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1 Institut de Radioprotection et de
Sûreté Nucléaire
BP 17, 92262 Fontenay-aux-Roses, France
(G.P.,
L.F.B.)
2 Laboratoire de Géophysique Interne
et Tectonophysique
Observatoire de Grenoble, Université Joseph Fourier and
CNRS
BP 53, 38041 Grenoble, France
(F.C., L.M.)
Correspondence: * Present address: AXA-RE, 39 rue de Colisée 75008, Paris, France.
Physical models that can be used to obtain realistic accelerograms usually
require a thorough knowledge of the source, path, and site effects. In addition,
the computational resources needed might be expensive. Thus, empirical models
still
represent a good alternative for simulating strong ground motion. In this work,
we
modify and improve the model developed by
Sabetta and Pugliese (1996).
This new
method models the time-domain accelerogram based on the assumption that the
phase
is random and that the time envelope can be represented by the so-called average
instantaneous power. This is, in turn, described as a lognormal distribution for
P and
S waves combined with an algebro-exponential function representing the
envelope
of coda waves. In addition, the frequency content of the signal is nonstationary
and
follows a modified
-square model. The method depends on four common
indicators
in earthquake engineering: peak ground acceleration, strong-motion duration,
Arias
intensity, and central frequency. These indicators are empirically connected to
a given
database by means of ground-motion prediction equations. In this study we
calibrate
the model using Japanese data recorded by the K-net array, which has
high-quality
digital accelerograms and station-site conditions characterized by geotechnical
measurements.
In addition, this technique permits the inclusion of the uncertainty of the
model parameters to take into account the ground-motion natural variability in
the
stochastic generation of the time histories. The main goal of this work is to
provide
the earthquake engineering community with a flexible tool to generate realistic
accelerograms
for dynamic studies.
This article has been cited by other articles:
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B. Edwards and A. Rietbrock A Comparative Study on Attenuation and Source-Scaling Relations in the Kanto, Tokai, and Chubu Regions of Japan, Using Data from Hi-Net and KiK-Net Bulletin of the Seismological Society of America, August 1, 2009; 99(4): 2435 - 2460. [Abstract] [Full Text] [PDF] |
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D. Galluzzo, G. Zonno, and E. Del Pezzo Stochastic Finite-Fault Ground-Motion Simulation in a Wave-Field Diffusive Regime: Case Study of the Mt. Vesuvius Volcanic Area Bulletin of the Seismological Society of America, June 1, 2008; 98(3): 1272 - 1288. [Abstract] [Full Text] [PDF] |
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