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Effect of K_0-condition on liquefaction characteristics of saturated sand

机译:K_0条件对饱和沙子液化特性的影响

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Examined are effect of an isotropic stress condition of sand on liquefaction and post-liquefaction behaviors. Both loose sand and dense sand are tested by means of cyclic torsional shear test in which both axial strain and radial stress are kept constant in order to reproduce an in-situ stress condition. The K_0-value at the time of consolidation before the cyclic loading (initial K_0-value), a ratio of lateral normal stress to the overburden stress, ranges from 0.67 to 2.5, while keeping the initial effective mean principal stress constant. Both liquefaction strength and post-liquefaction volumetric change caused by excess porewater pressure generation are examined. Liquefaction strength is the smallest when K_0 = 1.0, i.e., an isotropic stress states and increases as K_0-value increases or decreases. The increase is not so large for loose sand, but it increases up to 15% for dense sand. On the other hand, effect of K_0-value on the post-liquefaction volume change for dense sand is almost negligible. In case of loose sand, however, post-liquefaction volume change tends to increase with K_0-value.
机译:检查是沙子各向同性应力条件对液化和液化后行为的影响。通过循环扭转剪切测试测试松散的砂和致密的砂,其中轴向应变和径向应力均保持恒定,以便再现原位应力条件。在循环加载之前合并(初始K_0值)的k_0值,横向正常应力与覆盖压力的比率,范围为0.67至2.5,同时保持初始有效的平均主应力恒定。检查由过量沉降水压产生引起的液化强度和液化后体积变化。当K_0 = 1.0,即各向同性应力状态并且随着K_0值的增加而增加时,液化强度是最小的。松散的沙子的增加并不是那么大,但致密的沙子增加了15%。另一方面,K_0值对密集沙子的液化后体积变化的影响几乎可以忽略不计。然而,在松散的沙子的情况下,液化后体积变化趋于随K_0值而增加。

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