李瑞宽, 吴志坚, 梁庆国, 徐世民, 赵涛. 2018: 考虑微结构特征的黄土动力特性影响因素研究. 工程地质学报, 26(4): 905-914. DOI: 10.13544/j.cnki.jeg.2017-391
    引用本文: 李瑞宽, 吴志坚, 梁庆国, 徐世民, 赵涛. 2018: 考虑微结构特征的黄土动力特性影响因素研究. 工程地质学报, 26(4): 905-914. DOI: 10.13544/j.cnki.jeg.2017-391
    LI Ruikuan, WU Zhijian, LIANG Qingguo, XU Shimin, ZHAO Tao. 2018: INFLUENCE FACTORS OF DYNAMIC CHARACTERISTICS OF LOESS CONSIDERING THE MICROSTRUCTURE PROPERTIES. JOURNAL OF ENGINEERING GEOLOGY, 26(4): 905-914. DOI: 10.13544/j.cnki.jeg.2017-391
    Citation: LI Ruikuan, WU Zhijian, LIANG Qingguo, XU Shimin, ZHAO Tao. 2018: INFLUENCE FACTORS OF DYNAMIC CHARACTERISTICS OF LOESS CONSIDERING THE MICROSTRUCTURE PROPERTIES. JOURNAL OF ENGINEERING GEOLOGY, 26(4): 905-914. DOI: 10.13544/j.cnki.jeg.2017-391

    考虑微结构特征的黄土动力特性影响因素研究

    INFLUENCE FACTORS OF DYNAMIC CHARACTERISTICS OF LOESS CONSIDERING THE MICROSTRUCTURE PROPERTIES

    • 摘要: 选取1920年海原地震震中滑坡密集分布区宁夏回族自治区西吉县庞湾乡的黄土,分别进行了不同围压,不同含水率条件下的原状、重塑土动三轴试验。结合动三轴试验前后的微观变化图像,探讨围压和水分对黄土试样土颗粒的作用机制,从微结构的角度阐释了两者对黄土动力特性影响的特点。研究结果表明:所取试样动剪切模量与动剪应变的关系可以用H-D模型的推导式拟合,随含水率增加,围压减小,参数ab值增大;水分在原状试样和重塑试样的作用不同,随着含水率的增加,动剪切模量降低,阻尼比增大,原状试样动剪切模量和阻尼比的变化速率先快后慢,而重塑试样相应值的变化速率先慢后快;除了水分和围压等外在条件的影响,土样本身土体的微观特征如孔隙分布、颗粒大小、粒间间距、联结方式、密实程度等因素对土体动剪切模量和阻尼比等宏观特性产生重要影响。

       

      Abstract: Xijipangwan of Ningxia province is the intensive landslide area caused by the famous Haiyuan earthquake. Its loess is chosen as the research object. The dynamic triaxial tests are carried out on the undisturbed loess and the remolded loess under different water contents and different stress states. This paper examines the changes of microscopic images before and after dynamic triaxial tests. It discusses the action mechanism of confining pressure and moisture on loess soil particles and explains their influence characteristics on dynamic behaviors of loess from the perspective of the microstructure. The results indicate as follows. The relationship curve of dynamic shear modulus and dynamic shear strain can be regressed by derivation of the H-D model. With the increase of water content or the decrease of confining pressure, the value of parameter a and b increase. It is founded that there are some differences between the influence of water to undisturbed samples and remolded samples. With the increase of water content, dynamic shear modulus decreases, damping ratio increases. The dynamic characteristic parameters of remolded samples are transformed quickly before they are slow. Those parameters of undisturbed samples change slowly before they are quick. Besides the influence of external conditions(such as moisture and confining pressure), the microscopic characteristics of soil samples(such as pore size distribution, particle size, inter-particle spacing, connection mode and density) have great influence on the macroscopic behaviors(such as dynamic shear modulus and damping ratio) of loess.

       

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