田桂莉, 陈慧娥, 冷冠军, 姜亚玲, 牛岑岑. 2016: 排水对黄土动力特性及微观结构特征的影响研究. 工程地质学报, 24(s1): 1027-1033. DOI: 10.13544/j.cnki.jeg.2016.s1.148
    引用本文: 田桂莉, 陈慧娥, 冷冠军, 姜亚玲, 牛岑岑. 2016: 排水对黄土动力特性及微观结构特征的影响研究. 工程地质学报, 24(s1): 1027-1033. DOI: 10.13544/j.cnki.jeg.2016.s1.148
    TIAN Guili, CHEN Huie, LENG Guanjun, JIANG Yaling, NIU Cencen. 2016: INFLUENCE OF DRAINAGE ON DYNAMIC CHARACTERISTIC AND MICROSTRUCTURE OF LOESS. JOURNAL OF ENGINEERING GEOLOGY, 24(s1): 1027-1033. DOI: 10.13544/j.cnki.jeg.2016.s1.148
    Citation: TIAN Guili, CHEN Huie, LENG Guanjun, JIANG Yaling, NIU Cencen. 2016: INFLUENCE OF DRAINAGE ON DYNAMIC CHARACTERISTIC AND MICROSTRUCTURE OF LOESS. JOURNAL OF ENGINEERING GEOLOGY, 24(s1): 1027-1033. DOI: 10.13544/j.cnki.jeg.2016.s1.148

    排水对黄土动力特性及微观结构特征的影响研究

    INFLUENCE OF DRAINAGE ON DYNAMIC CHARACTERISTIC AND MICROSTRUCTURE OF LOESS

    • 摘要: 利用动三轴仪对原状黄土饱和后的试样进行了排水条件下的动载荷试验,分析了排水条件下土样的变形、孔压、应力应变滞回圈特点及试验前后微观结构的变化。动三轴试验分析结果显示,与不排水条件下的3个明显的变形阶段相比,排水条件下的变形阶段明显不同;排水条件下动三轴试验过程中孔压整体处于稳定水平;在振次N=1、N=50、N=100下的应力应变关系形成的滞回圈形状相差不大,但与传统的椭圆形滞回圈相似度不高。通过对扫描电镜试验和压汞试验的微观结构结果分析显示,试验前后土样的微观结构、颗粒之间的接触和孔隙的大小等都发生了明显改变。微观试验结果分析得出了动三轴试验前后土颗粒间的变化为:由相对松散状态转变为相对密实状态,由支架接触、接触面积较小变为镶嵌接触为主、接触面积增大;孔隙孔径的变化上,试验前后不同孔隙孔径所占的百分含量明显发生了变化,尤其大孔隙的变化最为明显,土样中的大孔隙明显减少,微、小孔隙增多。

       

      Abstract: The dynamic triaxial test is carried out on the saturated intact loess sample with dynamic triaxial apparatus on the drainage condition. And analyze the characteristics of the deformation, pore pressure, hysteresis loop and microstructure of the sample. The analysis results shows: the deformation stages on the drainage condition is obviously different from the three stages on undrainage condition, the pore pressure is on a stable level during the experiment, the hysteresis loops are similar in the vibration times of N=1,N=50 and N=100,but the similarity is a bit low compared with the traditional oval-shaped hysteresis loops. The microstructure analysis tests were obtained with SEM and Mercury porosimetry analyzer. The analysis result shows that the micro-structure of the soil samples, the contact between the particles and the size of the pores all change significantly. The changes of soil particles before and after the dynamic triaxial test are obtained by analyzing the results of microstructure tests. The main conclusions about the microstructure are as followings: the relative statuses between the soil particles change from a relatively loose state into a relatively dense state, the contact relationship from scaffold contact become to mosaic contact and the contact area increase after the test, the percentage of various pore diameter change greatly and the most obvious changes are the big pore diameter. The number of large pores obviously decreases and small and micro pores increases in the number.

       

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