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MACRO AND MICRO MECHANICAL BEHAVIOUR OF CRUSHABLE SOIL UNDER COMPRESSION

机译:压缩下可抵碎土壤的宏观和微力学行为

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The simulation for a numerical grain and its assembly using DEM and one-dimensional compression tests for many soils were carried out to understand the compression properties of sands through examination of particle crushing strengths. From the simulation, the tensile breaking modes led to large fragmentation of agglomerate in collective crushing (yield point) as similar to single agglomerate crushing. This common micro-mechanical feature gives a justifiable comparison between the yield stress and the single particle crushing strength, although the yield stress is also related to initial voids ratio, grain size and its distribution. But material having a higher particle crushing strength do not necessarily give a higher yield stress. This is because in a uniform material a small proportion of the particles transmit large forces.
机译:对数值晶粒及其组装使用DEM和一维压缩试验的模拟进行了许多土壤,以了解砂体通过粒子破碎强度的压缩性能。 从模拟中,拉伸破碎模式导致集体压碎(屈服点)的聚集体的大碎片化,与单聚集体压碎相似。 这种常见的微力特征在屈服应力和单颗粒破碎强度之间提供了正当的比较,尽管屈服应力也与初始空隙率,粒度及其分布有关。 但具有更高粒子破碎强度的材料不一定产生更高的屈服应力。 这是因为在统一的材料中,小比例的颗粒透射了大力。

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