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Image based local deformation measurement of saturated sand specimen in undrained cyclic triaxial tests

机译:不排水三轴试验中基于图像的饱和砂土局部变形测量

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To evaluate the local deformation properties of sand specimen directly in the undrained triaxial test, a procedure based on Particle Image Velocimetry was developed through using a transparent membrane. Cylindrical specimens using a mixture of silica sand particles in black and white colors were prepared by the moist tamping method with five sand layers and the air pluviation method. Comparisons of local deformations between the direct evaluation by sand particles patterns and indirect evaluation by dots pasted on the membrane were made for a single specimen. The results obtained in the undrained cyclic triaxial tests revealed that the local deformation properties of medium dense and dense silica sand specimens evaluated by the indirect observation were consistent with those evaluated by the direct observation before the onset of initial liquefaction, except for some regions near the bottom ends of the specimen. Unlike the air pluviation method, the moist tamping method induced undesirable stratification within the specimen, and this resulted in the occurrence of specimen necking. Meanwhile, a non-uniform local strain distribution was observed along the specimen prepared by moist tamping method even under an axial strain less than 2%. The relative movement between the membrane and sand specimen, or slippage, occurred at the liquefied status. The extent of vertical slippage was also impacted by the relative density of the specimen. (C) 2018 Production and hosting by Elsevier B.V. on behalf of The Japanese Geotechnical Society.
机译:为了在不排水的三轴试验中直接评估砂试样的局部变形特性,通过使用透明膜开发了一种基于粒子图像测速的程序。通过湿式夯实法(五个砂层)和空气浸没法,制备了使用黑色和白色硅砂颗粒混合物制成的圆柱试样。对于单个样本,比较了通过砂粒图案进行的直接评估与通过将其粘贴在膜上的点进行的间接评估之间的局部变形。在不排水的三轴试验中获得的结果表明,通过间接观察评估的中等致密和致密硅砂样品的局部变形特性与初始液化开始之前通过直接观察评估的局部变形特性相一致,除了附近的一些区域。样品的底端。与空气浸没法不同,湿式夯实法在样品内引起不希望的分层,这导致样品颈缩的发生。同时,即使在轴向应变小于2%的情况下,沿通过湿夯法制备的样品也观察到不均匀的局部应变分布。膜和砂样品之间的相对运动或打滑发生在液化状态。垂直滑移的程度也受样品的相对密度影响。 (C)2018年由Elsevier B.V.代表日本岩土工程学会制作和托管。

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