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自重、渗流及地震耦合作用下人工岛动力稳定性分析
引用本文:赖杰,郑颖人,李秀地. 自重、渗流及地震耦合作用下人工岛动力稳定性分析[J]. 振动与冲击, 2016, 35(5): 175-180
作者姓名:赖杰  郑颖人  李秀地
作者单位:1.后勤工程学院 军事土木工程系,重庆 401311;
2. 重庆市地质灾害防治工程技术研究中心,重庆 400041;
3.岩土力学与地质环境保护重庆市重点试验室,重庆 401311
摘    要:针对人工岛在自重、渗流、地震等耦合作用下动力稳定性研究较少的现状,以某人工岛边坡为例,首次将强度折减动力分析法引入到人工岛动力稳定性分析中,建立有限元数值分析模型,采用Finn-Byrne和修正Hardin-Drnevich动力本构,对多场耦合作用下人工岛液化范围、受力情况及动力稳定性进行分析。计算表明:1)在设防烈度地震作用下,人工岛能够满足动力稳定性要求,由于海底淤泥层抗剪强度很低,地震下的最终破裂面由抛填块石下部与淤泥层共同组成;2)岛内侧降水,使得海水渗流方向由岛外指向岛内,增加岛外侧土体有效应力,提高其抗液化能力,降低了岛内土体的有效应力,因此地震作用下内侧土体更易液化;3)由于受到周围土体的约束作用,土体局部液化不会产生液化大变形,只有液化土体较多才会产生大变形。研究结果为人工岛动力分析提供参考。

关 键 词:人工岛  渗流  强度折减动力分析法  液化  

Dynamic stability analysis on an artificial island triggered by self weight,seepage and earthquake#br#
LAI Jie,ZHENG Yingren,LI Xiudi. Dynamic stability analysis on an artificial island triggered by self weight,seepage and earthquake#br#[J]. Journal of Vibration and Shock, 2016, 35(5): 175-180
Authors:LAI Jie  ZHENG Yingren  LI Xiudi
Affiliation:1. Department of Civil Engineering,Logistical Engineering University,Chongqing 401311,China;2. Chongqing Engineering and Technology Research Center of Geological Hazard Prevention and Treatment, Chongqing 400041,China
Abstract:
Because there was little research on artificial island under the action of gravity, seepage, earthquake and other coupling forces, strength reduction dynamic analysis method was introduced to the dynamic stability on an artificial island. Establish finite element numerical model and use dynamic constitutive equations of Finn-Byrne as well as modified Hardin-Drnevich for this artificial island under earthquake. Analyze the scope of liquefaction, stress distribution, and dynamic stability. Calculation results show that: 1) this island can meet the requirement of dynamic stability. Because shear strength of muck layer is quite low, the final fracture surface is composed by the lower part of stone and mud layer under earthquake; 2) owing to precipitation, water seepage flow from outside to inside of the island, effective stress and liquefaction resistance of soil increase from the outside of the island, however, the ones from inside of the island get lower. So the soil from outside is more likely to be liquefied; 3) due to the constraints of surrounding soils, soil liquefaction won't lead to high deformation, only more liquefied soil can do. The results provide reference for dynamic analysis of the artificial island. 
Keywords:artificial island  seepage  strength reduction dynamic analysis method  liquefaction
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