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Stress-strain characteristics of remolded soil in the weathered layer of Beichuan sandy slate in Wenchuan seismic area

机译:汶川地震区北川沙滩岩土层倒塌土的应力 - 应变特征

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A great amount of surface destruction and soil disturbance are produced after the Wenchuan earthquake. The disturbed soil may easily cause erosion, collapse, landslide and other disasters. This paper studies the stress-strain relationship and strength of remolded soil through variables of confining pressure, shear rates, and consolidation time. The change of shear strength was discussed under different experimental conditions, and shearing process and deformation shapes were analyzed. The results show that stress-strain curves present strain-hardening phenomenon, and the confining pressure is the most influential among the variables. For the remolded soil, the cohesion is 20.99KPa and friction angle is 22.7°. When the soil strain reaches to 20%, there is no obvious failure surface, but only radial barrel deformation and well-balanced outside form.
机译:在汶川地震后产生了大量的表面破坏和土壤障碍。受扰动的土壤可能很容易引起侵蚀,塌陷,滑坡等灾难。本文通过限制压力,剪切速率和固结时间的变量研究重折叠土壤的应力 - 应变关系和强度。在不同的实验条件下讨论了剪切强度的变化,分析了剪切过程和变形形状。结果表明,应力 - 应变曲线存在应变硬化现象,并且限制压力是变量中最有影响力的。对于重折叠的土壤,凝聚力为20.99kpa,摩擦角为22.7°。当土壤应变达到20%时,没有明显的故障表面,但只有径向桶变形和良好的外部形式。

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