Discussion of “Seismic Response of Horizontal Soil Layers”

1969 ◽  
Vol 95 (3) ◽  
pp. 927-930
Author(s):  
Harold W. Olsen ◽  
Albert T.F. Chen
Keyword(s):  
1968 ◽  
Vol 94 (4) ◽  
pp. 1003-1031 ◽  
Author(s):  
Izzat M. Idriss ◽  
H. Bolton Seed
Keyword(s):  

Author(s):  
Liu Bingbing ◽  
Wang Haiyun ◽  
Jiang Weiping ◽  
Zhang Xu

2012 ◽  
Vol 166-169 ◽  
pp. 2060-2065
Author(s):  
Mian Shui Rong ◽  
Tao Lu ◽  
Bi Deng Liu

The current equivalent linearization method for evaluation of seismic response of soil layers has been widely used by engineers, but it obviously has limits while considering severe earthquake action and dealing with extremely soft soil layers. Developing a direct time-domain integral method is essential. In this paper, a direct-domain integral method is proposed. In the method, the dynamic skeleton curve constitutive model is introduced and it can fit test results of dynamic shear modules ration curve and damping ratio curve simultaneously, central difference integration method is used to solve the dynamic equation, multi-transmitting artificial boundary condition has been conducted to consider the effect of energy transmission through bedrock boundary. In order to implement this method, a program called Dymatlab has been compiled, strong motion records got from the NGA data base for site effects on strong ground motion have been used to analysis the offshore engineering site with thick soft soil layers. The results show that this program can be applied as a reasonable and feasible method for nonlinear seismic response of soil layers.


2014 ◽  
Vol 580-583 ◽  
pp. 1604-1608
Author(s):  
Liang Wang ◽  
Ya Su

This paper states the comparison research of calculation results from program LSSRLI-1 and program SHAKE2000, with the strong seismic records as well as the site soil conditions by using borehole arrays. The analytical results show that the site soil conditions have an amplification effect on the seismic PGA and response spectrum values, however, the actual seismic records are not consistent with the program calculations on the amplification effect. Besides, the site soil conditions also have an altering effect on the predominant period of seismic response spectrum, where actual seismic records and program calculation results of the altering effect are not the same either.


2021 ◽  
Vol 2021 ◽  
pp. 1-12
Author(s):  
Shun Yang ◽  
Xin Han ◽  
Qiyun Lei ◽  
Sihan Yu ◽  
Chao Liu

This paper presents a numerical analysis of two types of representative site profiles in the Yinchuan Plain under earthquake loading. The analyzed soil profiles, based on borehole investigations performed over the years, are used to explore the seismic response of the sites in this area. In total, eleven stratified soil models are used in this study, which can be grouped into two categories: a single interbedded soil model and multiple interbedded soil model. A one-dimensional equivalent linearization method is applied to evaluate the seismic response of different soil models under four exceeding probabilities in terms of peak ground acceleration (PGA), peak ground velocity (PGV), peak ground displacement (PGD), and spectral acceleration (Sa). The results show that the significant amplification effect of PGA occurs in rare and extremely rare earthquakes, with an amplification ratio of 1.4∼1.7 when the single silty clay layer is located at the model ground. In this scenario, the spectral acceleration is amplified at a period of approximately 1.0 s. For the multilayered soil cases, the amplification effect tends to decrease, whereas the characteristic periods increase with increasing numbers of soil layers and the ground acceleration is deamplified under a high motion intensity when the number of soil layers is ≥ 5. This study, to a certain degree, has reference value for seismic microzonation in this area.


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