Yielding of a quartz sand from saturated to dry state

The paper presents the results of an experimental work where we analyse the behaviour of an unsaturated quartz sand in a wide range of degree of saturation (from saturated to dry state). The possibility of anticipating the hydro-mechanical behaviour of the soils when they approach the dry state is f...

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Main Authors: Butticè Vincenzo, Ferrari Alessio, Rosone Marco
Format: Article
Language:English
Published: EDP Sciences 2020-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/55/e3sconf_e-unsat2020_03038.pdf
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spelling doaj-3da3a497fb45450782b2f17cb69fa97a2021-04-02T17:00:46ZengEDP SciencesE3S Web of Conferences2267-12422020-01-011950303810.1051/e3sconf/202019503038e3sconf_e-unsat2020_03038Yielding of a quartz sand from saturated to dry stateButticè Vincenzo0Ferrari AlessioRosone Marco1Dipatimento di Ingegneria – DI, Università degli Studi di PalermoDipatimento di Ingegneria – DI, Università degli Studi di PalermoThe paper presents the results of an experimental work where we analyse the behaviour of an unsaturated quartz sand in a wide range of degree of saturation (from saturated to dry state). The possibility of anticipating the hydro-mechanical behaviour of the soils when they approach the dry state is fundamental in many areas. An extensive experimental program, including controlled-suction and constant water content oedometric tests, was carried out to deeply analyse the water retention behaviour and the relationship between the yield stress and suction (Loading-Collapse curve). All elasto-plastic models provide a monotonically increase of the yield stress with suction. This assumption implies that the yield stress in the dry state is larger than the one relative to the saturated state, in contrast with the classical geotechnical points of view, which suggest that the yield stress of dry granular material must be approximately the same as that of the saturated one. The obtained results show that the yield stress of the sand does not increase monotonically with the suction, as predicted by commons models. In fact, the Loading - Collapse curve showed in this work presents a maximum point, and the yield stress for saturated condition is almost the same of the dried one.https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/55/e3sconf_e-unsat2020_03038.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Butticè Vincenzo
Ferrari Alessio
Rosone Marco
spellingShingle Butticè Vincenzo
Ferrari Alessio
Rosone Marco
Yielding of a quartz sand from saturated to dry state
E3S Web of Conferences
author_facet Butticè Vincenzo
Ferrari Alessio
Rosone Marco
author_sort Butticè Vincenzo
title Yielding of a quartz sand from saturated to dry state
title_short Yielding of a quartz sand from saturated to dry state
title_full Yielding of a quartz sand from saturated to dry state
title_fullStr Yielding of a quartz sand from saturated to dry state
title_full_unstemmed Yielding of a quartz sand from saturated to dry state
title_sort yielding of a quartz sand from saturated to dry state
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2020-01-01
description The paper presents the results of an experimental work where we analyse the behaviour of an unsaturated quartz sand in a wide range of degree of saturation (from saturated to dry state). The possibility of anticipating the hydro-mechanical behaviour of the soils when they approach the dry state is fundamental in many areas. An extensive experimental program, including controlled-suction and constant water content oedometric tests, was carried out to deeply analyse the water retention behaviour and the relationship between the yield stress and suction (Loading-Collapse curve). All elasto-plastic models provide a monotonically increase of the yield stress with suction. This assumption implies that the yield stress in the dry state is larger than the one relative to the saturated state, in contrast with the classical geotechnical points of view, which suggest that the yield stress of dry granular material must be approximately the same as that of the saturated one. The obtained results show that the yield stress of the sand does not increase monotonically with the suction, as predicted by commons models. In fact, the Loading - Collapse curve showed in this work presents a maximum point, and the yield stress for saturated condition is almost the same of the dried one.
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/55/e3sconf_e-unsat2020_03038.pdf
work_keys_str_mv AT butticevincenzo yieldingofaquartzsandfromsaturatedtodrystate
AT ferrarialessio yieldingofaquartzsandfromsaturatedtodrystate
AT rosonemarco yieldingofaquartzsandfromsaturatedtodrystate
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