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Relation between the Friction Angle of Sand at Triaxial Compression and Triaxial Extension and Plane Strain Conditions

机译:三轴压缩砂摩擦角与三轴延伸和平面应变条件的关系

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The strength of sand is usually characterized by the maximum value of the secant friction angle. The friction angle is a function of deformation mode, density, and stress level and is strongly correlated with dilatancy at failure. Most often, the friction angle is evaluated from results of conventional compression tests, and correlation between the friction angle of sand at triaxial compression and triaxial extension and plane strain conditions is a vital problem of soil mechanics. These correlations can be obtained from laboratory test results. The failure criteria for sand presented in literature also give the possibility of finding correlations between friction angles for different deformation modes. The general stress-dilatancy relationship obtained from the frictional state concept, with some additional assumptions, gives the possibility of finding theoretical relationships between the friction angle of sand at triaxial compression and triaxial extension and plane strain conditions. The theoretically obtained relationships presented in the paper are fully consistent with theoretical and experimental findings of soil mechanics.
机译:砂的强度通常是由分摩擦角的最大值的特征。摩擦角是变形模式,密度和应力水平的函数,并且与失效时的膨胀强烈地相关。通常,通常,从传统压缩试验的结果评估摩擦角,并且三轴压缩和三轴延伸和平面应变条件之间的砂的摩擦角之间的相关性是土壤力学的重要问题。这些相关性可以从实验室测试结果获得。文献中呈现的沙子的故障标准还提供了在不同变形模式下找到摩擦角之间的相关性的可能性。从摩擦状态概念获得的一般应力膨胀关系,其中一些额外的假设,具有在三轴压缩和三轴延伸和平面应变条件下发现砂摩擦角之间的理论关系。本文呈现的理论上获得的关系与土壤力学的理论和实验结果完全一致。

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