A influência das dolinas na vulnerabilidade do aquífero Urucuia, Chapadão Central - oeste da Bahia, Brasil

Detalhes bibliográficos
Autor(a) principal: Silva, Gisele Bispo da
Data de Publicação: 2023
Tipo de documento: Dissertação
Idioma: por
Título da fonte: Repositório Institucional da UFG
Texto Completo: http://repositorio.bc.ufg.br/tede/handle/tede/12762
Resumo: The karst system is generally known for developing in carbonate environments. Formed by the interaction between acidified water and soluble rocks, it sculpts the relief into different types and shapes by the process of dissolution. Studies have pointed out the development of karstic systems in siliciclastic rocks, such as sandstones, for example, and, differently from carbonates, in these rocks the main karst formation process is piping. Among the morphologies developed by karst, whether in carbonates or not, the dolines are the main surface features, also known as closed depressions, whose size varies from a few meters to hundreds of meters in depth and diameter. Due to this difference in size and shape, identifying them in the middle of distinct landscapes or in very large areas is sometimes difficult. Dolines are fragile features and are a connection between the surface and the underground. Because of this, they can act directly as potential contaminants of groundwater. For reason of having evidences of dolines developed in sandstones in Chapadão Central - West of Bahia, the area being directly affected by agricultural activities and being under domain of the Urucuia Aquifer System (SAU), the research had as objective to identify and to validate these features by means of mapping technique using Digital Elevation Model (DEM), with SRTM data - 30m and, by morphometric analysis and to relate them with the potential of contamination of the aquifer by means of the evaluation of intrinsic vulnerability applied by the COP method. The methodology that used the MDE for the identification of dolines presented good results for Chapadão. The database was adjusted to avoid possible errors, thus allowing the extraction of information from 109 dolines with precision. It is a low cost methodology and can be applied in areas of large territorial extension. The COP method also presented satisfactory results for Chapadão, showing that the area presents the 5 vulnerability classes (Very High, High, Moderate, Low and Very Low). The most vulnerable classes, considered as very high and high, are spatially distributed in the western portion of the Chapadão, corresponding directly with the presence of the dolines. This indicates that the use and occupation of the lands of Chapadão without an adequate environmental management can impact the dolines superficially and lead to a contamination of the Urucuia aquifer.
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spelling Cherem, Luis Felipe Soareshttp://lattes.cnpq.br/8363108286297687Cherem, Luis Felipe SoaresNunes, Elizon DiasZancopé, Márcio Henrique de Campos http://lattes.cnpq.br/5217101428798050Silva, Gisele Bispo da2023-04-19T11:32:48Z2023-04-19T11:32:48Z2023-02-06SILVA, G. B. A influência das dolinas na vulnerabilidade do aquífero Urucuia, Chapadão Central - oeste da Bahia, Brasil. 2023.89 f. Dissertação (Mestrado em Geografia) - Universidade Federal de Goiás, Goiânia, 2023.http://repositorio.bc.ufg.br/tede/handle/tede/12762ark:/38995/00130000018mfThe karst system is generally known for developing in carbonate environments. Formed by the interaction between acidified water and soluble rocks, it sculpts the relief into different types and shapes by the process of dissolution. Studies have pointed out the development of karstic systems in siliciclastic rocks, such as sandstones, for example, and, differently from carbonates, in these rocks the main karst formation process is piping. Among the morphologies developed by karst, whether in carbonates or not, the dolines are the main surface features, also known as closed depressions, whose size varies from a few meters to hundreds of meters in depth and diameter. Due to this difference in size and shape, identifying them in the middle of distinct landscapes or in very large areas is sometimes difficult. Dolines are fragile features and are a connection between the surface and the underground. Because of this, they can act directly as potential contaminants of groundwater. For reason of having evidences of dolines developed in sandstones in Chapadão Central - West of Bahia, the area being directly affected by agricultural activities and being under domain of the Urucuia Aquifer System (SAU), the research had as objective to identify and to validate these features by means of mapping technique using Digital Elevation Model (DEM), with SRTM data - 30m and, by morphometric analysis and to relate them with the potential of contamination of the aquifer by means of the evaluation of intrinsic vulnerability applied by the COP method. The methodology that used the MDE for the identification of dolines presented good results for Chapadão. The database was adjusted to avoid possible errors, thus allowing the extraction of information from 109 dolines with precision. It is a low cost methodology and can be applied in areas of large territorial extension. The COP method also presented satisfactory results for Chapadão, showing that the area presents the 5 vulnerability classes (Very High, High, Moderate, Low and Very Low). The most vulnerable classes, considered as very high and high, are spatially distributed in the western portion of the Chapadão, corresponding directly with the presence of the dolines. This indicates that the use and occupation of the lands of Chapadão without an adequate environmental management can impact the dolines superficially and lead to a contamination of the Urucuia aquifer.O sistema cárstico é conhecido geralmente por se desenvolver em ambientes carbonáticos. Formado pela interação entre a água acidificada e rochas solúveis, esculpe o relevo em diferentes tipos e formas pelo processo de dissolução. Estudos têm apontado o desenvolvimento de sistema cárstico em rochas siliciclásticas, como em arenitos por exemplo e, diferentemente dos carbonatos, nessas rochas o principal processo de formação do carste é o piping. Dentre as morfologias desenvolvidas pelo carste, seja em carbonatos ou não, as dolinas são as principais feições superficiais, conhecidas também como depressões fechadas, cujo tamanho varia de alguns metros a centenas de metros de profundidade e diâmetro. Devido a essa diferença de tamanhos e formas, identificá-las no meio de paisagens distintas ou em áreas muito extensas torna-se às vezes difícil. As dolinas são feições frágeis e fazem conexão entre a superfície e o subterrâneo. Em razão disso, podem atuar diretamente como potenciais contaminadoras das águas subterrâneas. Por motivo de haver evidências de dolinas desenvolvidas em arenitos no Chapadão Central – Oeste da Bahia, a área ser diretamente afetada pelas atividades agrícolas e estar sob domínio do Sistema Aquífero Urucuia (SAU), a pesquisa teve como objetivo identificar e validar essas feições por meio de técnica de mapeamento utilizando Modelo Digital de Elevação (MDE), com dados de SRTM – 30m e, por análise morfométrica e relacioná-las com o potencial de contaminação do aquífero por meio da avaliação de vulnerabilidade intrínseca aplicada pelo método COP. A metodologia que utilizou o MDE para identificação de dolinas apresentou bons resultados para o Chapadão. A base de dados foi ajustada para evitar possíveis erros, permitindo assim a extração de informações de 109 dolinas com precisão. Trata-se de uma metodologia de baixo custo e pode ser aplicada em áreas de grande extensão territorial. O método COP também apresentou resultados satisfatórios para o Chapadão, mostrando que a área apresenta as 5 classes de vulnerabilidade (Muito Alta, Alta, Moderada, Baixa e Muito Baixa). As classes mais vulneráveis, consideradas como muito alta e alta, estão distribuídas espacialmente na porção ocidental do Chapadão, correspondendo diretamente com a presença das dolinas. Isso indica que o uso e ocupação das terras do Chapadão sem uma gestão ambiental adequada, pode impactar superficialmente as dolinas e acarretar uma contaminação do aquífero Urucuia.Submitted by Dayane Basílio (dayanebasilio@ufg.br) on 2023-04-18T15:12:38Z No. of bitstreams: 2 Dissertação - Gisele Bispo da Silva - 2023.pdf: 4298470 bytes, checksum: 8f3f2aa7046c287df6c0557cb0540007 (MD5) license_rdf: 805 bytes, checksum: 4460e5956bc1d1639be9ae6146a50347 (MD5)Approved for entry into archive by Luciana Ferreira (lucgeral@gmail.com) on 2023-04-19T11:32:48Z (GMT) No. of bitstreams: 2 Dissertação - Gisele Bispo da Silva - 2023.pdf: 4298470 bytes, checksum: 8f3f2aa7046c287df6c0557cb0540007 (MD5) license_rdf: 805 bytes, checksum: 4460e5956bc1d1639be9ae6146a50347 (MD5)Made available in DSpace on 2023-04-19T11:32:48Z (GMT). No. of bitstreams: 2 Dissertação - Gisele Bispo da Silva - 2023.pdf: 4298470 bytes, checksum: 8f3f2aa7046c287df6c0557cb0540007 (MD5) license_rdf: 805 bytes, checksum: 4460e5956bc1d1639be9ae6146a50347 (MD5) Previous issue date: 2023-02-06Conselho Nacional de Pesquisa e Desenvolvimento Científico e Tecnológico - CNPqporUniversidade Federal de GoiásPrograma de Pós-graduação em Geografia (IESA)UFGBrasilInstituto de Estudos Socioambientais - IESA (RMG)Attribution-NonCommercial-NoDerivatives 4.0 Internationalhttp://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccessMapeamento de dolinasModelagem de vulnerabilidadeMétodo COPDolines mappingVulnerability modelingCOP methodCIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOGRAFIA FISICA::HIDROGEOGRAFIAA influência das dolinas na vulnerabilidade do aquífero Urucuia, Chapadão Central - oeste da Bahia, BrasilThe influence of dolines on the vulnerability of the Urucuia aquifer, Chapadão Central - western Bahia, Brazilinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesis61500500500500246780reponame:Repositório Institucional da UFGinstname:Universidade Federal de Goiás (UFG)instacron:UFGORIGINALDissertação - Gisele Bispo da Silva - 2023.pdfDissertação - Gisele Bispo da Silva - 2023.pdfapplication/pdf4298470http://repositorio.bc.ufg.br/tede/bitstreams/571f4e97-4c86-4f31-a78e-fe7a256b9d2f/download8f3f2aa7046c287df6c0557cb0540007MD53LICENSElicense.txtlicense.txttext/plain; charset=utf-81748http://repositorio.bc.ufg.br/tede/bitstreams/12f350f1-2e0c-490c-845b-6098c04a3daa/download8a4605be74aa9ea9d79846c1fba20a33MD51CC-LICENSElicense_rdflicense_rdfapplication/rdf+xml; charset=utf-8805http://repositorio.bc.ufg.br/tede/bitstreams/5667d37f-f13e-466c-9079-63b10a8d8170/download4460e5956bc1d1639be9ae6146a50347MD52tede/127622023-04-19 08:32:48.398http://creativecommons.org/licenses/by-nc-nd/4.0/Attribution-NonCommercial-NoDerivatives 4.0 Internationalopen.accessoai:repositorio.bc.ufg.br:tede/12762http://repositorio.bc.ufg.br/tedeRepositório InstitucionalPUBhttp://repositorio.bc.ufg.br/oai/requesttasesdissertacoes.bc@ufg.bropendoar:2023-04-19T11:32:48Repositório Institucional da UFG - Universidade Federal de Goiás (UFG)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
dc.title.pt_BR.fl_str_mv A influência das dolinas na vulnerabilidade do aquífero Urucuia, Chapadão Central - oeste da Bahia, Brasil
dc.title.alternative.eng.fl_str_mv The influence of dolines on the vulnerability of the Urucuia aquifer, Chapadão Central - western Bahia, Brazil
title A influência das dolinas na vulnerabilidade do aquífero Urucuia, Chapadão Central - oeste da Bahia, Brasil
spellingShingle A influência das dolinas na vulnerabilidade do aquífero Urucuia, Chapadão Central - oeste da Bahia, Brasil
Silva, Gisele Bispo da
Mapeamento de dolinas
Modelagem de vulnerabilidade
Método COP
Dolines mapping
Vulnerability modeling
COP method
CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOGRAFIA FISICA::HIDROGEOGRAFIA
title_short A influência das dolinas na vulnerabilidade do aquífero Urucuia, Chapadão Central - oeste da Bahia, Brasil
title_full A influência das dolinas na vulnerabilidade do aquífero Urucuia, Chapadão Central - oeste da Bahia, Brasil
title_fullStr A influência das dolinas na vulnerabilidade do aquífero Urucuia, Chapadão Central - oeste da Bahia, Brasil
title_full_unstemmed A influência das dolinas na vulnerabilidade do aquífero Urucuia, Chapadão Central - oeste da Bahia, Brasil
title_sort A influência das dolinas na vulnerabilidade do aquífero Urucuia, Chapadão Central - oeste da Bahia, Brasil
author Silva, Gisele Bispo da
author_facet Silva, Gisele Bispo da
author_role author
dc.contributor.advisor1.fl_str_mv Cherem, Luis Felipe Soares
dc.contributor.advisor1Lattes.fl_str_mv http://lattes.cnpq.br/8363108286297687
dc.contributor.referee1.fl_str_mv Cherem, Luis Felipe Soares
dc.contributor.referee2.fl_str_mv Nunes, Elizon Dias
dc.contributor.referee3.fl_str_mv Zancopé, Márcio Henrique de Campos
dc.contributor.authorLattes.fl_str_mv  http://lattes.cnpq.br/5217101428798050
dc.contributor.author.fl_str_mv Silva, Gisele Bispo da
contributor_str_mv Cherem, Luis Felipe Soares
Cherem, Luis Felipe Soares
Nunes, Elizon Dias
Zancopé, Márcio Henrique de Campos
dc.subject.por.fl_str_mv Mapeamento de dolinas
Modelagem de vulnerabilidade
Método COP
topic Mapeamento de dolinas
Modelagem de vulnerabilidade
Método COP
Dolines mapping
Vulnerability modeling
COP method
CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOGRAFIA FISICA::HIDROGEOGRAFIA
dc.subject.eng.fl_str_mv Dolines mapping
Vulnerability modeling
COP method
dc.subject.cnpq.fl_str_mv CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOGRAFIA FISICA::HIDROGEOGRAFIA
description The karst system is generally known for developing in carbonate environments. Formed by the interaction between acidified water and soluble rocks, it sculpts the relief into different types and shapes by the process of dissolution. Studies have pointed out the development of karstic systems in siliciclastic rocks, such as sandstones, for example, and, differently from carbonates, in these rocks the main karst formation process is piping. Among the morphologies developed by karst, whether in carbonates or not, the dolines are the main surface features, also known as closed depressions, whose size varies from a few meters to hundreds of meters in depth and diameter. Due to this difference in size and shape, identifying them in the middle of distinct landscapes or in very large areas is sometimes difficult. Dolines are fragile features and are a connection between the surface and the underground. Because of this, they can act directly as potential contaminants of groundwater. For reason of having evidences of dolines developed in sandstones in Chapadão Central - West of Bahia, the area being directly affected by agricultural activities and being under domain of the Urucuia Aquifer System (SAU), the research had as objective to identify and to validate these features by means of mapping technique using Digital Elevation Model (DEM), with SRTM data - 30m and, by morphometric analysis and to relate them with the potential of contamination of the aquifer by means of the evaluation of intrinsic vulnerability applied by the COP method. The methodology that used the MDE for the identification of dolines presented good results for Chapadão. The database was adjusted to avoid possible errors, thus allowing the extraction of information from 109 dolines with precision. It is a low cost methodology and can be applied in areas of large territorial extension. The COP method also presented satisfactory results for Chapadão, showing that the area presents the 5 vulnerability classes (Very High, High, Moderate, Low and Very Low). The most vulnerable classes, considered as very high and high, are spatially distributed in the western portion of the Chapadão, corresponding directly with the presence of the dolines. This indicates that the use and occupation of the lands of Chapadão without an adequate environmental management can impact the dolines superficially and lead to a contamination of the Urucuia aquifer.
publishDate 2023
dc.date.accessioned.fl_str_mv 2023-04-19T11:32:48Z
dc.date.available.fl_str_mv 2023-04-19T11:32:48Z
dc.date.issued.fl_str_mv 2023-02-06
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/masterThesis
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dc.identifier.citation.fl_str_mv SILVA, G. B. A influência das dolinas na vulnerabilidade do aquífero Urucuia, Chapadão Central - oeste da Bahia, Brasil. 2023.89 f. Dissertação (Mestrado em Geografia) - Universidade Federal de Goiás, Goiânia, 2023.
dc.identifier.uri.fl_str_mv http://repositorio.bc.ufg.br/tede/handle/tede/12762
dc.identifier.dark.fl_str_mv ark:/38995/00130000018mf
identifier_str_mv SILVA, G. B. A influência das dolinas na vulnerabilidade do aquífero Urucuia, Chapadão Central - oeste da Bahia, Brasil. 2023.89 f. Dissertação (Mestrado em Geografia) - Universidade Federal de Goiás, Goiânia, 2023.
ark:/38995/00130000018mf
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dc.publisher.none.fl_str_mv Universidade Federal de Goiás
dc.publisher.program.fl_str_mv Programa de Pós-graduação em Geografia (IESA)
dc.publisher.initials.fl_str_mv UFG
dc.publisher.country.fl_str_mv Brasil
dc.publisher.department.fl_str_mv Instituto de Estudos Socioambientais - IESA (RMG)
publisher.none.fl_str_mv Universidade Federal de Goiás
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