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    循环荷载下饱和砂土流动性的细观机制

    Meso-Mechanism of Flowability of Saturated Sand Under Cyclic Loading

    • 摘要: 开展了砂土试样不排水循环三轴试验的颗粒流数值模拟,将颗粒接触力链按照强度量级划分为强、中、弱3种力链,讨论了初始有效围压及孔隙率对砂土试样各级力链的影响,探究了循环荷载下砂土试样液化进程中的力链演化规律以及其与砂土相变孔压比和平均流动系数之间的关系,定义了界限力链强度,并提出了以界限力链强度作为判断饱和砂土固液相变的细观依据,揭示饱和砂土在循环荷载下流动性的产生和演变机制.研究结果表明:随着围压提高,土体内部中、弱力链数量逐渐减少,而强力链数量增加明显;中力链数量会随着孔隙率的增加逐渐减少,而强力链和弱力链数量受孔隙率影响不明显;强力链数量在孔压比达到约0.8时完全消失,试样平均流动系数急剧增大;孔压比达到1.0时,中力链数量降低为0,弱力链数量达到稳定;最后,验证了将相变孔压比对应的最大力链强度定义为界限力链强度的合理性.

       

      Abstract: The particle flow numerical simulation was conducted to investigate the undrained cyclic triaxial test of sand samples.The particle contact forces were classified into strong,medium,and weak force chains based on their strength levels.The influence of initial effective confining pressure and porosity on the behavior of these force chains were discussed.The evolution law of force chain in the liquefaction process of sand samples under cyclic loading was investigated,along with its correlation to the phase transition pore pressure ratio and average flow coefficient.The boundary force chain strength was defined and proposed as the microscopic basis for assessing the solid-liquid phase change of saturated sand,revealing the generation and evolution mechanism of the fluidity under cyclic loading.The results indicate that as the confining pressure increases,there is a gradual reduction in the number of medium and weak force chains,while the number of strong force chains significantly increases.The number of force chains will gradually decrease with the increase porosity,while the number of strong chains and weak chains is minimally affected by porosity.The presence of strong chains diminishes completely when the pore pressure ratio reaches 0.8,while the average flow coefficient of the sample exhibits a sharp increase.When the pore pressure ratio reaches 1.0,medium force chain numbers disappear,and weak force chain numbers stabilize.Finally,the validity of designating the boundary force chain strength as the maximum force chain strength corresponding to the phase transition pore pressure ratio is ultimately confirmed.

       

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