The Undrained Characteristics of Tengger Desert Sand from True Triaxial Testing

Aimed at the characteristics of aeolian sand under rapid construction conditions in desert geotechnical engineering, a series of the true triaxial undrained test were carried out on the GDS apparatus. The 3D deformation, failure, and other characteristics of the dense sand are obtained. Under the co...

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Main Authors: Xuefeng Li, Weinan Lu, Zhigang Ma, Ni Tuo
Format: Article
Language:English
Published: Hindawi Limited 2021-01-01
Series:Advances in Civil Engineering
Online Access:http://dx.doi.org/10.1155/2021/6320397
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spelling doaj-c128bff4748c457ab8dd5fe3f591694a2021-07-19T01:03:40ZengHindawi LimitedAdvances in Civil Engineering1687-80942021-01-01202110.1155/2021/6320397The Undrained Characteristics of Tengger Desert Sand from True Triaxial TestingXuefeng Li0Weinan Lu1Zhigang Ma2Ni Tuo3School of Physics and Electronic-Electronic EngineeringSchool of Physics and Electronic-Electronic EngineeringSchool of Physics and Electronic-Electronic EngineeringSchool of Physics and Electronic-Electronic EngineeringAimed at the characteristics of aeolian sand under rapid construction conditions in desert geotechnical engineering, a series of the true triaxial undrained test were carried out on the GDS apparatus. The 3D deformation, failure, and other characteristics of the dense sand are obtained. Under the condition of same pc, the state transition point where the void water pressure changes from increasing to decreasing appears earlier and leads to enhanced dilatancy with the increase of b, which means the enhanced dilatancy of dense sand caused the increase in strength. The results of the same b shows that the void water pressure generally indicates a decrease at low confining pressure and an increase at high confining pressure, indicating that the aeolian sand shows dilatancy at low confining pressure and contraction at high confining pressure. The state transition point increases with the increase of pc, but all points tend to the same critical state line and state transition line. When b = 0, the critical state line is q = 1.57 p′, and the state transition line is q = 1.23 p′. When b = 1, the critical state line is q = 1.24 p′, and the state transition line is q = 1.04 p′. The results at same b obtained the unified critical state line and the state transition line. Therefore, the true triaxial test can obtain the unified relationship of void ratio, pc and b, which overcomes the fact that the existing test cannot consider the influence of b. The test results provide a basis data for the design, construction, and maintenance of geotechnical engineering in Tengger Desert.http://dx.doi.org/10.1155/2021/6320397
collection DOAJ
language English
format Article
sources DOAJ
author Xuefeng Li
Weinan Lu
Zhigang Ma
Ni Tuo
spellingShingle Xuefeng Li
Weinan Lu
Zhigang Ma
Ni Tuo
The Undrained Characteristics of Tengger Desert Sand from True Triaxial Testing
Advances in Civil Engineering
author_facet Xuefeng Li
Weinan Lu
Zhigang Ma
Ni Tuo
author_sort Xuefeng Li
title The Undrained Characteristics of Tengger Desert Sand from True Triaxial Testing
title_short The Undrained Characteristics of Tengger Desert Sand from True Triaxial Testing
title_full The Undrained Characteristics of Tengger Desert Sand from True Triaxial Testing
title_fullStr The Undrained Characteristics of Tengger Desert Sand from True Triaxial Testing
title_full_unstemmed The Undrained Characteristics of Tengger Desert Sand from True Triaxial Testing
title_sort undrained characteristics of tengger desert sand from true triaxial testing
publisher Hindawi Limited
series Advances in Civil Engineering
issn 1687-8094
publishDate 2021-01-01
description Aimed at the characteristics of aeolian sand under rapid construction conditions in desert geotechnical engineering, a series of the true triaxial undrained test were carried out on the GDS apparatus. The 3D deformation, failure, and other characteristics of the dense sand are obtained. Under the condition of same pc, the state transition point where the void water pressure changes from increasing to decreasing appears earlier and leads to enhanced dilatancy with the increase of b, which means the enhanced dilatancy of dense sand caused the increase in strength. The results of the same b shows that the void water pressure generally indicates a decrease at low confining pressure and an increase at high confining pressure, indicating that the aeolian sand shows dilatancy at low confining pressure and contraction at high confining pressure. The state transition point increases with the increase of pc, but all points tend to the same critical state line and state transition line. When b = 0, the critical state line is q = 1.57 p′, and the state transition line is q = 1.23 p′. When b = 1, the critical state line is q = 1.24 p′, and the state transition line is q = 1.04 p′. The results at same b obtained the unified critical state line and the state transition line. Therefore, the true triaxial test can obtain the unified relationship of void ratio, pc and b, which overcomes the fact that the existing test cannot consider the influence of b. The test results provide a basis data for the design, construction, and maintenance of geotechnical engineering in Tengger Desert.
url http://dx.doi.org/10.1155/2021/6320397
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