Simple Harmonic Motion
Any restoring influence proportional to displacement produces the same sinusoidal motion, whatever is oscillating.
Simple harmonic motion arises whenever the restoring acceleration is proportional to displacement and directed back toward equilibrium.
Definition(W1.1.1)Restoring acceleration proportional to displacementTotal mechanical energy in an oscillator is constant, continuously exchanged between kinetic and potential forms.
Result(W1.2.1)Total energy of an oscillator from its amplitudeFor small swing angles, a pendulum's restoring torque is proportional to angular displacement, satisfying the SHM condition.
Result(W1.3.1)Period of a simple pendulumFriction or drag removes energy from a real oscillator, gradually decaying its amplitude — underdamped (oscillates while decaying), critically damped (returns to equilibrium fastest without oscillating), or overdamped (returns slowly, no oscillation). Driving an oscillator periodically produces resonance: the amplitude peaks sharply when the driving frequency matches the system's natural frequency.
Wave Motion
A wave carries energy and pattern through a medium without transporting the medium itself.
A travelling wave is a disturbance that repeats in both space (wavelength λ) and time (period T), moving at fixed shape and speed.
Definition(W2.1.1)Displacement of a travelling sinusoidal waveWave speed on a string is set by the balance between the restoring effect of tension and the inertia of the string's mass.
Result(W2.2.1)Wave speed from tension and mass densityA wave carries energy at the rate its source supplies it, proportional to the square of both amplitude and frequency.
Result(W2.3.1)Average power carried by a wave on a stringA wave meeting a boundary between two media partially reflects and partially transmits. Reflecting from a denser medium (a fixed end) inverts the wave; reflecting from a less dense medium (a free end) does not. The fraction reflected versus transmitted depends on how sharply the wave impedance changes at the boundary.
Sound
Sound is a longitudinal pressure wave; its speed, loudness scale, and frequency shifts all follow from that.
Sound is a longitudinal wave: alternating compressions and rarefactions of the medium, oscillating along the same direction the wave travels rather than perpendicular to it.
Result(W3.1.1)Speed of sound from a medium's stiffness and densityThe audible range of intensities spans many orders of magnitude, compressed onto a manageable logarithmic scale.
Definition(W3.2.1)Sound level on the decibel scaleRelative motion between a sound source and an observer shifts the observed frequency.
Result(W3.3.1)Frequency shift from relative motion of source and observerA source moving faster than the wave speed leaves its wavefronts unable to outrun it, piling them into a cone.
Result(W3.4.1)Half-angle of the shock cone behind a supersonic sourceSuperposition
Waves add linearly; the pattern that results — reinforcement, cancellation, or a beat — depends only on their relative phase.
Two coherent waves reaching the same point combine constructively or destructively depending on the difference in the distance each has travelled.
Result(W4.1.1)Constructive or destructive condition from path differenceTwo identical waves travelling in opposite directions combine into a pattern that oscillates in place rather than travelling.
Result(W4.2.1)Displacement pattern of a standing waveA string fixed at both ends supports only wavelengths that fit an integer number of half-wavelengths between the fixed points.
Result(W4.3.1)Allowed frequencies of a string fixed at both endsTwo sound sources of nearly equal frequency produce a slowly pulsing loudness, rather than two separately audible tones.
Result(W4.4.1)Pulsing frequency from two close source frequencies