Creep of a C-S-H gel: a micromechanical approach

Detalhes bibliográficos
Autor(a) principal: Sanahuja,Julien
Data de Publicação: 2010
Outros Autores: Dormieux,Luc
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Anais da Academia Brasileira de Ciências (Online)
Texto Completo: http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652010000100004
Resumo: Both clays and calcium silicate hydrates(the main hydration products of Portland cements) exhibit a microstructure made up of lamellar particles. The microscopic mechanism responsible for the macroscopic creep of such materials is often described as the relative sliding of the sheets. This paper proposes a micromechanical approach to estimate the macroscopic creep behavior rising from this microscopic mechanism. The asymptotic evolution of creep at both short- and long-term is especially investigated. More precisely, a non-vanishing initial elastic strain is retrieved. At long-term, a threshold on porosity appears. At lower porosities, the creep evolution admits an asymptotic strain. At higher porosities, it admits an asymptotic strain rate.
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spelling Creep of a C-S-H gel: a micromechanical approachhomogenizationcreepcement pasteC-S-H gelBoth clays and calcium silicate hydrates(the main hydration products of Portland cements) exhibit a microstructure made up of lamellar particles. The microscopic mechanism responsible for the macroscopic creep of such materials is often described as the relative sliding of the sheets. This paper proposes a micromechanical approach to estimate the macroscopic creep behavior rising from this microscopic mechanism. The asymptotic evolution of creep at both short- and long-term is especially investigated. More precisely, a non-vanishing initial elastic strain is retrieved. At long-term, a threshold on porosity appears. At lower porosities, the creep evolution admits an asymptotic strain. At higher porosities, it admits an asymptotic strain rate.Academia Brasileira de Ciências2010-03-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652010000100004Anais da Academia Brasileira de Ciências v.82 n.1 2010reponame:Anais da Academia Brasileira de Ciências (Online)instname:Academia Brasileira de Ciências (ABC)instacron:ABC10.1590/S0001-37652010000100004info:eu-repo/semantics/openAccessSanahuja,JulienDormieux,Luceng2010-02-25T00:00:00Zoai:scielo:S0001-37652010000100004Revistahttp://www.scielo.br/aabchttps://old.scielo.br/oai/scielo-oai.php||aabc@abc.org.br1678-26900001-3765opendoar:2010-02-25T00:00Anais da Academia Brasileira de Ciências (Online) - Academia Brasileira de Ciências (ABC)false
dc.title.none.fl_str_mv Creep of a C-S-H gel: a micromechanical approach
title Creep of a C-S-H gel: a micromechanical approach
spellingShingle Creep of a C-S-H gel: a micromechanical approach
Sanahuja,Julien
homogenization
creep
cement paste
C-S-H gel
title_short Creep of a C-S-H gel: a micromechanical approach
title_full Creep of a C-S-H gel: a micromechanical approach
title_fullStr Creep of a C-S-H gel: a micromechanical approach
title_full_unstemmed Creep of a C-S-H gel: a micromechanical approach
title_sort Creep of a C-S-H gel: a micromechanical approach
author Sanahuja,Julien
author_facet Sanahuja,Julien
Dormieux,Luc
author_role author
author2 Dormieux,Luc
author2_role author
dc.contributor.author.fl_str_mv Sanahuja,Julien
Dormieux,Luc
dc.subject.por.fl_str_mv homogenization
creep
cement paste
C-S-H gel
topic homogenization
creep
cement paste
C-S-H gel
description Both clays and calcium silicate hydrates(the main hydration products of Portland cements) exhibit a microstructure made up of lamellar particles. The microscopic mechanism responsible for the macroscopic creep of such materials is often described as the relative sliding of the sheets. This paper proposes a micromechanical approach to estimate the macroscopic creep behavior rising from this microscopic mechanism. The asymptotic evolution of creep at both short- and long-term is especially investigated. More precisely, a non-vanishing initial elastic strain is retrieved. At long-term, a threshold on porosity appears. At lower porosities, the creep evolution admits an asymptotic strain. At higher porosities, it admits an asymptotic strain rate.
publishDate 2010
dc.date.none.fl_str_mv 2010-03-01
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
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status_str publishedVersion
dc.identifier.uri.fl_str_mv http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652010000100004
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652010000100004
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 10.1590/S0001-37652010000100004
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 Academia Brasileira de Ciências
publisher.none.fl_str_mv Academia Brasileira de Ciências
dc.source.none.fl_str_mv Anais da Academia Brasileira de Ciências v.82 n.1 2010
reponame:Anais da Academia Brasileira de Ciências (Online)
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reponame_str Anais da Academia Brasileira de Ciências (Online)
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