyone who answers "half the distance, so half the time" gets these questions wrong every time. Time is proportional to the angle, never to the displacement.

Where the particle spends its time

The same idea answers a favourite question: what fraction of each cycle does the particle spend within A2\dfrac{A}{2} of the centre?

On the circle, xA2\lvert x \rvert \le \dfrac{A}{2} means the radius lies between 60°60° and 120°120°, or between 240°240° and 300°300° — two arcs of 60°60° each, 120°120° out of 360°360°. So the particle is in the middle half of its range for only T3\dfrac{T}{3} of every period, and in the two outer quarters for 2T3\dfrac{2T}{3}. Equal lengths, twice the time.

[JEE Tip] The answer is the angle actually swept, so the direction of travel matters as much as the two displacements. A particle at +A2+\dfrac{A}{2} that is heading towards the mean position reaches +A+A only after going all the way out to A-A and back — 300°300° of arc, or 5T6\dfrac{5T}{6} — while one already heading outwards gets there in T6\dfrac{T}{6}. Same two displacements, five times the wait.

Two Perpendicular Simple Harmonic Motions

We finish by running the whole argument backwards. If a circular motion contains two perpendicular simple harmonic motions, what happens if you start with two perpendicular SHMs and combine them?

Let a particle be given one simple harmonic motion along xx and another along yy, of the same angular frequency: x=Acosωt,y=Bcos(ωt+δ)x = A\cos\omega t, \qquad y = B\cos(\omega t + \delta) where δ\delta is the constant phase difference between them. Both motions have the same period, so the particle retraces its path once every TT. What that path is depends on δ\delta and on the ratio of the amplitudes — and on nothing else.

Six paths for phase differences zero to pi including line, ellipse and circle

The three cases that matter

δ=0\delta = 0 — a straight line. With no phase difference, y=BAxy = \dfrac{B}{A}x at every instant. The particle moves back and forth along a straight line through the origin of slope BA\dfrac{B}{A}, and that motion is itself simple harmonic, of amplitude A2+B2\sqrt{A^2 + B^2}.

δ=π\delta = \pi — the other straight line. Now y=BAxy = -\dfrac{B}{A}x: the same thing with the line sloping the other way.

δ=π2\delta = \dfrac{\pi}{2} with A=BA = B — a circle. Here x=Acosωtx = A\cos\omega t and y=Acos(ωt+π2)=Asinωty = A\cos\left(\omega t + \dfrac{\pi}{2}\right) = -A\sin\omega t, so x2+y2=A2cos2ωt+A2sin2ωt=A2x^2 + y^2 = A^2\cos^2\omega t + A^2\sin^2\omega t = A^2 a circle of radius AA, traced at constant angular speed ω\omega. This is the reference circle again, built rather than dismantled.

Key Point: Two perpendicular simple harmonic motions of equal amplitude and the same angular frequency, a quarter cycle out of step, add up to uniform circular motion. With δ=+π2\delta = +\dfrac{\pi}{2} the circle is traced clockwise, with δ=π2\delta = -\dfrac{\pi}{2} anticlockwise.

Everything in between

For any other δ\delta the path is an ellipse. Eliminating tt from the two equations gives the general result x2A2+y2B22xycosδAB=sin2δ\frac{x^2}{A^2} + \frac{y^2}{B^2} - \frac{2xy\cos\delta}{AB} = \sin^2\delta which contains all the cases at once. Put δ=0\delta = 0 or π\pi and the right-hand side vanishes, leaving a perfect square — the two straight lines. Put δ=π2\delta = \dfrac{\pi}{2} and the cross term vanishes, leaving x2A2+y2B2=1\frac{x^2}{A^2} + \frac{y^2}{B^2} = 1 an ellipse with its axes along the coordinate axes, which becomes a circle when A=BA = B. Any other δ\delta keeps the xyxy term, and the ellipse is tilted.

Phase difference δ\delta Path
00 straight line, slope +BA+\dfrac{B}{A}
between 00 and π2\dfrac{\pi}{2} tilted ellipse
π2\dfrac{\pi}{2} ellipse with axes along xx and yy; a circle if A=BA = B
between π2\dfrac{\pi}{2} and π\pi tilted ellipse, leaning the other way
π\pi straight line, slope BA-\dfrac{B}{A}

[JEE Tip] For this whole family the angular frequency of the two motions must be the same. Two perpendicular SHMs with different angular frequencies produce the much more elaborate Lissajous figures, which close into a repeating pattern only when the ratio of the frequencies is a ratio of whole numbers. Check that the two ω\omega values match before reaching for the table above.

Solved Examples

Conventions used throughout: the standard form is x=Acos(ωt+ϕ)x = A\cos(\omega t + \phi), angles are in radians with the degree equivalent given alongside where it helps, and the reference circle is drawn anticlockwise unless a question says otherwise. ω\omega is the angular frequency in rad/s and ν\nu the frequency in hertz. π=3.1416\pi = 3.1416.

Example 1: Drawing the reference circle for a given SHM

A particle moves as x=4cos(2t+π3)x = 4\cos\left(2t + \dfrac{\pi}{3}\right), with xx in centimetres and tt in seconds. Describe its reference circle completely, and state where the shadow is at t=0t = 0.

Solution:

  1. Read the three constants. Comparing with x=Acos(ωt+ϕ)x = A\cos(\omega t + \phi): A=4A = 4 cm, ω=2\omega = 2 rad/s, ϕ=π3\phi = \dfrac{\pi}{3} rad =60°= 60°.

  2. The circle. Radius =A=4= A = 4 cm, centred on the mean position.

  3. The reference particle. It goes round anticlockwise at 2 rad/s, starting at 60°60° above the +x+x axis.

  4. The timing. T=2πω=2π2=3.1416 s,ν=1T=ω2π=0.318 HzT = \frac{2\pi}{\omega} = \frac{2\pi}{2} = 3.1416 \text{ s}, \qquad \nu = \frac{1}{T} = \frac{\omega}{2\pi} = 0.318 \text{ Hz} Note the units: 2 rad/s is the angular frequency, and the frequency is 0.318 Hz — one is not the other.

  5. The shadow at t=0t = 0. Drop the perpendicular from the starting point: x(0)=4cos60°=4×0.5=2 cmx(0) = 4\cos 60° = 4 \times 0.5 = 2 \text{ cm} and since the reference particle starts in the upper half of the circle and is heading anticlockwise, the shadow is moving in the x-x direction.

Takeaway: the equation and the circle carry identical information — amplitude to radius, angular frequency to angular speed, phase constant to starting angle.

Example 2: Reading an SHM off an anticlockwise circle

A reference particle moves anticlockwise on a circle of radius 3 cm with a period of 4 s. At t=0t = 0 the radius OPOP makes an angle of 45°45° with the positive xx-axis. Obtain the SHM performed by the xx-projection.

Solution:

  1. Amplitude: A=3A = 3 cm, the radius.

  2. Angular frequency: ω=2πT=2π4=π2=1.571\omega = \dfrac{2\pi}{T} = \dfrac{2\pi}{4} = \dfrac{\pi}{2} = 1.571 rad/s, and ν=14=0.25\nu = \dfrac{1}{4} = 0.25 Hz.

  3. Starting angle: θ0=45°=π4\theta_0 = 45° = \dfrac{\pi}{4} rad.

  4. Sense: anticlockwise, so the angle increases and ϕ=+θ0\phi = +\theta_0. At time tt the radius makes an angle π2t+π4\dfrac{\pi}{2}t + \dfrac{\pi}{4}, and the projection is x(t)=3cos(πt2+π4) cmx(t) = 3\cos\left(\frac{\pi t}{2} + \frac{\pi}{4}\right) \text{ cm}

  5. Check at t=0t = 0: x(0)=3cos45°=2.12x(0) = 3\cos 45° = 2.12 cm, which is indeed where the perpendicular from a 45°45° starting point lands.

Takeaway: anticlockwise means the starting angle goes straight into the equation as ϕ\phi, sign unchanged.

Example 3: Reading an SHM off a clockwise circle

A reference particle starts on the positive yy-axis of a circle of radius 5 cm and moves clockwise with a period of 30 s. Find the SHM of its xx-projection, and state the phase constant.

Solution:

  1. Amplitude and angular frequency: A=5A = 5 cm; ω=2π30=π15=0.209\omega = \dfrac{2\pi}{30} = \dfrac{\pi}{15} = 0.209 rad/s, so ν=130=0.0333\nu = \dfrac{1}{30} = 0.0333 Hz.

  2. Starting angle: on the +y+y axis, so θ0=90°=π2\theta_0 = 90° = \dfrac{\pi}{2}.

  3. Sense: clockwise, so the angle decreases. After a time tt the radius makes an angle π2πt15\dfrac{\pi}{2} - \dfrac{\pi t}{15} with the +x+x axis, and x(t)=5cos(π2πt15)=5sin(πt15) cmx(t) = 5\cos\left(\frac{\pi}{2} - \frac{\pi t}{15}\right) = 5\sin\left(\frac{\pi t}{15}\right) \text{ cm}

  4. In standard form. Using cos(α)=cosα\cos(-\alpha) = \cos\alpha, x(t)=5cos(πt15π2) cmϕ=π2x(t) = 5\cos\left(\frac{\pi t}{15} - \frac{\pi}{2}\right) \text{ cm} \qquad \Longrightarrow \qquad \phi = -\frac{\pi}{2} The phase constant is negative, exactly as the clockwise rule promises: ϕ=θ0\phi = -\theta_0.

  5. Sanity check: x(0)=0x(0) = 0 and the shadow immediately moves towards +x+x — correct, because the reference particle starts at the top and swings clockwise towards the +x+x axis.

Takeaway: clockwise costs you nothing but a minus sign on the starting angle. The amplitude and the period do not care which way the particle goes round.

Example 4: From the mean position to half the amplitude

A particle performs SHM with amplitude 6 cm and period 2.4 s. How long does it take to travel from the mean position to a displacement of 3 cm?

Solution:

  1. Set up the circle. Radius 6 cm. The mean position is the top of the circle, at 90°90°; the displacement 3 cm sits at θ=cos1(36)=cos1(0.5)=60°\theta = \cos^{-1}\left(\frac{3}{6}\right) = \cos^{-1}(0.5) = 60°

  2. Angle swept: from 90°90° to 60°60°, that is 30°30°.

  3. Time: t=30°360°T=T12=2.412=0.2 st = \frac{30°}{360°}\,T = \frac{T}{12} = \frac{2.4}{12} = 0.2 \text{ s}

Takeaway: mean position to half the amplitude is T12\dfrac{T}{12}, whatever the amplitude — the AA cancels, because only the ratio xA\dfrac{x}{A} sets the angle.

Example 5: The two halves of the same journey

A particle in SHM of period 1.2 s starts from rest at x=+Ax = +A. Find (a) the time to reach x=A2x = \dfrac{A}{2}, (b) the further time to reach the mean position, and (c) comment on the two answers.

Solution:

(a) The particle starts at the +x+x axis, θ=0\theta = 0. It reaches A2\dfrac{A}{2} at θ=cos1(0.5)=60°\theta = \cos^{-1}(0.5) = 60°. So t1=60°360°T=T6=1.26=0.2 st_1 = \frac{60°}{360°}\,T = \frac{T}{6} = \frac{1.2}{6} = 0.2 \text{ s}

(b) From 60°60° to the mean position at 90°90° is a further 30°30°: t2=30°360°T=T12=1.212=0.1 st_2 = \frac{30°}{360°}\,T = \frac{T}{12} = \frac{1.2}{12} = 0.1 \text{ s}

(c) The two legs cover the same distance, A2\dfrac{A}{2} each, but t1t2=0.20.1=2\frac{t_1}{t_2} = \frac{0.2}{0.1} = 2 The outer leg takes twice as long, because the particle is barely moving near the extreme and fastest near the centre. As a check, t1+t2=0.3t_1 + t_2 = 0.3 s =T4= \dfrac{T}{4}, which is the quarter period from an extreme to the mean position.

Takeaway: never split a time in proportion to distance in SHM. Split the angle.

Example 6: Across the middle

A particle in SHM has a period of 0.6 s. Find the shortest time it takes to go from x=A2x = -\dfrac{A}{2} to x=+A2x = +\dfrac{A}{2}.

Solution:

  1. The two angles. x=+A2x = +\dfrac{A}{2} is at θ=cos1(0.5)=60°\theta = \cos^{-1}(0.5) = 60°, and x=A2x = -\dfrac{A}{2} is at θ=cos1(0.5)=120°\theta = \cos^{-1}(-0.5) = 120°.

  2. Angle swept, going directly: 120°60°=60°120° - 60° = 60°.

  3. Time: t=60°360°T=T6=0.66=0.1 st = \frac{60°}{360°}\,T = \frac{T}{6} = \frac{0.6}{6} = 0.1 \text{ s}

Notice that this is the same as the time from A2\dfrac{A}{2} to AA — a journey covering only half the distance. The middle stretch is crossed quickly.

Why "shortest"? Because a particle sitting at A2-\dfrac{A}{2} might instead be heading outwards, towards A-A. It would then reach +A2+\dfrac{A}{2} only after turning round at the far extreme — on the circle that is a sweep from 120°120° to 300°300°, or 180°180°, taking T2=0.3\dfrac{T}{2} = 0.3 s. The circle handles both routes without ambiguity; the direction of motion decides which one the question means.

Takeaway: the answer is the angle actually swept, divided by ω\omega. Decide the route first, then read the angle.

Example 7: Two displacements that are not standard fractions

A particle in SHM has amplitude 5 cm and period 2 s. It is at x=+3x = +3 cm and moving towards the negative side. How long does it take to reach x=4x = -4 cm?

Solution:

  1. First angle. θ1=cos1(35)=cos1(0.6)=53.13°\theta_1 = \cos^{-1}\left(\dfrac{3}{5}\right) = \cos^{-1}(0.6) = 53.13°.

  2. Second angle. θ2=cos1(45)=cos1(0.8)=143.13°\theta_2 = \cos^{-1}\left(\dfrac{-4}{5}\right) = \cos^{-1}(-0.8) = 143.13°.

  3. Angle swept. The particle is heading towards x-x, so on the circle it is climbing through the upper half and the angle increases: Δθ=143.13°53.13°=90°\Delta\theta = 143.13° - 53.13° = 90°

  4. Time. t=90°360°T=T4=24=0.5 st = \frac{90°}{360°}\,T = \frac{T}{4} = \frac{2}{4} = 0.5 \text{ s}

The two awkward numbers 3 and 4 with a 5 cm amplitude were never awkward at all: they form a 3-4-5 right triangle, and the two radii turn out to be exactly perpendicular.

Takeaway: the method does not need round numbers. Two inverse cosines, one subtraction, one division by 360°360°.

Example 8: Working backwards from a measured time

A particle in SHM takes 0.1 s to travel from one extreme position to the point where its displacement is half the amplitude. Find the period, the frequency and the angular frequency.

Solution:

  1. Identify the angle. Extreme to half amplitude is 0° to 60°60°, so 60°60° is swept.

  2. Set up the equation. 0.1=60°360°T=T6T=0.6 s0.1 = \frac{60°}{360°}\,T = \frac{T}{6} \qquad \Longrightarrow \qquad T = 0.6 \text{ s}

  3. The other two quantities, with their units. ν=1T=10.6=1.67 Hz,ω=2πν=2π0.6=10.47 rad/s\nu = \frac{1}{T} = \frac{1}{0.6} = 1.67 \text{ Hz}, \qquad \omega = 2\pi\nu = \frac{2\pi}{0.6} = 10.47 \text{ rad/s}

Quote the one the question asked for: 1.67 Hz is the frequency, 10.47 rad/s is the angular frequency, and they differ by the factor 2π2\pi.

Takeaway: any single time interval between two known displacements fixes the whole timing of the motion.

Example 9: Where does the particle spend its time?

A particle executes SHM of amplitude AA. What fraction of each period does it spend at displacements whose magnitude is less than A2\dfrac{A}{2}?

Solution:

  1. Translate to angles. x<A2\lvert x \rvert < \dfrac{A}{2} means cosθ<12\lvert \cos\theta \rvert < \dfrac{1}{2}.

  2. Find the arcs. In one revolution, cosθ\cos\theta lies between 12-\dfrac{1}{2} and +12+\dfrac{1}{2} for θ\theta between 60°60° and 120°120°, and again between 240°240° and 300°300°.

  3. Add them up. Two arcs of 60°60° each, so 120°120° out of 360°360°: fraction of the period=120°360°=13\text{fraction of the period} = \frac{120°}{360°} = \frac{1}{3}

So the particle spends T3\dfrac{T}{3} inside the middle half of its range and 2T3\dfrac{2T}{3} in the two outer quarters — even though those regions are the same total length. That is exactly why a pendulum bob photographed at equal intervals appears bunched up near the ends of its swing.

Takeaway: "what fraction of the time" questions become "what fraction of the circle" questions, and those are just arcs.

Example 10: Two perpendicular SHMs — the circular case

A particle has x=4sin2tx = 4\sin 2t and y=4cos2ty = 4\cos 2t, both in centimetres with tt in seconds. Identify the path, its size, the sense in which it is traced and the speed of the particle.

Solution:

  1. Eliminate the time. x2+y2=16sin22t+16cos22t=16x^2 + y^2 = 16\sin^2 2t + 16\cos^2 2t = 16 so the path is a circle of radius 4 cm centred on the origin.

  2. Why: the two motions have equal amplitude and the same ω=2\omega = 2 rad/s, and writing x=4cos(2tπ2)x = 4\cos\left(2t - \dfrac{\pi}{2}\right) shows the phase difference between them is exactly π2\dfrac{\pi}{2}.

  3. The sense. At t=0t = 0 the particle is at (0,4)(0, 4), the top. An instant later xx has become positive while yy has fallen slightly, so it moves to the right and down: clockwise.

  4. The speed. The angle 2t2t increases at a steady 2 rad/s, so the motion is uniform circular motion and v=ωA=2×4=8 cm/sv = \omega A = 2 \times 4 = 8 \text{ cm/s} constant in magnitude, with period T=2π2=3.14T = \dfrac{2\pi}{2} = 3.14 s.

Takeaway: equal amplitudes plus a quarter-cycle phase difference plus one common ω\omega equals uniform circular motion — the reference circle, assembled from its two shadows.

Example 11: Two perpendicular SHMs — the straight-line case

A particle has x=3cosωtx = 3\cos\omega t and y=4cosωty = 4\cos\omega t centimetres. Find the path and the amplitude of the resulting motion.

Solution:

  1. The phase difference is zero, so divide one equation by the other: yx=43y=43x\frac{y}{x} = \frac{4}{3} \qquad \Longrightarrow \qquad y = \frac{4}{3}x a straight line through the origin of slope 43\dfrac{4}{3}.

  2. The motion along that line is simple harmonic, since the distance from the origin is r=x2+y2=9cos2ωt+16cos2ωt=5cosωtr = \sqrt{x^2 + y^2} = \sqrt{9\cos^2\omega t + 16\cos^2\omega t} = 5\lvert \cos\omega t \rvert

  3. Amplitude: the particle runs from one end of the line at r=5r = 5 cm through the origin to the other end, so the amplitude is A2+B2=32+42=5 cm\sqrt{A^2 + B^2} = \sqrt{3^2 + 4^2} = 5 \text{ cm}

Takeaway: in-phase perpendicular SHMs give SHM along a slanted line, with amplitudes adding like perpendicular vectors — A2+B2\sqrt{A^2+B^2}, never A+BA + B.

Example 12: Two perpendicular SHMs — the elliptical case

A particle has x=2cosωtx = 2\cos\omega t and y=3cos(ωt+π2)y = 3\cos\left(\omega t + \dfrac{\pi}{2}\right) metres. Find the path and describe it.

Solution:

  1. Simplify the second equation. cos(θ+π2)=sinθ\cos\left(\theta + \dfrac{\pi}{2}\right) = -\sin\theta, so y=3sinωty = -3\sin\omega t.

  2. Eliminate the time. x2=cosωt,y3=sinωtx24+y29=1\frac{x}{2} = \cos\omega t, \qquad \frac{y}{3} = -\sin\omega t \qquad \Longrightarrow \qquad \frac{x^2}{4} + \frac{y^2}{9} = 1

  3. Describe it. An ellipse with its axes along the coordinate axes, semi-axis 2 m along xx and 3 m along yy. It is not a circle because the two amplitudes differ; had they been equal it would have been.

  4. The sense. At t=0t = 0 the particle is at (2,0)(2, 0) and yy is about to go negative, so it is traced clockwise, and it completes one circuit every T=2πωT = \dfrac{2\pi}{\omega}.

Takeaway: a phase difference of π2\dfrac{\pi}{2} always gives an ellipse aligned with the axes; equal amplitudes make that ellipse a circle, and any other phase difference tilts it.