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Pseudo relative velocity spectra of earthquake ground motion at high frequencies
Author(s) -
Trifunac M. D.
Publication year - 1995
Publication title -
earthquake engineering and structural dynamics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.218
H-Index - 127
eISSN - 1096-9845
pISSN - 0098-8847
DOI - 10.1002/eqe.4290240806
Subject(s) - extrapolation , amplitude , acceleration , spectral line , peak ground acceleration , scaling , range (aeronautics) , ground motion , seismology , physics , geology , geodesy , mathematics , engineering , geometry , mathematical analysis , classical mechanics , optics , astronomy , aerospace engineering
The currently available empirical scaling laws for estimation of spectral amplitudes are limited to periods longer than 0–04 s. However, for design of equipment and stiff structures on multiple and distant supports, exposed to strong shaking near faults where peak accelerations can exceed 1 g , specification of design ground motions at higher frequencies is required. This paper presents a method for extrapolation of pseudo‐relative velocity spectral amplitudes of strong earthquake shaking to short periods (0–01 < T < 0–04 sec). The extrapolated spectra can be used as a physical basis for defining design spectral amplitudes in this higher‐frequency range. The analysis in this paper implies that for typical strong motion accelerations, particularly on sedimentary sites in California, the peak ground accelerations are projected to be unaffected by frequencies higher than those recorded. Consequently, in California, the high‐frequency pseudo‐acceleration spectra can be approximated from the recorded absolute peak accelerations.