Geoquímica dos sedimentos superdiciais de fundo do Estuário do Rio Maracanã, NE do Pará

Detalhes bibliográficos
Ano de defesa: 2006
Autor(a) principal: DELFINO, Smaily Bastos lattes
Orientador(a): EL-ROBRINI, Maâmar lattes
Banca de defesa: Não Informado pela instituição
Tipo de documento: Dissertação
Tipo de acesso: Acesso aberto
Idioma: por
Instituição de defesa: Universidade Federal do Pará
Programa de Pós-Graduação: Programa de Pós-Graduação em Geologia e Geoquímica
Departamento: Instituto de Geociências
País: Brasil
Palavras-chave em Português:
Área do conhecimento CNPq:
Link de acesso: http://repositorio.ufpa.br/jspui/handle/2011/4234
Resumo: The Maracanã estuary is located in the northeastern of Pará State, within the Extraction Marine Reserve (Law 9.985/00), which has as primary goal to the sustainable use and conservation of the renewable ressources, protecting living conditions and the culture of the population, which consists of fisherman, small seliers and the local community. Due to its environmental characteristics, this area represents an important pole for the regional development. In this work, one of the aims was to search a geochemical formality to an interpretation of analytical results related to the geochemistry of the superficial sediments of the estuary of Maracanã bottom in order to determine the amount of heavy metais (Cd, Co, Cr, Cu, Fe, Mn, Ni, Pb, Zn) of the granulometry with smaller fractions than 0,64 tem by atomic absorption spectrometry, to obtain the current inexistent background leveis. In the Maracanã estuary, it was registered much more silt-clay fraction than sand fraction, besides mineralogical similarity that indicates presence of kaolinite, illite and smectite. The amount of organic matter (MO) (5,4±0,70%) in sediments was homogeneously distributed. The pH didn't vary much, only between weakly acid (6,48) and weakly alkaline (7,13). Heavy metais - 1) in Maracanã river estuary cadmium concentrations were under of the equipment detection limit (0,009 ppm); 2) Cobalt varied from 46 to 55 ppm (50,97 ± 2,31 ppm) in total fraction, and from 5 to 7 ppm (6 ± 0,37 ppm) in bio-available fraction; 3) Cromo varied from 126 to 152 ppm (140,33±6,56 ppm) in total fraction and from 17 to 24 ppm (20,73±1,7 ppm) in bio-available fraction; 4) Copper varied from 17 to 21 ppm (18,97±1,19 ppm) in total fraction and from 6 to 9 ppm (7,0 ± 0,69 ppm) in bio-available fraction; 5) Iron varied from 3,4 to 4,6 % (4,14± 0,24 %) in total fraction and from 1,5 to 1,9 % (1,66± 0,1 %) in bio-available fraction; 6) Manganese varied from 293 to 545 ppm (423,53±74,63 ppm) in total fraction and from 168 to 499 ppm (335,1±91,3 ppm) in bio-available fraction; 7) Nickel varied from 44 to 53 ppm (48,77 ± 2,27 ppm) in total fraction and from 7 to 9 ppm (8,03±0,56 ppm) in bio-available fraction; 8) Lead varied from 42 to 48 ppm (45,63±1,69 ppm) in total fraction and from 14 to 17 ppm (15,13±0,78 ppm) in bio-available fraction; 9) Zinc varied from 72 to 85 ppm (78,83±3,44 ppm) in total fraction and from 26 to 32 ppm (29,43±1,65 ppm) in bio-available fraction. Concentration values of the bio-available heavy metal analyzed are smaller than those VGQS (Guide-Value of Sediment Quality), established by the "Canada Environmental Agency" (AAC) and the "National Oceanic and Atmospheric Administration"(NOAA), indicating that it should rarely occur bad effect on local biota. Considering that the area is an extraction reserve and that were not found evidence of anthropic contamination associated with the heavy metais, neither in their total fractions nor in their bio-available fractions in the Maracanã estuary, it is possible to consider that the data obtained from both analyzed geochemical fractions of heavy metais represent a value dose to the characteristical background of the region. Therefore, the Maracanã estuary is a reference cite to study the biogeochemistry and ecotoxicoiogy of the sediments of similar environments in Coastal of the Pará State. Besides that, the data obtained in this work can provide a subside for future geochemical and environmental surveys in the area, once that concentration ranges and reference values for many heavy metais that are present in the bottom sediments of this estuary were established.
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spelling 2013-09-10T15:05:03Z2013-09-10T15:05:03Z2006-04-05DELFINO, Ismaily Bastos. Geoquímica dos sedimentos superdiciais de fundo do Estuário do Rio Maracanã, NE do Pará. Orientador: Maâmar El-Robrini. 2006. 150 f. Dissertação (Mestrado em Geologia e Geoquímica) - Centro de Geociências, Universidade Federal do Pará, Belém, 2006. Disponível em: http://repositorio.ufpa.br:8080/jspui/handle/2011/4234. Acesso em:.http://repositorio.ufpa.br/jspui/handle/2011/4234The Maracanã estuary is located in the northeastern of Pará State, within the Extraction Marine Reserve (Law 9.985/00), which has as primary goal to the sustainable use and conservation of the renewable ressources, protecting living conditions and the culture of the population, which consists of fisherman, small seliers and the local community. Due to its environmental characteristics, this area represents an important pole for the regional development. In this work, one of the aims was to search a geochemical formality to an interpretation of analytical results related to the geochemistry of the superficial sediments of the estuary of Maracanã bottom in order to determine the amount of heavy metais (Cd, Co, Cr, Cu, Fe, Mn, Ni, Pb, Zn) of the granulometry with smaller fractions than 0,64 tem by atomic absorption spectrometry, to obtain the current inexistent background leveis. In the Maracanã estuary, it was registered much more silt-clay fraction than sand fraction, besides mineralogical similarity that indicates presence of kaolinite, illite and smectite. The amount of organic matter (MO) (5,4±0,70%) in sediments was homogeneously distributed. The pH didn't vary much, only between weakly acid (6,48) and weakly alkaline (7,13). Heavy metais - 1) in Maracanã river estuary cadmium concentrations were under of the equipment detection limit (0,009 ppm); 2) Cobalt varied from 46 to 55 ppm (50,97 ± 2,31 ppm) in total fraction, and from 5 to 7 ppm (6 ± 0,37 ppm) in bio-available fraction; 3) Cromo varied from 126 to 152 ppm (140,33±6,56 ppm) in total fraction and from 17 to 24 ppm (20,73±1,7 ppm) in bio-available fraction; 4) Copper varied from 17 to 21 ppm (18,97±1,19 ppm) in total fraction and from 6 to 9 ppm (7,0 ± 0,69 ppm) in bio-available fraction; 5) Iron varied from 3,4 to 4,6 % (4,14± 0,24 %) in total fraction and from 1,5 to 1,9 % (1,66± 0,1 %) in bio-available fraction; 6) Manganese varied from 293 to 545 ppm (423,53±74,63 ppm) in total fraction and from 168 to 499 ppm (335,1±91,3 ppm) in bio-available fraction; 7) Nickel varied from 44 to 53 ppm (48,77 ± 2,27 ppm) in total fraction and from 7 to 9 ppm (8,03±0,56 ppm) in bio-available fraction; 8) Lead varied from 42 to 48 ppm (45,63±1,69 ppm) in total fraction and from 14 to 17 ppm (15,13±0,78 ppm) in bio-available fraction; 9) Zinc varied from 72 to 85 ppm (78,83±3,44 ppm) in total fraction and from 26 to 32 ppm (29,43±1,65 ppm) in bio-available fraction. Concentration values of the bio-available heavy metal analyzed are smaller than those VGQS (Guide-Value of Sediment Quality), established by the "Canada Environmental Agency" (AAC) and the "National Oceanic and Atmospheric Administration"(NOAA), indicating that it should rarely occur bad effect on local biota. Considering that the area is an extraction reserve and that were not found evidence of anthropic contamination associated with the heavy metais, neither in their total fractions nor in their bio-available fractions in the Maracanã estuary, it is possible to consider that the data obtained from both analyzed geochemical fractions of heavy metais represent a value dose to the characteristical background of the region. Therefore, the Maracanã estuary is a reference cite to study the biogeochemistry and ecotoxicoiogy of the sediments of similar environments in Coastal of the Pará State. Besides that, the data obtained in this work can provide a subside for future geochemical and environmental surveys in the area, once that concentration ranges and reference values for many heavy metais that are present in the bottom sediments of this estuary were established.O Estuário do rio Maracanã localizado na mesoregião Nordeste do Pará, esta situado na Reserva Extrativista Marinha de Maracanã (Lei 9.985/00), ao qual tem como principal objetivo garantir o uso sustentável e conservação dos recursos renováveis, protegendo as condições de vida e cultura da população que, em geral, são pescadores, pequenos comerciantes e a própria comunidade local. Devido as suas características geoambientais, representar um importante pólo de desenvolvimento regional, buscou-se nesta dissertação, o formalismo geoquímico para a interpretação de resultados analíticos relacionados com a geoquímica dos sedimentos superficiais de fundo do estuário do rio Maracanã para a determinação de metais pesados (MP) (Cd, Co, Cr, Cu, Fe, Mn, Ni, Pb, Zn), nas frações granulométricas menores que 0,64 11m, por espectrometria de absorção atômica de maneira a conhecer os níveis de background atualmente inexistentes para realização de futuros trabalhos de monitoramento ambiental na região nordeste do estado do Pará. Neste estuário, registrou-se a predominância das frações silte-argila em relação a fração areia, além de identificar semelhança mineralógica, indicando a presença de caulinita, ilita e esmectita. De um modo geral o teor de matéria orgânica (MO) (5,4:t0,70%) nos sedimentos foi distribuído de forma homogênia, e o pH não sofreu grandes variações, oscilando entre fracamente ácidos (6,48) e fracamente alcalinos (7,13). Com relação aos MP, verificou-se que: 1) no estuário do rio Maracanã as concentrações de cádmio ficar~m abaixo do limite de detecção do aparelho (0,009 ppm); 2) o cobalto variou de 46 a 55 ppm (50,97:t2,31 ppm) na fração total, e de de 5 a 7 ppm (6:tO,37 ppm) na fração biodisponível; 3) o cromo variou de 126 a 152 ppm (140,33:t6,56 ppm) na fração total, e de 17 a 24 ppm (20,73:t1, 7 ppm) na fração biodisponível; 4) o cobre variou de 17 a 21 ppm (18,97:t1, 19 ppm) na fração total, e de 6 a 9 ppm (7,0 :t 0,69 ppm) na fração biodisponivel; 5) o Ferro variou de 3,4 a 4,6% (4,14:t 0,24 %) na fração total, e de 1,5 a 1,9 % (1,66:t 0,1 %) na fração biodisponível; 6) o manganês variou de 293 a 545 ppm (423,53:t74,63 ppm) na fração total, e de 168 a 499 ppm (335,1 :t91,3 ppm) na fração biodisponível; 7) o níquel variou de 44 a 53 ppm (48,77 :t: 2,27 ppm) na fração total, e de 7 a 9 ppm (8,03:t:O,56 ppm) na fração biodisponível; 8) o chumbo variou de 42 a 48 ppm (45,63:t:1,69 ppm) na fração total, e de 14 a 17 ppm (15,13:t:O,78 ppm) na fração biodisponível; 9) o zinco variou de 72 a 85 ppm (78,83:t:3,44 ppm) na fração total, e de 26 a 32 ppm (29,43:t:1,65 ppm) na fração biodisponível. A concentração dos MP biodisponíveis analisados para o Estuário do rio Maracanã encontram-se abaixo dos VGQS (valores guias de qualidade de sedimentos) estabelecidos pela Agência Ambiental do Canadá (AAC) , pela National Oceanic and Atmospheric Administratíon (NOM) indicando que raramente devem ocorrer algum efeito adverso para biota da região. Considerando que a região é uma Reserva Extrativista e que não foram encontradas evidências de contaminação antrópica associadas aos MP selecionados nas suas frações total e biodisponível no estuário do rio Maracanã, é possível considerar que os dados obtidos para as concentrações de MP selecionada nas duas frações geoquímicas analisadas, representam o valor próximo ao "background" característico desta região. Desta forma o estuário do rio Maracanã torna-se um sítio de referência para estudos biogeoquímicos e de ecotoxicologia de sedimentos de ambientes similares na costa paraense, além do mais, os dados obtidos nesta dissertação poderão servir como subsídio para futuras investigações geoquímicas e ambientais na região, uma vez que se estabeleceram faixas de concentração e relações de referências para vários MP presentes nos sedimentos de fundo deste estuário.CVRD - Companhia Vale do Rio DoceCAPES - Coordenação de Aperfeiçoamento de Pessoal de Nível SuperiorporUniversidade Federal do ParáPrograma de Pós-Graduação em Geologia e GeoquímicaUFPABrasilInstituto de GeociênciasCNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOLOGIA::GEOQUIMICACNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOLOGIA::SEDIMENTOLOGIAGeoquímicaGeoquímica de sedimentosEstuáriosRio Maracanã - PAPará - EstadoAmazônia brasileiraMetais pesadosEspectrometria de absorção atômicaGeoquímica dos sedimentos superdiciais de fundo do Estuário do Rio Maracanã, NE do Paráinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesisEL-ROBRINI, Maâmarhttp://lattes.cnpq.br/5707365981163429http://lattes.cnpq.br/9809164630125017DELFINO, Smaily Bastosinfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da UFPAinstname:Universidade Federal do Pará (UFPA)instacron:UFPAORIGINALDissertacao_GeoquimicaSedimentosSuperficiais.pdfDissertacao_GeoquimicaSedimentosSuperficiais.pdfapplication/pdf138469795http://repositorio.ufpa.br/oai/bitstream/2011/4234/1/Dissertacao_GeoquimicaSedimentosSuperficiais.pdffd67241519b33d5554737e429424f7e3MD51CC-LICENSElicense_urllicense_urltext/plain; charset=utf-852http://repositorio.ufpa.br/oai/bitstream/2011/4234/2/license_url3d480ae6c91e310daba2020f8787d6f9MD52license_textlicense_texttext/html; charset=utf-80http://repositorio.ufpa.br/oai/bitstream/2011/4234/3/license_textd41d8cd98f00b204e9800998ecf8427eMD53license_rdflicense_rdfapplication/rdf+xml; charset=utf-823898http://repositorio.ufpa.br/oai/bitstream/2011/4234/4/license_rdfe363e809996cf46ada20da1accfcd9c7MD54LICENSElicense.txtlicense.txttext/plain; charset=utf-81774http://repositorio.ufpa.br/oai/bitstream/2011/4234/5/license.txtf0aa1a71c97d9c3e771021efac6d65e7MD552011/42342019-05-22 10:01:32.89oai:repositorio.ufpa.br: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Repositório InstitucionalPUBhttp://repositorio.ufpa.br/oai/requestriufpabc@ufpa.bropendoar:21232019-05-22T13:01:32Repositório Institucional da UFPA - Universidade Federal do Pará (UFPA)false
dc.title.pt_BR.fl_str_mv Geoquímica dos sedimentos superdiciais de fundo do Estuário do Rio Maracanã, NE do Pará
title Geoquímica dos sedimentos superdiciais de fundo do Estuário do Rio Maracanã, NE do Pará
spellingShingle Geoquímica dos sedimentos superdiciais de fundo do Estuário do Rio Maracanã, NE do Pará
DELFINO, Smaily Bastos
CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOLOGIA::GEOQUIMICA
CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOLOGIA::SEDIMENTOLOGIA
Geoquímica
Geoquímica de sedimentos
Estuários
Rio Maracanã - PA
Pará - Estado
Amazônia brasileira
Metais pesados
Espectrometria de absorção atômica
title_short Geoquímica dos sedimentos superdiciais de fundo do Estuário do Rio Maracanã, NE do Pará
title_full Geoquímica dos sedimentos superdiciais de fundo do Estuário do Rio Maracanã, NE do Pará
title_fullStr Geoquímica dos sedimentos superdiciais de fundo do Estuário do Rio Maracanã, NE do Pará
title_full_unstemmed Geoquímica dos sedimentos superdiciais de fundo do Estuário do Rio Maracanã, NE do Pará
title_sort Geoquímica dos sedimentos superdiciais de fundo do Estuário do Rio Maracanã, NE do Pará
author DELFINO, Smaily Bastos
author_facet DELFINO, Smaily Bastos
author_role author
dc.contributor.advisor1.fl_str_mv EL-ROBRINI, Maâmar
dc.contributor.advisor1Lattes.fl_str_mv http://lattes.cnpq.br/5707365981163429
dc.contributor.authorLattes.fl_str_mv http://lattes.cnpq.br/9809164630125017
dc.contributor.author.fl_str_mv DELFINO, Smaily Bastos
contributor_str_mv EL-ROBRINI, Maâmar
dc.subject.cnpq.fl_str_mv CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOLOGIA::GEOQUIMICA
CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOLOGIA::SEDIMENTOLOGIA
topic CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOLOGIA::GEOQUIMICA
CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOLOGIA::SEDIMENTOLOGIA
Geoquímica
Geoquímica de sedimentos
Estuários
Rio Maracanã - PA
Pará - Estado
Amazônia brasileira
Metais pesados
Espectrometria de absorção atômica
dc.subject.por.fl_str_mv Geoquímica
Geoquímica de sedimentos
Estuários
Rio Maracanã - PA
Pará - Estado
Amazônia brasileira
Metais pesados
Espectrometria de absorção atômica
description The Maracanã estuary is located in the northeastern of Pará State, within the Extraction Marine Reserve (Law 9.985/00), which has as primary goal to the sustainable use and conservation of the renewable ressources, protecting living conditions and the culture of the population, which consists of fisherman, small seliers and the local community. Due to its environmental characteristics, this area represents an important pole for the regional development. In this work, one of the aims was to search a geochemical formality to an interpretation of analytical results related to the geochemistry of the superficial sediments of the estuary of Maracanã bottom in order to determine the amount of heavy metais (Cd, Co, Cr, Cu, Fe, Mn, Ni, Pb, Zn) of the granulometry with smaller fractions than 0,64 tem by atomic absorption spectrometry, to obtain the current inexistent background leveis. In the Maracanã estuary, it was registered much more silt-clay fraction than sand fraction, besides mineralogical similarity that indicates presence of kaolinite, illite and smectite. The amount of organic matter (MO) (5,4±0,70%) in sediments was homogeneously distributed. The pH didn't vary much, only between weakly acid (6,48) and weakly alkaline (7,13). Heavy metais - 1) in Maracanã river estuary cadmium concentrations were under of the equipment detection limit (0,009 ppm); 2) Cobalt varied from 46 to 55 ppm (50,97 ± 2,31 ppm) in total fraction, and from 5 to 7 ppm (6 ± 0,37 ppm) in bio-available fraction; 3) Cromo varied from 126 to 152 ppm (140,33±6,56 ppm) in total fraction and from 17 to 24 ppm (20,73±1,7 ppm) in bio-available fraction; 4) Copper varied from 17 to 21 ppm (18,97±1,19 ppm) in total fraction and from 6 to 9 ppm (7,0 ± 0,69 ppm) in bio-available fraction; 5) Iron varied from 3,4 to 4,6 % (4,14± 0,24 %) in total fraction and from 1,5 to 1,9 % (1,66± 0,1 %) in bio-available fraction; 6) Manganese varied from 293 to 545 ppm (423,53±74,63 ppm) in total fraction and from 168 to 499 ppm (335,1±91,3 ppm) in bio-available fraction; 7) Nickel varied from 44 to 53 ppm (48,77 ± 2,27 ppm) in total fraction and from 7 to 9 ppm (8,03±0,56 ppm) in bio-available fraction; 8) Lead varied from 42 to 48 ppm (45,63±1,69 ppm) in total fraction and from 14 to 17 ppm (15,13±0,78 ppm) in bio-available fraction; 9) Zinc varied from 72 to 85 ppm (78,83±3,44 ppm) in total fraction and from 26 to 32 ppm (29,43±1,65 ppm) in bio-available fraction. Concentration values of the bio-available heavy metal analyzed are smaller than those VGQS (Guide-Value of Sediment Quality), established by the "Canada Environmental Agency" (AAC) and the "National Oceanic and Atmospheric Administration"(NOAA), indicating that it should rarely occur bad effect on local biota. Considering that the area is an extraction reserve and that were not found evidence of anthropic contamination associated with the heavy metais, neither in their total fractions nor in their bio-available fractions in the Maracanã estuary, it is possible to consider that the data obtained from both analyzed geochemical fractions of heavy metais represent a value dose to the characteristical background of the region. Therefore, the Maracanã estuary is a reference cite to study the biogeochemistry and ecotoxicoiogy of the sediments of similar environments in Coastal of the Pará State. Besides that, the data obtained in this work can provide a subside for future geochemical and environmental surveys in the area, once that concentration ranges and reference values for many heavy metais that are present in the bottom sediments of this estuary were established.
publishDate 2006
dc.date.issued.fl_str_mv 2006-04-05
dc.date.accessioned.fl_str_mv 2013-09-10T15:05:03Z
dc.date.available.fl_str_mv 2013-09-10T15:05:03Z
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.citation.fl_str_mv DELFINO, Ismaily Bastos. Geoquímica dos sedimentos superdiciais de fundo do Estuário do Rio Maracanã, NE do Pará. Orientador: Maâmar El-Robrini. 2006. 150 f. Dissertação (Mestrado em Geologia e Geoquímica) - Centro de Geociências, Universidade Federal do Pará, Belém, 2006. Disponível em: http://repositorio.ufpa.br:8080/jspui/handle/2011/4234. Acesso em:.
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identifier_str_mv DELFINO, Ismaily Bastos. Geoquímica dos sedimentos superdiciais de fundo do Estuário do Rio Maracanã, NE do Pará. Orientador: Maâmar El-Robrini. 2006. 150 f. Dissertação (Mestrado em Geologia e Geoquímica) - Centro de Geociências, Universidade Federal do Pará, Belém, 2006. Disponível em: http://repositorio.ufpa.br:8080/jspui/handle/2011/4234. Acesso em:.
url http://repositorio.ufpa.br/jspui/handle/2011/4234
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dc.publisher.none.fl_str_mv Universidade Federal do Pará
dc.publisher.program.fl_str_mv Programa de Pós-Graduação em Geologia e Geoquímica
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dc.publisher.country.fl_str_mv Brasil
dc.publisher.department.fl_str_mv Instituto de Geociências
publisher.none.fl_str_mv Universidade Federal do Pará
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