Análise de estabilidade de falésias na zona costeira de Baía Formosa - RN

Detalhes bibliográficos
Ano de defesa: 2013
Autor(a) principal: Souza Júnior, Carlos de
Orientador(a): Não Informado pela instituição
Banca de defesa: Não Informado pela instituição
Tipo de documento: Dissertação
Tipo de acesso: Acesso aberto
Idioma: por
Instituição de defesa: Universidade Federal do Rio Grande do Norte
Brasil
UFRN
PROGRAMA DE PÓS-GRADUAÇÃO EM ENGENHARIA CIVIL
Programa de Pós-Graduação: Não Informado pela instituição
Departamento: Não Informado pela instituição
País: Não Informado pela instituição
Palavras-chave em Português:
Link de acesso: https://repositorio.ufrn.br/jspui/handle/123456789/19368
Resumo: The natural and anthropogenic changes that are occurring at the coastal zone around the world represent the greatest problem to society in this century. This problem becomes more evident due to high density of coastal cities, to growing tourist-estate speculation of those areas and to climate change that tend to trigger and accelerate the erosive processes that operating in the littoral. In this context, it‟s possible perceive ever more a significant increase of problems associated to the coastal erosion and retreat of cliffs in the state of Rio Grande do Norte, where this study area of this search is located. The area is located in the coastal zone of the city of Baía Formosa/RN, in south-eastern coast of Rio Grande do Norte, and has a extension of about 1200 meters along the Porto beach. The main objective of this study is to analyze the stability of these cliffs in this region. Through field investigations, testings and computational analysis using the Finite Element Method and Equilibrium Limit Methods. The area was divided into four sections, and were applied checklists, and also realized characterization tests and direct shear tests with materials obtained along these sections. In this manner, it was found that the segments of cliff in this coastal zone have heights around 4 meters to 14 meters and inclinations of approximately 40° to 90°.However the constituents soils of the cliffs were classified, in general terms in accordance to Unified Soil Classification System (USCS), as clayey sands or silty sands, clays of low plasticity, clayey gravels and poorly graduaded sands. The most variegated and clayey soils belong to base of the cliff. The stability analysis showed that the safety factors ranged in section 01, from 1.92 to 4.93, in the section 02, from 1.00 to 1.43, in the section 03, from 1.36 to 1.75 , and section 04, from 1.00 to 3.64. Thus, the sections 02 and 03 were considered more unstable. However, the section 03 can be considered as the most critical section due to the absence of coastal protection structures and the narrow strip of beach.
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spelling Análise de estabilidade de falésias na zona costeira de Baía Formosa - RNAnalysis of cliffs stability at the coastal zone of Baía Formosa - RNEstabilidade de falésiasErosão costeiraDinâmica costeiraBaía Formosa - RNCNPQ::ENGENHARIAS::ENGENHARIA CIVILThe natural and anthropogenic changes that are occurring at the coastal zone around the world represent the greatest problem to society in this century. This problem becomes more evident due to high density of coastal cities, to growing tourist-estate speculation of those areas and to climate change that tend to trigger and accelerate the erosive processes that operating in the littoral. In this context, it‟s possible perceive ever more a significant increase of problems associated to the coastal erosion and retreat of cliffs in the state of Rio Grande do Norte, where this study area of this search is located. The area is located in the coastal zone of the city of Baía Formosa/RN, in south-eastern coast of Rio Grande do Norte, and has a extension of about 1200 meters along the Porto beach. The main objective of this study is to analyze the stability of these cliffs in this region. Through field investigations, testings and computational analysis using the Finite Element Method and Equilibrium Limit Methods. The area was divided into four sections, and were applied checklists, and also realized characterization tests and direct shear tests with materials obtained along these sections. In this manner, it was found that the segments of cliff in this coastal zone have heights around 4 meters to 14 meters and inclinations of approximately 40° to 90°.However the constituents soils of the cliffs were classified, in general terms in accordance to Unified Soil Classification System (USCS), as clayey sands or silty sands, clays of low plasticity, clayey gravels and poorly graduaded sands. The most variegated and clayey soils belong to base of the cliff. The stability analysis showed that the safety factors ranged in section 01, from 1.92 to 4.93, in the section 02, from 1.00 to 1.43, in the section 03, from 1.36 to 1.75 , and section 04, from 1.00 to 3.64. Thus, the sections 02 and 03 were considered more unstable. However, the section 03 can be considered as the most critical section due to the absence of coastal protection structures and the narrow strip of beach.As mudanças naturais e antrópicas que vêm ocorrendo na zona costeira em todo o mundo representam um dos maiores problemas para a sociedade neste século. Essa importância se torna mais evidente devido à elevada densidade das cidades litorâneas, à crescente especulação turístico-imobiliária dessas áreas e às alterações climáticas que tendem a desencadear e acelerar esses processos. Nesse contexto, percebe-se cada vez mais um aumento significativo dos problemas relacionados à erosão costeira e recuo de falésias no estado do Rio Grande do Norte. A área de estudo desta pesquisa localiza-se na zona costeira do município de Baía Formosa/RN, no litoral oriental-sul do Rio Grande do Norte, e possui uma extensão de cerca de 1200 m ao longo da praia do Porto. O objetivo principal deste trabalho é analisar a estabilidade dessas falésias, através de investigações de campo, ensaios e análises computacionais utilizando o Método dos Elementos Finitos e o Método de Bishop. Para atender aos objetivos deste trabalho, a área foi subdividida em quatro trechos, e foram aplicados checklists e também realizados ensaios de caracterização e de cisalhamento direto com materiais obtidos ao longo desses trechos. Os segmentos de falésia nessa zona costeira possuem alturas variando em torno de 4 m e 14 m e inclinações de aproximadamente 40º a 90º. Os solos constituintes das falésias foram classificados, em termos gerais, como areias argilosas ou siltosas e argilas arenosas, sendo os solos mais argilosos e variegados pertencentes à base da falésia. As análises de estabilidade mostraram que os fatores de segurança variaram, no trecho 01, de 2,38 a 6,06, no trecho 02, de 1,01 a 1,62, no trecho 03, de 1,29 a 1,78, e no trecho 04, de 0,83 a 2,48. Assim, os trechos 02 e 03, foram considerados como mais instáveis. Entretanto, pode-se considerar o trecho 03 como o mais crítico devido à ausência de estruturas de proteção costeira e à estreita faixa de praia. Fato que não ocorre no trecho 02, o qual possui uma extensa faixa de praia e é protegido por um muro de arrimo que restringe o acesso dos banhistas às áreas adjacentes do pé da falésia.Universidade Federal do Rio Grande do NorteBrasilUFRNPROGRAMA DE PÓS-GRADUAÇÃO EM ENGENHARIA CIVILSantos Júnior, Olavo Francisco doshttp://lattes.cnpq.br/8075615191010617http://lattes.cnpq.br/1573496204231636Scudelari, Ada Cristinahttp://lattes.cnpq.br/6556306307432176Freitas Neto, Osvaldo dehttp://lattes.cnpq.br/6335708403185496Amaro, Venerando Eustáquiohttp://lattes.cnpq.br/4215328958233942Souza Júnior, Carlos de2015-11-16T13:32:44Z2015-11-16T13:32:44Z2013-12-20info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesisapplication/pdfSOUZA JÚNIOR, Carlos de. Análise de estabilidade de falésias na zona costeira de Baía Formosa - RN. 2013. 169f. Dissertação (Mestrado em Engenharia Civil) - Centro de Tecnologia, Universidade Federal do Rio Grande do Norte, Natal, 2013.https://repositorio.ufrn.br/jspui/handle/123456789/19368porinfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da UFRNinstname:Universidade Federal do Rio Grande do Norte (UFRN)instacron:UFRN2017-11-02T22:43:42Zoai:repositorio.ufrn.br:123456789/19368Repositório InstitucionalPUBhttp://repositorio.ufrn.br/oai/repositorio@bczm.ufrn.bropendoar:2017-11-02T22:43:42Repositório Institucional da UFRN - Universidade Federal do Rio Grande do Norte (UFRN)false
dc.title.none.fl_str_mv Análise de estabilidade de falésias na zona costeira de Baía Formosa - RN
Analysis of cliffs stability at the coastal zone of Baía Formosa - RN
title Análise de estabilidade de falésias na zona costeira de Baía Formosa - RN
spellingShingle Análise de estabilidade de falésias na zona costeira de Baía Formosa - RN
Souza Júnior, Carlos de
Estabilidade de falésias
Erosão costeira
Dinâmica costeira
Baía Formosa - RN
CNPQ::ENGENHARIAS::ENGENHARIA CIVIL
title_short Análise de estabilidade de falésias na zona costeira de Baía Formosa - RN
title_full Análise de estabilidade de falésias na zona costeira de Baía Formosa - RN
title_fullStr Análise de estabilidade de falésias na zona costeira de Baía Formosa - RN
title_full_unstemmed Análise de estabilidade de falésias na zona costeira de Baía Formosa - RN
title_sort Análise de estabilidade de falésias na zona costeira de Baía Formosa - RN
author Souza Júnior, Carlos de
author_facet Souza Júnior, Carlos de
author_role author
dc.contributor.none.fl_str_mv Santos Júnior, Olavo Francisco dos

http://lattes.cnpq.br/8075615191010617

http://lattes.cnpq.br/1573496204231636
Scudelari, Ada Cristina

http://lattes.cnpq.br/6556306307432176
Freitas Neto, Osvaldo de

http://lattes.cnpq.br/6335708403185496
Amaro, Venerando Eustáquio

http://lattes.cnpq.br/4215328958233942
dc.contributor.author.fl_str_mv Souza Júnior, Carlos de
dc.subject.por.fl_str_mv Estabilidade de falésias
Erosão costeira
Dinâmica costeira
Baía Formosa - RN
CNPQ::ENGENHARIAS::ENGENHARIA CIVIL
topic Estabilidade de falésias
Erosão costeira
Dinâmica costeira
Baía Formosa - RN
CNPQ::ENGENHARIAS::ENGENHARIA CIVIL
description The natural and anthropogenic changes that are occurring at the coastal zone around the world represent the greatest problem to society in this century. This problem becomes more evident due to high density of coastal cities, to growing tourist-estate speculation of those areas and to climate change that tend to trigger and accelerate the erosive processes that operating in the littoral. In this context, it‟s possible perceive ever more a significant increase of problems associated to the coastal erosion and retreat of cliffs in the state of Rio Grande do Norte, where this study area of this search is located. The area is located in the coastal zone of the city of Baía Formosa/RN, in south-eastern coast of Rio Grande do Norte, and has a extension of about 1200 meters along the Porto beach. The main objective of this study is to analyze the stability of these cliffs in this region. Through field investigations, testings and computational analysis using the Finite Element Method and Equilibrium Limit Methods. The area was divided into four sections, and were applied checklists, and also realized characterization tests and direct shear tests with materials obtained along these sections. In this manner, it was found that the segments of cliff in this coastal zone have heights around 4 meters to 14 meters and inclinations of approximately 40° to 90°.However the constituents soils of the cliffs were classified, in general terms in accordance to Unified Soil Classification System (USCS), as clayey sands or silty sands, clays of low plasticity, clayey gravels and poorly graduaded sands. The most variegated and clayey soils belong to base of the cliff. The stability analysis showed that the safety factors ranged in section 01, from 1.92 to 4.93, in the section 02, from 1.00 to 1.43, in the section 03, from 1.36 to 1.75 , and section 04, from 1.00 to 3.64. Thus, the sections 02 and 03 were considered more unstable. However, the section 03 can be considered as the most critical section due to the absence of coastal protection structures and the narrow strip of beach.
publishDate 2013
dc.date.none.fl_str_mv 2013-12-20
2015-11-16T13:32:44Z
2015-11-16T13:32:44Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/masterThesis
format masterThesis
status_str publishedVersion
dc.identifier.uri.fl_str_mv SOUZA JÚNIOR, Carlos de. Análise de estabilidade de falésias na zona costeira de Baía Formosa - RN. 2013. 169f. Dissertação (Mestrado em Engenharia Civil) - Centro de Tecnologia, Universidade Federal do Rio Grande do Norte, Natal, 2013.
https://repositorio.ufrn.br/jspui/handle/123456789/19368
identifier_str_mv SOUZA JÚNIOR, Carlos de. Análise de estabilidade de falésias na zona costeira de Baía Formosa - RN. 2013. 169f. Dissertação (Mestrado em Engenharia Civil) - Centro de Tecnologia, Universidade Federal do Rio Grande do Norte, Natal, 2013.
url https://repositorio.ufrn.br/jspui/handle/123456789/19368
dc.language.iso.fl_str_mv por
language por
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Universidade Federal do Rio Grande do Norte
Brasil
UFRN
PROGRAMA DE PÓS-GRADUAÇÃO EM ENGENHARIA CIVIL
publisher.none.fl_str_mv Universidade Federal do Rio Grande do Norte
Brasil
UFRN
PROGRAMA DE PÓS-GRADUAÇÃO EM ENGENHARIA CIVIL
dc.source.none.fl_str_mv reponame:Repositório Institucional da UFRN
instname:Universidade Federal do Rio Grande do Norte (UFRN)
instacron:UFRN
instname_str Universidade Federal do Rio Grande do Norte (UFRN)
instacron_str UFRN
institution UFRN
reponame_str Repositório Institucional da UFRN
collection Repositório Institucional da UFRN
repository.name.fl_str_mv Repositório Institucional da UFRN - Universidade Federal do Rio Grande do Norte (UFRN)
repository.mail.fl_str_mv repositorio@bczm.ufrn.br
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