Evaluation of the internal stability of well-graded silty sand through the long-term seepage test

Abstract Suffusion is the phenomenon responsible for internal erosion, and is the process by which finer soil particles are moved through the constrictions between the larger soil particles by seepage forces. Generally, gap-graded soil is known to be susceptible to suffusion. Meanwhile, suffusion of...

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Main Authors: Hee-Jun Lee, In-Hyun Kim, Choong-Ki Chung
Format: Article
Language:English
Published: SpringerOpen 2021-08-01
Series:International Journal of Geo-Engineering
Subjects:
Online Access:https://doi.org/10.1186/s40703-021-00151-6
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spelling doaj-e399c8b3d972421f82a26f3c35e173492021-08-08T11:33:12ZengSpringerOpenInternational Journal of Geo-Engineering2092-91962198-27832021-08-0112111310.1186/s40703-021-00151-6Evaluation of the internal stability of well-graded silty sand through the long-term seepage testHee-Jun Lee0In-Hyun Kim1Choong-Ki Chung2Department of Civil and Environmental Engineering, Seoul National UniversityDepartment of Civil and Environmental Engineering, Seoul National UniversityDepartment of Civil and Environmental Engineering, Seoul National UniversityAbstract Suffusion is the phenomenon responsible for internal erosion, and is the process by which finer soil particles are moved through the constrictions between the larger soil particles by seepage forces. Generally, gap-graded soil is known to be susceptible to suffusion. Meanwhile, suffusion of well-graded silty sand and the resulting soil behavior are not well understood. Moreover, the previous researches on laboratory suffusion tests focused on the study of the critical hydraulic gradient, which triggers the internal instability of the soils within a short period of time. Therefore, in this study, long-term suffusion tests were conducted on well-graded silty sand under a hydraulic gradient lower than the critical value. As a result, abrupt increases in permeability and amount of soil discharged were observed due to the progressive migration of the soil particles, resulting in suffusion even at a relatively low hydraulic gradient.https://doi.org/10.1186/s40703-021-00151-6Internal erosionInternal instabilitySuffusionWell-graded silty sand
collection DOAJ
language English
format Article
sources DOAJ
author Hee-Jun Lee
In-Hyun Kim
Choong-Ki Chung
spellingShingle Hee-Jun Lee
In-Hyun Kim
Choong-Ki Chung
Evaluation of the internal stability of well-graded silty sand through the long-term seepage test
International Journal of Geo-Engineering
Internal erosion
Internal instability
Suffusion
Well-graded silty sand
author_facet Hee-Jun Lee
In-Hyun Kim
Choong-Ki Chung
author_sort Hee-Jun Lee
title Evaluation of the internal stability of well-graded silty sand through the long-term seepage test
title_short Evaluation of the internal stability of well-graded silty sand through the long-term seepage test
title_full Evaluation of the internal stability of well-graded silty sand through the long-term seepage test
title_fullStr Evaluation of the internal stability of well-graded silty sand through the long-term seepage test
title_full_unstemmed Evaluation of the internal stability of well-graded silty sand through the long-term seepage test
title_sort evaluation of the internal stability of well-graded silty sand through the long-term seepage test
publisher SpringerOpen
series International Journal of Geo-Engineering
issn 2092-9196
2198-2783
publishDate 2021-08-01
description Abstract Suffusion is the phenomenon responsible for internal erosion, and is the process by which finer soil particles are moved through the constrictions between the larger soil particles by seepage forces. Generally, gap-graded soil is known to be susceptible to suffusion. Meanwhile, suffusion of well-graded silty sand and the resulting soil behavior are not well understood. Moreover, the previous researches on laboratory suffusion tests focused on the study of the critical hydraulic gradient, which triggers the internal instability of the soils within a short period of time. Therefore, in this study, long-term suffusion tests were conducted on well-graded silty sand under a hydraulic gradient lower than the critical value. As a result, abrupt increases in permeability and amount of soil discharged were observed due to the progressive migration of the soil particles, resulting in suffusion even at a relatively low hydraulic gradient.
topic Internal erosion
Internal instability
Suffusion
Well-graded silty sand
url https://doi.org/10.1186/s40703-021-00151-6
work_keys_str_mv AT heejunlee evaluationoftheinternalstabilityofwellgradedsiltysandthroughthelongtermseepagetest
AT inhyunkim evaluationoftheinternalstabilityofwellgradedsiltysandthroughthelongtermseepagetest
AT choongkichung evaluationoftheinternalstabilityofwellgradedsiltysandthroughthelongtermseepagetest
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