Playbook
Oscillations
Simple harmonic motion, springs and pendulums. Lighter than in the early papers; time-period questions dominate.
- Questions in the bank
- 120
- q/paper in 2025–26
- 0.68
- Numeric answer
- 32%
- Notes pages
- 5
Tier: Long tail
When you’ll see it
A body moving to and fro about a mean position: an SHM equation, the period of a spring or pendulum, the energy at a displacement, or a new amplitude after a push.
How this chapter is tested
Oscillations sits in the long tail and has shrunk on the recent papers, but many of its questions ask for a number. Nearly all of it is simple harmonic motion, and almost every question comes down to two numbers, ω and the amplitude, from which a phase, a time, a speed or an energy follows in a line or two.
The harder step is finding ω for a new set-up: a cut spring, a block between two springs, two free masses, a physical pendulum, a lift, a height above the earth. Write the restoring force per unit displacement, divide by the mass, and the rest is the standard SHM page.
Marks are lost on a factor: springs read as series when they act in parallel, half the amplitude taken as half the time, or a height R taken as a distance R from the centre. The effective-g ideas come from Gravitation, the physical pendulum from Rotational Motion, and the same sine equation returns in Waves.
The sub-skills
The distinct skills inside the chapter, in the order to learn them.
The SHM equation
Read the phase in x = A sin(ωt + φ), choose the initial phase by the starting direction, and use v = ω√(A² − x²) and a = −ω²x.
Timing and combining SHMs
The time between two positions is the phase covered divided by ω; two SHMs of one frequency on a line add as vectors; two different frequencies never make SHM.
Springs and restoring forces
ω² = force per unit displacement ÷ mass: a cut spring is stiffer, a block between walls is parallel, two free masses use the reduced mass, a physical pendulum uses I about the pivot.
Simple pendulum and effective g
T = 2π√(L/g) whatever the bob's mass; a height, a planet, a lift or a liquid changes only the g in that formula.
Energy, amplitude changes and damping
Total energy ½kA²; kinetic equals potential at A/√2; a mass added at the mean shares momentum and lowers the amplitude; damped energy decays twice as fast as amplitude.
Traps to expect
Distractor shapes this chapter reuses. The Traps page covers the ones that cut across chapters.
A block between two walls read as series
Springs on opposite sides of a block look like a chain, but both stretch by the same x and both push back, so k = k₁ + k₂.
Equal distances in equal times
Mean to A/2 takes T/12, but A/2 to the extreme takes T/6, because the particle slows down near the extreme.
A height R read as a distance R
At a height equal to the earth's radius the distance from the centre is 2R, so g falls to a quarter and the period doubles.
Equal energies at half the amplitude
At A/2 the potential energy is only a quarter of the total. Kinetic and potential energy are equal at A/√2.
Learn it before you drill it
This chapter has full teaching notes — foundations, worked examples, self-checks and a mastery check for each page. Read the notes once, then drill page by page below.
Oscillations notesDrill every Oscillations question
120 questions from the bank, across 5 subtopics.
Drill one subtopic at a time
The 5 subtopics, in teaching order.
- SHM Equation, Velocity and AccelerationDrill SHM Equation, Velocity and Acceleration
- Timing in SHM and Combining SHMsDrill Timing in SHM and Combining SHMs
- Spring Systems and Restoring ForcesDrill Spring Systems and Restoring Forces
- Simple Pendulum and Effective gDrill Simple Pendulum and Effective g
- Energy in SHM, Amplitude Changes and DampingDrill Energy in SHM, Amplitude Changes and Damping
Related playbooks
Often paired with this one — the technique or the trap overlaps. Drill these next.