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Material Strength, Capillary Effect and Fabric Anisotropies of Unsaturated Granular Materials in thePendular State

机译:材料强度,毛细血管效应和织物围绕不饱和颗粒材料的各向异性

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Water content is an important parameter affecting soil properties which is concerned in slope stability analysis and surface excavations.With a small amount of water adding into a granular material,generally less than 20% degree of saturation,isolated water bridges are formed between soil particles in contact or within a small distance.This state is named as thependular state.The air-water interfacial energy and the air-water pressure difference (the matric suction) are acting through the liquid bridges as cohesive forces and the soil strength and dilatancy are increased.With the aid of the Discrete Element Method (DEM), this paper aims to investigate the relationship between material strength, capillary effect and fabric anisotropies in the wet granular material, which could enhance the fundamental principles of unsaturated soil mechanics.By implementing the capillary effect between spherical particles,unsaturated granular materials are simulated in DEM and the mechanical properties and the micro-mechanisms are investigated by triaxial compression tests.The directional statistical theory is employed and the internal fabrics and particle scale interactions are formulated by direction tensors.By decomposing the total stress into a contact stress tensor which is associated with mechanical contacts and a capillary stress tensor determined by capillary effect,a Stress-Force-Fabric (SFF) relationship is proposed for unsaturated granular materials.It links the the material strength with the mean contact and capillary force level, solid contact and water bridge intensity and the anisotropic effects in solid skeleton and water bridge network respectively.By applying the SFF theory,it is observed that the solid skeleton in wet granular materials is less anisotropic than that in a dry sample undertriaxial shearing.The water phase anisotropy evolves with the soil skeleton deformation but it is less significant than that in the solid phase.This work also explains that the capillary cohesion is mainly induced by the capillary bonding effect on coordination numbers and mean contact force levels.
机译:含水量是影响缺陷稳定性分析和表面挖掘的土壤性质的重要参数。将少量的水加入粒状材料,通常小于20%的饱和度,在土壤颗粒之间形成分离的水桥触点或在较小的距离内。该状态被命名为截头状态。空气 - 水界面能量和空气 - 水压差(测距吸力)通过液体桥接作为粘性力,土壤强度和稀释性增加与离散元素法(DEM)的帮助,本文旨在探讨湿颗粒材料中材料强度,毛细血管效应和织物各向异性之间的关系,这可以增强不饱和土机械的基本原理。在实施毛细管球形颗粒之间的效果,在DEM和机械性能中模拟不饱和颗粒材料通过三轴压缩试验研究了微机构。采用定向统计理论,并通过方向张量配制内部织物和粒子刻度相互作用。将总应力分解成与机械触点相关的接触应力张量。毛细应力张量来确定通过毛细管作用,一 - 力 - 织物应力(SFF)关系,提出了不饱和的粒状materials.It链路的材料强度与平均接触和毛细管力水平,固体接触和水桥强度和各向异性效果在固体骨架和水桥网络中分别。施加SFF理论,观察到湿颗粒材料中的固体骨架比在干燥样品下剪切的各向异性较小。水相各向异性随着土壤骨架变形而发展,但它比固体相当不大。这项工作也解释说,Capil淋式的内聚力主要由毛细血管键合效应对配位数和平均接触力水平诱导。

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