摘要
以南京、盐城、常州、泰州、启东和上海的6个典型场地作为长江下游地区深厚软弱场地的代表,探讨了深厚软弱场地的地震效应特性。选用Taft、El Centro和Northridge地震记录作为输入地震动,将Taft、El Centro和Northridge地震波加速度时程的峰值水平分别调整为0.35 m/s2、0.70 m/s2、0.98m/s2,对6个场地进行了输入不同地震波、不同峰值加速度水平的54种组合的地震反应分析,并得出一些有意义的规律。
In this paper 6 deep soft sites which are from Nanjing, Yancheng, Changzhou, Taizhou, Qidong, Shanghai are represented as typical deep soft sites in the lower reaches of the Yangtze River, and the characteristics of the seismic effect of the deep soft sites are discussed. Taft , El Centro and Northridge earthquake records are regarded as inputting ground motions, and their acceleration peak values are adjusted to 0.35m/s^2,0. 70 m/s^2 and 0.98 m/s^2. The site seismic effect of 54 cases under different input ground motions and different acceleration peak values for six sites is analyzed, and some rules have been obtained.
出处
《世界地震工程》
CSCD
北大核心
2009年第1期117-121,共5页
World Earthquake Engineering
关键词
深厚软弱场地
地震效应
输入地震动
放大系数
互层土
deep soft site
seismic effect
input ground motion
amplification factor interbedded strata