An oscillation is any motion that repeats itself about a central equilibrium position. Think of a pendulum swinging, a mass bouncing on a spring, or a guitar string vibrating. Before defining SHM, we need the vocabulary.
Oscillation Terminology
- Displacement x — distance from the equilibrium position (positive or negative)
- Amplitude A — maximum displacement from equilibrium
- Period T — time for one complete oscillation (s)
- Frequency f — number of oscillations per unit time (Hz = s⁻¹)
- Angular frequency ω — rate of change of phase (rad s⁻¹)
- Phase difference — fraction of a cycle by which one oscillation leads or lags another, measured in radians or degrees
The Defining Condition
Motion is simple harmonic if and only if the acceleration is:
- Proportional to the displacement from equilibrium, and
- Directed towards the equilibrium position.
The minus sign is crucial — it guarantees the restoring force always pushes the object back towards equilibrium. When displacement is positive, acceleration is negative; when displacement is negative, acceleration is positive.
To prove a system undergoes SHM, start from Newton's second law and show that the resulting acceleration has the form a = −ω²x. You must identify what ω represents for that specific system (e.g. ω = √(k/m) for a mass–spring system).
Examples of SHM
Any system where the restoring force obeys Hooke's law produces SHM (for small oscillations):
- Mass on a spring — restoring force F = −kx, so a = −(k/m)x giving ω² = k/m
- Simple pendulum (small angles) — restoring force F ≈ −(mg/L)x giving ω² = g/L
- Atoms in a crystal lattice — interatomic forces approximate SHM for small vibrations
- Buoyancy oscillator — a floating object bobbing up and down