›› 2015, Vol. 36 ›› Issue (6): 1721-1736.doi: 10.16285/j.rsm.2015.06.026

• 岩土工程研究 • 上一篇    下一篇

河口盆地非线性地震效应及设计地震动参数

陈国兴1, 2,金丹丹1, 2,朱 姣1, 2,李小军3, 1   

  1. 1. 南京工业大学 岩土工程研究所,江苏 南京210009;2. 江苏省土木工程防震技术研究中心,江苏 南京210009; 3. 中国地震局地球物理研究所,北京100081
  • 收稿日期:2014-04-06 出版日期:2015-06-11 发布日期:2018-06-14
  • 通讯作者: 金丹丹,女,1987年生,博士研究生,主要研究场地地震效应。E-mail: jddnjut@163.com E-mail:gxchen@njut.edu.cn
  • 作者简介:陈国兴,男,1963年生,博士,教授,主要从事土动力学与岩土地震工程研究。
  • 基金资助:

    国家重点基础研究发展计划项目(No.2011CB013601);国家自然科学基金项目(No.51378258);国家自然科学青年基金项目(No.5130892)。

Nonlinear seismic response of estuarine basin and design parameters of ground motion

CHEN Guo-xing1, 2,JIN Dan-dan1, 2,ZHU Jiao1, 2,LI Xiao-jun3, 1   

  1. 1. Institute of Geotechnical Engineering, Nanjing Tech. University, Nanjing, Jiangsu 210009, China; 2. Civil Engineering & Earthquake Disaster Prevention Center of Jiangsu Province, Nanjing, Jiangsu 210009, China; 3. Institute of Geophysics, China Earthquake Administration, Beijing 100081, China
  • Received:2014-04-06 Online:2015-06-11 Published:2018-06-14

摘要: 针对基岩明显起伏、土层非均匀分布的典型河口盆地场地,考虑土体非线性特征,采用黏弹性人工边界模拟无限域对地震波动的影响,建立大尺度精细化二维有限元模型,分析了盆地地表地震动幅值、频谱、持时、传递函数特征,探讨了基岩起伏土层的地震动聚集效应及盆地边缘效应。结果表明:(1)盆地近地表土层表现出不同程度的地震动放大效应,且随土层深度增加呈非单调递减特征,基岩突变处地震动聚集效应明显,盆地两侧产生较为显著的边缘效应;场地中、长周期地震动的放大作用显著;(2)多遇地震、偶遇地震和罕遇地震水平时,场地卓越周期依次介于0.35~0.65 s、0.40~0.75 s和0.50~1.05 s之间;给出了盆地地表PGA(地表峰值加速度)、卓越周期均值等值线图及地表加速度反应谱放大因子建议值,地表设计地震动参数amax(地震影响系数)与Tg(特征周期)明显大于现行《建筑抗震设计规范》取值;(3)盆地特殊位置地表地震动持时得到不同幅度增长,且与输入地震动特性相关;(4)该盆地对0.5~2.0 Hz频段基岩地震动的放大效应比较显著,对小于0.2 Hz或大于2.5 Hz的基岩地震动,该盆地地震动放大效应不明显;(5)福州城区及其邻近区域地震动放大效应普遍较大。大尺度二维非线性分析一定程度上能合理反映微地形起伏、土层分布及土体非线性对地震波传播过程的影响。

关键词: 河口盆地, 非线性地震效应, 聚集效应, 边缘效应, 地表峰值加速度, 地震动持时, 设计地震动参数

Abstract: Based on the explicit FE method and parallel computing cluster platform of ABAQUS, a large-scale refined two-dimensional (2D) nonlinear FE model is developed in the time domain with considering the heterogeneity of ground soils, for a typical site on the estuarine basin with undulating bedrock and nonuniformly distributed soil layers. The artificial viscoelastic boundary condition is proposed for simulating the semi-infinite field, the main characteristics of basin surface ground motion are analyzed, including the motion amplitude, spectrum, duration and transfer functions, and the accumulation effect of ground motion and edge effect of basin are investigated. The results show that: (1) The amplification effect at different observation points on the basin ground surface is observed; and the peak ground acceleration(PGA)of basin ground surface displays a non-monotonic decrease with soil depth; the prominent accumulation effect is found to be at particular positions where the bedrock surface sharply undulates, and the pronounced edge effect is found to be on both sides of basin; the moderate and long-period ground motions of the basin are significantly amplified compared to the short-period motions. (2) For the earthquakes with high, moderate and low occurrence probabilities, the predominant periods of the basin are 0.35-0.65 s, 0.40-0.75 s and 0.50-1.05 s, respectively;the mean value contours of the peak ground acceleration and site predominant periods of the basin are plotted, and the recommended values of the amplification factor of ground motion acceleration response spectra for different period intervals are given. The seismic effect coefficient amax and characteristic period Tg of the design parameters of ground motion by this paper are significantly larger than those of the Chinese code for seismic design of buildings. (3) Ground motion durations at different points of basin ground surface extend over several orders, and the duration is also closely related to the bedrock motion characteristics. (4) Amplification effect and accumulating effect of the basin ground motion are more significant for the frequency band from 0.5 Hz to 2 Hz; while for the frequency band lower than 0.2 Hz or higher than 2.5 Hz, the ground motion amplification characteristics are insignificant. (5) Ground motion amplification effects in Fuzhou city downtown area and its adjacent areas of the basin are generally larger, compared to other areas. It is indicated that the large-scale two-dimensional nonlinear FE model can describe the influence of micro topographic relief and nonuniformly distributed basin soil layers on seismic wave propagation.

Key words: estuarine basin, nonlinear site seismic effect, focusing effect, edge effect, peak ground acceleration, duration of ground motion, design parameters of ground motion.

中图分类号: 

  • TU 475+1
[1] 许成顺, 豆鹏飞, 高畄成, 陈 苏, 杜修力, . 地震动持时压缩比对可液化地基地震反应 影响的振动台试验[J]. 岩土力学, 2019, 40(1): 147-155.
[2] 朱 姣,许汉刚,陈国兴, . 苏州第四纪深厚沉积层一维等效线性和非线性地震反应对比分析[J]. , 2018, 39(4): 1479-1490.
[3] 孔梦云 ,陈国兴 ,李小军 ,常向东 ,周国良,. 以剪切波速与地表峰值加速度为依据的地震液化确定性及概率判别法[J]. , 2015, 36(5): 1239-1252.
[4] 陈国兴 ,孔梦云 ,李小军 ,常向东 ,周国良,. 以标贯试验为依据的砂土液化确定性及概率判别法[J]. , 2015, 36(1): 9-27.
[5] 战吉艳 ,陈国兴 ,刘建达 ,李小军 . 远场大地震作用下大尺度深软场地的非线性地震效应分析[J]. , 2013, 34(11): 3229-3238.
[6] 战吉艳 ,陈国兴 ,刘建达. 深软场地大地震远场地震动反应特性分析[J]. , 2011, 32(S1): 507-0514.
[7] 刘建达,高俊锁,董卫国. 岩土工程中的设计地震动参数确定[J]. , 2007, 28(S1): 769-772.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 楚锡华,徐远杰. 基于形状改变比能对M-C准则与 D-P系列准则匹配关系的研究[J]. , 2009, 30(10): 2985 -2990 .
[2] 刘豆豆,陈卫忠,杨建平,谭贤君,周喜德. 脆性岩石卸围压强度特性试验研究[J]. , 2009, 30(9): 2588 -2594 .
[3] 王桂尧,李 斌,罗 军,付宏渊. 粉土基质吸力的新型量测装置与土-水特征研究[J]. , 2010, 31(11): 3678 -3682 .
[4] 卢应发,陈朱蕾,谢文良,吕志中. 垃圾卫生填埋中的一些岩土工程技术[J]. , 2009, 30(1): 91 -98 .
[5] 贾 强,应惠清,张 鑫. 锚杆静压桩技术在既有建筑物增设地下空间中的应用[J]. , 2009, 30(7): 2053 -2057 .
[6] 路军富,王明年,贾媛媛,喻 渝,谭忠盛. 高速铁路大断面黄土隧道二次衬砌施作时机研究[J]. , 2011, 32(3): 843 -848 .
[7] 王成华,安建国. 含扩径桩的群桩基础竖向承载性状数值分析[J]. , 2011, 32(S2): 580 -585 .
[8] 方 焘 ,刘新荣 ,耿大新 ,罗 照 ,纪孝团 ,郑明新 . 大直径变径桩竖向承载特性模型试验研究(I)[J]. , 2012, 33(10): 2947 -2952 .
[9] 胡万雨 ,陈向浩 ,林 江 ,况磊强 . 瀑布沟水电站砾石土心墙初次蓄水期原位钻孔渗流试验研究[J]. , 2013, 34(5): 1259 -1263 .
[10] 朱 星 ,许 强 ,汤明高 ,付小敏 ,周建斌 . 典型岩石破裂产生次声波试验研究[J]. , 2013, 34(5): 1306 -1312 .