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    王忠涛

    • 教授     博士生导师   硕士生导师
    • 主要任职:科学技术研究院副院长兼科技发展研究院院长、人文社科研究院院长
    • 性别:男
    • 毕业院校:大连理工大学
    • 学位:博士
    • 所在单位:土木工程系
    • 学科:岩土工程
    • 办公地点:综合实验1号楼213室
    • 联系方式:Zhongtao@dlut.edu.cn
    • 电子邮箱:zhongtao@dlut.edu.cn

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    复杂应力条件下原状饱和海洋黏土孔压与强度特性

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    论文类型:期刊论文

    发表时间:2022-06-29

    发表刊物:岩土工程学报

    所属单位:建设工程学部

    卷号:33

    期号:1

    页面范围:150-158

    ISSN号:1000-4548

    摘要:The apparatus for static and dynamic universal triaxial and torsional
       shear soil tests is employed to perform stress-controlled coupling
       vertical and torsional shear tests under different three-dimensional
       initial anisotropic consolidation stress conditions. Through
       experimental tests the effects of the initial orientation angle of the
       major principal stress, the ratio of the two stress components and the
       cyclic stress level on the pore water pressure and the strength of the
       saturated marine clay are examined. The initial orientation angle of the
       major principal stress has a significant influence on the
       characteristics of pore water pressure: as the angle increases, both the
       residual pore water pressure and the amplitude of fluctuated pore water
       pressure increase. Meanwhile, the relations between the normalized
       residual pore water pressure ratio and the cyclic number ratio with
       different initial orientation angles of the major principal stress are
       established. Under the conditions of keeping the area bounded by the
       elliptical stress path unchanged, there exists a certain critical value
       for the ratio of the axial and torsional shear stresses. At this
       critical value, the residual pore water pressure is the lowest. Both the
       fluctuated pore water pressure and the residual pore water pressure
       increase with increasing cyclic stress ratio. However, there is great
       difference between the high and the low stress levels. Furthermore, the
       critical cyclic stress ratio is determined according to the time history
       curves of pore water pressure under different cyclic stress ratios. The
       initial orientation angle of the major principal stress has a
       significant influence on the dynamic strength: as the angle increases,
       the dynamic strength decreases. The dynamic strength curve indicates
       that there is basically a linear relationship between the cyclic stress
       ratio and the logarithm of the cyclic number required at failure

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