Analysis of nonlinear seismic effects of large-scale deep soft site under far-field large earthquake
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Analysis of nonlinear seismic effects of large-scale deep soft site under far-field large earthquake
Vol. 34, Issue 11, (2013)
作者机构:
1. 南京工业大学 岩土工程研究所,南京,210009
2. 江苏省土木工程防震技术研究中心,南京,210009
3. 江苏省地震局,南京,210014
4. 中国地震局地球物理研究所,北京,100081
作者简介:
基金信息:
DOI:
CLC:P65
Online First:11 November 2013,
Published:2013
稿件说明:
移动端阅览
ZHAN ji-yan, CHEN Guo-xing, LIU Jian-da, et al. Analysis of nonlinear seismic effects of large-scale deep soft site under far-field large earthquake[J]. 2013, 34(11).
DOI:
ZHAN ji-yan, CHEN Guo-xing, LIU Jian-da, et al. Analysis of nonlinear seismic effects of large-scale deep soft site under far-field large earthquake[J]. 2013, 34(11).DOI:
Analysis of nonlinear seismic effects of large-scale deep soft site under far-field large earthquake
Based on the parallel computing cluster platform of ABAQUS
according to the typical stratigraphic profile of downtown area in Suzhou city
a two-dimensional nonlinear analytical model of large-scale deep soft site was established. Comparison of nonlinear seismic effects under artificial seismic wave and far-field ground motion of large earthquake were conducted. The results indicate that: (1) The amplification effect of peak ground acceleration (PGA) under far-field ground motion of large earthquake is especially significant compared with that under artificial seismic wave. There is obvious variability among the PGA of ground surface in different locations due to the horizontal heterogeneity and nonlinearity of ground soils. (2) The deep soft site has a significant filtering effect on the high-frequency ground motion wave whose period is less than 0.3 s. When it is under far-field ground motion
there exists an obvious amplification effect on the long-period seismic wave whose period ranging from 0.85 s to 1.65 s. However
there is also apparent filtering effect on the long-period seismic wave whose period ranging from 2.5 s to 7.0 s. (3) It presents fluctuation phenomenon of PGA distribution with depth and along the lateral direction. There are prominent local focusing effects and filtering reduction phenomenon near the contact surface between different soil layers and in the horizontal heterogeneous soil area; and the PGA amplification effect of soils above 20 m depth is relatively larger than that of other soil layers. (4) Both the spectral characteristics of seismic wave and horizontal heterogeneity of ground soils have obvious influence on the shape of ? spectrum. Besides
three-dimensional curves of spectrum shape those describe the acceleration response spectrum changing with depth are given
which can directly show the soil depth in deep soft site where long and thin underground constructions may occur resonance phenomenon.