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A discrete element analysis of the micromechanical interaction of non-spherical particles in cohesionless granular solids under Ko condition

机译:在KO条件下粘性颗粒固体中非球形颗粒的微机械相互作用的离散元素分析

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The coefficient of earth pressure at rest Ko is often used to determine the stress state of a soil in the design of retaining walls, excavations and foundations. The most commonly used equation was proposed originally by Jaky (1944) which expresses the ratio of horizontal to vertical stress in a normally consolidated soil as K_0 = 1 - sin Φ, where Φ is the effective angle of internal friction of the soil. This raises the question as to why the at rest stress state in a soil, which is not at failure,should be governed by the failure friction angle of the soil. The expression is often reported as empirical in nature however, Jaky arrived at the expression from an analytical approach. This paper explores the micromechanics of cohesionless soils by investigating the effect of soil fabric and the evolution of the lateral pressure under confined compression using the Discrete Element Method (DEM). Many DEM models use spherical particles due to their greater efficiency. However, particle sphericity leads to the over-prediction of the lateral pressure ratio for a typical granular soil during a confined K_0 compression test. The lack of particle interlocking that is associated with spherical particles leads to a greater transmission of forces laterally in an assembly under confined compression, resulting in a higher K_0 value.
机译:静止KO的地球压力系数通常用于确定挡土墙,挖掘和基础设计中的土壤的应力状态。最初由Jaky(1944)最初提出了最常用的方程,其表示水平与垂直应力的比率在通常固结的土壤中作为K_0 = 1 - SINφ,其中φ是土壤的内部摩擦的有效角度。这提出了为什么在土壤中的静静压力状态为什么不发生故障的原因,应该受土壤的失效摩擦角度的管辖。表述通常作为实证在自然中被报告,抖动从分析方法到达表达。本文通过采用分立元素法(DEM)来研究土壤织物的影响和横向压力下横向压力下横向压力的效果来探讨粘性土壤的微机械。许多DEM模型由于其提高效率而使用球形颗粒。然而,颗粒球性导致在狭窄的K_0压缩试验期间典型粒状土壤的横向压力比的过度预测。缺乏与球形颗粒相关的粒子互锁导致在限制压缩下横向横向延伸的力较大,导致较高的K_0值。

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