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岑君, 彭好, 魏骁, 杨仲轩, 杨峻, 程延. 循环三轴荷载作用下砂土孔隙水压的发展规律[J]. 岩土工程学报, 2023, 45(S2): 264-269. DOI: 10.11779/CJGE2023S20038
引用本文: 岑君, 彭好, 魏骁, 杨仲轩, 杨峻, 程延. 循环三轴荷载作用下砂土孔隙水压的发展规律[J]. 岩土工程学报, 2023, 45(S2): 264-269. DOI: 10.11779/CJGE2023S20038
CEN Jun, PENG Hao, WEI Xiao, YANG Zhongxuan, YANG Jun, CHENG Yan. Generation of excess pore pressure in sands subjected to cyclic triaxial loading[J]. Chinese Journal of Geotechnical Engineering, 2023, 45(S2): 264-269. DOI: 10.11779/CJGE2023S20038
Citation: CEN Jun, PENG Hao, WEI Xiao, YANG Zhongxuan, YANG Jun, CHENG Yan. Generation of excess pore pressure in sands subjected to cyclic triaxial loading[J]. Chinese Journal of Geotechnical Engineering, 2023, 45(S2): 264-269. DOI: 10.11779/CJGE2023S20038

循环三轴荷载作用下砂土孔隙水压的发展规律

Generation of excess pore pressure in sands subjected to cyclic triaxial loading

  • 摘要: 地震荷载在土体中诱导产生的超孔隙水压发展会导致砂土液化和破坏。准确合理地表征超孔隙水压在循环荷载作用下的发展规律对液化分析至关重要。采用净砂和细粒含量为10%的含粉粒砂土开展了一系列不排水循环三轴试验,基于两种超孔隙水压模型(均匀循环应力模型和能量耗散模型)对数据进行了分析,提出了一个能更好表征孔隙水压发展的均匀循环应力模型并标定了模型参数,同时对一个单参数能量耗散模型进行了参数标定和分析。数据表明,均匀循环应力模型参数主要受到应力循环幅值的影响,且表现出一定的土体特异性;能量耗散模型的参数则主要受到土体密实度的影响和土体类型的影响。

     

    Abstract: The excess pore pressure induced by seismic loading leads to soil liquefaction. Proper characterization of the pore pressure generation due to cyclic loadings is essential for liquefaction analysis of soils. The results of a series of undrained cyclic triaxial tests based on clean sand and silty sand with fines of 10% are introduced. The data are analyzed in the framework of two pore pressure models (uniform cyclic stress model and energy dissipation model). A new uniform cyclic stress model is proposed to better characterize the pore pressure generation, and the model parameters are calibrated. Meanwhile, a one-parameter energy dissipation model is calibrated and analyzed as well. It is found that the parameters of the uniform cyclic stress model are mainly affected by the amplitude of the stress cycles and mildly affected by the fines content, while the parameters of the energy dissipation model are mainly affected by the packing density and soil type.

     

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