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含倾斜砂土夹层的人工岛地震液化灾害分析

胡记磊 唐小微 白旭 张西文

大连理工大学学报Issue(5):504-510,7.
大连理工大学学报Issue(5):504-510,7.DOI:10.7511/dllgxb201505009

含倾斜砂土夹层的人工岛地震液化灾害分析

Analyses of seismic liquefaction induced disaster in artificial island with sloping sand layer

胡记磊 1唐小微 2白旭 1张西文2

作者信息

  • 1. 大连理工大学 海岸和近海工程国家重点实验室,辽宁 大连 116024
  • 2. 大连理工大学 岩土工程研究所,辽宁 大连 116024
  • 折叠

摘要

Abstract

Liquefaction due to strong earthquake easily causes permanent displacement and strain of sloping sand layer in the fundament and induces the phenomena of flow slides,and then brings serious damages to the superstructure. Considering sloping sand layers' gradient, thickness, depth and seawater level synthetically, a two-dimensional offshore artificial island model was simulated numerically by FE-FD coupling finite element analysis method.The experimental results indicate that these four influence factors have different effects on the large deformation of artificial island in the course of seismic liquefaction.The influence of gradient is the greatest,and the influence of seawater level is the most non-obvious,and especially,its effect on excess pore water pressure is very small. Lateral spreading of artificial island j ust occurs after total liquefaction of saturated sloping sand layer in the course of seismic,which is a limit slide along the slope during a period of time.Its degree of damage is much bigger than that of damage induced by liquefaction of horizontal sand layer,and it easily causes serious differential settlement and damage of revetment of artificial island. These analytical results can provide reference for hazard evaluation of offshore engineering due to seismic liquefaction.

关键词

人工岛/地震/数值模拟/液化/倾斜砂土夹层/侧向滑移/沉降

Key words

artificial island/earthquake/numerical simulation/liquefaction/sloping sand layer/lateral spreading/settlement

分类

建筑与水利

引用本文复制引用

胡记磊,唐小微,白旭,张西文..含倾斜砂土夹层的人工岛地震液化灾害分析[J].大连理工大学学报,2015,(5):504-510,7.

基金项目

“九七三”国家重点基础研究发展计划资助项目(2011CB013605-2) (2011CB013605-2)

国家自然科学基金资助项目(51078062) (51078062)

大连理工大学学报

OA北大核心CSCDCSTPCD

1000-8608

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