The Flat Dilatometer Test in an Unsaturated Tropical Soil Site

Detalhes bibliográficos
Autor(a) principal: Rocha, Breno Padovezi
Data de Publicação: 2021
Outros Autores: Rodrigues, Roger Augusto [UNESP], Giacheti, Heraldo Luiz [UNESP]
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UNESP
Texto Completo: http://dx.doi.org/10.1007/s10706-021-01849-1
http://hdl.handle.net/11449/233159
Resumo: The site characterization of unsaturated soils is well stablished based on laboratory tests, which are expensive and time-consuming. In-situ testing methods, such as the flat dilatometer test (DMT), are an alternative to the traditional approach of drilling, sampling, and laboratory testing. The literature on DMT interpretation is well established on saturated and well-behaved soils. Only few studies deal with DMT interpretation in unusual soils, and little is known about the influence of soil suction on this test. This paper presents and discusses the influence of soil suction on four DMT campaigns carried out in an unsaturated tropical soil site, also incorporating the soil suction influence on the DMT interpretation. Soil suction was estimated by the soil–water characteristic curve (SWCC) and water content profiles. The water content profiles range from 11.3 to 19.7% which corresponds to a suction range estimated by SWCCs mostly between 6 and 200 kPa. Soil suction significantly influenced DMT data up to 5 m depth at the studied site (the unsaturated active zone) increasing the intermediate DMT parameters. The average horizontal stress index (KD) was equal to about 1.7 and the average dilatometer modulus (ED) was about 4.7 MPa in the active zone and practically doubled their values due to in situ soil suction. The estimated peak friction angle (ϕ) was 20–30% higher due to soil suction influence on DMT assuming the soil behaves as a sand like material. Soil suction must be considered to assess the behavior of the investigated soil by the DMT. The suction influence should be incorporated in the effective stress and this approach considerably improved the site characterization of the studied site.
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spelling The Flat Dilatometer Test in an Unsaturated Tropical Soil SiteFlat dilatometer testSoil–water characteristic curveSuctionWater content profileThe site characterization of unsaturated soils is well stablished based on laboratory tests, which are expensive and time-consuming. In-situ testing methods, such as the flat dilatometer test (DMT), are an alternative to the traditional approach of drilling, sampling, and laboratory testing. The literature on DMT interpretation is well established on saturated and well-behaved soils. Only few studies deal with DMT interpretation in unusual soils, and little is known about the influence of soil suction on this test. This paper presents and discusses the influence of soil suction on four DMT campaigns carried out in an unsaturated tropical soil site, also incorporating the soil suction influence on the DMT interpretation. Soil suction was estimated by the soil–water characteristic curve (SWCC) and water content profiles. The water content profiles range from 11.3 to 19.7% which corresponds to a suction range estimated by SWCCs mostly between 6 and 200 kPa. Soil suction significantly influenced DMT data up to 5 m depth at the studied site (the unsaturated active zone) increasing the intermediate DMT parameters. The average horizontal stress index (KD) was equal to about 1.7 and the average dilatometer modulus (ED) was about 4.7 MPa in the active zone and practically doubled their values due to in situ soil suction. The estimated peak friction angle (ϕ) was 20–30% higher due to soil suction influence on DMT assuming the soil behaves as a sand like material. Soil suction must be considered to assess the behavior of the investigated soil by the DMT. The suction influence should be incorporated in the effective stress and this approach considerably improved the site characterization of the studied site.Federal Institute of São Paulo, 164, Tucuruí AveSão Paulo State University, 14-01, Eng. Luiz Edmundo Carrijo Coube AveSão Paulo State University, 14-01, Eng. Luiz Edmundo Carrijo Coube AveFederal Institute of São PauloUniversidade Estadual Paulista (UNESP)Rocha, Breno PadoveziRodrigues, Roger Augusto [UNESP]Giacheti, Heraldo Luiz [UNESP]2022-05-01T05:29:02Z2022-05-01T05:29:02Z2021-01-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://dx.doi.org/10.1007/s10706-021-01849-1Geotechnical and Geological Engineering.1573-15290960-3182http://hdl.handle.net/11449/23315910.1007/s10706-021-01849-12-s2.0-85108017630Scopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengGeotechnical and Geological Engineeringinfo:eu-repo/semantics/openAccess2024-06-28T12:56:41Zoai:repositorio.unesp.br:11449/233159Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462024-08-05T19:46:49.125287Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false
dc.title.none.fl_str_mv The Flat Dilatometer Test in an Unsaturated Tropical Soil Site
title The Flat Dilatometer Test in an Unsaturated Tropical Soil Site
spellingShingle The Flat Dilatometer Test in an Unsaturated Tropical Soil Site
Rocha, Breno Padovezi
Flat dilatometer test
Soil–water characteristic curve
Suction
Water content profile
title_short The Flat Dilatometer Test in an Unsaturated Tropical Soil Site
title_full The Flat Dilatometer Test in an Unsaturated Tropical Soil Site
title_fullStr The Flat Dilatometer Test in an Unsaturated Tropical Soil Site
title_full_unstemmed The Flat Dilatometer Test in an Unsaturated Tropical Soil Site
title_sort The Flat Dilatometer Test in an Unsaturated Tropical Soil Site
author Rocha, Breno Padovezi
author_facet Rocha, Breno Padovezi
Rodrigues, Roger Augusto [UNESP]
Giacheti, Heraldo Luiz [UNESP]
author_role author
author2 Rodrigues, Roger Augusto [UNESP]
Giacheti, Heraldo Luiz [UNESP]
author2_role author
author
dc.contributor.none.fl_str_mv Federal Institute of São Paulo
Universidade Estadual Paulista (UNESP)
dc.contributor.author.fl_str_mv Rocha, Breno Padovezi
Rodrigues, Roger Augusto [UNESP]
Giacheti, Heraldo Luiz [UNESP]
dc.subject.por.fl_str_mv Flat dilatometer test
Soil–water characteristic curve
Suction
Water content profile
topic Flat dilatometer test
Soil–water characteristic curve
Suction
Water content profile
description The site characterization of unsaturated soils is well stablished based on laboratory tests, which are expensive and time-consuming. In-situ testing methods, such as the flat dilatometer test (DMT), are an alternative to the traditional approach of drilling, sampling, and laboratory testing. The literature on DMT interpretation is well established on saturated and well-behaved soils. Only few studies deal with DMT interpretation in unusual soils, and little is known about the influence of soil suction on this test. This paper presents and discusses the influence of soil suction on four DMT campaigns carried out in an unsaturated tropical soil site, also incorporating the soil suction influence on the DMT interpretation. Soil suction was estimated by the soil–water characteristic curve (SWCC) and water content profiles. The water content profiles range from 11.3 to 19.7% which corresponds to a suction range estimated by SWCCs mostly between 6 and 200 kPa. Soil suction significantly influenced DMT data up to 5 m depth at the studied site (the unsaturated active zone) increasing the intermediate DMT parameters. The average horizontal stress index (KD) was equal to about 1.7 and the average dilatometer modulus (ED) was about 4.7 MPa in the active zone and practically doubled their values due to in situ soil suction. The estimated peak friction angle (ϕ) was 20–30% higher due to soil suction influence on DMT assuming the soil behaves as a sand like material. Soil suction must be considered to assess the behavior of the investigated soil by the DMT. The suction influence should be incorporated in the effective stress and this approach considerably improved the site characterization of the studied site.
publishDate 2021
dc.date.none.fl_str_mv 2021-01-01
2022-05-01T05:29:02Z
2022-05-01T05:29:02Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://dx.doi.org/10.1007/s10706-021-01849-1
Geotechnical and Geological Engineering.
1573-1529
0960-3182
http://hdl.handle.net/11449/233159
10.1007/s10706-021-01849-1
2-s2.0-85108017630
url http://dx.doi.org/10.1007/s10706-021-01849-1
http://hdl.handle.net/11449/233159
identifier_str_mv Geotechnical and Geological Engineering.
1573-1529
0960-3182
10.1007/s10706-021-01849-1
2-s2.0-85108017630
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv Geotechnical and Geological Engineering
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.source.none.fl_str_mv Scopus
reponame:Repositório Institucional da UNESP
instname:Universidade Estadual Paulista (UNESP)
instacron:UNESP
instname_str Universidade Estadual Paulista (UNESP)
instacron_str UNESP
institution UNESP
reponame_str Repositório Institucional da UNESP
collection Repositório Institucional da UNESP
repository.name.fl_str_mv Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)
repository.mail.fl_str_mv
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