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Analysis of bender element test interpretation using the discrete element method

机译:弯曲单元测试解释的离散单元法分析

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摘要

While bender element testing is now well-established as a laboratory technique to determine soil stiffness, a robust technique to interpret the data remains elusive. A discrete element method (DEM) model of a face-centred cubic packing of uniform spheres was created to simulate bender element tests to investigate this test from a fundamental perspective. During the DEM simulations transmitter and receiver signals were recorded, analogous to the data available in laboratory tests, and these macro-scale data were supplemented with particle scale measurements (forces, stresses and displacements). A range of approaches previously applied in experimental and numerical studies were used to analyse the resulting data in both the time and frequency domains. The shortcomings in these approaches are clear from the differences in the resultant shear stiffness values and the frequency-dependent nature of the values. The particle-scale data enabled visualization of the passage of the wave through the sample, and it was found not to be possible to precisely link the arrival of the shear wave at the receiver and any of the previously proposed character- istic points along the signal recorded at the receiver. The most reliable determination of the shear wave velocity was obtained by applying a two-dimensional fast Fourier transform (2D FFT) to the data describing the velocity of the particles lying between the transmitter and receiver elements. Use of the DEM model and this 2D FFT approach facilitated the sensitivity of the system response to small variations in the interparticle force-displacement law (the contact model) to be established.
机译:现在,弯曲机元件测试已经成为一种确定土壤刚度的实验室技术,而可靠的解释数据的技术仍然难以捉摸。创建了均匀球面为中心的立方堆积的离散元素方法(DEM)模型,以模拟弯曲器元素测试,以从基本的角度研究该测试。在DEM模拟过程中,记录了发射机和接收机的信号,类似于实验室测试中可用的数据,并且这些宏尺度数据还附加了微粒尺度测量(力,应力和位移)。先前在实验和数值研究中应用的一系列方法被用来分析时域和频域中的结果数据。这些方法的缺点从所得的剪切刚度值的差异以及这些值的频率相关性质中可以明显看出。粒子尺度数据可以使波穿过样品的过程可视化,并且发现不可能精确地将剪切波到达接收器和沿信号的任何先前提出的特征点联系起来记录在接收器上。剪切波速度的最可靠确定是通过对描述发射器和接收器元件之间的粒子速度的数据进行二维快速傅里叶变换(2D FFT)获得的。 DEM模型和这种2D FFT方法的使用提高了系统对要建立的粒子间力-位移定律(接触模型)的微小变化的敏感性。

著录项

  • 来源
    《Granular matter》 |2015年第2期|197-216|共20页
  • 作者单位

    Ground Engineering Buro Happold, 17 Newman St., London W1T 1PD, UK;

    Department of Civil and Environmental Engineering, Imperial College London, South Kensington, London SW6 2AZ, UK;

    School of Geosciences, Utrecht University, 3584 CD Utrecht, The Netherlands;

    Division of Civil Engineering, University of Dundee, Dundee DD1 4HN, UK;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    DEM; Wave propagation; Small-strain stiffness; Contact model;

    机译:DEM;波传播;小应变刚度;接触模型;

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