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施维成, 朱俊高, 张 博, 余 挺. 粗粒土在平面应变条件下的强度特性研究[J]. 岩土工程学报, 2011, 33(12): 1974-1979.
引用本文: 施维成, 朱俊高, 张 博, 余 挺. 粗粒土在平面应变条件下的强度特性研究[J]. 岩土工程学报, 2011, 33(12): 1974-1979.
SHI Wei-cheng, ZHU Jun-gao, ZHANG Bo, YU Ting. Strength characteristics of coarse-grained soil under plane strain condition[J]. Chinese Journal of Geotechnical Engineering, 2011, 33(12): 1974-1979.
Citation: SHI Wei-cheng, ZHU Jun-gao, ZHANG Bo, YU Ting. Strength characteristics of coarse-grained soil under plane strain condition[J]. Chinese Journal of Geotechnical Engineering, 2011, 33(12): 1974-1979.

粗粒土在平面应变条件下的强度特性研究

Strength characteristics of coarse-grained soil under plane strain condition

  • 摘要: 使用河海大学新型真三轴仪,对粗粒土分别进行 σ3 保持不变的等σ3平面应变试验和 b =0 (即常规三轴压缩)、 b =0.25 的等σ3等 bb=(σ23)/(σ13)试验,研究了粗粒土在平面应变条件下的应力路径、破坏时的中主应力系数、内摩擦角及破坏应力比的特点。试验结果表明,等 σ3平面应变试验的应力路径介于 b =0 与 b =0.25 的等 σ3 等 bb=(σ23)/(σ13) 试验之间 ; 粗粒土在 平面应变条件下 破坏时的中主应力系数 b 介于 0.15 ~ 0.2 之间;粗粒土在平面应变条件下的内摩擦角比常 规三轴压缩条件下的大 5% ~ 7% ,而破坏应力比则比常规三轴压缩条件下的小 13% ~ 18% 。最后提出一个 由粗粒土常规三轴压缩试验测得的内摩擦角 φ tc 求平面应变条件下的破坏应力比 M fp 的计算公式 M fp =2.3sin φ tc ,可较好地模拟试验结果。

     

    Abstract: Plane strain compression tests in which σ3 keeps invariable and experiments in which both σ3 and bb=(σ23)/(σ13) keep constant are performed on coarse-grained soil by means of the true triaxial apparatus recently developed in Hohai University. The characteristics of stress paths, parameter b at failure, angles of internal friction and peak values of stress ratio M fp =( q/ p) fp of coarse-grained soil under plane strain conditions are studied. The experimental results show that the stress paths of the plane strain tests exist between the b-constant tests in which b equals 0 and 0.25; the parameter b at failure is between 0.15 and 0.2 for coarse-grained soil under plane strain conditions; the angles of internal friction of coarse-grained soil under plane strain conditions are 5%~7% larger than those under triaxial compression conditions while the peak values of stress ratio of coarse-grained soil under plane strain conditions are 13%~18% smaller than those under triaxial compression conditions. Finally a formula expressed as M fp =2.3sin φ tc , which is verified by the test results of coarse-grained soil, is proposed to calculate the peak value of stress ratio, M fp , under plane strain conditions from the angle of internal friction, φ tc , obtained from conventional triaxial compression tests.

     

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