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Compressibility according to compacted soil suction

机译:根据压实的土壤吸力可压缩

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Compacted soils are widely used in geotechnical engineering. To ensure the stability of the structures involving compacted soils, it is essential to well understand the volume change behavior which depends on unsaturated soil mechanical parameters which are highly variable both in time and space because they depend on soil structure and soil hydrous state. In this paper we carried out oedometric compression tests with a control of soil suction by an osmotic method to study the compressibility of a compacted loamy soil in North France for re-wetted samples with soil powder sieved at 2 mm, with an initial density of 1.1 Mg m−3 under the combined mechanical (vertical stress) and hydrous (suction) effects. The results show that the compression index λ varies little with suction in the range 10–200 kPa for the compacted soil.
机译:压实的土壤广泛用于岩土工程中。为了确保涉及压实土壤的结构的稳定性,必须充分了解取决于非饱和土壤力学参数的体积变化行为,该参数在时间和空间上都高度可变,因为它们取决于土壤结构和土壤含水状态。在本文中,我们通过渗透压法控制了土壤吸力,进行了测压试验,以研究法国北部压实的壤土在2毫米筛分,初始密度为1.1的情况下重新润湿的样品的可压缩性。 Mg m −3 在机械(垂直应力)和含水(吸力)作用下共同作用。结果表明,对于压实土壤,在10–200 kPa范围内,压缩系数λ随吸力变化很小。

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