@ ŒfÚŽGŽi˜ajF “ú–{’nkHŠwƒVƒ“ƒ|ƒWƒEƒ€u‰‰W VolF 4Šª ”NF 1975”N •ÅF 1051-1058•Å ’˜ŽÒi˜ajF - ƒ^ƒCƒgƒ‹i˜ajF - ´˜^i˜ajF
- ƒL[ƒ[ƒhi˜ajF - ŒfÚŽGŽi‰pjF PROCEEDINGS OF JAPAN EARTHQUAKE ENGINEERING SYMPOSIUM ’˜ŽÒi‰pjF Masaru HOSHIYA, Toshiaki CHIBA ƒ^ƒCƒgƒ‹i‰pjF PHYSICAL SPECTRUM OF EARTHQUAKE ACCELERATION ´˜^i‰pjF
With the fact that earthquake ground surface motions are nonstationary in the amplitude and frequency contents, this study discussed a method, (1) to measure the nonstationary characteristics by a physically meaningful nonstationary spectrum, and (2) to generate an artificial earthquake acceleration with the same nonstationary characteristics representing an original earthquake record. In order to throw light on the nonstationary characteristics of earthquake data, this paper uses a physical spectrum defined by S(¡,¡GW) = E ¡W(t-u)x(u)e ¡ ; ¡ < ¡ < ¡ where is a time window function which satisfies ¡(t) dt = 1 A Niigata acceleration record of N-S component is actually analyzed and based on the estimated spectrum of a Niigata record, a stochastic simulation of a nonstationary random process is theoretically developed. The following conclusions are made ; (1) Physical spectral concept can be of great use for analysis of nonstationary earthquake data. (2) Theory of simulation of a nonstationary earthquakth prescribed amplitude and frequency nonstationarities is established. ƒL[ƒ[ƒhi‰pjF - ‹LŽ–‹æ•ªF - ‹æ•ª @@@ˆÏˆõ‰ï˜_•¶W