Análise geoquímica dos sedimentos de fundo do Arroio do Salso, Porto Alegre-RS-Brasil
Autor(a) principal: | |
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Data de Publicação: | 2004 |
Outros Autores: | , , |
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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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. |
publishDate |
2004 |
dc.date.issued.fl_str_mv |
2004 |
dc.date.accessioned.fl_str_mv |
2010-05-20T04:16:22Z |
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http://hdl.handle.net/10183/22614 |
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1518-2398 |
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http://hdl.handle.net/10183/22614 |
dc.language.iso.fl_str_mv |
por |
language |
por |
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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