基于PFC2D的土石混合料剪切强度数值模拟分析
Numerical simulation of shear strength of rock-soil mixtures by using PFC2D
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摘要: 广泛应用于高填方工程中的土石混合料,具有显著的非均质、非连续特征,工程特性不仅取决于土和石本身的力学性质,也与土石相对比例、粒组组成等因素密切相关。结合PFC2D离散元数值模拟,分析不同开缝宽度下缺失中间粒径土石混合料的抗剪强度变化规律,深入探讨缺失中间粒径土石混合料骨架结构的力传递路径、强度形成机理及混合料变形破坏机制,结果表明:上下剪切盒之间开缝宽度对其抗剪强度有重要影响,土石混合料的峰值强度随开缝宽度的增加而降低,抗剪强度-水平位移曲线表现为应变软化;开缝宽度对土石混合料骨架构成也有重要影响,开缝越大,构成骨架的颗粒数目就越少,骨架颗粒分布范围也越小,剪切带越靠近上剪切盒;不同开缝宽度情况下,尽管剪切带分布不同,骨架上颗粒法向接触力分布基本上是均匀的,说明骨架上各个颗粒受力是相对均匀的,骨架颗粒受力与开缝宽度并无明显关系;不同的开缝宽度下,剪切面在各剪切阶段均不是一个平面,随着水平剪切位移的增加,土骨架上的接触力链和剪切带分布也不断发生变化,试样内部受力极不均匀;试样内部脱空现象除与土石混合料骨架组成、颗粒摩擦系数及级配有关外,开缝宽度对其也有重要影响,开缝越宽,剪切过程中试样的脱空现象就越明显。Abstract: The soil-rock mixture widely used in high-fill projects is characterized by significant heterogeneity and discontinuity. The engineering characteristics of the mixture depend on the mechanical properties of soil and stone and closely relate to the relative proportion of earth and stone, particle composition and other factors. Based on the PFC2D discrete element numerical simulation, the change rules of shear strength of the soil-rock mixture with missing intermediate particle size under different opening widths are analyzed, and the force transfer path, strength formation mechanism and deformation and failure mechanism of the mixture skeleton structure with missing intermediate particle size are deeply disscussed. The results show that the width of the opening between the upper and lower shear boxes has an important influence on the shear strength. The peak strength of the earth-rock mixture decreases with the increase of the opening width, and the shear strength-horizontal displacement curve shows strain softening. The opening width also has a significant influence on the skeleton composition of the earth-rock mixture. The larger the opening is, the less the number of the skeleton particles is, the larger the distribution range of skeleton particles is, the closer the shear band is to the upper shear box. Although the distribution of shear band is different under different opening widths, the distribution of normal contact force of particles on the skeleton is basically uniform, which shows that the stress of particles on the skeleton is relatively uniform, and there is no obvious relationship between the stress of particles on the skeleton and the opening width. Under different opening widths, the shear plane is not a plane at each shear stage. With the increase of horizontal shear displacement, the distribution of contact force chain and shear band on the skeleton also changes constantly, and the stress inside the samples is extremely uneven. The phenomenon of void inside the samples is related to the skeleton composition, friction coefficient of particles and gradation of the earth-rock mixture, and the opening width also has an important influence on them. The wider the opening, the more obvious the void phenomenon of the sample during the shear process.