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首页> 外文期刊>International journal of geomechanics >Liquefaction of Level Ground Unsaturated Sand Deposits Using a Validated Fully Coupled Analysis Procedure
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Liquefaction of Level Ground Unsaturated Sand Deposits Using a Validated Fully Coupled Analysis Procedure

机译:使用经过验证的全耦合分析程序液化地面不饱和砂土沉积物

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Liquefaction of unsaturated sands has been observed in laboratory tests and in the field. A comprehensive investigation of unsaturated sand deposits subjected to seismic loading, especially using validated computational tools, is still lacking. This paper presents an analysis procedure to study the response of level ground unsaturated sand deposits subjected to seismic loading. The analysis procedure is a fully coupled flow-deformation finite element code with solid skeleton displacements, pore water pressure, and pore air pressure as nodal variables. The stress-strain behavior of unsaturated sands is described by a coupled hydro-mechanical elastoplastic constitutive model that includes the hysteretic model for soil water characteristic curves and the hydro-mechanical coupling mechanisms. The finite element code is first validated by comparing simulations with centrifuge test results. Reasonable comparisons of surface accelerations, ground settlements, and lateral deformations are obtained. A parametric study is then conducted to investigate the effects of initial degree of saturation, relative density, and effective overburden pressure on the seismic response of level ground unsaturated sand deposits. The results of the parametric study show that the thickness of the liquefied layer increases with an increase in degree of saturation. The potential for liquefaction reduced with increases in relative density and effective overburden stress. The results also reveal a drastic reduction in surface accelerations following liquefaction of a sand deposit. (c) 2018 American Society of Civil Engineers.
机译:在实验室测试和现场中已经观察到不饱和砂的液化。仍然缺乏对地震荷载作用下的非饱和砂沉积物的综合研究,特别是使用经过验证的计算工具进行研究。本文提出了一种分析程序,以研究地震荷载作用下平整地面非饱和砂土沉积物的响应。分析过程是一个完全耦合的流动变形有限元代码,其中固体骨架位移,孔隙水压力和孔隙空气压力为节点变量。通过耦合的水力-弹塑性本构模型描述了非饱和砂土的应力-应变行为,该模型包括土壤水分特征曲线的滞回模型和水力耦合机制。首先通过将模拟与离心机测试结果进行比较来验证有限元代码。获得了表面加速度,地面沉降和横向变形的合理比较。然后进行参数研究,以研究初始饱和度,相对密度和有效上覆压力对水平地面非饱和砂沉积物地震响应的影响。参数研究的结果表明,液化层的厚度随饱和度的增加而增加。液化的可能性随着相对密度和有效上覆应力的增加而降低。结果还表明,在砂沉积物液化之后,表面加速度急剧降低。 (c)2018年美国土木工程师学会。

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