Weight resolves into a component along the path (restoring force) and one perpendicular to it.
The weight's component along the swing, −mg sinθ, is the restoring force. By Newton's 2nd law:
a = −g sinθ
For small angles (θ ≤ 10°), sinθ ≈ s/L, and arc length s ≈ x, giving:
a = −gx/L = −(2πf)²x
Comparing with T = 1/f gives the pendulum period:
T = 2π√(l/g)
Finding g: squaring gives T² = 4π²(l/g) — a graph of T² against l is a straight line through the origin with gradient 4π²/g.
Mass–spring systems
The same logic applies to a mass on a spring, combining three equations:
F = ma F = ke a = −(2πf)²x
Substituting gives:
−ke = −m(2πf)²x
Extension e and displacement x are both lengths and cancel, rearranging to:
T = 2π√(m/k)
Key difference: unlike the pendulum, the spring's period depends on mass (not gravity) — this is why mass–spring oscillators can be used to measure mass in space, where weighing scales don't work.
Quick contrast
Pendulum: T depends on l and g only — independent of mass and amplitude (for small angles).
Spring: T depends on m and k only — independent of g and amplitude.
Exam essentials
Key equations
T = 2π√(l/g) — pendulum.
T = 2π√(m/k) — mass–spring.
Small-angle condition: θ ≤ 10° (≈0.17 rad).
What each depends on
Pendulum: length & g only — not mass or amplitude.
Spring: mass & spring constant only — not g or amplitude.
Common slips
Pendulum formula only holds within the small-angle approximation.
On a T²–l graph, the gradient is 4π²/g, not g itself.
Don't confuse extension e with displacement x — equal in magnitude here, but conceptually different quantities.