Nonlinear site amplification factors for constraining the NGA models

被引:111
作者
Walling, Melanie [1 ]
Silva, Walter [2 ]
Abrahamson, Norman [3 ]
机构
[1] Univ Calif Berkeley, Dept Civil & Environm Engn, Berkeley, CA 94720 USA
[2] Pacific Engn & Anal, El Cerrito, CA 94546 USA
[3] Pacific Gas & Elect Co, San Francisco, CA 94105 USA
关键词
D O I
10.1193/1.2934350
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Amplification factors computed from the equivalent-linear method using the program RASCALS are used to develop constraints on the nonlinear soil response for possible use by the NGA ground-motion model developers. The site response computations covered site conditions with average V-S30 values ranging from 160 to 900 m/s, soil depths from 15 to 914 m, and peak accelerations of the input rock motion (V-S30=1100 m/s) between 0.01 g and 1.5 g. Four sets of nonlinear properties of the soils are used: EPRI, Peninsular Range, Imperial Valley, and Bay Mud. The first two soil models are used for V-S30 >= 270 m/s and the later two are used for V-S30 <= 190 m/s. Simple parametric models of the nonlinear amplification factors that are functions of the PGA on rock and V-S30 are developed for the EPRI and Peninsula models.
引用
收藏
页码:243 / 255
页数:13
相关论文
共 23 条
[1]  
Abrahamson NA., 1997, Seismol. Res. Lett, V68, P94, DOI DOI 10.1785/GSSRL.68.1.94
[2]   Comparisons of the NGA ground-motion relations [J].
Abrahamson, Norman ;
Atkinson, Gail ;
Boore, David ;
Bozorgnia, Yousef ;
Campbell, Kenneth ;
Chiou, Brian ;
Idriss, I. M. ;
Silva, Walter ;
Youngs, Robert .
EARTHQUAKE SPECTRA, 2008, 24 (01) :45-66
[3]  
Boore D.M., 1997, Seismol. Res. Lett, V68, P128, DOI DOI 10.1785/GSSRL.68.1.128
[4]   Ground-motion prediction equations for the average horizontal component of PGA, PGV, and 5%-damped PSA at spectral periods between 0.01 s and 10.0 s [J].
Boore, David M. ;
Atkinson, Gail M. .
EARTHQUAKE SPECTRA, 2008, 24 (01) :99-138
[5]  
BOORE DM, 1987, B SEISMOL SOC AM, V77, P440
[6]  
BOORE DM, 1983, B SEISMOL SOC AM, V73, P1865
[7]   NGA ground motion model for the geometric mean horizontal component of PGA, PGV, PGD and 5% damped linear elastic response spectra for periods ranging from 0.01 to 10 s [J].
Campbell, Kenneth W. ;
Bozorgnia, Yousef .
EARTHQUAKE SPECTRA, 2008, 24 (01) :139-171
[8]   Updated near-source ground-motion (attenuation) relations for the horizontal and vertical components of peak ground acceleration and acceleration response spectra [J].
Campbell, KW ;
Bozorgnia, Y .
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2003, 93 (01) :314-331
[9]   An NGA model for the average horizontal component of peak ground motion and response spectra [J].
Chiou, Brian S. -J. ;
Youngs, Robert R. .
EARTHQUAKE SPECTRA, 2008, 24 (01) :173-215
[10]   Nonlinear site amplification as function of 30 m shear wave velocity [J].
Choi, Y ;
Stewart, JP .
EARTHQUAKE SPECTRA, 2005, 21 (01) :1-30