Slope stability analysis at highway BR-153 using numerical models

Detalhes bibliográficos
Autor(a) principal: Hundelshaussen Rubio, Ricardo José
Data de Publicação: 2016
Outros Autores: Flórez Gálvez, Jorge Hernán, Zingano, Andre Cezar
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UFRGS
Texto Completo: http://hdl.handle.net/10183/143934
Resumo: An existing cut slope on Highway RS-471/BR-153 is studied. The slope is composed of the Serra Geral Formation's material: a highly altered volcanic breccia and above it a slightly altered and very fractured rhyolite. A numerical analysis of the slope is carried out in two dimensions. Fracturing of the rhyolite necessitates the use of a constitutive model for materials with families of discontinuities (Ubiquitous-joint). To simplify the analysis of the problem and to examine some of the most sensitive variables, two more analyses are made, replacing the initial model by a Mohr’s constitutive model, which considers the material as continuous. The results obtained from the Ubiquitous-joint model provide an acceptable representation of the field conditions, showing a failure mechanism type of rockfall from the face of the slope in the rhyolite, and the rupture surface of the breccia, without propagation of surface failure. In the analysis, when considering both materials as continuous, it is not possible to take account the fault conditions simultaneously, and this analysis also requires values of the mechanical parameters different from those recommended in literature.
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spelling Hundelshaussen Rubio, Ricardo JoséFlórez Gálvez, Jorge HernánZingano, Andre Cezar2016-07-23T02:18:24Z20161807-0353http://hdl.handle.net/10183/143934000996959An existing cut slope on Highway RS-471/BR-153 is studied. The slope is composed of the Serra Geral Formation's material: a highly altered volcanic breccia and above it a slightly altered and very fractured rhyolite. A numerical analysis of the slope is carried out in two dimensions. Fracturing of the rhyolite necessitates the use of a constitutive model for materials with families of discontinuities (Ubiquitous-joint). To simplify the analysis of the problem and to examine some of the most sensitive variables, two more analyses are made, replacing the initial model by a Mohr’s constitutive model, which considers the material as continuous. The results obtained from the Ubiquitous-joint model provide an acceptable representation of the field conditions, showing a failure mechanism type of rockfall from the face of the slope in the rhyolite, and the rupture surface of the breccia, without propagation of surface failure. In the analysis, when considering both materials as continuous, it is not possible to take account the fault conditions simultaneously, and this analysis also requires values of the mechanical parameters different from those recommended in literature.application/pdfengRem: revista Escola de Minas. Ouro Preto, MG. Vol. 69, no. 2 (Apr./June 2016), p. 185-191Estabilidade de taludesMecânica dos solosAnálise numéricaVolcanic brecciaSerra geral formationUbiquitous-jointNumerical modelsSlope stability analysis at highway BR-153 using numerical modelsinfo:eu-repo/semantics/articleinfo:eu-repo/semantics/otherinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da UFRGSinstname:Universidade Federal do Rio Grande do Sul (UFRGS)instacron:UFRGSORIGINAL000996959.pdf000996959.pdfTexto completo (inglês)application/pdf4976185http://www.lume.ufrgs.br/bitstream/10183/143934/1/000996959.pdf9648750683b0593a72e0e0d45681adedMD51TEXT000996959.pdf.txt000996959.pdf.txtExtracted Texttext/plain19332http://www.lume.ufrgs.br/bitstream/10183/143934/2/000996959.pdf.txte35d30b0ff1817493e05b1510e2e53cdMD52THUMBNAIL000996959.pdf.jpg000996959.pdf.jpgGenerated Thumbnailimage/jpeg2071http://www.lume.ufrgs.br/bitstream/10183/143934/3/000996959.pdf.jpg545354a6929ab4bcf671d32dbb3be38bMD5310183/1439342021-05-07 05:13:15.916914oai:www.lume.ufrgs.br:10183/143934Repositório de PublicaçõesPUBhttps://lume.ufrgs.br/oai/requestopendoar:2021-05-07T08:13:15Repositório Institucional da UFRGS - Universidade Federal do Rio Grande do Sul (UFRGS)false
dc.title.pt_BR.fl_str_mv Slope stability analysis at highway BR-153 using numerical models
title Slope stability analysis at highway BR-153 using numerical models
spellingShingle Slope stability analysis at highway BR-153 using numerical models
Hundelshaussen Rubio, Ricardo José
Estabilidade de taludes
Mecânica dos solos
Análise numérica
Volcanic breccia
Serra geral formation
Ubiquitous-joint
Numerical models
title_short Slope stability analysis at highway BR-153 using numerical models
title_full Slope stability analysis at highway BR-153 using numerical models
title_fullStr Slope stability analysis at highway BR-153 using numerical models
title_full_unstemmed Slope stability analysis at highway BR-153 using numerical models
title_sort Slope stability analysis at highway BR-153 using numerical models
author Hundelshaussen Rubio, Ricardo José
author_facet Hundelshaussen Rubio, Ricardo José
Flórez Gálvez, Jorge Hernán
Zingano, Andre Cezar
author_role author
author2 Flórez Gálvez, Jorge Hernán
Zingano, Andre Cezar
author2_role author
author
dc.contributor.author.fl_str_mv Hundelshaussen Rubio, Ricardo José
Flórez Gálvez, Jorge Hernán
Zingano, Andre Cezar
dc.subject.por.fl_str_mv Estabilidade de taludes
Mecânica dos solos
Análise numérica
topic Estabilidade de taludes
Mecânica dos solos
Análise numérica
Volcanic breccia
Serra geral formation
Ubiquitous-joint
Numerical models
dc.subject.eng.fl_str_mv Volcanic breccia
Serra geral formation
Ubiquitous-joint
Numerical models
description An existing cut slope on Highway RS-471/BR-153 is studied. The slope is composed of the Serra Geral Formation's material: a highly altered volcanic breccia and above it a slightly altered and very fractured rhyolite. A numerical analysis of the slope is carried out in two dimensions. Fracturing of the rhyolite necessitates the use of a constitutive model for materials with families of discontinuities (Ubiquitous-joint). To simplify the analysis of the problem and to examine some of the most sensitive variables, two more analyses are made, replacing the initial model by a Mohr’s constitutive model, which considers the material as continuous. The results obtained from the Ubiquitous-joint model provide an acceptable representation of the field conditions, showing a failure mechanism type of rockfall from the face of the slope in the rhyolite, and the rupture surface of the breccia, without propagation of surface failure. In the analysis, when considering both materials as continuous, it is not possible to take account the fault conditions simultaneously, and this analysis also requires values of the mechanical parameters different from those recommended in literature.
publishDate 2016
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dc.relation.ispartof.pt_BR.fl_str_mv Rem: revista Escola de Minas. Ouro Preto, MG. Vol. 69, no. 2 (Apr./June 2016), p. 185-191
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