Precompression stress and compression index depend on the property used to represent the soil deformation in the compression curve

Detalhes bibliográficos
Autor(a) principal: Gubiani,Paulo Ivonir
Data de Publicação: 2016
Outros Autores: Jong Van Lier,Quirijn de, Reichert,José Miguel, Goulart,Rafael Ziani, Fontanela,Eracilda
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Ciência Rural
Texto Completo: http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0103-84782016000100076
Resumo: ABSTRACT: During linear deformation (h) in a soil sample, the variation of the void ratio with respect to deformation (dε/dh) and the respective variation of soil bulk density (dρ/dh) are identical only for a specific value of h. Consequently, if two compression curves are drawn for the same soil sample, one using ρ and the other using ε, there are differences in both the calculated precompression stress (σp) and compression index (Ic). In this study, we highlight the causes by a mathematical analysis and an experimental investigation, quantifying the differences in σp and Ic when using ε and ρ. σp and Ic were calculated for 103 compression curves of an ultisol and 193 of an oxisol. The σp (kPa) using ρ (σpρ) was greater than when using ε (σpε), and differences were rather independent of the soil type. The relations found by linear regression relating σpρ to σpε were σpρ=0.8186σpε+34.202 for the ultisol and σpρ=0.8878σpε+34.875 for the oxisol. In contrast, the used soil property (ρ or ε) as well as soil type affected Ic. Ic calculated using ρ was greater than when using ε in almost all (96%) of the cases for the ultisol, and in only 12% of the cases for the oxisol. For a wide range of ρ, evidence from this study indicated that the use of ρ overestimates σp when compared to the use of ε.
id UFSM-2_3583409e261395ccb1d76353a8f78028
oai_identifier_str oai:scielo:S0103-84782016000100076
network_acronym_str UFSM-2
network_name_str Ciência rural (Online)
repository_id_str
spelling Precompression stress and compression index depend on the property used to represent the soil deformation in the compression curvevoid ratioparticle densitysoil bulk densityABSTRACT: During linear deformation (h) in a soil sample, the variation of the void ratio with respect to deformation (dε/dh) and the respective variation of soil bulk density (dρ/dh) are identical only for a specific value of h. Consequently, if two compression curves are drawn for the same soil sample, one using ρ and the other using ε, there are differences in both the calculated precompression stress (σp) and compression index (Ic). In this study, we highlight the causes by a mathematical analysis and an experimental investigation, quantifying the differences in σp and Ic when using ε and ρ. σp and Ic were calculated for 103 compression curves of an ultisol and 193 of an oxisol. The σp (kPa) using ρ (σpρ) was greater than when using ε (σpε), and differences were rather independent of the soil type. The relations found by linear regression relating σpρ to σpε were σpρ=0.8186σpε+34.202 for the ultisol and σpρ=0.8878σpε+34.875 for the oxisol. In contrast, the used soil property (ρ or ε) as well as soil type affected Ic. Ic calculated using ρ was greater than when using ε in almost all (96%) of the cases for the ultisol, and in only 12% of the cases for the oxisol. For a wide range of ρ, evidence from this study indicated that the use of ρ overestimates σp when compared to the use of ε.Universidade Federal de Santa Maria2016-01-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0103-84782016000100076Ciência Rural v.46 n.1 2016reponame:Ciência Ruralinstname:Universidade Federal de Santa Maria (UFSM)instacron:UFSM10.1590/0103-8478cr20141495info:eu-repo/semantics/openAccessGubiani,Paulo IvonirJong Van Lier,Quirijn deReichert,José MiguelGoulart,Rafael ZianiFontanela,Eracildaeng2016-01-20T00:00:00ZRevista
dc.title.none.fl_str_mv Precompression stress and compression index depend on the property used to represent the soil deformation in the compression curve
title Precompression stress and compression index depend on the property used to represent the soil deformation in the compression curve
spellingShingle Precompression stress and compression index depend on the property used to represent the soil deformation in the compression curve
Gubiani,Paulo Ivonir
void ratio
particle density
soil bulk density
title_short Precompression stress and compression index depend on the property used to represent the soil deformation in the compression curve
title_full Precompression stress and compression index depend on the property used to represent the soil deformation in the compression curve
title_fullStr Precompression stress and compression index depend on the property used to represent the soil deformation in the compression curve
title_full_unstemmed Precompression stress and compression index depend on the property used to represent the soil deformation in the compression curve
title_sort Precompression stress and compression index depend on the property used to represent the soil deformation in the compression curve
author Gubiani,Paulo Ivonir
author_facet Gubiani,Paulo Ivonir
Jong Van Lier,Quirijn de
Reichert,José Miguel
Goulart,Rafael Ziani
Fontanela,Eracilda
author_role author
author2 Jong Van Lier,Quirijn de
Reichert,José Miguel
Goulart,Rafael Ziani
Fontanela,Eracilda
author2_role author
author
author
author
dc.contributor.author.fl_str_mv Gubiani,Paulo Ivonir
Jong Van Lier,Quirijn de
Reichert,José Miguel
Goulart,Rafael Ziani
Fontanela,Eracilda
dc.subject.por.fl_str_mv void ratio
particle density
soil bulk density
topic void ratio
particle density
soil bulk density
description ABSTRACT: During linear deformation (h) in a soil sample, the variation of the void ratio with respect to deformation (dε/dh) and the respective variation of soil bulk density (dρ/dh) are identical only for a specific value of h. Consequently, if two compression curves are drawn for the same soil sample, one using ρ and the other using ε, there are differences in both the calculated precompression stress (σp) and compression index (Ic). In this study, we highlight the causes by a mathematical analysis and an experimental investigation, quantifying the differences in σp and Ic when using ε and ρ. σp and Ic were calculated for 103 compression curves of an ultisol and 193 of an oxisol. The σp (kPa) using ρ (σpρ) was greater than when using ε (σpε), and differences were rather independent of the soil type. The relations found by linear regression relating σpρ to σpε were σpρ=0.8186σpε+34.202 for the ultisol and σpρ=0.8878σpε+34.875 for the oxisol. In contrast, the used soil property (ρ or ε) as well as soil type affected Ic. Ic calculated using ρ was greater than when using ε in almost all (96%) of the cases for the ultisol, and in only 12% of the cases for the oxisol. For a wide range of ρ, evidence from this study indicated that the use of ρ overestimates σp when compared to the use of ε.
publishDate 2016
dc.date.none.fl_str_mv 2016-01-01
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0103-84782016000100076
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0103-84782016000100076
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 10.1590/0103-8478cr20141495
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv text/html
dc.publisher.none.fl_str_mv Universidade Federal de Santa Maria
publisher.none.fl_str_mv Universidade Federal de Santa Maria
dc.source.none.fl_str_mv Ciência Rural v.46 n.1 2016
reponame:Ciência Rural
instname:Universidade Federal de Santa Maria (UFSM)
instacron:UFSM
instname_str Universidade Federal de Santa Maria (UFSM)
instacron_str UFSM
institution UFSM
reponame_str Ciência Rural
collection Ciência Rural
repository.name.fl_str_mv
repository.mail.fl_str_mv
_version_ 1749140548572151808