Nonlinear Site Models Derived from 1D Analyses for Ground-Motion Prediction Equations Using Site Class as the Site Parameter

被引:34
|
作者
Zhao, John X. [1 ,4 ]
Hu, Junsheng [1 ]
Jiang, Fei [1 ]
Zhou, Jun [1 ]
Zhang, Yingbin [1 ]
An, Xiaowen [2 ]
Lu, Ming [3 ]
Rhoades, David. A. [4 ]
机构
[1] Southwest Jiaotong Univ, Minist Educ, Key Lab Transportat Tunnel Engn, Chengdu 610031, Sichuan, Peoples R China
[2] Yunnan Inst Earthquake Engn, Kunming 50204, Yunnan Province, Peoples R China
[3] China Earthquake Adm, Inst Crustal Dynam, Beijing 100085, Peoples R China
[4] GNS Sci, Lower Hutt 65040, New Zealand
基金
美国国家科学基金会;
关键词
SPECTRAL AMPLIFICATION RATIOS; AVERAGE HORIZONTAL COMPONENT; RECORDS; BEHAVIOR; PERIODS; PGV; NET;
D O I
10.1785/0120150019
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Nonlinear site models are an important part of ground-motion prediction equations (GMPEs) and can be constructed in a number of ways. If numerous soil-site strong-motion records contain the effect of strong nonlinear soil response, the parameters for the nonlinear model can be a part of the regression parameters for GMPEs. It is also possible to derive nonlinear site models by numerical simulation. However, the number of strong-motion records from Japan that contain the effect of strong nonlinear soil response is still too small to derive nonlinear site terms. We present a model of nonlinear site terms using site class as the site parameter in GMPEs based on a 1D equivalent linear model. The 1D model was constructed based on the shear-wave velocity profiles from the KiK-net strong-motion stations with a wide range of site periods, soil depth, and impedance ratios. The rock-site strong-motion records were from different earthquake categories in Japan and the Pacific Earthquake Engineering Research Center dataset. Those records had a wide range of earthquake magnitudes, source distances, and peak ground accelerations. A random effects regression model was fitted to the calculated spectral amplification ratios, accounting for the effect of site impedance ratios, earthquake magnitudes, and source distances of the rock-site records. We also designed a method to adjust the 1D model so it can be used in a GMPE, accounting for the fact that a 1D model is an overly simplistic assumption for many real strong-motion recording stations in many parts of the world.
引用
收藏
页码:2010 / 2022
页数:13
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