Ground motion
Input accelerogram
Spectrum settings
Response spectra
SDOF response — selected period
Method
The SDOF equation of motion is m·x″(t) + c·x′(t) + k·x(t) = -m·ag(t), normalized as x″ + 2ζωnx′ + ωn2x = -ag(t).
Between two consecutive samples of the accelerogram the ground acceleration is treated as linear in time. With this piecewise-linear assumption, the SDOF response advances by a 2×2 transition matrix plus a forcing contribution that depends only on the two end-point accelerations. The matrix entries are evaluated once per period from ζ, ωn, Δt (Nigam & Jennings, 1969). The result is exact rather than an approximation and is the standard method used in modern response-spectrum codes.
The synthetic ground motion is filtered white noise through a Kanai-Tajimi filter H(ω) = (ωg2 + 2iζgωgω)/((ωg2-ω2) + 2iζgωgω), modulated by the Saragoni-Hart envelope e(t) = (t/t0)α exp(-β(t-t0)), and rescaled to the target peak ground acceleration.
References
- Nigam, N.C.; Jennings, P.C. (1969). Calculation of Response Spectra from Strong-Motion Earthquake Records. Bulletin of the Seismological Society of America, 59(2), 909-922.
- Chopra, A.K. (2017). Dynamics of Structures: Theory and Applications to Earthquake Engineering, 5th ed., Pearson. Sections 5.2 and 6.
- Kanai, K. (1957). Semi-Empirical Formula for the Seismic Characteristics of the Ground. Bulletin of the Earthquake Research Institute, 35, 309-325. Tajimi, H. (1960). A Statistical Method of Determining the Maximum Response of a Building Structure During an Earthquake. Proc. 2nd WCEE.