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Article |
Institute of Physics of the Earth, Russian Academy of
Sciences
B. Gruzinskaya 10
Moscow 123995,
Russia
olga{at}synapse.ru
To study the effects of nonlinearity in the seismic response of soils, a
numerical simulation of the propagation of vertically incident seismic waves
in horizontal soil layers were performed. Shear noiselike and monochromatic
seismic waves of various intensities were used as input signals. The behavior
of soils was described by a nonlinear hysteretic model. To extract and study
nonlinear components in the ground response, the nonlinear system
identification method and analysis of higher-order spectra of oscillations on
the surface were applied. Even for weak input signals, the response of the
simulated soils contained a noticeable nonlinear component. An increase in the
intensity of input signals led to increasing distortions of propagating
signals, due to the generation and growth of combination-frequency harmonics.
The results show that odd types of nonlinearity are most typical for soils,
such as cubic and fifth-order nonlinearities, causing generation of the third
and fifth higher harmonics of main frequencies of input signals.
Nonlinearities of even types, such as quadratic, fourth-order, and
sixth-order, concerned with asymmetry, or skewness, of oscillations (i.e.,
quasi-static deformations of the surface) are usually weak, except some
special cases, in which a stress-strain relationship of a soil can be
represented by functions with noticeable even components. A weak nonlinearity
results in an increase in high-frequency components, due to the generation of
higher harmonics. In cases of strong nonlinearity, in which a decrease in
amplification and in shear moduli become noticeable, changes in spectra of
propagating signals achieve their maximum. As a result, input signals with
arbitrary spectra are transformed into output signals with spectra of the type
of E(f)
fk, where k
depends on the properties of the medium.
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O. V. Pavlenko and K. Irikura Nonlinear Behavior of Soils Revealed from the Records of the 2000 Tottori, Japan, Earthquake at Stations of the Digital Strong-Motion Network Kik-Net Bulletin of the Seismological Society of America, December 1, 2006; 96(6): 2131 - 2145. [Abstract] [Full Text] [PDF] |
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