Anisotropy characterization of upper shanghai clays: Shear strength and small-strain stiffness

Comprehensive investigations have been conducted to study the structure and overconsolidation of upper Shanghai clays, i.e. Layers 2–6 clays, typically located at depths of 30–40 m. However, limited information is available on their anisotropy, and even less is known about the correlation between st...

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Main Authors: Lixin Lan, Wenxuan Zhu, Guanlin Ye, Qi Zhang, Tongshuai Yang
Format: Article
Language:English
Published: Elsevier 2025-01-01
Series:Journal of Rock Mechanics and Geotechnical Engineering
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Online Access:http://www.sciencedirect.com/science/article/pii/S1674775524002348
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author Lixin Lan
Wenxuan Zhu
Guanlin Ye
Qi Zhang
Tongshuai Yang
author_facet Lixin Lan
Wenxuan Zhu
Guanlin Ye
Qi Zhang
Tongshuai Yang
author_sort Lixin Lan
collection DOAJ
description Comprehensive investigations have been conducted to study the structure and overconsolidation of upper Shanghai clays, i.e. Layers 2–6 clays, typically located at depths of 30–40 m. However, limited information is available on their anisotropy, and even less is known about the correlation between structure, overconsolidation, and anisotropy. In this study, the undrained anisotropy characteristics of shear strength and small-strain shear stiffness in upper Shanghai Layers 2–6 clays were thoroughly assessed using a series of K0-consolidated undrained triaxial compression (TC) and triaxial extension (TE) tests (K0 is the coefficient of lateral earth pressure at rest). The effective stress paths, shear strength, and small-strain shear stiffness from the undrained TC and TE tests demonstrate the anisotropic behaviors in upper Shanghai clays. Analyses of data from upper Shanghai clays and other clays worldwide indicate that the shear strength anisotropy ratio (Ks) converges at 0.8 as the overconsolidation ratio (OCR) and plasticity index (Ip) increase, while the small-strain shear stiffness anisotropy ratio (Re) converges at 1.0. The influence of OCR on Ks and Re is more pronounced than that of Ip and sensitivity (St). Nevertheless, no clear correlation between Ks and Re is observed in upper Shanghai clays.
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institution Kabale University
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publishDate 2025-01-01
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series Journal of Rock Mechanics and Geotechnical Engineering
spelling doaj-art-f90497347944413597abea9f97a7fdaf2025-01-17T04:49:09ZengElsevierJournal of Rock Mechanics and Geotechnical Engineering1674-77552025-01-01171493508Anisotropy characterization of upper shanghai clays: Shear strength and small-strain stiffnessLixin Lan0Wenxuan Zhu1Guanlin Ye2Qi Zhang3Tongshuai Yang4Department of Civil Engineering, State Key Laboratory of Ocean Engineering, Shanghai Key Laboratory for Digital Maintenance of Buildings and Infrastructure, Shanghai Jiao Tong University, Shanghai, 200240, ChinaDepartment of Civil Engineering, Shanghai Jiao Tong University, Shanghai, 200240, ChinaDepartment of Civil Engineering, State Key Laboratory of Ocean Engineering, Shanghai Key Laboratory for Digital Maintenance of Buildings and Infrastructure, Shanghai Jiao Tong University, Shanghai, 200240, China; Corresponding author.Department of Civil Engineering, Shanghai Jiao Tong University, Shanghai, 200240, ChinaThe Fourth Construction Co., Ltd. of China Construction Eighth Engineering Division, Qingdao, 266100, ChinaComprehensive investigations have been conducted to study the structure and overconsolidation of upper Shanghai clays, i.e. Layers 2–6 clays, typically located at depths of 30–40 m. However, limited information is available on their anisotropy, and even less is known about the correlation between structure, overconsolidation, and anisotropy. In this study, the undrained anisotropy characteristics of shear strength and small-strain shear stiffness in upper Shanghai Layers 2–6 clays were thoroughly assessed using a series of K0-consolidated undrained triaxial compression (TC) and triaxial extension (TE) tests (K0 is the coefficient of lateral earth pressure at rest). The effective stress paths, shear strength, and small-strain shear stiffness from the undrained TC and TE tests demonstrate the anisotropic behaviors in upper Shanghai clays. Analyses of data from upper Shanghai clays and other clays worldwide indicate that the shear strength anisotropy ratio (Ks) converges at 0.8 as the overconsolidation ratio (OCR) and plasticity index (Ip) increase, while the small-strain shear stiffness anisotropy ratio (Re) converges at 1.0. The influence of OCR on Ks and Re is more pronounced than that of Ip and sensitivity (St). Nevertheless, no clear correlation between Ks and Re is observed in upper Shanghai clays.http://www.sciencedirect.com/science/article/pii/S1674775524002348Shanghai claysAnisotropyShear strengthSmall-strain stiffness
spellingShingle Lixin Lan
Wenxuan Zhu
Guanlin Ye
Qi Zhang
Tongshuai Yang
Anisotropy characterization of upper shanghai clays: Shear strength and small-strain stiffness
Journal of Rock Mechanics and Geotechnical Engineering
Shanghai clays
Anisotropy
Shear strength
Small-strain stiffness
title Anisotropy characterization of upper shanghai clays: Shear strength and small-strain stiffness
title_full Anisotropy characterization of upper shanghai clays: Shear strength and small-strain stiffness
title_fullStr Anisotropy characterization of upper shanghai clays: Shear strength and small-strain stiffness
title_full_unstemmed Anisotropy characterization of upper shanghai clays: Shear strength and small-strain stiffness
title_short Anisotropy characterization of upper shanghai clays: Shear strength and small-strain stiffness
title_sort anisotropy characterization of upper shanghai clays shear strength and small strain stiffness
topic Shanghai clays
Anisotropy
Shear strength
Small-strain stiffness
url http://www.sciencedirect.com/science/article/pii/S1674775524002348
work_keys_str_mv AT lixinlan anisotropycharacterizationofuppershanghaiclaysshearstrengthandsmallstrainstiffness
AT wenxuanzhu anisotropycharacterizationofuppershanghaiclaysshearstrengthandsmallstrainstiffness
AT guanlinye anisotropycharacterizationofuppershanghaiclaysshearstrengthandsmallstrainstiffness
AT qizhang anisotropycharacterizationofuppershanghaiclaysshearstrengthandsmallstrainstiffness
AT tongshuaiyang anisotropycharacterizationofuppershanghaiclaysshearstrengthandsmallstrainstiffness