粒径多分散性和摩擦系数对湿式颗粒材料抗压强度的影响

Vo Thanh Trung, N. Kien
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引用次数: 0

摘要

采用离散元模拟方法,数值研究了湿颗粒粒径多分散性和摩擦系数对湿颗粒直径压缩强度的影响。数值方法与毛细黏聚规律相结合,毛细黏聚规律因颗粒间的内聚力而增强。湿颗粒由初生球形颗粒组成,颗粒间的摩擦系数在0.1 ~ 1.0之间,分散度在1 ~ 10之间。在准静态状态下,对顶板施加恒定的压缩速度,使颗粒变形,但由于颗粒之间的内聚作用和原生颗粒的重排,颗粒不会突然破裂。这种不突然破裂的特征是在颗粒开始破坏之前,在长垂直应变中出现峰值压应力。颗粒的抗压强度随摩擦系数的增加而增加,但当摩擦系数大于0.5时,颗粒的抗压强度呈下降趋势,当摩擦系数大于0.5时,颗粒的抗压强度趋于平稳。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effects of the size polydispersity and friction coefficient on the compressive strength of wet granular materials
We numerically study the effects of the size polydispersity and the friction coefficient on the compressive strength of wet granules under a diametrical compression test by using discrete element simulations. The nu-merical method is coupled with the capillary cohesion law which is enhanced by the cohesive forces between grains in the pendular regime. The wet granules are composed of primary spherical particles whose size poly-dispersity is varied from1 to 10 and the friction coefficient between grains is varied from0.1 to 1.0. By applying a constant compression velocity on the top plate in quasi-static regime, the granule is deformed but does not abruptly rupture due to the cohesive effects between grains and the rearrangement of primary particles. This no abrupt rupture is characterized by the appearance of the peak compressive stress in a long vertical strain before the onset failure of the granule. The compressive strength of the granule increases with increasing the friction coefficient for all cases of the size polydispersity but seemly declines for low values of the size polydispersity and almost level-off for high-size polydispersity with the friction coefficient larger than 0.5.
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