Abstract

It is known that, while the stochastic Green’s function method is suitable for generating ground motions with short periods, the three-dimensional finite difference method (FDM) is appropriate for ground motions with rather long periods. In the previous research, the stochastic Green’s function method was used for finding the critical earthquake ground motion for variable fault rupture slip (slip distribution and rupture front). However, it cannot be used for ground with irregularities and for wave component with rather long periods. In responding to this request, the FDM is used in this paper for finding the critical ground motion for structures with rather long natural period. Since the FDM is time-consuming, it seems unfavorable to use it in a simple sensitivity algorithm where an independent response sensitivity is calculated for many design parameters. To overcome this difficulty, the bi-cubic spline interpolation of uncertain parameter distributions (seismic moment distribution in this paper) and the response surface method for predicting the response surface from some sampling points are used effectively in this paper. The uncertainty parameter is the fault rupture slip distribution described in terms of seismic moments. It is found that the critical ground motion for structures with rather long natural period can be found effectively by the proposed method.

Highlights

  • There was common understanding that earthquake ground motions can be classified into a few types (Abrahamson et al, 1998)

  • The uncertain parameter is the fault rupture slip distribution described in terms of seismic moments at the control points

  • The uncertain parameter is the fault rupture slip distribution described in terms of seismic moments M0

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Summary

INTRODUCTION

There was common understanding that earthquake ground motions can be classified into a few types (Abrahamson et al, 1998). In another previous research (Makita et al, 2018b), the stochastic Green’s function method was used for finding the critical earthquake ground motion for variable fault rupture slip (slip distribution and rupture front) It cannot be used for ground with irregularities and for wave component with rather long periods. The uncertain parameter is the fault rupture slip distribution described in terms of seismic moments at the control points. The uncertain parameter is the fault rupture slip distribution described in terms of seismic moments M0. Multiple point sources are placed at the difference grid points on the source layer and the seismic moment is released by considering the time delay due to the rupture propagation.

Result
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