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Open Access

Uniaxial Compressive Mechanical Properties of Fissured Loess after Dry-Wet Cycles

Liyang Zhou1, Jian Xu1,2( ), Ke Hu1, Yanfeng Li1, Zhipeng Wu1
School of Civil Engineering, Xi’an University of Architecture and Technology, Xi’an 710055, P.R. China
Shaanxi Key Laboratory of Geotechnical and Underground Space Engineering, Xi’an University of Architecture and Technology, Xi’an 710055, P.R. China
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Abstract

Uniaxial compression tests on fissured loess after dry-wet cycles were carried out systematically, and the fissure evolution pattern and mechanical properties of fissured loess were deeply investigated. The results show that the surface crack rate Rsc and fractal dimension Df of samples with different angles increase after more dry-wet cycles, while the growth rate gradually slows down. The dry-wet cycling has no significant influence on the types and characteristics of stress-strain curves; the initial slope of the stress-strain curve declines with the increase of dry-wet cycles. The stress-strain curves of loess samples with different angles all show the characteristics of strain softening, and the samples with 45° show bimodal characteristics. In addition, the uniaxial compression strength of samples with different angles exhibits decelerated attenuation with growing dry-wet cycles. The relationship between uniaxial compression strength and fissure angle unanimously presents characteristics of “double valley” after different dry-wet cycles.

CLC number: TU444 Document code: A Article ID: 1673-0836(2023)01-0133-08

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Chinese Journal of Underground Space and Engineering
Pages 133-140

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Cite this article:
Zhou L, Xu J, Hu K, et al. Uniaxial Compressive Mechanical Properties of Fissured Loess after Dry-Wet Cycles. Chinese Journal of Underground Space and Engineering, 2023, 19(1): 133-140. https://doi.org/10.20174/j.juse.2023.01.015

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Received: 02 March 2022
Published: 01 February 2023
© 2023 Chinese Journal of Underground Space and Engineering

This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).