The Flat Dilatometer Test in an Unsaturated Tropical Soil Site
Autor(a) principal: | |
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Data de Publicação: | 2021 |
Outros Autores: | , |
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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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 |
|
_version_ |
1808129117481074688 |