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唐朝生, 施斌, 崔玉军(法国), Tang Anh-Minh. 重塑COx泥岩在饱和过程中应力应变的演化规律[J]. 岩土工程学报, 2010, 32(8).
引用本文: 唐朝生, 施斌, 崔玉军(法国), Tang Anh-Minh. 重塑COx泥岩在饱和过程中应力应变的演化规律[J]. 岩土工程学报, 2010, 32(8).
Stress and strain evolution of remoulded COx argillite during saturation[J]. Chinese Journal of Geotechnical Engineering, 2010, 32(8).
Citation: Stress and strain evolution of remoulded COx argillite during saturation[J]. Chinese Journal of Geotechnical Engineering, 2010, 32(8).

重塑COx泥岩在饱和过程中应力应变的演化规律

Stress and strain evolution of remoulded COx argillite during saturation

  • 摘要: 粉碎后的Callovo-Oxfordian(COx)泥岩在法国被提议为可选回填材料用于充填核废料处置库中的一些通道。通过一系列的一维固结实验,研究了高压实COx泥岩粉末在饱和过程中应力的发展规律和体积变形特征,重点探讨了初始轴向应力大小和粒度成分对土样水力学性质的影响。结果表明:在初始高轴向应力作用下,粗颗粒土样发生体积塌陷,轴向应力逐渐减小,而细颗粒土样的体积则呈现塌陷—膨胀—再塌陷的现象,轴向应力呈减小—增加—再减小的趋势;当初始轴向应力较低时,粗颗粒和细颗粒土样均表现出明显的膨胀性,轴向应力逐渐增加;饱和结束后,细颗粒土样的最终平衡轴向应力均高于粗颗粒土;通过计算,土样干密度达到2.0 g/cm3后,饱和后渗透系数小于10-11 m/s。

     

    Abstract: The crushed Callovo-Oxfordian (COx) argillite powder is proposed as an alternative backfilling material in France, which will be used in the engineering barrier of high-level radioactive waste (HLW) repository. In this investigation, one-dimensional oedometer tests are carried out on highly compacted (dry density of 2.0 g/cm3) crushed COx argillite powder. The evolution of axial stress and the volumetric deformation characteristics of the samples are studied during saturation process. The effects of the initial axial stress level and the grain size distribution (GSD) on the hydro-mechanical behaviors are discussed. The results show that the volumetric deformation characteristics of samples greatly depend on the applied initial axial stress during saturation. Under the initial condition of higher axial stress, the monotone collapse behaviors are observed for the coarser powder samples. Whereas the finer powder samples present collapse-swelling-collapse behaviors, and the axial stress decreases firstly, then increases and finally decreases again. The initial lower axial stress causes obvious swelling behaviors for both the coarser and finer powder samples and the corresponding axial stress increases gradually. After saturation, the equilibrium axial stresses of finer powder samples are higher than those of coarser powder samples. The hydraulic conductivity is less than 10-11 m/s for all the studied samples after the dry density of 2.0 g/cm3 is reached.

     

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