Properties of Drained Shear Strength of Expansive Soil Considering Low Stresses and Its Influencing Factors
Autor: | He-ping Yang, Tang Xianyuan, Junhui Zhang, Jie Xiao |
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Rok vydání: | 2017 |
Předmět: |
Expansive clay
021105 building & construction 0211 other engineering and technologies Cohesion (geology) Geotechnical engineering 02 engineering and technology Direct shear test Water content Dry density Triaxial compression Geology 021101 geological & geomatics engineering Civil and Structural Engineering |
Zdroj: | International Journal of Civil Engineering. 16:1389-1398 |
ISSN: | 2383-3874 1735-0522 |
DOI: | 10.1007/s40999-017-0268-6 |
Popis: | The shallow failure of most expansive soil slopes undergoing wet–dry cycles occurs during or after long-term rainfall. According to the actual failure state of an expansive soil slope, the conventional direct shear equipment with low normal stresses was used to evaluate the effects of initial dry density, initial moisture content, and number of wet-dry cycle with or without loading on drained shear strength for the compacted expansive soil from Nanning, China. The saturated drained direct shear tests were also performed on the natural expansive soil specimens from Nanning by considering the influence of wet–dry cycles with loading and low normal stresses. Furthermore, consolidated drained triaxial compression tests on compacted specimens were conducted. The test results show that the drained shear strength of expansive soil was primarily affected by the magnitude of normal stresses, and also influenced by the initial moisture content, initial dry density, and number and type of wet–dry cycles. It is more realistic to consider the effect of loading during wet–dry cycles than that without loading. The effective drained shear strength envelopes with low normal stresses were plotted and well fitted by the generalized power function. At low normal stress levels, the drained shear strength still decreased with the increasing number of wet–dry cycles, and the effective cohesion intersects tended to be zero after being subjected to eight wet–dry cycles. This provided a theoretical basis for properly interpreting the shallow failure of expansive soil slopes. |
Databáze: | OpenAIRE |
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