南海非饱和钙质砂动力特性三轴试验研究

    Triaxial Test on Dynamic Characteristics of Unsaturated Calcareous Sand in South China Sea

    • 摘要: 为了解决南海非饱和钙质砂动力特性问题,选取南海地区钙质砂开展动三轴试验,系统研究不同参数对非饱和钙质砂力学特性影响规律.试验表明:非饱和钙质砂动应变和动孔压发展规律与饱和钙质砂存在明显差异.动孔压在饱和状态下试验前期发展较慢,近似呈线性增长,试验中后期波动较大,而在非饱和状态下的发展规律与之相反;钙质砂在非饱和状态时动应变曲线只有低围压下才有明显失稳点,100、150 kPa有效围压下无明显失稳点,在饱和状态时各有效围压下均有明显失稳点;非饱和状态下动孔压发展趋势受基质吸力影响较大,随基质吸力增大,最大动孔压整体呈现递减趋势,高基质吸力下试样破坏时的最大动孔压小于低基质吸力下试样破坏时的最大动孔压.

       

      Abstract: To solve the problem of dynamic characteristics of unsaturated calcareous sand in the South China Sea, calcareous sand was selected to carry out dynamic triaxial test and effects of different parameters on the mechanical properties were studied systematically in this paper. Results show that the development law of dynamic strain and dynamic pore pressure of unsaturated calcareous sand is obviously different from that of saturated calcareous sand. Under the saturated state, the dynamic pore pressure developed slowly and kept near-linearly increasing in the early stage of the test, and the dynamic pore pressure fluctuations was large in the middle and late stage of the test. By contrast, the development law of calcareous sand in an unsaturated state was opposite. The dynamic strain curve of unsaturated calcareous sand had obvious instability point only under the low confining pressure. There was no obvious instability point under the effective confining pressure of 100 kPa and 150 kPa, and there was obvious instability point under each effective confining pressure in the saturated state. The development trend of dynamic pore pressure under the unsaturated state was greatly affected by the matric suction, and with the increase of the matric suction, the maximum dynamic pore pressure showed an overall decreasing trend. The maximum dynamic pore pressure under the high matric suction was smaller than that under the low matric suction.

       

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