Heavy metal concentrations in soils from a remote oceanic island, Fernando de Noronha, Brazil

Detalhes bibliográficos
Autor(a) principal: Oliveira,Sonia M.B. de
Data de Publicação: 2011
Outros Autores: Pessenda,Luiz C.R., Gouveia,Suzy E.M., Favaro,Deborah I.T.
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Anais da Academia Brasileira de Ciências (Online)
Texto Completo: http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652011000400007
Resumo: This paper examines the role of parent rock, pedogenetic processes and airborne pollution in heavy metal accumulation in soils from a remote oceanic island, Fernando de Noronha, Brazil. We studied five soil profiles developed from different volcanic rocks. Mineralogical composition and total concentrations of major and trace elements were determined in 43 samples. The obtained concentrations range for heavy metals were: Co: 26-261 ppm; Cu: 35-97 ppm; Cr: 350-1446 ppm; Ni: 114-691 ppm; Zn: 101-374 ppm; Hg: 2-150 ppb. The composition of soils is strongly affected by the geochemical character of the parent rock. Pedogenesis appears to be responsible for the accumulation of Zn, Co, and, to a lesser extent, of Ni and Cu, in the upper, Mn- and organic carbon-enriched horizons of the soil profiles. Pedogenic influence may also explain the relationship observed between Cr and the Fe. Hg is likely to have been added to the soil profile by long-range atmospheric transport. Its accumulation in the topsoil was further favoured by the formation of stable complexes with organic matter. Clay minerals do not appear to play an important role in the fixation of heavy metals.
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spelling Heavy metal concentrations in soils from a remote oceanic island, Fernando de Noronha, Brazilheavy metalssoilsanthropogenic mercuryFernando de NoronhaThis paper examines the role of parent rock, pedogenetic processes and airborne pollution in heavy metal accumulation in soils from a remote oceanic island, Fernando de Noronha, Brazil. We studied five soil profiles developed from different volcanic rocks. Mineralogical composition and total concentrations of major and trace elements were determined in 43 samples. The obtained concentrations range for heavy metals were: Co: 26-261 ppm; Cu: 35-97 ppm; Cr: 350-1446 ppm; Ni: 114-691 ppm; Zn: 101-374 ppm; Hg: 2-150 ppb. The composition of soils is strongly affected by the geochemical character of the parent rock. Pedogenesis appears to be responsible for the accumulation of Zn, Co, and, to a lesser extent, of Ni and Cu, in the upper, Mn- and organic carbon-enriched horizons of the soil profiles. Pedogenic influence may also explain the relationship observed between Cr and the Fe. Hg is likely to have been added to the soil profile by long-range atmospheric transport. Its accumulation in the topsoil was further favoured by the formation of stable complexes with organic matter. Clay minerals do not appear to play an important role in the fixation of heavy metals.Academia Brasileira de Ciências2011-12-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652011000400007Anais da Academia Brasileira de Ciências v.83 n.4 2011reponame:Anais da Academia Brasileira de Ciências (Online)instname:Academia Brasileira de Ciências (ABC)instacron:ABC10.1590/S0001-37652011005000042info:eu-repo/semantics/openAccessOliveira,Sonia M.B. dePessenda,Luiz C.R.Gouveia,Suzy E.M.Favaro,Deborah I.T.eng2011-11-29T00:00:00Zoai:scielo:S0001-37652011000400007Revistahttp://www.scielo.br/aabchttps://old.scielo.br/oai/scielo-oai.php||aabc@abc.org.br1678-26900001-3765opendoar:2011-11-29T00:00Anais da Academia Brasileira de Ciências (Online) - Academia Brasileira de Ciências (ABC)false
dc.title.none.fl_str_mv Heavy metal concentrations in soils from a remote oceanic island, Fernando de Noronha, Brazil
title Heavy metal concentrations in soils from a remote oceanic island, Fernando de Noronha, Brazil
spellingShingle Heavy metal concentrations in soils from a remote oceanic island, Fernando de Noronha, Brazil
Oliveira,Sonia M.B. de
heavy metals
soils
anthropogenic mercury
Fernando de Noronha
title_short Heavy metal concentrations in soils from a remote oceanic island, Fernando de Noronha, Brazil
title_full Heavy metal concentrations in soils from a remote oceanic island, Fernando de Noronha, Brazil
title_fullStr Heavy metal concentrations in soils from a remote oceanic island, Fernando de Noronha, Brazil
title_full_unstemmed Heavy metal concentrations in soils from a remote oceanic island, Fernando de Noronha, Brazil
title_sort Heavy metal concentrations in soils from a remote oceanic island, Fernando de Noronha, Brazil
author Oliveira,Sonia M.B. de
author_facet Oliveira,Sonia M.B. de
Pessenda,Luiz C.R.
Gouveia,Suzy E.M.
Favaro,Deborah I.T.
author_role author
author2 Pessenda,Luiz C.R.
Gouveia,Suzy E.M.
Favaro,Deborah I.T.
author2_role author
author
author
dc.contributor.author.fl_str_mv Oliveira,Sonia M.B. de
Pessenda,Luiz C.R.
Gouveia,Suzy E.M.
Favaro,Deborah I.T.
dc.subject.por.fl_str_mv heavy metals
soils
anthropogenic mercury
Fernando de Noronha
topic heavy metals
soils
anthropogenic mercury
Fernando de Noronha
description This paper examines the role of parent rock, pedogenetic processes and airborne pollution in heavy metal accumulation in soils from a remote oceanic island, Fernando de Noronha, Brazil. We studied five soil profiles developed from different volcanic rocks. Mineralogical composition and total concentrations of major and trace elements were determined in 43 samples. The obtained concentrations range for heavy metals were: Co: 26-261 ppm; Cu: 35-97 ppm; Cr: 350-1446 ppm; Ni: 114-691 ppm; Zn: 101-374 ppm; Hg: 2-150 ppb. The composition of soils is strongly affected by the geochemical character of the parent rock. Pedogenesis appears to be responsible for the accumulation of Zn, Co, and, to a lesser extent, of Ni and Cu, in the upper, Mn- and organic carbon-enriched horizons of the soil profiles. Pedogenic influence may also explain the relationship observed between Cr and the Fe. Hg is likely to have been added to the soil profile by long-range atmospheric transport. Its accumulation in the topsoil was further favoured by the formation of stable complexes with organic matter. Clay minerals do not appear to play an important role in the fixation of heavy metals.
publishDate 2011
dc.date.none.fl_str_mv 2011-12-01
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
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dc.identifier.uri.fl_str_mv http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652011000400007
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652011000400007
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 10.1590/S0001-37652011005000042
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv text/html
dc.publisher.none.fl_str_mv Academia Brasileira de Ciências
publisher.none.fl_str_mv Academia Brasileira de Ciências
dc.source.none.fl_str_mv Anais da Academia Brasileira de Ciências v.83 n.4 2011
reponame:Anais da Academia Brasileira de Ciências (Online)
instname:Academia Brasileira de Ciências (ABC)
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instname_str Academia Brasileira de Ciências (ABC)
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reponame_str Anais da Academia Brasileira de Ciências (Online)
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repository.name.fl_str_mv Anais da Academia Brasileira de Ciências (Online) - Academia Brasileira de Ciências (ABC)
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