A Constitutive Relationship for Gravelly Soil Considering Fine Particle Suffusion

Suffusion erosion may occur in sandy gravel dam foundations that use suspended cutoff walls. This erosion causes a loss of fine particles, degrades the soil strength and deformation moduli, and adversely impacts the cutoff walls of the dam foundation, as well as the overlying dam body. A comprehensi...

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Main Authors: Yuning Zhang, Yulong Chen
Format: Article
Language:English
Published: MDPI AG 2017-10-01
Series:Materials
Subjects:
Online Access:https://www.mdpi.com/1996-1944/10/10/1217
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spelling doaj-63dd742cdf9242d9953eec6618dc43a32020-11-24T20:46:39ZengMDPI AGMaterials1996-19442017-10-011010121710.3390/ma10101217ma10101217A Constitutive Relationship for Gravelly Soil Considering Fine Particle SuffusionYuning Zhang0Yulong Chen1School of Civil and Architectural Engineering, Yangtze Normal University, Chongqing 408100, ChinaState Key Laboratory of Hydroscience and Engineering, Tsinghua University, Beijing 100084, ChinaSuffusion erosion may occur in sandy gravel dam foundations that use suspended cutoff walls. This erosion causes a loss of fine particles, degrades the soil strength and deformation moduli, and adversely impacts the cutoff walls of the dam foundation, as well as the overlying dam body. A comprehensive evaluation of these effects requires models that quantitatively describe the effects of fine particle losses on the stress-strain relationships of sandy gravels. In this work, we propose an experimental scheme for studying these types of models, and then perform triaxial and confined compression tests to determine the effects of particle losses on the stress-strain relationships. Considering the Duncan-Chang E-B model, quantitative expressions describing the relationship between the parameters of the model and the particle losses were derived. The results show that particle losses did not alter the qualitative stress-strain characteristics of the soils; however, the soil strength and deformation moduli were degraded. By establishing the relationship between the parameters of the model and the losses, the same model can then be used to describe the relationship between sandy gravels and erosion levels that vary in both time and space.https://www.mdpi.com/1996-1944/10/10/1217suffusionfine particle lossesgravelly soilconstitutive model
collection DOAJ
language English
format Article
sources DOAJ
author Yuning Zhang
Yulong Chen
spellingShingle Yuning Zhang
Yulong Chen
A Constitutive Relationship for Gravelly Soil Considering Fine Particle Suffusion
Materials
suffusion
fine particle losses
gravelly soil
constitutive model
author_facet Yuning Zhang
Yulong Chen
author_sort Yuning Zhang
title A Constitutive Relationship for Gravelly Soil Considering Fine Particle Suffusion
title_short A Constitutive Relationship for Gravelly Soil Considering Fine Particle Suffusion
title_full A Constitutive Relationship for Gravelly Soil Considering Fine Particle Suffusion
title_fullStr A Constitutive Relationship for Gravelly Soil Considering Fine Particle Suffusion
title_full_unstemmed A Constitutive Relationship for Gravelly Soil Considering Fine Particle Suffusion
title_sort constitutive relationship for gravelly soil considering fine particle suffusion
publisher MDPI AG
series Materials
issn 1996-1944
publishDate 2017-10-01
description Suffusion erosion may occur in sandy gravel dam foundations that use suspended cutoff walls. This erosion causes a loss of fine particles, degrades the soil strength and deformation moduli, and adversely impacts the cutoff walls of the dam foundation, as well as the overlying dam body. A comprehensive evaluation of these effects requires models that quantitatively describe the effects of fine particle losses on the stress-strain relationships of sandy gravels. In this work, we propose an experimental scheme for studying these types of models, and then perform triaxial and confined compression tests to determine the effects of particle losses on the stress-strain relationships. Considering the Duncan-Chang E-B model, quantitative expressions describing the relationship between the parameters of the model and the particle losses were derived. The results show that particle losses did not alter the qualitative stress-strain characteristics of the soils; however, the soil strength and deformation moduli were degraded. By establishing the relationship between the parameters of the model and the losses, the same model can then be used to describe the relationship between sandy gravels and erosion levels that vary in both time and space.
topic suffusion
fine particle losses
gravelly soil
constitutive model
url https://www.mdpi.com/1996-1944/10/10/1217
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