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PREDICTION OF LIQUEFACTION-INDUCED GROUND DEFORMATION

机译:预测液化引起的地面变形

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Prediction of liquefaction-induced ground deformation requires that the behavior of sand undergoing very low effective stress is understood experimentally. Previous 1-g model tests revealed a rate-dependent, or viscous, nature of liquefied sand. Since it was therein difficult to evaluate the rate-dependency more accurately, the present study carried out triaxial compression tests in a drained manner on Yurakucho sand with fines. The effective stress was maintained very low during shear by supplying high backpressure from outside. Creep tests in triaxial compression revealed that the shear stress consists of an inviscid frictional component and a rate-dependent component, and the study was focused on the latter. The test results demonstrated that the rate-dependent behavior of sand is similar to the Bingham model and that the effective stress of sand increases the magnitude of the viscous stress, enabling the rate-dependent deformation only under low effective stress. In contrast, the density of sand does not affect the rate-dependent nature significantly. The results of triaxial compression were supplemented by tests on triaxial extension as well as tests on special lightweight grains, where lower or null effective stresses were obtained. Finally, it is inferred that the cause of rate dependency is partly the vortex of pore fluid and partly the grain-to-grain collisions during shear deformation.
机译:液化引起的地面变形的预测要求通过实验了解砂子承受非常低的有效应力的行为。先前的1-g模型测试显示液化沙子具有速率依赖性或粘性。由于在其中难以更准确地评估速率相关性,因此本研究对细砂有乐町砂进行了排水的三轴压缩试验。通过从外部提供高背压,在剪切过程中有效应力保持非常低。在三轴压缩中的蠕变测试表明,剪切应力由不粘的摩擦分量和速率相关的分量组成,并且研究主要集中在后者上。测试结果表明,砂的速率依赖性行为与Bingham模型相似,并且有效应力提高了粘滞应力的大小,仅在低有效应力下才允许速率依赖性变形。相反,沙子的密度不会显着影响速率依赖性。三轴压缩的结果通过三轴延伸的测试以及特殊轻质晶粒的测试得到了补充,其中获得了较低或无效的有效应力。最后,可以推断出速率依赖性的原因部分是孔隙流体的涡旋,部分是剪切变形过程中的颗粒间碰撞。

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