2010
DOI: 10.1007/s12205-011-1074-3
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A phase model of earthquake motions based on stochastic differential equation

Abstract: In this paper, a method is proposed to simulate Group Delay Time (GDT) of earthquake ground motion by using Stochastic Differential Equation (SDE). The random characteristic of GDT is expressed by a stochastic differential equation whose mean and variance processes are defined by ordinary differential equations. An algorithm is developed to identify the coefficients of the ordinary differential equations. Regression surfaces of the coefficients are developed as functions of earthquake magnitude, epicentral dis… Show more

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Cited by 9 publications
(2 citation statements)
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“…23 The nonrepeatability and unpredictability of natural seismic waves mean that the above fitting methods often fail to produce satisfactory frequency distribution characteristics in the artificial phase difference spectrum. 24 The research results show that the physical meaning of the phase difference spectrum of natural seismic wave can be expressed as peak arrival time. Moreover, the variation laws of acceleration time-history curve of natural seismic wave can be transformed into its energy distribution characteristics in the time domain.…”
Section: Introductionmentioning
confidence: 93%
“…23 The nonrepeatability and unpredictability of natural seismic waves mean that the above fitting methods often fail to produce satisfactory frequency distribution characteristics in the artificial phase difference spectrum. 24 The research results show that the physical meaning of the phase difference spectrum of natural seismic wave can be expressed as peak arrival time. Moreover, the variation laws of acceleration time-history curve of natural seismic wave can be transformed into its energy distribution characteristics in the time domain.…”
Section: Introductionmentioning
confidence: 93%
“…Boore [22] used the stochastic differential equation to simulate the GDT. Additionally, Zhang et al [23] developed a method to apply the stochastic differential equation in relation to earthquake magnitude, epicenter distance, and local soil conditions. Chai et al [24] used the GDT concept to model phase spectra according to the compact support of the Meyer wavelet.…”
Section: Introductionmentioning
confidence: 99%