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张建民, 宋飞. 砂土的压剪效应与渐近状态准则[J]. 岩土工程学报, 2008, 30(2): 166-171.
引用本文: 张建民, 宋飞. 砂土的压剪效应与渐近状态准则[J]. 岩土工程学报, 2008, 30(2): 166-171.
ZHANG Jianmin, SONG Fei. Compression-dilatancy coupling effect and asymptotic state criterion of sand[J]. Chinese Journal of Geotechnical Engineering, 2008, 30(2): 166-171.
Citation: ZHANG Jianmin, SONG Fei. Compression-dilatancy coupling effect and asymptotic state criterion of sand[J]. Chinese Journal of Geotechnical Engineering, 2008, 30(2): 166-171.

砂土的压剪效应与渐近状态准则

Compression-dilatancy coupling effect and asymptotic state criterion of sand

  • 摘要: 以往的研究结果表明:砂土在沿着等应变增量比路径加载时存在一个稳定的应力状态,即渐近状态;渐近状态随应变增量比的变化而变化;渐近状态是比临界状态更为广泛的一个概念,临界状态是渐近状态在体应变增量为零时的特殊情况。在一系列应变路径试验的基础上揭示了渐近状态随应变增量比的变化而变化的物理机制是加载过程中的压缩变形与剪切变形的所占比例不断调整的结果,将压缩变形与剪切变形耦合变化的力学行为及其对土的应力应变响应的影响定义为压剪耦合效应(简称压剪效应),在此基础上,提出定量描述渐近状态应力比随应变增量比变化的二维和三维渐近状态准则,并且通过试验结果验证了准则的有效性。

     

    Abstract: The previous studies show that there exists a steady stress state,defined as asymptotic state,when sand is loaded along constant strain increment ratio paths.Asymptotic states varies with the strain increment ratio.And asymptotic state is a more common concept than critical state,which is a particular case when volumetric strain increment equals zero.In this study,based on the observation of a series of strain path tests,the reason why asymptotic states change varing with the strain increment ratio was revealed as that the proportion of deformation due to the variation of effective mean principal stress and shear stress changes during a loading process.The mechanical behavior that the deformation due to compression and that due to stress-dilatancy occurred simultaneously and varied together during a loading process was defined as compression-dilatancy coupling effect.On this basis,two-and three-dimensional asymptotic state criteria were formulated to determine the relation between the mobilized stress ratio of asymptotic states and the strain increment ratio.In addition,the effectiveness of the criteria was proved by the test results.

     

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