Contribuições da morfodinâmica no zoneamento territorial em Goiana, litoral norte de Pernambuco, Brasil

Detalhes bibliográficos
Ano de defesa: 2022
Autor(a) principal: Madruga, Marcelo Menezes Diniz
Orientador(a): Freire, George Satander Sá
Banca de defesa: Não Informado pela instituição
Tipo de documento: Tese
Tipo de acesso: Acesso aberto
Idioma: por
Instituição de defesa: Não Informado pela instituição
Programa de Pós-Graduação: Não Informado pela instituição
Departamento: Não Informado pela instituição
País: Não Informado pela instituição
Palavras-chave em Português:
Morfodinâmica praial
Profundidade de fechamento
Zona não edificante
Link de acesso: http://www.repositorio.ufc.br/handle/riufc/70172
Resumo: This research carried out the analysis of the morphodynamic characteristics of the coastal cord formed by Barra de Catuama, Catuama, Ponta de Pedras and Carne de Vaca beaches, located on the northern coast of the State of Pernambuco, in Goiana city. The approach adopted was based on the bimonthly collection of topographic profiles of the beaches and sedimentological sampling in three sectors of the beach, which were carried out between the months of July 2017 and May 2019. The coastal cord studied. Bathymetry was accomplished in the studied area and thus the closing depth of the shallow continental shelf was determined. With this, it was possible to define the maximum high tide line and establish the non-edifying zone. The comparison of the surveyed topographic profiles indicated that the sedimentary balance was positive (deposition) in only one point of the studied littoral cord. Profile P4, surveyed on Ponta de Pedras beach, showed the smallest volume variation (- 6.27m³/m), despite being an intensely occupied stretch. The correlation of the topographic profiles with the sedimentological analysis allowed us to identify the influence of the Itapessoca and Goiana rivers on the P2, P3 and P7 profiles. Profiles P1, P2, P3 and P7 have quartz composition. However, the profiles P4, P5 and P6 are composed predominantly in the shoreshore sector by carbonate sediments, mainly by halimedas. For the hydrodynamic characterization, the area was subdivided into five sectors and a non-edifying zone was established for each sector. For each sector, an optimistic and pessimistic estimate of the sea advance until 2100 was made. All sectors had a non-building zone area greater than the 33 meters stipulated by law, with sector 1 being the largest of them, with 303.37 m of retreat in the pessimistic estimate
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spelling Madruga, Marcelo Menezes DinizSoares Junior, Carlos Fernando de AndradeFreire, George Satander Sá2023-01-20T11:59:39Z2023-01-20T11:59:39Z2022MADRUGA, Marcelo Menezes Diniz. Contribuições da morfodinâmica no zoneamento territorial em Goiana, litoral norte de Pernambuco, Brasil. 2022. 149 f. Tese (Doutorado em Geologia) - Universidade Federal do Ceará, Fortaleza, 2022.http://www.repositorio.ufc.br/handle/riufc/70172This research carried out the analysis of the morphodynamic characteristics of the coastal cord formed by Barra de Catuama, Catuama, Ponta de Pedras and Carne de Vaca beaches, located on the northern coast of the State of Pernambuco, in Goiana city. The approach adopted was based on the bimonthly collection of topographic profiles of the beaches and sedimentological sampling in three sectors of the beach, which were carried out between the months of July 2017 and May 2019. The coastal cord studied. Bathymetry was accomplished in the studied area and thus the closing depth of the shallow continental shelf was determined. With this, it was possible to define the maximum high tide line and establish the non-edifying zone. The comparison of the surveyed topographic profiles indicated that the sedimentary balance was positive (deposition) in only one point of the studied littoral cord. Profile P4, surveyed on Ponta de Pedras beach, showed the smallest volume variation (- 6.27m³/m), despite being an intensely occupied stretch. The correlation of the topographic profiles with the sedimentological analysis allowed us to identify the influence of the Itapessoca and Goiana rivers on the P2, P3 and P7 profiles. Profiles P1, P2, P3 and P7 have quartz composition. However, the profiles P4, P5 and P6 are composed predominantly in the shoreshore sector by carbonate sediments, mainly by halimedas. For the hydrodynamic characterization, the area was subdivided into five sectors and a non-edifying zone was established for each sector. For each sector, an optimistic and pessimistic estimate of the sea advance until 2100 was made. All sectors had a non-building zone area greater than the 33 meters stipulated by law, with sector 1 being the largest of them, with 303.37 m of retreat in the pessimistic estimateEsta pesquisa realizou a análise das características morfodinâmicas do cordão litorâneo formado pelas praias de Barra de Catuama, Catuama, Ponta de Pedras e Carne de Vaca, localizadas no litoral norte do Estado de Pernambuco, no munícipio de Goiana. A abordagem adotada baseou-se na coleta bimestral de perfis topográficos das praias e amostragem sedimentológica em três setores da praia, que foram executados entre os meses de julho de 2017 e maio de 2019. Ao todo foram coletados dados em sete perfis ao longo de todo o cordão litorâneo estudado. Foi realizada a batimetria na área estudada e assim determinada a profundidade de fechamento da plataforma continental rasa. Com isso, foi possível definir a linha de preamar máxima e estabelecer a zona não edificante. A comparação dos perfis topográficos levantados indicou que o balanço sedimentar foi positivo (deposição) em apenas um ponto do cordão litorâneo estudado. O perfil P4, levantado na praia de Ponta de Pedras, apresentou a menor variação de volume (-6,27m³/m), apesar de ser um trecho intensamente ocupado. A correlação dos perfis topográficos com a análise sedimentológica permitiu identificar a influência dos rios Itapessoca e Goiana nos perfis P2, P3 e P7. Os perfis P1, P2, P3 e P7 apresentam composição quartzosa. Contudo, os perfis P4, P5 e P6 são compostos predominantemente no setor de antepraia por sedimentos carbonáticos, principalmente por halimedas. Para a caracterização hidrodinâmica, a área foi subdividida em cinco setores e para cada setor foi estabelecida uma zona não edificante. Para cada setor foi feita uma estimativa otimista e pessimista de avanço do mar até 2100. Todos os setores apresentaram a área de zona não edificante superior aos 33 metros estipulado por lei, sendo o setor 1 o maior deles, com 303,37m de recuo na estimativa pessimistaMorfodinâmica praialProfundidade de fechamentoZona não edificanteContribuições da morfodinâmica no zoneamento territorial em Goiana, litoral norte de Pernambuco, BrasilContributions of morphodynamics in territorial zoning in Goiana, north coast of Pernambuco, Brazilinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/doctoralThesisporreponame:Repositório Institucional da Universidade Federal do Ceará (UFC)instname:Universidade Federal do Ceará (UFC)instacron:UFCinfo:eu-repo/semantics/openAccessORIGINAL2022_tese_mmdmadruga.pdf2022_tese_mmdmadruga.pdfapplication/pdf10766693http://repositorio.ufc.br/bitstream/riufc/70172/3/2022_tese_mmdmadruga.pdf057633766c7d2d521f48c276b5d468beMD53LICENSElicense.txtlicense.txttext/plain; charset=utf-81748http://repositorio.ufc.br/bitstream/riufc/70172/4/license.txt8a4605be74aa9ea9d79846c1fba20a33MD54riufc/701722023-01-20 09:01:49.635oai:repositorio.ufc.br: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Repositório InstitucionalPUBhttp://www.repositorio.ufc.br/ri-oai/requestbu@ufc.br || repositorio@ufc.bropendoar:2023-01-20T12:01:49Repositório Institucional da Universidade Federal do Ceará (UFC) - Universidade Federal do Ceará (UFC)false
dc.title.pt_BR.fl_str_mv Contribuições da morfodinâmica no zoneamento territorial em Goiana, litoral norte de Pernambuco, Brasil
dc.title.en.pt_BR.fl_str_mv Contributions of morphodynamics in territorial zoning in Goiana, north coast of Pernambuco, Brazil
title Contribuições da morfodinâmica no zoneamento territorial em Goiana, litoral norte de Pernambuco, Brasil
spellingShingle Contribuições da morfodinâmica no zoneamento territorial em Goiana, litoral norte de Pernambuco, Brasil
Madruga, Marcelo Menezes Diniz
Morfodinâmica praial
Profundidade de fechamento
Zona não edificante
title_short Contribuições da morfodinâmica no zoneamento territorial em Goiana, litoral norte de Pernambuco, Brasil
title_full Contribuições da morfodinâmica no zoneamento territorial em Goiana, litoral norte de Pernambuco, Brasil
title_fullStr Contribuições da morfodinâmica no zoneamento territorial em Goiana, litoral norte de Pernambuco, Brasil
title_full_unstemmed Contribuições da morfodinâmica no zoneamento territorial em Goiana, litoral norte de Pernambuco, Brasil
title_sort Contribuições da morfodinâmica no zoneamento territorial em Goiana, litoral norte de Pernambuco, Brasil
author Madruga, Marcelo Menezes Diniz
author_facet Madruga, Marcelo Menezes Diniz
author_role author
dc.contributor.co-advisor.none.fl_str_mv Soares Junior, Carlos Fernando de Andrade
dc.contributor.author.fl_str_mv Madruga, Marcelo Menezes Diniz
dc.contributor.advisor1.fl_str_mv Freire, George Satander Sá
contributor_str_mv Freire, George Satander Sá
dc.subject.por.fl_str_mv Morfodinâmica praial
Profundidade de fechamento
Zona não edificante
topic Morfodinâmica praial
Profundidade de fechamento
Zona não edificante
description This research carried out the analysis of the morphodynamic characteristics of the coastal cord formed by Barra de Catuama, Catuama, Ponta de Pedras and Carne de Vaca beaches, located on the northern coast of the State of Pernambuco, in Goiana city. The approach adopted was based on the bimonthly collection of topographic profiles of the beaches and sedimentological sampling in three sectors of the beach, which were carried out between the months of July 2017 and May 2019. The coastal cord studied. Bathymetry was accomplished in the studied area and thus the closing depth of the shallow continental shelf was determined. With this, it was possible to define the maximum high tide line and establish the non-edifying zone. The comparison of the surveyed topographic profiles indicated that the sedimentary balance was positive (deposition) in only one point of the studied littoral cord. Profile P4, surveyed on Ponta de Pedras beach, showed the smallest volume variation (- 6.27m³/m), despite being an intensely occupied stretch. The correlation of the topographic profiles with the sedimentological analysis allowed us to identify the influence of the Itapessoca and Goiana rivers on the P2, P3 and P7 profiles. Profiles P1, P2, P3 and P7 have quartz composition. However, the profiles P4, P5 and P6 are composed predominantly in the shoreshore sector by carbonate sediments, mainly by halimedas. For the hydrodynamic characterization, the area was subdivided into five sectors and a non-edifying zone was established for each sector. For each sector, an optimistic and pessimistic estimate of the sea advance until 2100 was made. All sectors had a non-building zone area greater than the 33 meters stipulated by law, with sector 1 being the largest of them, with 303.37 m of retreat in the pessimistic estimate
publishDate 2022
dc.date.issued.fl_str_mv 2022
dc.date.accessioned.fl_str_mv 2023-01-20T11:59:39Z
dc.date.available.fl_str_mv 2023-01-20T11:59:39Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/doctoralThesis
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dc.identifier.citation.fl_str_mv MADRUGA, Marcelo Menezes Diniz. Contribuições da morfodinâmica no zoneamento territorial em Goiana, litoral norte de Pernambuco, Brasil. 2022. 149 f. Tese (Doutorado em Geologia) - Universidade Federal do Ceará, Fortaleza, 2022.
dc.identifier.uri.fl_str_mv http://www.repositorio.ufc.br/handle/riufc/70172
identifier_str_mv MADRUGA, Marcelo Menezes Diniz. Contribuições da morfodinâmica no zoneamento territorial em Goiana, litoral norte de Pernambuco, Brasil. 2022. 149 f. Tese (Doutorado em Geologia) - Universidade Federal do Ceará, Fortaleza, 2022.
url http://www.repositorio.ufc.br/handle/riufc/70172
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