Stress path during pressuremeter test and link between shear modulus and Menard pressuremeter modulus in unsaturated fine soils

This paper presents the stress path before and during a pressumeter test using a Modified Cam-Clay model. This model have been used for unsaturated clay with continuous water phase (D2 domain according to Boutonnier 2007) and for silty to clayey soils with discontinuous water phase (D1 domain – ibid...

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Main Authors: Savatier Vincent, Savatier Maxime
Format: Article
Language:English
Published: EDP Sciences 2016-01-01
Series:E3S Web of Conferences
Online Access:http://dx.doi.org/10.1051/e3sconf/20160909010
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spelling doaj-2b5b5b57fe4943d4b8c18bf5bf5a2c7f2021-02-02T00:27:25ZengEDP SciencesE3S Web of Conferences2267-12422016-01-0190901010.1051/e3sconf/20160909010e3sconf_eunsat2016_09010Stress path during pressuremeter test and link between shear modulus and Menard pressuremeter modulus in unsaturated fine soilsSavatier Vincent0Savatier Maxime1EGIS Geotechnique1 rue des rempartsThis paper presents the stress path before and during a pressumeter test using a Modified Cam-Clay model. This model have been used for unsaturated clay with continuous water phase (D2 domain according to Boutonnier 2007) and for silty to clayey soils with discontinuous water phase (D1 domain – ibid.). After reminding the stress distribution around a pressuremeter cell and the meaning of the Menard pressuremeter modulus which is linked to the soil shear modulus, we explain the stress state during pressuremeter modulus measurement. Then, we show that this stress path diagram can be used to explain classical observations made using Menard pressuremeter tests in continental area and typically: Measurement of high ratio “Menard pressuremeter modulus / pressuremeter limit pressure” in clay subjected to drought. Limit pressure and Ménard pressuremeter modulus variation with respect to drought in silty clay situated in water-table fluctuation area. Finally, we will try to show the consequences of these stress paths for performing and interpreting pressuremeter test in unsaturated and collapsible soils.http://dx.doi.org/10.1051/e3sconf/20160909010
collection DOAJ
language English
format Article
sources DOAJ
author Savatier Vincent
Savatier Maxime
spellingShingle Savatier Vincent
Savatier Maxime
Stress path during pressuremeter test and link between shear modulus and Menard pressuremeter modulus in unsaturated fine soils
E3S Web of Conferences
author_facet Savatier Vincent
Savatier Maxime
author_sort Savatier Vincent
title Stress path during pressuremeter test and link between shear modulus and Menard pressuremeter modulus in unsaturated fine soils
title_short Stress path during pressuremeter test and link between shear modulus and Menard pressuremeter modulus in unsaturated fine soils
title_full Stress path during pressuremeter test and link between shear modulus and Menard pressuremeter modulus in unsaturated fine soils
title_fullStr Stress path during pressuremeter test and link between shear modulus and Menard pressuremeter modulus in unsaturated fine soils
title_full_unstemmed Stress path during pressuremeter test and link between shear modulus and Menard pressuremeter modulus in unsaturated fine soils
title_sort stress path during pressuremeter test and link between shear modulus and menard pressuremeter modulus in unsaturated fine soils
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2016-01-01
description This paper presents the stress path before and during a pressumeter test using a Modified Cam-Clay model. This model have been used for unsaturated clay with continuous water phase (D2 domain according to Boutonnier 2007) and for silty to clayey soils with discontinuous water phase (D1 domain – ibid.). After reminding the stress distribution around a pressuremeter cell and the meaning of the Menard pressuremeter modulus which is linked to the soil shear modulus, we explain the stress state during pressuremeter modulus measurement. Then, we show that this stress path diagram can be used to explain classical observations made using Menard pressuremeter tests in continental area and typically: Measurement of high ratio “Menard pressuremeter modulus / pressuremeter limit pressure” in clay subjected to drought. Limit pressure and Ménard pressuremeter modulus variation with respect to drought in silty clay situated in water-table fluctuation area. Finally, we will try to show the consequences of these stress paths for performing and interpreting pressuremeter test in unsaturated and collapsible soils.
url http://dx.doi.org/10.1051/e3sconf/20160909010
work_keys_str_mv AT savatiervincent stresspathduringpressuremetertestandlinkbetweenshearmodulusandmenardpressuremetermodulusinunsaturatedfinesoils
AT savatiermaxime stresspathduringpressuremetertestandlinkbetweenshearmodulusandmenardpressuremetermodulusinunsaturatedfinesoils
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