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Experimental study of consolidation properties of unsaturated soils during draining

机译:排水过程中非饱和土固结特性的试验研究

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Changes in groundwater elevation may cause a change in the net normal stress and matric potential within the soil mass, which results in volume changes of unsaturated soil. This research investigated the relationship between the drawdown of groundwater and the characteristics of volumetric compressibility of unsaturated soil. Sand column experiments were designed and conducted to measure the volume changes of coarse and fine sands under different types of drainage conditions at fast and slow drainage rates. The finite element program Femwater was calibrated and used to simulate the distributions of stress, tension and moisture content within the sands. Finally, based on the changes of net normal stress and matric potential and the observed volume change of the sands, a least-square method was applied to determine the volumetric consolidation parameters of the unsaturated soils.
机译:地下水水位的变化可能会导致土壤团块内净正应力和基质势的变化,从而导致非饱和土壤的体积变化。本研究探讨了地下水位下降与非饱和土体积压缩特性之间的关系。设计并进行了砂柱实验,以测量不同类型排水条件下快速和慢速排水条件下粗砂和细砂的体积变化。有限元程序Femwater被校准并用于模拟砂土中应力,张力和水分含量的分布。最后,根据净法向应力和基体电位的变化以及观测到的砂土体积变化,采用最小二乘法确定非饱和土的体积固结参数。

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