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Articles

Experimental study of drained anisotropy of granular soils involving rotation of principal stress direction

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Pages 431-454 | Received 04 Nov 2014, Accepted 01 Apr 2015, Published online: 05 May 2015
 

Abstract

A series of drained tests were conducted on the medium dense Toyoura standard sands using a hollow cylinder apparatus, including both F tests (sheared with a fixed principal stress direction) and R tests (sheared with a constant deviatoric stress but rotating the principal stress directions). The effects of anisotropy on the deformation characteristics were examined, including both the inherent anisotropy that formed in the process of sand sample preparation and the anisotropy which induced due to the ‘inclined’ consolidation. The results of F tests showed that the effect of the inherent anisotropy was significant on the stress–strain behaviour and failure strength of sand. It was also seen that the deformation characteristics of R tests, including the development of strain components, the nominal strain increments and the degree of non-coaxiality, were considerably dependent on both the ‘inclined’ consolidation directions and the deviatoric stress level. It was also noted that the development of nominal strain increments and volumetric strain was affected by the number of cycles due to the densification of the sand under cyclic rotation of principal stress axes under drained conditions.

Acknowledgements

The work presented in this study is supported by the National Outstanding Youth Science Foundation of China under grant number 51025827, National Natural Science Foundation of China under Grant No. 51408441, Natural Science Foundation of Zhejiang Province under Grant No. LQ14E080011. These financial supports are gratefully acknowledged.

Disclosure statement

No potential conflict of interest was reported by the authors.

Additional information

Funding

The work was supported by the National Outstanding Youth Science Foundation of China [grant number 51025827]; National Natural Science Foundation of China [grant number 51408441]; Natural Science Foundation of Zhejiang Province [grant number LQ14E080011].

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