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Microscopic contact model of lunar regolith for high efficiency discrete element analyses

机译:用于高效离散元素分析的月牙石的微观接触模型

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摘要

The grains of lunar regolith are characterized with rough surfaces, angular shapes and mutual adhesions due to short-range interactions. These features control the macroscopic mechanical behavior of lunar regolith but have not been completely captured by contact models in previous Discrete Element method (DEM) analyses. In this paper, a simplified two-dimensional microscopic contact model is proposed for high efficiency DEM analyses of lunar regolith. The model consists of three components in the normal, tangential and rolling directions respectively, plus two new parameters. A shape parameter is used to control the rolling resistance ability at the contact area between two particles to capture the features of grain shape and interlocking. The second parameter, micro-separation, which denotes the nominal minimum distance between the molecules of the two contacting particles, is introduced to account for van der Waals force as the major component of the short-range interactions that contribute to the adhesion of regolith grains in lunar environment conditions. The novel model has been implemented in a two-dimensional DEM code for numerical simulations of biaxial compression tests on lunar regolith. The effects of interparticle friction, grain shape, lunar environment conditions and void ratio on the strength of lunar regolith were numerically investigated. The results show that soils in the simulated lunar environment exhibit greater strength and more apparent strain-softening and shear dilatancy than on the Earth. The proposed model can capture the main features of the mechanical behavior of lunar regolith (apparent cohesion and high peak friction angle) and a wide range of strength indices can be obtained by the contact model.
机译:由于短程相互作用,月牙长石的颗粒具有粗糙的表面,角形和相互粘附的特征。这些特征控制着月球重石的宏观力学行为,但在先前的离散元素方法(DEM)分析中并未被接触模型完全捕获。本文提出了一种简化的二维微观接触模型,用于月球巨石的高效DEM分析。该模型分别由在法线,切向和滚动方向上的三个组件组成,外加两个新参数。形状参数用于控制两个粒子之间接触区域的滚动阻力能力,以捕获晶粒形状和互锁的特征。第二个参数是微分离,它表示两个接触粒子的分子之间的标称最小距离,它被引入来说明范德华力是短程相互作用的主要组成部分,这有助于重新形成go石颗粒在月球环境条件下。该新型模型已在二维DEM代码中实现,用于对月球巨石进行双轴压缩测试的数值模拟。数值研究了颗粒间的摩擦,晶粒形状,月球环境条件和空隙率对月球巨石强度的影响。结果表明,与地球相比,模拟月球环境下的土壤具有更大的强度,更明显的应变软化和剪胀性。所提出的模型可以捕获月牙巨石的力学行为的主要特征(表观内聚力和高峰值摩擦角),并且通过接触模型可以获得广泛的强度指标。

著录项

  • 来源
    《Computers and Geotechnics》 |2013年第10期|104-116|共13页
  • 作者单位

    Department of Geotechnical Engineering, College of Civil Engineering, Tongji University, Shanghai 200092, China,Key Laboratory of Geotechnical and Underground Engineering of Ministry of Education, Tongji University, Shanghai 200092, China;

    Department of Geotechnical Engineering, College of Civil Engineering, Tongji University, Shanghai 200092, China,Key Laboratory of Geotechnical and Underground Engineering of Ministry of Education, Tongji University, Shanghai 200092, China;

    School of Chemical Engineering, University of Birmingham, Edgbaston, Birmingham B15 2TT, UK;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Lunar regolith; Discrete Element method; Contact model; Rolling resistance; Van der Waals force;

    机译:月球离散元法;接触模型;滚动阻力;范德华力;

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