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Experimental investigation on the creep behavior of an unsaturated clay

机译:非饱和黏土蠕变特性的实验研究

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To better understand the long-term deformation of landslides with consideration of the influence of water content variation, a series of triaxial creep tests with suction control was conducted on clay specimens taken from one large-scale landslide in the Three Gorges Reservoir area in China. Results indicate that, in the double-logarithmic coordinates, the axial strain increases linearly and the axial strain-rate decreases linearly with the elapsed time; the axial strain and strain rate increase with increasing deviator stress levels and decreasing matric suction. For theoretical analysis, based on the simulation of the test results by an empirical creep model developed for saturated soils, a linear relationship was established between suction and one of the parameters of the model. Then, a revised model with consideration of suction effects was developed. In the revised model, a power function was adopted for the description of the strain-time relationship and a hyperbolic function was employed for the stress-strain relationship. Verification indicated that the calculated results were in good agreement with the experimental ones.
机译:为了更好地理解滑坡的长期变形,并考虑到水含量变化的影响,对三峡库区一个大型滑坡的黏土标本进行了一系列带吸力控制的三轴蠕变试验。结果表明,在双对数坐标系中,轴向应变随着时间的增长线性增加,轴向应变率随时间线性下降。轴向应变和应变率随偏应力水平的增加和基体吸力的减小而增加。为了进行理论分析,基于针对饱和土壤开发的经验蠕变模型对测试结果进行模拟,在吸力与模型参数之一之间建立了线性关系。然后,开发了考虑吸力效应的修正模型。在修改后的模型中,采用幂函数来描述应变-时间关系,并采用双曲线函数来描述应力-应变关系。验证表明,计算结果与实验结果吻合良好。

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