Determination of oxadiazon residues in the field treated soil with and without organic matter incorporated

Detalhes bibliográficos
Autor(a) principal: Reis, Marcelo Rodrigues dos
Data de Publicação: 2016
Outros Autores: Mendes, Kassio Ferreira, Passos, Ana Beatriz Rocha de Jesus, Inoue, Miriam Hiroko, Silva, Antônio Alberto, Silva, Daniel Valadão
Tipo de documento: Artigo
Idioma: eng
Título da fonte: LOCUS Repositório Institucional da UFV
Texto Completo: http://dx.doi.org/10.1007/s12665-015-5061-8
http://www.locus.ufv.br/handle/123456789/22012
Resumo: The behavior of oxadiazon (5-tert-butyl-3-(2,4-dichloro-5-isopropoxyphenyl)-1,3,4-oxadiazol-2 (3H)-one) in the soil may be influenced by organic material content. The objective of this study was to chromatographically determine soil oxadiazon residue content as a function of organic material and soil depth. A randomized block design was used, with treatments arranged in a scheme comprising 2 × 4 × 8 + 1 sub-subdivided plots with four repetitions. Plots were comprised of soil with (8 t ha−1) and without organic material incorporated, together with a control (0 t ha−1 and 0 g ha−1 of oxadiazon). Subplots were based on soil depth (0.00–0.05; 0.05–0.10; 0.10–0.15 and 0.15–0.20 m) and sub-subplots on soil collection time (0, 2, 4, 8, 16, 32, 64 and 128 days after application—DAA). Oxadiazon was applied at 1 kg ha−1. For residue determination, samples were quantified via high performance liquid chromatography (HPLC) using the solid–liquid extraction with low temperature partitioning (SLE-LTP) technique. In the superficial layer at 0.00–0.05 m, dissipation t 1/2 of oxadiazon took between 56 and 51 days in soil with and without organic material incorporated, respectively. Oxadiazon was found in the upper layer (0.00–0.10 m) of soil until 64 DAA and did not occur at any other depth, demonstrating low soil mobility potential. In soils containing incorporated organic material, higher concentrations of oxadiazon were observed over different depths and evaluation periods.
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spelling Reis, Marcelo Rodrigues dosMendes, Kassio FerreiraPassos, Ana Beatriz Rocha de JesusInoue, Miriam HirokoSilva, Antônio AlbertoSilva, Daniel Valadão2018-09-26T23:59:24Z2018-09-26T23:59:24Z2016-01-2518666299http://dx.doi.org/10.1007/s12665-015-5061-8http://www.locus.ufv.br/handle/123456789/22012The behavior of oxadiazon (5-tert-butyl-3-(2,4-dichloro-5-isopropoxyphenyl)-1,3,4-oxadiazol-2 (3H)-one) in the soil may be influenced by organic material content. The objective of this study was to chromatographically determine soil oxadiazon residue content as a function of organic material and soil depth. A randomized block design was used, with treatments arranged in a scheme comprising 2 × 4 × 8 + 1 sub-subdivided plots with four repetitions. Plots were comprised of soil with (8 t ha−1) and without organic material incorporated, together with a control (0 t ha−1 and 0 g ha−1 of oxadiazon). Subplots were based on soil depth (0.00–0.05; 0.05–0.10; 0.10–0.15 and 0.15–0.20 m) and sub-subplots on soil collection time (0, 2, 4, 8, 16, 32, 64 and 128 days after application—DAA). Oxadiazon was applied at 1 kg ha−1. For residue determination, samples were quantified via high performance liquid chromatography (HPLC) using the solid–liquid extraction with low temperature partitioning (SLE-LTP) technique. In the superficial layer at 0.00–0.05 m, dissipation t 1/2 of oxadiazon took between 56 and 51 days in soil with and without organic material incorporated, respectively. Oxadiazon was found in the upper layer (0.00–0.10 m) of soil until 64 DAA and did not occur at any other depth, demonstrating low soil mobility potential. In soils containing incorporated organic material, higher concentrations of oxadiazon were observed over different depths and evaluation periods.engEnvironmental Earth SciencesVolume 75, Issue 3, Article 222, P. 01- 08, February 2016Springer Nature Switzerland AG.info:eu-repo/semantics/openAccessBehavior herbicide in the soilThe protox inhibitorTropical soilsLeachingSorptionDetermination of oxadiazon residues in the field treated soil with and without organic matter incorporatedinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfreponame:LOCUS Repositório Institucional da UFVinstname:Universidade Federal de Viçosa (UFV)instacron:UFVORIGINALartigo.pdfartigo.pdftexto completoapplication/pdf658301https://locus.ufv.br//bitstream/123456789/22012/1/artigo.pdf2350261deb898f9a39c7608c496d565cMD51LICENSElicense.txtlicense.txttext/plain; charset=utf-81748https://locus.ufv.br//bitstream/123456789/22012/2/license.txt8a4605be74aa9ea9d79846c1fba20a33MD52THUMBNAILartigo.pdf.jpgartigo.pdf.jpgIM Thumbnailimage/jpeg5184https://locus.ufv.br//bitstream/123456789/22012/3/artigo.pdf.jpg899940c4fa8a1f5f4e248f1f2bffd328MD53123456789/220122018-09-26 23:00:35.346oai:locus.ufv.br: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Repositório InstitucionalPUBhttps://www.locus.ufv.br/oai/requestfabiojreis@ufv.bropendoar:21452018-09-27T02:00:35LOCUS Repositório Institucional da UFV - Universidade Federal de Viçosa (UFV)false
dc.title.en.fl_str_mv Determination of oxadiazon residues in the field treated soil with and without organic matter incorporated
title Determination of oxadiazon residues in the field treated soil with and without organic matter incorporated
spellingShingle Determination of oxadiazon residues in the field treated soil with and without organic matter incorporated
Reis, Marcelo Rodrigues dos
Behavior herbicide in the soil
The protox inhibitor
Tropical soils
Leaching
Sorption
title_short Determination of oxadiazon residues in the field treated soil with and without organic matter incorporated
title_full Determination of oxadiazon residues in the field treated soil with and without organic matter incorporated
title_fullStr Determination of oxadiazon residues in the field treated soil with and without organic matter incorporated
title_full_unstemmed Determination of oxadiazon residues in the field treated soil with and without organic matter incorporated
title_sort Determination of oxadiazon residues in the field treated soil with and without organic matter incorporated
author Reis, Marcelo Rodrigues dos
author_facet Reis, Marcelo Rodrigues dos
Mendes, Kassio Ferreira
Passos, Ana Beatriz Rocha de Jesus
Inoue, Miriam Hiroko
Silva, Antônio Alberto
Silva, Daniel Valadão
author_role author
author2 Mendes, Kassio Ferreira
Passos, Ana Beatriz Rocha de Jesus
Inoue, Miriam Hiroko
Silva, Antônio Alberto
Silva, Daniel Valadão
author2_role author
author
author
author
author
dc.contributor.author.fl_str_mv Reis, Marcelo Rodrigues dos
Mendes, Kassio Ferreira
Passos, Ana Beatriz Rocha de Jesus
Inoue, Miriam Hiroko
Silva, Antônio Alberto
Silva, Daniel Valadão
dc.subject.pt-BR.fl_str_mv Behavior herbicide in the soil
The protox inhibitor
Tropical soils
Leaching
Sorption
topic Behavior herbicide in the soil
The protox inhibitor
Tropical soils
Leaching
Sorption
description The behavior of oxadiazon (5-tert-butyl-3-(2,4-dichloro-5-isopropoxyphenyl)-1,3,4-oxadiazol-2 (3H)-one) in the soil may be influenced by organic material content. The objective of this study was to chromatographically determine soil oxadiazon residue content as a function of organic material and soil depth. A randomized block design was used, with treatments arranged in a scheme comprising 2 × 4 × 8 + 1 sub-subdivided plots with four repetitions. Plots were comprised of soil with (8 t ha−1) and without organic material incorporated, together with a control (0 t ha−1 and 0 g ha−1 of oxadiazon). Subplots were based on soil depth (0.00–0.05; 0.05–0.10; 0.10–0.15 and 0.15–0.20 m) and sub-subplots on soil collection time (0, 2, 4, 8, 16, 32, 64 and 128 days after application—DAA). Oxadiazon was applied at 1 kg ha−1. For residue determination, samples were quantified via high performance liquid chromatography (HPLC) using the solid–liquid extraction with low temperature partitioning (SLE-LTP) technique. In the superficial layer at 0.00–0.05 m, dissipation t 1/2 of oxadiazon took between 56 and 51 days in soil with and without organic material incorporated, respectively. Oxadiazon was found in the upper layer (0.00–0.10 m) of soil until 64 DAA and did not occur at any other depth, demonstrating low soil mobility potential. In soils containing incorporated organic material, higher concentrations of oxadiazon were observed over different depths and evaluation periods.
publishDate 2016
dc.date.issued.fl_str_mv 2016-01-25
dc.date.accessioned.fl_str_mv 2018-09-26T23:59:24Z
dc.date.available.fl_str_mv 2018-09-26T23:59:24Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
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dc.identifier.uri.fl_str_mv http://dx.doi.org/10.1007/s12665-015-5061-8
http://www.locus.ufv.br/handle/123456789/22012
dc.identifier.issn.none.fl_str_mv 18666299
identifier_str_mv 18666299
url http://dx.doi.org/10.1007/s12665-015-5061-8
http://www.locus.ufv.br/handle/123456789/22012
dc.language.iso.fl_str_mv eng
language eng
dc.relation.ispartofseries.pt-BR.fl_str_mv Volume 75, Issue 3, Article 222, P. 01- 08, February 2016
dc.rights.driver.fl_str_mv Springer Nature Switzerland AG.
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eu_rights_str_mv openAccess
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publisher.none.fl_str_mv Environmental Earth Sciences
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