FIELD AND LABORATORY INVESTIGATIONS INTO THE BEHAVIOR OF SILTY SANDS THAT LEADS TO LIQUEFACTION TRIGGERING

FIELD AND LABORATORY INVESTIGATIONS INTO THE BEHAVIOR OF SILTY SANDS THAT LEADS TO LIQUEFACTION TRIGGERING
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对导致液化触发的粉砂行为进行现场和实验室调查

DOI:
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发表时间:
2016
期刊:
影响因子:
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通讯作者:
F. Menq
F. Menq
中科院分区:
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文献类型:
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作者:
J. Roberts;K. Stokoe;F. Menq

文献摘要

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自20世纪80年代以来,加州帝国谷的野生动物液化阵列(WLA)一直是正在进行的地震和土壤液化研究的焦点。在本文中,从五个独立的土壤液化研究的结果进行了检查和数据相结合,开发一个更全面的分析,在WLA网站的可液化土壤的行为。实验数据来自三种类型的现场试验(CPT,跨孔地震和全尺寸,原位振动试验)和两种类型的室内试验(共振柱和循环三轴)。本文介绍的工作是努力确认和推进现场液化试验,使用大型,液压操作的振动筛,通过检查以前的三个实验的结果,并将它们与实验室测试和数据拟合模型的结果进行比较的一部分。作者认为,超静孔压的产生导致土壤液化的触发是一个应变控制的现象,目前的结果进一步支持这一理论。针对WLA场地可液化土壤的关键发现包括:(1)孔隙压力产生阈值应变(γt)的现场识别,(2)开发孔隙压力产生模型的现场数据,以及(3)开发修改后的双曲线剪切模量折减关系。
Since the 1980s, the instrumented Wildlife Liquefaction Array (WLA) in Imperial Valley, California, has been the focus of ongoing seismic and soil-liquefaction research. In this paper, the results from five separate soil liquefaction studies are examined and the data are combined to develop a more comprehensive analysis regarding the behavior of liquefiable soils at the WLA site. The experiment data are derived from three types of field tests (CPT, crosshole seismic, and full-scale, in-situ shaking tests) and two types of laboratory tests (resonant column and cyclic triaxial). The work presented herein is part of an effort to confirm and advance in-situ liquefaction testing using large, hydraulically-operated shakers by examining the results of three previous experiments and comparing them with the results from laboratory testing and data-fitted models. The authors believe that the triggering of excess pore pressure generation leading to soil liquefaction is a strain-controlled phenomenon and present results in further support of this theory. Key findings specific to the liquefiable soil at the WLA site include: (1) field identification of the threshold strain for pore pressure generation (γt), (2) field data for development of a pore pressure generation model, and (3) development of a modified hyperbolic shear modulus reduction relationship.