Compute displacement, velocity, and acceleration for traveling and standing harmonic waves. Includes wave profile tables, key relationships, and visual displacement indicator.
The harmonic wave equation y(x, t) = A·sin(kx − ωt + φ) is the mathematical backbone of classical wave physics. This deceptively simple formula encodes everything about a sinusoidal wave: its amplitude A determines the maximum displacement, the wave number k = 2π/λ captures the spatial repetition, the angular frequency ω = 2πf describes the temporal oscillation, and the phase constant φ sets the wave's initial alignment. From sound waves in concert halls to electromagnetic waves carrying wifi signals, this equation describes the fundamental behavior of virtually all linear wave phenomena.
For traveling waves, the entire waveform moves through space at velocity v = ω/k = fλ, carrying energy from source to destination. Standing waves, formed when two identical waves travel in opposite directions, create fixed nodes (zero displacement) and antinodes (maximum displacement) — the basis of resonance in musical instruments, laser cavities, and microwave ovens. The standing wave equation y(x, t) = 2A·sin(kx)·cos(ωt) shows this factorization into a spatial envelope and a temporal oscillation.
This calculator evaluates both wave types at any point in space and time, computing the instantaneous displacement, particle velocity, and acceleration. It generates a spatial wave profile table with visual indicators, and provides a comprehensive summary of all derived quantities including period, wavelength, wave number, and maximum kinematic values.
This calculator brings the abstract wave equation to life by computing concrete values at specified points, generating spatial profiles, and displaying all derived quantities together. Physics and engineering students can verify homework solutions, explore parameter relationships, and build intuition for wave behavior. Keep these notes focused on your operational context. Tie the context to the calculator’s intended domain.
Traveling wave: y(x,t) = A·sin(kx − ωt + φ). Standing wave: y(x,t) = 2A·sin(kx)·cos(ωt + φ). Where: ω = 2πf, k = 2π/λ, λ = v/f, T = 1/f. Particle velocity: dy/dt. Particle acceleration: d²y/dt².
Result: y(1, 0) = 0.000951 m
For A = 0.001 m, f = 440 Hz, v = 343 m/s: λ = 343/440 = 0.7795 m, k = 8.063 rad/m, ω = 2764.6 rad/s. y(1, 0) = 0.001·sin(8.063·1 − 0 + 0) = 0.001·sin(8.063) ≈ 0.000951 m.
| Type | Equation | Energy Transport | Examples | |---|---|---|---| | Traveling (progressive) | y = A·sin(kx − ωt) | Yes | Sound, light, water waves | | Standing | y = 2A·sin(kx)·cos(ωt) | No (energy trapped) | Guitar strings, organ pipes |
The harmonic wave equation is a solution to the one-dimensional wave equation: ∂²y/∂t² = v² · ∂²y/∂x². This partial differential equation governs all linear, non-dispersive wave phenomena. Its general solution is d'Alembert's formula: y(x,t) = f(x − vt) + g(x + vt), representing rightward and leftward traveling waves of arbitrary shape.
When two or more waves overlap in the same medium, the total displacement is the algebraic sum of individual displacements (principle of superposition). This leads to constructive interference (in-phase waves amplify) and destructive interference (out-of-phase waves cancel). Standing waves are a special case where constructive and destructive interference create fixed spatial patterns.
A traveling wave moves through space, transporting energy from one location to another. A standing wave is formed by the superposition of two identical waves traveling in opposite directions, creating fixed nodes and antinodes that do not propagate.
The wave number k = 2π/λ represents the spatial frequency of the wave — the number of radians of phase change per meter. It is the spatial analog of angular frequency ω, which measures phase change per second.
Wave speed v = fλ is the speed at which the wave pattern moves through space. Particle velocity dy/dt is the speed at which a point on the medium moves up and down (transverse wave) or back and forth (longitudinal wave). They are perpendicular for transverse waves.
Standing waves form when a wave reflects from a boundary and interferes with the incoming wave. The key condition is that the string/cavity length must be an integer multiple of half-wavelengths for constructive interference at the boundary conditions.
The phase constant φ sets the initial condition of the wave at x = 0, t = 0. Different sources may emit waves with different phase constants. When two waves with different φ values interfere, the phase difference determines constructive or destructive interference.
Both are equally valid — the choice between sin and cos simply shifts the phase constant by π/2. The sine form starts at zero displacement for φ = 0, while cosine starts at maximum displacement. The convention is a matter of preference.