ŒfÚŽGŽi˜ajF | “ú–{’nkHŠwƒVƒ“ƒ|ƒWƒEƒ€˜_•¶W |
VolF | 11Šª |
”NF |
2002”N
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•ÅF |
521-526•Å
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’˜ŽÒi˜ajF |
Žº–ì@„—²C‘ºã@¹•FC²“¡@’‰M
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ƒ^ƒCƒgƒ‹i˜ajF |
’f‘w‹ß–T’nk“®‚̈ʑŠ“Á«‚ÌŒoŒ±“I‚ȃ‚ƒfƒ‹‰»
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´˜^i˜ajF |
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ƒL[ƒ[ƒhi˜ajF |
ŒQ’x‰„ŽžŠÔC’f‘w‹ß–T’nk“®C‰ñ‹Aƒ‚ƒfƒ‹
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ŒfÚŽGŽi‰pjF |
THE EARTHQUAKE ENGINEERING SYMPOSIUM PROCEEDINGS
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’˜ŽÒi‰pjF |
Yoshitaka Murono, Masahiko Murakami, Tadanobu Sato
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ƒ^ƒCƒgƒ‹i‰pjF |
EXPERIMENTAL MODELING OF PHASE SPECTRUM OF NEAR-FAULT EARTHQUAKE MOTION
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´˜^i‰pjF |
Modeling the phase of earthquake ground motion is required in order to synthesize design ground motion. A simple method is presented for modeling the phase characteristics of earthquake motion using the concept of group delay time and wavelet analysis. Using the data set of observed near-fault earthquake motions, we calculated the group delay time of each earthquake motion on each compact support of the mother wavelet. Because of the fluctuating nature of the group delay time on each support, the mean of the group delay times and standard deviation were calculated. The group delay time at the near source region is strongly affected by a rupture directivity of the fault. We therefore derive here regression equations for mean and standard deviation of group delay that can take the rupture directivity into account. Simulated sample phase spectra were used to simulate earthquake motions assuming that Fourier amplitude spectra are given at observation stations. Their time histories are compared with the observed ones.
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ƒL[ƒ[ƒhi‰pjF |
group delay time, near fault earthquake motion, regression equation
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‹LŽ–‹æ•ªF |
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‹æ•ªF |
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