Empirical Quantification of the Impact of Nonlinear Soil Behavior on Site Response

被引:30
|
作者
Regnier, Julie [1 ]
Cadet, Heloise [2 ]
Bard, Pierre-Yves [3 ]
机构
[1] CEREMA, DTer Mediterranee, 56 Blvd Stalingrad, F-06300 Nice, France
[2] ADRGT, 2 Rue Condamine ZI de Mayencin, F-38610 Grenoble, France
[3] ISTerre, 1381 Rue Piscine, F-38610 Grenoble, France
关键词
GROUND-MOTION AMPLIFICATION; ARRAY RECORDINGS; EARTHQUAKE; SEDIMENTS; VELOCITY; MODELS;
D O I
10.1785/0120150199
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
We present an extensive analysis of the quantitative impact of the nonlinear soil behavior on site response at 174 sites of the Japanese Kiban-Kyoshin (KiK-net) network. The nonlinear to linear site-response ratio (RSRNL-L) is calculated by comparing the surface/downhole Fourier spectral ratio for strong events and for weak events. Three thresholds of surface peak ground acceleration (PGA) are tested to characterize the strong events: 100, 200, and 300 cm/s(2), whereas weak events correspond to surface PGA in the 0: 1-25 cm/s(2) range. This ratio exhibits a typical shape; with a low-frequency part above 1 and a high-frequency part generally below 1, separated by a transition zone around a site-dependent frequency labeled f(NL) (characterized by RSRNL-L = 1). The average maximum amplitudes of RSRNL-L are 1.4, 1.5, and 1.6, and the minimums are 0.6, 0.5, and 0.5 for PGA thresholds 100, 200, and 300 cm/s(2), respectively, showing that nonlinear soil behavior results in significant site-response modifications even for moderate PGA values of 100 cm/s(2). The f(NL) value exhibits a satisfactory correlation with site classifications based on either V-S30 (travel-time averaged shear-wave velocity over the top 30 m) or f(0) (site fundamental frequency): f(NL) decreases when either V-S30 or f(0) decreases. In addition, the amount of the low-frequency amplification increase depends on V-S30 and reaches a maximum of 1.6 for high V-S30 soil classes associated with shallow thin soft-soil layer underlain by stiff substratum. The average high-frequency decrease is about 0.5 for all soil classes defined from either V-S30 or f(0); for a few sites, however, this decrease is replaced by an increase as reported in previous studies, in relation with water contents and pore-pressure issues. The increase of amplification below f(NL) is found to be a quasi-systematic consequence of nonlinear soil behavior, which should be emphasized, because it can reach up to 1.6 for high V-S30 sites.
引用
收藏
页码:1710 / 1719
页数:10
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