Creep of calcareous sand in Tunisia: effect of particle breakage at low stress level

Abstract Aims/hypothesis One of the critical mechanisms determining creep in granular materials is the breakage of soil particles. This study aims at evaluating the time-dependent creep deformation of calcareous sand at low effective stress conditions. Methods K0 creep tests were performed for both...

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Main Authors: Hyunwook Choo, Minhyuk Kwon, Lamia Touiti, Young-Hoon Jung
Format: Article
Language:English
Published: SpringerOpen 2020-10-01
Series:International Journal of Geo-Engineering
Subjects:
Online Access:http://link.springer.com/article/10.1186/s40703-020-00123-2
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spelling doaj-2bc2f2a6f02947f1b960601d47e9ffc82020-11-25T03:41:50ZengSpringerOpenInternational Journal of Geo-Engineering2092-91962198-27832020-10-011111510.1186/s40703-020-00123-2Creep of calcareous sand in Tunisia: effect of particle breakage at low stress levelHyunwook Choo0Minhyuk Kwon1Lamia Touiti2Young-Hoon Jung3Department of Civil Engineering, Kyung Hee UniversityDepartment of Civil Engineering, Kyung Hee UniversityCivil Engineering Laboratory LGC, University of Tunis El Manar, ENIT TunisDepartment of Civil Engineering, Kyung Hee UniversityAbstract Aims/hypothesis One of the critical mechanisms determining creep in granular materials is the breakage of soil particles. This study aims at evaluating the time-dependent creep deformation of calcareous sand at low effective stress conditions. Methods K0 creep tests were performed for both calcareous and silica sands at low stresses of 65 and 120 kPa, and the results of creep tests were compared with the results of constant rate of strain (CRS) tests at high stress levels up to 12 MPa. For a quantitative evaluation of the effect of the particle breakage on the creep deformation of calcareous sand, the relative breakage ( $$B_{r}$$ B r ) was determined based on the results of sieve analyses. Results The results demonstrate that Tunisia calcareous sand experiences significant particle breakage during creep and the consequent creep deformation at low stress level. The determined $$B_{r}$$ B r after creep at low stress level is comparable with that after the CRS test at high stress level. Conclusions High potential of particle breakage inherited by characteristic minerology of the calcareous Tunisia sand significantly influences the creep deformation at low stress level.http://link.springer.com/article/10.1186/s40703-020-00123-2CreepParticle breakageCalcareous sandRelative breakage
collection DOAJ
language English
format Article
sources DOAJ
author Hyunwook Choo
Minhyuk Kwon
Lamia Touiti
Young-Hoon Jung
spellingShingle Hyunwook Choo
Minhyuk Kwon
Lamia Touiti
Young-Hoon Jung
Creep of calcareous sand in Tunisia: effect of particle breakage at low stress level
International Journal of Geo-Engineering
Creep
Particle breakage
Calcareous sand
Relative breakage
author_facet Hyunwook Choo
Minhyuk Kwon
Lamia Touiti
Young-Hoon Jung
author_sort Hyunwook Choo
title Creep of calcareous sand in Tunisia: effect of particle breakage at low stress level
title_short Creep of calcareous sand in Tunisia: effect of particle breakage at low stress level
title_full Creep of calcareous sand in Tunisia: effect of particle breakage at low stress level
title_fullStr Creep of calcareous sand in Tunisia: effect of particle breakage at low stress level
title_full_unstemmed Creep of calcareous sand in Tunisia: effect of particle breakage at low stress level
title_sort creep of calcareous sand in tunisia: effect of particle breakage at low stress level
publisher SpringerOpen
series International Journal of Geo-Engineering
issn 2092-9196
2198-2783
publishDate 2020-10-01
description Abstract Aims/hypothesis One of the critical mechanisms determining creep in granular materials is the breakage of soil particles. This study aims at evaluating the time-dependent creep deformation of calcareous sand at low effective stress conditions. Methods K0 creep tests were performed for both calcareous and silica sands at low stresses of 65 and 120 kPa, and the results of creep tests were compared with the results of constant rate of strain (CRS) tests at high stress levels up to 12 MPa. For a quantitative evaluation of the effect of the particle breakage on the creep deformation of calcareous sand, the relative breakage ( $$B_{r}$$ B r ) was determined based on the results of sieve analyses. Results The results demonstrate that Tunisia calcareous sand experiences significant particle breakage during creep and the consequent creep deformation at low stress level. The determined $$B_{r}$$ B r after creep at low stress level is comparable with that after the CRS test at high stress level. Conclusions High potential of particle breakage inherited by characteristic minerology of the calcareous Tunisia sand significantly influences the creep deformation at low stress level.
topic Creep
Particle breakage
Calcareous sand
Relative breakage
url http://link.springer.com/article/10.1186/s40703-020-00123-2
work_keys_str_mv AT hyunwookchoo creepofcalcareoussandintunisiaeffectofparticlebreakageatlowstresslevel
AT minhyukkwon creepofcalcareoussandintunisiaeffectofparticlebreakageatlowstresslevel
AT lamiatouiti creepofcalcareoussandintunisiaeffectofparticlebreakageatlowstresslevel
AT younghoonjung creepofcalcareoussandintunisiaeffectofparticlebreakageatlowstresslevel
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