Formulation of reference solutions for compaction process in sedimentary basins

Detalhes bibliográficos
Autor(a) principal: Lemos, Paulo Sérgio Baumbach
Data de Publicação: 2020
Outros Autores: Brüch, André Reinert, Maghous, Samir
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UFRGS
Texto Completo: http://hdl.handle.net/10183/216696
Resumo: This paper is devoted to the development of semianalytical solutions for the deformation induced by gravitational compaction in sedimentary basins. Formulated within the framework of coupled plasticity–viscoplasticity at large strains, the modeling dedicates special emphasis to the effects of material densification associated with large irreversible porosity changes on the stiffness and hardening of the sediment material. At material level, the purely mechanical compaction taking place in the upper layers of the basin is handled in the context of finite elastoplasticity, whereas the viscoplastic component of behavior is intended to address creep-like deformation resulting from chemomechanical that prevails at deeper layers. Semianalytical solutions describing the evolution of mechanical state of the sedimentary basin along both the accretion and postaccretion periods are presented in the simplified oedometric setting. These solutions can be viewed as reference solutions for verification and benchmarks of basin simulators. The proposed approach may reveal suitable for parametric analyses because it requires only standard mathematics-based software for PDE system resolution. The numerical illustrations provide a quantitative comparison between the derived solutions and finite element predictions from an appropriate basin simulator, thus showing the ability of the approach to accurately capture essential features of basin deformation.
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spelling Lemos, Paulo Sérgio BaumbachBrüch, André ReinertMaghous, Samir2020-12-18T04:13:42Z20201096-9853http://hdl.handle.net/10183/216696001119620This paper is devoted to the development of semianalytical solutions for the deformation induced by gravitational compaction in sedimentary basins. Formulated within the framework of coupled plasticity–viscoplasticity at large strains, the modeling dedicates special emphasis to the effects of material densification associated with large irreversible porosity changes on the stiffness and hardening of the sediment material. At material level, the purely mechanical compaction taking place in the upper layers of the basin is handled in the context of finite elastoplasticity, whereas the viscoplastic component of behavior is intended to address creep-like deformation resulting from chemomechanical that prevails at deeper layers. Semianalytical solutions describing the evolution of mechanical state of the sedimentary basin along both the accretion and postaccretion periods are presented in the simplified oedometric setting. These solutions can be viewed as reference solutions for verification and benchmarks of basin simulators. The proposed approach may reveal suitable for parametric analyses because it requires only standard mathematics-based software for PDE system resolution. The numerical illustrations provide a quantitative comparison between the derived solutions and finite element predictions from an appropriate basin simulator, thus showing the ability of the approach to accurately capture essential features of basin deformation.application/pdfengInternational journal for numerical and analytical methods in geomechanics [recurso eletrônico]. Hoboken, NJ : Wiley. Vol. 44, no. 16 (Nov. 2020), p. 2135-2166ViscoplasticidadeCompactação do soloBacias sedimentaresCoupled plasticity–viscoplasticityGravitational compactionHardeningLarge strainsSedimentary basinFormulation of reference solutions for compaction process in sedimentary basinsEstrangeiroinfo:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da UFRGSinstname:Universidade Federal do Rio Grande do Sul (UFRGS)instacron:UFRGSTEXT001119620.pdf.txt001119620.pdf.txtExtracted Texttext/plain89593http://www.lume.ufrgs.br/bitstream/10183/216696/2/001119620.pdf.txt6aff1c4bca04b6349b47e8c2427fae6cMD52ORIGINAL001119620.pdfTexto completo (inglês)application/pdf2847559http://www.lume.ufrgs.br/bitstream/10183/216696/1/001119620.pdf6109606c50468c8607b37288b59b2975MD5110183/2166962021-11-20 05:59:40.450605oai:www.lume.ufrgs.br:10183/216696Repositório de PublicaçõesPUBhttps://lume.ufrgs.br/oai/requestopendoar:2021-11-20T07:59:40Repositório Institucional da UFRGS - Universidade Federal do Rio Grande do Sul (UFRGS)false
dc.title.pt_BR.fl_str_mv Formulation of reference solutions for compaction process in sedimentary basins
title Formulation of reference solutions for compaction process in sedimentary basins
spellingShingle Formulation of reference solutions for compaction process in sedimentary basins
Lemos, Paulo Sérgio Baumbach
Viscoplasticidade
Compactação do solo
Bacias sedimentares
Coupled plasticity–viscoplasticity
Gravitational compaction
Hardening
Large strains
Sedimentary basin
title_short Formulation of reference solutions for compaction process in sedimentary basins
title_full Formulation of reference solutions for compaction process in sedimentary basins
title_fullStr Formulation of reference solutions for compaction process in sedimentary basins
title_full_unstemmed Formulation of reference solutions for compaction process in sedimentary basins
title_sort Formulation of reference solutions for compaction process in sedimentary basins
author Lemos, Paulo Sérgio Baumbach
author_facet Lemos, Paulo Sérgio Baumbach
Brüch, André Reinert
Maghous, Samir
author_role author
author2 Brüch, André Reinert
Maghous, Samir
author2_role author
author
dc.contributor.author.fl_str_mv Lemos, Paulo Sérgio Baumbach
Brüch, André Reinert
Maghous, Samir
dc.subject.por.fl_str_mv Viscoplasticidade
Compactação do solo
Bacias sedimentares
topic Viscoplasticidade
Compactação do solo
Bacias sedimentares
Coupled plasticity–viscoplasticity
Gravitational compaction
Hardening
Large strains
Sedimentary basin
dc.subject.eng.fl_str_mv Coupled plasticity–viscoplasticity
Gravitational compaction
Hardening
Large strains
Sedimentary basin
description This paper is devoted to the development of semianalytical solutions for the deformation induced by gravitational compaction in sedimentary basins. Formulated within the framework of coupled plasticity–viscoplasticity at large strains, the modeling dedicates special emphasis to the effects of material densification associated with large irreversible porosity changes on the stiffness and hardening of the sediment material. At material level, the purely mechanical compaction taking place in the upper layers of the basin is handled in the context of finite elastoplasticity, whereas the viscoplastic component of behavior is intended to address creep-like deformation resulting from chemomechanical that prevails at deeper layers. Semianalytical solutions describing the evolution of mechanical state of the sedimentary basin along both the accretion and postaccretion periods are presented in the simplified oedometric setting. These solutions can be viewed as reference solutions for verification and benchmarks of basin simulators. The proposed approach may reveal suitable for parametric analyses because it requires only standard mathematics-based software for PDE system resolution. The numerical illustrations provide a quantitative comparison between the derived solutions and finite element predictions from an appropriate basin simulator, thus showing the ability of the approach to accurately capture essential features of basin deformation.
publishDate 2020
dc.date.accessioned.fl_str_mv 2020-12-18T04:13:42Z
dc.date.issued.fl_str_mv 2020
dc.type.driver.fl_str_mv Estrangeiro
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dc.identifier.uri.fl_str_mv http://hdl.handle.net/10183/216696
dc.identifier.issn.pt_BR.fl_str_mv 1096-9853
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dc.language.iso.fl_str_mv eng
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dc.relation.ispartof.pt_BR.fl_str_mv International journal for numerical and analytical methods in geomechanics [recurso eletrônico]. Hoboken, NJ : Wiley. Vol. 44, no. 16 (Nov. 2020), p. 2135-2166
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