Decomposition of 14C-Malathion in three brazilian soil samples
Autor(a) principal: | |
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Data de Publicação: | 2014 |
Outros Autores: | , |
Tipo de documento: | Artigo |
Idioma: | por |
Título da fonte: | Pesquisa Agropecuária Brasileira (Online) |
Texto Completo: | https://seer.sct.embrapa.br/index.php/pab/article/view/15627 |
Resumo: | The degradation of 14C-malathion in soil was examined using gas chromatography and radiotracer techniques. About half of the malathion added was degraded within a day in soil from three regions of Brazil. Almost all the radiolabelled material extracted from the Red Latosol (Londrina, PR) was malathion, but metabolites were extracted from the "Sandy" cerrado soil (Planaltina, DF.) and Dark-Red Latosol (Passo Fundo. RS). The proportion of metabolites in the extracts increased until most of the malathion was degraded, after four days. Radiocarbon dioxide was liberated from all three soils at similar rates. When about half of the label had been recovered as carbon dioxide after eight weeks, the rate of evolution diminished. |
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Decomposition of 14C-Malathion in three brazilian soil samplesDecomposição do 14C-Malation em amostras de três solos do BrasilCerrado; latosol; radiometric techniquesmalation; Cerrado; latossolo; técnicas radiométricasThe degradation of 14C-malathion in soil was examined using gas chromatography and radiotracer techniques. About half of the malathion added was degraded within a day in soil from three regions of Brazil. Almost all the radiolabelled material extracted from the Red Latosol (Londrina, PR) was malathion, but metabolites were extracted from the "Sandy" cerrado soil (Planaltina, DF.) and Dark-Red Latosol (Passo Fundo. RS). The proportion of metabolites in the extracts increased until most of the malathion was degraded, after four days. Radiocarbon dioxide was liberated from all three soils at similar rates. When about half of the label had been recovered as carbon dioxide after eight weeks, the rate of evolution diminished.A decomposição do 14C-malation em solo foi examinada usando-se cromatografia a gás e técnicas radiométricas. Aproximadamente metade do malation adicionado foi decomposto em um dia, em solos de três regiões do Brasil. Quase todo o material radioativo extraído do Latossolo Roxo (Londrina, PR) era malation, mas metabolitos foram extraídos do solo tipo "Arenoso" do Cerrado (Planaltina, DF) e do Latossolo Vermelho-Escuro Distrófico (Passo Fundo, RS). A proporção de metabolitos nos extratos aumentou até que a maior parte do malation se degradasse em quatro dias. Dióxido de radiocarbono foi liberado dos três solos na mesma taxa, mas quando aproximadamente metade do 14C aplicado foi recuperado na forma de 14CO2, após oito semanas, a taxa de evolução diminuiu.Pesquisa Agropecuaria BrasileiraPesquisa Agropecuária BrasileiraHelene, Cecilia GusmãoRüegg, Elza FloresLord, Kenneth Alan2014-04-16info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://seer.sct.embrapa.br/index.php/pab/article/view/15627Pesquisa Agropecuaria Brasileira; v.17, n.2, fev. 1982; 293-298Pesquisa Agropecuária Brasileira; v.17, n.2, fev. 1982; 293-2981678-39210100-104xreponame:Pesquisa Agropecuária Brasileira (Online)instname:Empresa Brasileira de Pesquisa Agropecuária (Embrapa)instacron:EMBRAPAporhttps://seer.sct.embrapa.br/index.php/pab/article/view/15627/9629info:eu-repo/semantics/openAccess2014-04-16T12:24:17Zoai:ojs.seer.sct.embrapa.br:article/15627Revistahttp://seer.sct.embrapa.br/index.php/pabPRIhttps://old.scielo.br/oai/scielo-oai.phppab@sct.embrapa.br || sct.pab@embrapa.br1678-39210100-204Xopendoar:2014-04-16T12:24:17Pesquisa Agropecuária Brasileira (Online) - Empresa Brasileira de Pesquisa Agropecuária (Embrapa)false |
dc.title.none.fl_str_mv |
Decomposition of 14C-Malathion in three brazilian soil samples Decomposição do 14C-Malation em amostras de três solos do Brasil |
title |
Decomposition of 14C-Malathion in three brazilian soil samples |
spellingShingle |
Decomposition of 14C-Malathion in three brazilian soil samples Helene, Cecilia Gusmão Cerrado; latosol; radiometric techniques malation; Cerrado; latossolo; técnicas radiométricas |
title_short |
Decomposition of 14C-Malathion in three brazilian soil samples |
title_full |
Decomposition of 14C-Malathion in three brazilian soil samples |
title_fullStr |
Decomposition of 14C-Malathion in three brazilian soil samples |
title_full_unstemmed |
Decomposition of 14C-Malathion in three brazilian soil samples |
title_sort |
Decomposition of 14C-Malathion in three brazilian soil samples |
author |
Helene, Cecilia Gusmão |
author_facet |
Helene, Cecilia Gusmão Rüegg, Elza Flores Lord, Kenneth Alan |
author_role |
author |
author2 |
Rüegg, Elza Flores Lord, Kenneth Alan |
author2_role |
author author |
dc.contributor.none.fl_str_mv |
|
dc.contributor.author.fl_str_mv |
Helene, Cecilia Gusmão Rüegg, Elza Flores Lord, Kenneth Alan |
dc.subject.por.fl_str_mv |
Cerrado; latosol; radiometric techniques malation; Cerrado; latossolo; técnicas radiométricas |
topic |
Cerrado; latosol; radiometric techniques malation; Cerrado; latossolo; técnicas radiométricas |
description |
The degradation of 14C-malathion in soil was examined using gas chromatography and radiotracer techniques. About half of the malathion added was degraded within a day in soil from three regions of Brazil. Almost all the radiolabelled material extracted from the Red Latosol (Londrina, PR) was malathion, but metabolites were extracted from the "Sandy" cerrado soil (Planaltina, DF.) and Dark-Red Latosol (Passo Fundo. RS). The proportion of metabolites in the extracts increased until most of the malathion was degraded, after four days. Radiocarbon dioxide was liberated from all three soils at similar rates. When about half of the label had been recovered as carbon dioxide after eight weeks, the rate of evolution diminished. |
publishDate |
2014 |
dc.date.none.fl_str_mv |
2014-04-16 |
dc.type.none.fl_str_mv |
|
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://seer.sct.embrapa.br/index.php/pab/article/view/15627 |
url |
https://seer.sct.embrapa.br/index.php/pab/article/view/15627 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
https://seer.sct.embrapa.br/index.php/pab/article/view/15627/9629 |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Pesquisa Agropecuaria Brasileira Pesquisa Agropecuária Brasileira |
publisher.none.fl_str_mv |
Pesquisa Agropecuaria Brasileira Pesquisa Agropecuária Brasileira |
dc.source.none.fl_str_mv |
Pesquisa Agropecuaria Brasileira; v.17, n.2, fev. 1982; 293-298 Pesquisa Agropecuária Brasileira; v.17, n.2, fev. 1982; 293-298 1678-3921 0100-104x reponame:Pesquisa Agropecuária Brasileira (Online) instname:Empresa Brasileira de Pesquisa Agropecuária (Embrapa) instacron:EMBRAPA |
instname_str |
Empresa Brasileira de Pesquisa Agropecuária (Embrapa) |
instacron_str |
EMBRAPA |
institution |
EMBRAPA |
reponame_str |
Pesquisa Agropecuária Brasileira (Online) |
collection |
Pesquisa Agropecuária Brasileira (Online) |
repository.name.fl_str_mv |
Pesquisa Agropecuária Brasileira (Online) - Empresa Brasileira de Pesquisa Agropecuária (Embrapa) |
repository.mail.fl_str_mv |
pab@sct.embrapa.br || sct.pab@embrapa.br |
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1793416680257355776 |