不同沉积方向下兰州黄土动剪切模量和阻尼比试验

    Dynamic shear modulus and damping ratio tests of Lanzhou loess under different depositional directions

    • 摘要: 原状黄土是一种具有各向异性的特殊性岩土,而各向异性对于黄土地区工程建设中边坡、隧道、地下空间工程的稳定性影响较大。为研究不同沉积方向下黄土动力参数变化规律,选取兰州地铁#1线不同站点试样为研究对象,对不同取样深度、不同取样角度(垂直向和水平向)的黄土试样进行了动三轴试验,获得了不同工况条件下黄土的动力特性参数。分析了黄土动强度、动剪切模量、阻尼比与取样方向、土层深度之间的关系。结果表明:不同沉积方向上兰州黄土在弹性阶段的动本构关系均符合Hardin-Dinevich双曲线模型。同一取样深度时,黄土在垂直向的动强度要高于水平向;动剪切模量从大到小依次为七里河 > 拱星墩 > 陈官营 > 迎门滩;横向方向动剪切模量从大到小依次为迎门滩 > 陈官营 > 七里河 > 拱星墩。同一沉积方向下,取样深度对黄土Gd/Gdmax的影响较大,Gd/Gdmax曲线随着土层深度的增加曲线向上移动;取样深度对阻尼的影响表现为,土层越深,土的非线性特性表现的越弱,阻尼比越小。

       

      Abstract: Undisturbed loess is a special geotechnical material with anisotropy, and anisotropy has a greater impact on the stability of slopes, tunnels and underground space projects in loess areas. In order to study the variation rule of loess dynamic parameters under different depositional directions, this paper selects different station samples of Lanzhou Metro Line 1 as the research object, and carries out dynamic triaxial tests on loess samples with different sampling depths and different sampling angles (vertical and horizontal), and obtains the dynamic characteristic parameters of loess under different working conditions. The relationships between the dynamic strength, dynamic shear modulus and damping ratio of loess and the sampling direction and soil depth are analysed, and the results show that: The dynamic constitutive relationships of the Lanzhou loess during the elastic phase in different depositional directions are consistent with the Hardin-Dinevich hyperbolic model. At the same sampling depth, the dynamic strength of loess in the vertical direction is higher than that in the horizontal direction; the dynamic shear modulus ratios in descending order are as follows: Qilihe > Gongxingdun > Chenguanying > Yingmentan. And in the horizontal direction: the dynamic shear modulus ratios in descending order are as follows: Yingmentan > Chenguanying > Qilihe > Gongxingdun. Under the same depositional direction, the sampling depth has a greater effect on the Gd/Gdmax of loess, and the Gd/Gdmax curve shifts upward with the increase of the soil depth. The effect of the sampling depth on the damping is manifested in the fact that the deeper the soil layer is, the weaker the nonlinear characteristics of the soil are manifested, and the smaller the damping ratio is.

       

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