Análise geoquímica dos sedimentos de fundo do Arroio do Salso, Porto Alegre-RS-Brasil

Detalhes bibliográficos
Autor(a) principal: Soares, Maria Cristina Cerveira
Data de Publicação: 2004
Outros Autores: Mizusaki, Ana Maria Pimentel, Guerra, Teresinha, Vignol, Maria Lídia Medeiros
Tipo de documento: Artigo
Idioma: por
Título da fonte: Repositório Institucional da UFRGS
Texto Completo: http://hdl.handle.net/10183/22614
Resumo: This paper presents the results of a study performed on bedload samples from the Salso Creek in the Porto Alegre City (Rio Grande do Sul State) rural area where agricultural and pastoral activities are carried out within urban areas. Sediment sampling took place on the 16th September 2001 (winter) and 21th January 2002 (summer), at five sites along the Salso Creek. The Salso Creek bed load changes from granules and pebbles (upstream reaches), through coarse- to medium-grained sand (mid reaches) to fine-to very fine-grained sand in the Salso Creek mouth region. Organic matter content increases throughout the summer low discharge due to the accumulation of the suspended load on the creek bed surface. Grains larger then 0.062 mm feature the following estimated mineralogical composition: feldspar (55-50%), quartz (30-40%), opaque (5-10%) and acessory (5-10%) minerals. Among the finegrained sediments (< 0.062 mm) kaolinite dominates being followed by a minor amount of muscovite/illite as well as quartz, feldspar and smectite traces. The chemical composition of the fine-grained sediments reveals that, among the major (Al, Fe, Mn, Ca, Mg, Na and K) and trace (Cr, Cu, Ni, Pb and Zn) analyzed elements, the Al content is high, probably a result of the kaolinite-rich (Al4(Si4O10)(OH)8) composition of the fine-grained fraction. Geo- Accumulation Index calculation shows no significant accumulation of any of the analyzed elements within the finegrained fraction, hence indicating slightly to moderately polluted sediments. On the other hand Contamination Factor computation for the sediments fine-grained fraction pointed out a Cu, Ni and Zn enrichment, indicating considerable to high contamination, especially for those places directly under domestic sewerage influence. These elements are probably being concentrated in the fine-grained fraction of the bed load.
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spelling Soares, Maria Cristina CerveiraMizusaki, Ana Maria PimentelGuerra, TeresinhaVignol, Maria Lídia Medeiros2010-05-20T04:16:22Z20041518-2398http://hdl.handle.net/10183/22614000442812This paper presents the results of a study performed on bedload samples from the Salso Creek in the Porto Alegre City (Rio Grande do Sul State) rural area where agricultural and pastoral activities are carried out within urban areas. Sediment sampling took place on the 16th September 2001 (winter) and 21th January 2002 (summer), at five sites along the Salso Creek. The Salso Creek bed load changes from granules and pebbles (upstream reaches), through coarse- to medium-grained sand (mid reaches) to fine-to very fine-grained sand in the Salso Creek mouth region. Organic matter content increases throughout the summer low discharge due to the accumulation of the suspended load on the creek bed surface. Grains larger then 0.062 mm feature the following estimated mineralogical composition: feldspar (55-50%), quartz (30-40%), opaque (5-10%) and acessory (5-10%) minerals. Among the finegrained sediments (< 0.062 mm) kaolinite dominates being followed by a minor amount of muscovite/illite as well as quartz, feldspar and smectite traces. The chemical composition of the fine-grained sediments reveals that, among the major (Al, Fe, Mn, Ca, Mg, Na and K) and trace (Cr, Cu, Ni, Pb and Zn) analyzed elements, the Al content is high, probably a result of the kaolinite-rich (Al4(Si4O10)(OH)8) composition of the fine-grained fraction. Geo- Accumulation Index calculation shows no significant accumulation of any of the analyzed elements within the finegrained fraction, hence indicating slightly to moderately polluted sediments. On the other hand Contamination Factor computation for the sediments fine-grained fraction pointed out a Cu, Ni and Zn enrichment, indicating considerable to high contamination, especially for those places directly under domestic sewerage influence. These elements are probably being concentrated in the fine-grained fraction of the bed load.application/pdfporPesquisas em Geociências. Porto Alegre, RS. Vol. 31, n. 1 (2004), p. 39-50Geoquímica : Rio Grande do SulBed loadMajor elementsTrace elementsGeochemistryAnálise geoquímica dos sedimentos de fundo do Arroio do Salso, Porto Alegre-RS-Brasilinfo:eu-repo/semantics/articleinfo:eu-repo/semantics/otherinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da UFRGSinstname:Universidade Federal do Rio Grande do Sul (UFRGS)instacron:UFRGSTEXT000442812.pdf.txt000442812.pdf.txtExtracted Texttext/plain40129http://www.lume.ufrgs.br/bitstream/10183/22614/2/000442812.pdf.txtb2f7b6bcec24521619458da4116f716fMD52ORIGINAL000442812.pdf000442812.pdfTexto completoapplication/pdf106345http://www.lume.ufrgs.br/bitstream/10183/22614/1/000442812.pdf2def4103ab0c03fba43956f4b228d464MD51THUMBNAIL000442812.pdf.jpg000442812.pdf.jpgGenerated Thumbnailimage/jpeg1602http://www.lume.ufrgs.br/bitstream/10183/22614/3/000442812.pdf.jpg2e58ced03922f940e7f4fb034152c17dMD5310183/226142018-10-08 08:00:00.62oai:www.lume.ufrgs.br:10183/22614Repositório de PublicaçõesPUBhttps://lume.ufrgs.br/oai/requestopendoar:2018-10-08T11:00Repositório Institucional da UFRGS - Universidade Federal do Rio Grande do Sul (UFRGS)false
dc.title.pt_BR.fl_str_mv Análise geoquímica dos sedimentos de fundo do Arroio do Salso, Porto Alegre-RS-Brasil
title Análise geoquímica dos sedimentos de fundo do Arroio do Salso, Porto Alegre-RS-Brasil
spellingShingle Análise geoquímica dos sedimentos de fundo do Arroio do Salso, Porto Alegre-RS-Brasil
Soares, Maria Cristina Cerveira
Geoquímica : Rio Grande do Sul
Bed load
Major elements
Trace elements
Geochemistry
title_short Análise geoquímica dos sedimentos de fundo do Arroio do Salso, Porto Alegre-RS-Brasil
title_full Análise geoquímica dos sedimentos de fundo do Arroio do Salso, Porto Alegre-RS-Brasil
title_fullStr Análise geoquímica dos sedimentos de fundo do Arroio do Salso, Porto Alegre-RS-Brasil
title_full_unstemmed Análise geoquímica dos sedimentos de fundo do Arroio do Salso, Porto Alegre-RS-Brasil
title_sort Análise geoquímica dos sedimentos de fundo do Arroio do Salso, Porto Alegre-RS-Brasil
author Soares, Maria Cristina Cerveira
author_facet Soares, Maria Cristina Cerveira
Mizusaki, Ana Maria Pimentel
Guerra, Teresinha
Vignol, Maria Lídia Medeiros
author_role author
author2 Mizusaki, Ana Maria Pimentel
Guerra, Teresinha
Vignol, Maria Lídia Medeiros
author2_role author
author
author
dc.contributor.author.fl_str_mv Soares, Maria Cristina Cerveira
Mizusaki, Ana Maria Pimentel
Guerra, Teresinha
Vignol, Maria Lídia Medeiros
dc.subject.por.fl_str_mv Geoquímica : Rio Grande do Sul
topic Geoquímica : Rio Grande do Sul
Bed load
Major elements
Trace elements
Geochemistry
dc.subject.eng.fl_str_mv Bed load
Major elements
Trace elements
Geochemistry
description This paper presents the results of a study performed on bedload samples from the Salso Creek in the Porto Alegre City (Rio Grande do Sul State) rural area where agricultural and pastoral activities are carried out within urban areas. Sediment sampling took place on the 16th September 2001 (winter) and 21th January 2002 (summer), at five sites along the Salso Creek. The Salso Creek bed load changes from granules and pebbles (upstream reaches), through coarse- to medium-grained sand (mid reaches) to fine-to very fine-grained sand in the Salso Creek mouth region. Organic matter content increases throughout the summer low discharge due to the accumulation of the suspended load on the creek bed surface. Grains larger then 0.062 mm feature the following estimated mineralogical composition: feldspar (55-50%), quartz (30-40%), opaque (5-10%) and acessory (5-10%) minerals. Among the finegrained sediments (< 0.062 mm) kaolinite dominates being followed by a minor amount of muscovite/illite as well as quartz, feldspar and smectite traces. The chemical composition of the fine-grained sediments reveals that, among the major (Al, Fe, Mn, Ca, Mg, Na and K) and trace (Cr, Cu, Ni, Pb and Zn) analyzed elements, the Al content is high, probably a result of the kaolinite-rich (Al4(Si4O10)(OH)8) composition of the fine-grained fraction. Geo- Accumulation Index calculation shows no significant accumulation of any of the analyzed elements within the finegrained fraction, hence indicating slightly to moderately polluted sediments. On the other hand Contamination Factor computation for the sediments fine-grained fraction pointed out a Cu, Ni and Zn enrichment, indicating considerable to high contamination, especially for those places directly under domestic sewerage influence. These elements are probably being concentrated in the fine-grained fraction of the bed load.
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dc.relation.ispartof.pt_BR.fl_str_mv Pesquisas em Geociências. Porto Alegre, RS. Vol. 31, n. 1 (2004), p. 39-50
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