Variation characteristics analysis of sandstone strength parameters in discrete element method by using internal scale ratio

IF 2.8 3区 工程技术 Q1 MATHEMATICS, INTERDISCIPLINARY APPLICATIONS
Yao Zhang, Shaoqiang Guo, Xiaotao Yin
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Abstract

The mesostructural characteristics of sandstone determine its macro-engineering characteristics. To better understand the relationship between cohesion of sandstone particles and strength in the present study, the FISH programming language was used to design a particle flow test program and conduct uniaxial compression tests of geomaterials. Twelve numerical specimens with diameters of 0.05, 0.1, 0.2, 0.4, 0.6, 0.8, 1.0, 1.2, 1.4, 1.6, 1.8, and 2.0?mm were designed for uniaxial compression tests. A total of 41 tests were carried out to simulate three bond strengths between particles with no friction and 19 internal friction angles from 0° to 90° under weak and strong bonding conditions. According to the failure modes and stress–strain curves of the specimens, the influence of the inner scale ratio on the particle flow was analyzed. The following particular phenomena were observed: (1) With the increase in the bond strength between particles, it was more difficult for the particles to rupture, and the number of micro-cracks was drastically reduced. (2) When the bond strength remained constant, the failure modes before and after the internal friction angle of 45° were completely different, which was related to the shear failure angle. (3) The curve dropped significantly after the strong bonding peak, and the brittle failure characteristics were evident. (4) The changes in the strength parameters between particles did not change the energy transfer mode, and the change of the bond strength increased the proportion of the strain energy in the input energy. (5) In the case of weak bonding, the proportion of the strain energy in the input energy gradually decreased with the increase in the internal friction angle. When the bond was strong, the proportion of the strain energy was stable, with an insignificant decrease as the internal friction angle increased.

Abstract Image

采用内标度比的离散元法分析砂岩强度参数变化特征
砂岩的细观结构特征决定了其宏观工程特征。为了更好地理解砂岩颗粒的黏聚力与强度之间的关系,本研究采用FISH编程语言设计颗粒流试验程序,对岩土材料进行单轴压缩试验。12个直径为0.05、0.1、0.2、0.4、0.6、0.8、1.0、1.2、1.4、1.6、1.8和2.0的数值试样?Mm为单轴压缩试验设计。共进行了41次试验,模拟了弱和强粘结条件下无摩擦颗粒间的3种粘结强度和0°~ 90°19个内摩擦角。根据试样的破坏模式和应力-应变曲线,分析了内垢比对颗粒流动的影响。观察到以下特殊现象:(1)随着颗粒间结合强度的增加,颗粒破裂的难度增大,微裂纹数量急剧减少。(2)粘结强度一定时,内摩擦角为45°前后的破坏模式完全不同,这与剪切破坏角有关。(3)强粘结峰后曲线明显下降,脆性破坏特征明显。(4)颗粒间强度参数的变化并未改变能量传递方式,粘结强度的变化增加了应变能在输入能量中的比例。(5)在弱粘结情况下,应变能占输入能量的比例随着内摩擦角的增大而逐渐减小。当粘结较强时,应变能所占比例稳定,随着内摩擦角的增大,应变能所占比例降低不显著。
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来源期刊
Computational Particle Mechanics
Computational Particle Mechanics Mathematics-Computational Mathematics
CiteScore
5.70
自引率
9.10%
发文量
75
期刊介绍: GENERAL OBJECTIVES: Computational Particle Mechanics (CPM) is a quarterly journal with the goal of publishing full-length original articles addressing the modeling and simulation of systems involving particles and particle methods. The goal is to enhance communication among researchers in the applied sciences who use "particles'''' in one form or another in their research. SPECIFIC OBJECTIVES: Particle-based materials and numerical methods have become wide-spread in the natural and applied sciences, engineering, biology. The term "particle methods/mechanics'''' has now come to imply several different things to researchers in the 21st century, including: (a) Particles as a physical unit in granular media, particulate flows, plasmas, swarms, etc., (b) Particles representing material phases in continua at the meso-, micro-and nano-scale and (c) Particles as a discretization unit in continua and discontinua in numerical methods such as Discrete Element Methods (DEM), Particle Finite Element Methods (PFEM), Molecular Dynamics (MD), and Smoothed Particle Hydrodynamics (SPH), to name a few.
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