Complex frequency response
The exact amplitude describes the infinite-time particular solution. The actual trajectory also contains a homogeneous transient set by the initial displacement and velocity.
M064 · Oscillations / frequency response
A sinusoidal force actuator drives a spring and dashpot. Drag the frequency cursor, inspect startup transients and measure amplitude and phase over three complete drive cycles. Sweep nineteen independently integrated experiments against the exact response curve; track drive work, dissipation and stored energy.
Physics tutorial
BackgroundA periodic actuator continually supplies energy while damping removes it. The resulting motion combines a decaying startup transient with a steady response at the drive frequency. Amplitude alone misses the phase and power balance.
Why it mattersOpenStax University Physics Volume 1, section 15.6 supplies the forced-oscillation reference. Nineteen independent numerical trajectories and a three-cycle Fourier measurement put the response curve through an actual measurement pipeline.
Start with the essentials
The exact amplitude describes the infinite-time particular solution. The actual trajectory also contains a homogeneous transient set by the initial displacement and velocity.
Displacement lags force. Above the stated damping threshold amplitude falls monotonically from zero frequency. The peak action is restricted to the displayed scan band, so it can select its lower boundary.
Absorbed power peaks at natural frequency even when displacement peaks elsewhere. The exact power half-maximum width is not the displacement half-height width; the displayed bandwidth converts angular frequency to cycles per second.
Sine and cosine projections use only the last three complete drive cycles, with 128 uniform phase samples per cycle. Startup transients contaminate this projection and appear in the nonharmonic residual. Work and dissipation are integrated independently.
Typical misconceptionDisplacement and absorbed power must peak at the same frequency.
Better mental modelIncrease damping and locate the displacement peak. Power still peaks at natural frequency; strong damping removes an interior displacement peak.
Typical misconceptionThree complete periods automatically measure steady state.
Better mental modelMeasure early and late. The Fourier projection is defined at both times, but the early residual and phase can reveal startup contamination.
Typical misconceptionThe power bandwidth is the displacement half-height width.
Better mental modelThe displayed width belongs to absorbed power and is exact for this viscously damped model. Do not apply it to another response curve.
Scrub through the first three drive cycles, then measure the current frequency at the endpoint.
What to observe: A measurement is unavailable before a full window; its later amplitude and phase approach the steady reference.Measure nineteen frequencies and drag the amplitude cursor across the peak.
What to observe: Each blue point comes from an independent solved experiment, not a copy of the analytical curve.Increase damping, find the amplitude peak and compare absorbed power at natural frequency.
What to observe: The displacement peak shifts down; power resonance remains at natural frequency.Compare drive work with dissipated energy and stored energy late in the run.
What to observe: Work can exceed the current stored energy because the dashpot continuously removes energy.