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蔡国庆, ASREAZADSaman, 刘超, 赵成刚. 非饱和粉砂临界状态的试验研究[J]. 岩土工程学报, 2018, 40(S1): 8-8. DOI: 10.11779/CJGE2018S1002
引用本文: 蔡国庆, ASREAZADSaman, 刘超, 赵成刚. 非饱和粉砂临界状态的试验研究[J]. 岩土工程学报, 2018, 40(S1): 8-8. DOI: 10.11779/CJGE2018S1002
CAI Guo-qing, ASREAZAD Saman, LIU Chao, ZHAO Cheng-gang. Experimental study on critical state of unsaturated silty sand[J]. Chinese Journal of Geotechnical Engineering, 2018, 40(S1): 8-8. DOI: 10.11779/CJGE2018S1002
Citation: CAI Guo-qing, ASREAZAD Saman, LIU Chao, ZHAO Cheng-gang. Experimental study on critical state of unsaturated silty sand[J]. Chinese Journal of Geotechnical Engineering, 2018, 40(S1): 8-8. DOI: 10.11779/CJGE2018S1002

非饱和粉砂临界状态的试验研究

Experimental study on critical state of unsaturated silty sand

  • 摘要: 非饱和土临界状态给出了土变形过程的终点,对于分析土的基本力学性质和建立相应的本构模型十分重要。以非饱和粉砂为研究对象,利用非饱和土双压力室三轴试验系统(GDS)开展相关试验研究,对不同干密度粉砂在不同净应力和吸力条件下剪切至临界状态过程中,分别测定了强度、体变、含水率及饱和度等相关状态参量的变化规律。结果表明:剪切至临界状态过程中,不同干密度非饱和粉砂的强度和变形特性差异明显;随轴向应变的不断增加,不同初始干密度粉砂试样的偏应力、体应变以及饱和度曲线最终趋于稳定值,试样剪切达到临界状态。基于试验结果,揭示了临界状态条件下非饱和粉砂强度、孔隙比、孔隙水比体积随吸力的变化规律,并建立了q-、ν-、νw-平面内的临界状态线方程,提出了从强度、变形和孔隙水三个方面对非饱和粉砂临界状态进行综合描述的方法。

     

    Abstract: The critical state of soil shows the end of its deformation process, which is very important for analysis and establishment of constitutive model for soil. The unsaturated silty sand is used in this study. The triaxial testing system (GDS) is used to study the critical state of soil with different dry densities, net stresses and suctions, and the variations of soil strength, volume change, water content and saturation during the process are investigated. The results show that in the process of shearing to critical state, the strength and deformation characteristics of unsaturated silty sand with different dry densities are different. With the increase of axial strain, the curve of deviatoric stress, strain and saturation of silty sand specimens with different initial dry densities tend to a stable value, which indicate the specimens are sheared to critical state. Based on the test results, linear critical state equation in the plane of q-, ν- and νw- are established. The critical state of unsaturated soil are finally discussed based on the variation of strength, deformation and pore water.

     

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