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陈国兴, 卜屹凡, 周正龙, 张书菡, 许汉刚. 沉积相和深度对第四纪土动剪切模量和阻尼比的影响[J]. 岩土工程学报, 2017, 39(7): 1344-1350. DOI: 10.11779/CJGE201707022
引用本文: 陈国兴, 卜屹凡, 周正龙, 张书菡, 许汉刚. 沉积相和深度对第四纪土动剪切模量和阻尼比的影响[J]. 岩土工程学报, 2017, 39(7): 1344-1350. DOI: 10.11779/CJGE201707022
CHEN Guo-xing, BU Yi-fan, ZHOU Zheng-long, ZHANG Shu-han, XU Han-gang. Influence of sedimentary facies and depth on normalized dynamic shear modulus and damping ratio of quaternary soils[J]. Chinese Journal of Geotechnical Engineering, 2017, 39(7): 1344-1350. DOI: 10.11779/CJGE201707022
Citation: CHEN Guo-xing, BU Yi-fan, ZHOU Zheng-long, ZHANG Shu-han, XU Han-gang. Influence of sedimentary facies and depth on normalized dynamic shear modulus and damping ratio of quaternary soils[J]. Chinese Journal of Geotechnical Engineering, 2017, 39(7): 1344-1350. DOI: 10.11779/CJGE201707022

沉积相和深度对第四纪土动剪切模量和阻尼比的影响

Influence of sedimentary facies and depth on normalized dynamic shear modulus and damping ratio of quaternary soils

  • 摘要: 依据苏州第四纪地层特点,使用GCTS循环三轴试验仪对取自典型钻孔剖面100 m以浅的40个原状土样进行了剪应变10-5~10-2量级的动剪切模量和阻尼比试验,研究了土的沉积环境、深度和土类对土体的规准化动剪切模量比G/Gmax和阻尼比λ的影响。当剪应变γ<;
    1×;
    10-4时,G/Gmax折减很小,土体处于非线性弹性状态。沉积相、土层深度和土类对苏州第四纪地层土的G/Gmax,λ与γ关系曲线的影响有明显差异。相同沉积相的同类土,土层深度越深,G/Gmax随γ增长而衰退越慢,λ越小;深度相近的同类土,滨海相土比河泛相土具有更为明显的非线性,而滨海相土的λ略高于河泛相土。沉积相相同、深度相近时,粉砂、粉质黏土、黏土的G/Gmax随γ增长而衰退的速率依次减慢;应变水平相同时,粉砂的λ最小,粉质黏土的次之,黏土的最大。;

     

    Abstract: To contribute to a better fundamental understanding of the deformation behavior for Suzhou quaternary sedimentary soils, using GCTS cylinder apparatus cyclic loading testing system, a total of 40 cyclic triaxial tests are performed on various kinds of undisturbed soils at depth less than 100 m corresponding to a wide strain range in the order of 10-5 to 10-2. It is revealed that the variation characteristics of the normalized dynamic shear modulus (G/Gmax) and damping ratio (λ) with the increasing shear strain (γ) are strongly influenced by the sedimentary facies, depths and types of soils. The reduction of G/Gmax with the increasing values of γ when γ <10-4 is small, and the soils show nonlinear elasticity. Under the identical conditions, the test results demonstrate that the increasing depth shifts the values of G/Gmax and the relationship between λ and γ. Moreover, the sediments of flooded plain facies are more linear and have slightly smaller values of λ with the increasing values of γ than the sediments of littoral facies. Under the same sedimentary facies and similar depth, the reduction rates of G/Gmax with the increasing values of γ for silty sand, silty clay and clay have a descending order, and the values of λ under the same γ for silty sand, silty clay and clay increase successively.

     

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