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Experimental validation study of 3D direct simple shear DEM simulations

机译:3D直接简单剪切DEM模拟的实验验证研究

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Simple shear element tests can be used to examine numerous geotechnical problems; however, the cylindrical sample (NGI-type) direct simple shear (DSS) device has been criticized for its inability to apply uniform stresses and strains, as well as for its inability to fully define the stress state of the soil during shearing. Discrete element method (DEM) simulations offer researchers a means to explore the fundamental mechanisms driving the overall behavior of granular soil in simple shear and to improve the understanding of the DSS device itself. Here, three-dimensional DEM simulations of laminar NGI-type direct simple shear element tests and equivalent physical tests are compared to validate the numerical model. This study examines the sensitivity of the DEM simulation results to sample size, contact model and stiffness inputs, and ring wall boundary effects. Sample inhomogeneities are also considered by examining the radial and vertical void ratio distributions throughout the samples. Both the physical experiments and the DEM simulations presented herein indicate that the observed material response is highly sensitive to the particle size relative to the sample dimensions. The results show that samples with a small number of relatively large particles are very sensitive to small changes in packing; and thus, an exact match with the DEM simulation data cannot be expected. While increasing the number of particles greatly improved the agreement of the volumetric and stress strain responses, the dense DEM samples were still initially much stiffer than the experimental results. This is most likely due to the fact that the inter-particle friction was artificially lowered, during the sample preparation for the DEM simulations, in order to increase the sample density. (C) 2016 The Japanese Geotechnical Society. Production and hosting by Elsevier B.V. All rights reserved.
机译:简单的剪切单元测试可以用来检查许多岩土工程问题。然而,圆柱形样品(NGI型)直接简单剪切(DSS)设备因无法施加均匀的应力和应变,并且无法完全确定剪切过程中土壤的应力状态而受到批评。离散元素法(DEM)模拟为研究人员提供了一种方法,可探索在简单剪切条件下驱动粒状土壤整体行为的基本机制,并增进对DSS设备本身的了解。在此,比较了层状NGI型直接简单剪切元件测试和等效物理测试的三维DEM仿真,以验证数值模型。这项研究检查了DEM模拟结果对样本大小,接触模型和刚度输入以及环壁边界效应的敏感性。还可以通过检查整个样品的径向和垂直空隙率分布来考虑样品的不均匀性。本文介绍的物理实验和DEM模拟均表明,相对于样品尺寸,观察到的材料响应对粒径高度敏感。结果表明,带有少量相对较大颗粒的样品对堆积的细微变化非常敏感。因此,无法期望与DEM仿真数据完全匹配。尽管增加颗粒数量大大改善了体积和应力应变响应的一致性,但最初的致密DEM样品仍比实验结果坚硬得多。这很可能是由于在增加DEM模拟的样品制备过程中,人为降低了颗粒间摩擦的事实。 (C)2016年日本岩土学会。 Elsevier B.V制作和托管。保留所有权利。

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