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📈 Response Spectrum Explorer

Every possible structure, one ground motion. Watch a full response spectrum build live as you change damping — the peak response of an SDOF system swept across a full range of periods, all subjected to the same synthetic ground motion. No score, no target — just a feel for why the response spectrum is the single most important chart in seismic design.

Parameters

At Selected Period

Peak displacement—
Spectral accel. (pseudo)—
Amplification vs PGA—

Response Spectrum (Sd vs Period)

Ground Motion Used

This simulation sweeps ~40 periods, each fully solved by the same verified Newmark-β integrator (engine/dynamics.js → sdofNewmark) used in the Seismic Response Explorer and the site's SDOF calculators. The ground motion is a synthetic sum of four sine waves at different frequencies with exponential decay — chosen deliberately (not a single pure tone) so the spectrum has genuine peaks and valleys to explore, but it is not a real recorded earthquake. Damping reduction with increasing ζ was verified independently before publishing: at a fixed period, ζ=2%→20% reduced peak response monotonically (129mm → 42mm in the reference case), matching expected physics.

Method

SpectrumFor each period Tn, an independent SDOF (mass=1000kg, stiffness/damping set from Tn and ζ) is solved for its full time-history under the same ground motion; the peak displacement Sd(Tn) is plotted. This is the classical shock/response spectrum construction (Chopra ch.6).
Pseudo-SaPseudo-spectral acceleration Sa ≈ ωn²·Sd (Chopra §6.6) — an approximation valid for lightly damped systems, shown for reference alongside the true peak displacement.
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Visual explanation

Site amplification and local soil effects. Soft soil amplifies ground motion at its natural frequency; demand rises for long-period structures
Figure 33. Site amplification and local soil effectsSource: Kramer (1996), Geotechnical Earthquake Engineering; TBDY 2018 Ch. 2. Curves computed.