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Unique determination of cyclic instability state in flow liquefaction of sand

机译:砂液化循环失稳状态的独特测定

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Flow liquefaction is a catastrophic failure phenomenon of loose sand when subjected to wave or seismic load, and an instability state can be regarded as the onset of flow liquefaction. Most of the previous studies focused mainly on the static instability state, while the investigations on cyclic instability state (CIS) are very limited and unsystematic. The characteristics of CIS are complex and there is no clear consensus about the determination of CIS. Therefore, this study aims to investigate the characteristics of CIS in flow liquefaction via a series of undrained triaxial tests performed on saturated loose sand. The testing program covers a broad range of initial deviatoric stressesq(s), cyclic stress amplitudesq(cyc), and relative densitiesD(r). The test results indicate that CIS will occur at either compressive side or extensive side, depending uniquely on the ratio ofq(s)/q(cyc). The slopes of CIS lines increase with an increase in the relative density. Under the sameq(cyc), the mean effective stress at CIS first decreases and then increases asq(s)increases. Finally, CIS is predicted by a useful method, which is able to monitor CIS both in situ and in laboratory tests.
机译:流动液化是松散砂在波浪或地震荷载作用下的灾难性破坏现象,失稳状态可视为流动液化的开始。以往的研究大多主要集中在静态失稳态,而对循环失稳态(CIS)的研究非常有限且不系统。CIS的特点复杂,对CIS的确定尚无明确的共识。因此,本研究旨在通过对饱和松散砂进行一系列不排水三轴试验,研究流动液化中CIS的特征。测试程序涵盖广泛的初始偏应力q(s)、循环应力振幅sq(cyc)和相对密度D(r)。测试结果表明,CIS将发生在压缩侧或广泛侧,唯一取决于q(s)/q(cyc)的比值。CIS线的斜率随着相对密度的增加而增加。在相同q(cyc)下,CIS处的平均有效应力先减小后增大。最后,CIS是通过一种有用的方法预测的,该方法能够在原位和实验室测试中监测CIS。

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