Sorção e dessorção competitiva de fósforo e citrato em solos de textura muito argilosa e média

Detalhes bibliográficos
Ano de defesa: 2013
Autor(a) principal: Souza, Matheus Fonseca de
Orientador(a): Soares, Emanuelle Mercês Barros lattes
Banca de defesa: Villani, Ecila Mercês de Albuquerque lattes, Novais, Roberto Ferreira de lattes
Tipo de documento: Dissertação
Tipo de acesso: Acesso aberto
Idioma: por
Instituição de defesa: Universidade Federal de Viçosa
Programa de Pós-Graduação: Mestrado em Solos e Nutrição de Plantas
Departamento: Fertilidade do solo e nutrição de plantas; Gênese, Morfologia e Classificação, Mineralogia, Química,
País: BR
Palavras-chave em Português:
Palavras-chave em Inglês:
Área do conhecimento CNPq:
Link de acesso: http://locus.ufv.br/handle/123456789/5504
Resumo: Phosphorus (P) is one of the nutrients that often limit plant growth, mainly in highly weathered soils, such as Oxisols. However, low molecular weight organic acids can reduce P sorption in these soils. The aim of the study was to evaluate the P and citrate competitive sorption in clayey and sandy loamy soils using a stirred-flow system. Experiments were performed with soil samples (0-20 cm layer) from clayey (RYL_clay) and sandy loam (RYL_sand_loam) Red-Yellow Latosols (Oxisols). In the first study citrate effect on the P sorption was evaluated. Treatments were set up according to a 2 x 5 factorial, with two soils types and five forms of P application (only P, P and citrate, and citrate addition 7, 22, 52 min before P addition), three replicates in a completely randomized block design. The highest P sorption in the RYL_clay and RYL_sand_loam corresponding to 44.1 e 25.2 % of P added, respectively, was found with no citrate application. In the presence of citrate, P sorption was lower for all treatments evaluated. Citrate and P together reduced the sorption of P initially added to 25.8 % in RYL_clay and 16.7 % in RYL_sand_loam, in comparison to P application only. In the second assay was evaluated the P application effect on the citrate sorption. Treatments were defined according to a 2 x 2 factorial, with two soils two forms of P and citrate application (only citrate, citrate and P) in three replications in randomized blocks. The highest citrate sorption in RYL_clay and RYL_sand_loam occurred when there was no P application, corresponding to 32.0 and 30.2 % of citrate applied, respectively. With P application citrate sorption was reduced to 26.4 and 19.7 % of citrate initially added in RYL_clay and RYL_sand_loam, respectively. In the study assay it was evaluated the kinetics of desorption of previously adsorbed as affected by citrate addition. Each soil received a P dose (RYL_clay = 0.545 mg g-1 and RYL_sand_loam = 0.2 mg g-1) corresponding to 50 % of P sorption maximum capacity (PSMC) and they were incubated for 0, 6, 24, 240, 480 and 960 h before evaluating the kinetics of P desorption. Treatments were defined according to a 2 x 2 x 6 factorial scheme, with two soils, two extractors (citrate and water) and six incubation times. The P viiidesorption was greater when citrate was use as extractor. P desorption with citrate and water was initially higher (up to 24 h incubation of P) in the RYL_clay and RYL_sand_loam, consisting in an initially rapid phase, followed by a slow release phase, suggesting that depending on the time of contact of P with the soil colloids the previously adsorbed P may be released to the soil solution if effectively competing ligands such as citrates are present.
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spelling Souza, Matheus Fonseca dehttp://lattes.cnpq.br/5534798832058753Silva, Ivo Ribeiro dahttp://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4799432D0Soares, Emanuelle Mercês Barroshttp://lattes.cnpq.br/2680869902625278Villani, Ecila Mercês de Albuquerquehttp://lattes.cnpq.br/3982959345685556Novais, Roberto Ferreira dehttp://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4783732H42015-03-26T13:53:28Z2013-06-262015-03-26T13:53:28Z2013-02-28SOUZA, Matheus Fonseca de. Competitive sorption and desorption of phosphate and citrate in clayey and sandy loam soils. 2013. 32 f. Dissertação (Mestrado em Fertilidade do solo e nutrição de plantas; Gênese, Morfologia e Classificação, Mineralogia, Química,) - Universidade Federal de Viçosa, Viçosa, 2013.http://locus.ufv.br/handle/123456789/5504Phosphorus (P) is one of the nutrients that often limit plant growth, mainly in highly weathered soils, such as Oxisols. However, low molecular weight organic acids can reduce P sorption in these soils. The aim of the study was to evaluate the P and citrate competitive sorption in clayey and sandy loamy soils using a stirred-flow system. Experiments were performed with soil samples (0-20 cm layer) from clayey (RYL_clay) and sandy loam (RYL_sand_loam) Red-Yellow Latosols (Oxisols). In the first study citrate effect on the P sorption was evaluated. Treatments were set up according to a 2 x 5 factorial, with two soils types and five forms of P application (only P, P and citrate, and citrate addition 7, 22, 52 min before P addition), three replicates in a completely randomized block design. The highest P sorption in the RYL_clay and RYL_sand_loam corresponding to 44.1 e 25.2 % of P added, respectively, was found with no citrate application. In the presence of citrate, P sorption was lower for all treatments evaluated. Citrate and P together reduced the sorption of P initially added to 25.8 % in RYL_clay and 16.7 % in RYL_sand_loam, in comparison to P application only. In the second assay was evaluated the P application effect on the citrate sorption. Treatments were defined according to a 2 x 2 factorial, with two soils two forms of P and citrate application (only citrate, citrate and P) in three replications in randomized blocks. The highest citrate sorption in RYL_clay and RYL_sand_loam occurred when there was no P application, corresponding to 32.0 and 30.2 % of citrate applied, respectively. With P application citrate sorption was reduced to 26.4 and 19.7 % of citrate initially added in RYL_clay and RYL_sand_loam, respectively. In the study assay it was evaluated the kinetics of desorption of previously adsorbed as affected by citrate addition. Each soil received a P dose (RYL_clay = 0.545 mg g-1 and RYL_sand_loam = 0.2 mg g-1) corresponding to 50 % of P sorption maximum capacity (PSMC) and they were incubated for 0, 6, 24, 240, 480 and 960 h before evaluating the kinetics of P desorption. Treatments were defined according to a 2 x 2 x 6 factorial scheme, with two soils, two extractors (citrate and water) and six incubation times. The P viiidesorption was greater when citrate was use as extractor. P desorption with citrate and water was initially higher (up to 24 h incubation of P) in the RYL_clay and RYL_sand_loam, consisting in an initially rapid phase, followed by a slow release phase, suggesting that depending on the time of contact of P with the soil colloids the previously adsorbed P may be released to the soil solution if effectively competing ligands such as citrates are present.O P é considerado um dos nutrientes mais limitantes para o crescimento e desenvolvimento das plantas, principalmente em solos mais intemperizados como os Latossolos. Todavia, o aumento de ácidos orgânicos pode induzir à redução da sorção de P destes solos. O presente trabalho teve como objetivo avaliar a sorção competitiva de P e citrato em solos de textura muito argilosa e média, utilizando o sistema stirred-flow. Foram realizados três ensaios com amostras da camada de 0 a 20 cm de dois Latossolos Vermelho-Amarelos, texturas muito argilosa (LVA_arg) e média (LVA_med). No primeiro ensaio foi avaliado o efeito do citrato na sorção de P. Os tratamentos foram estabelecidos segundo o fatorial 2 x 5 sendo dois solos e cinco formas de aplicação de P no solo (apenas P, P e citrato juntos, e citrato 7, 22, 52 min antes do P), com três repetições em blocos casualizados. O valor máximo da sorção de P no LVA_arg e LVA_med foi observado na testemunha sem aplicação de citrato, correspondendo a 44,1 e 25,2 % do P aplicado, respectivamente. Com a aplicação de citrato, a sorção de P foi estatisticamente inferior em todos os tratamentos. A aplicação de citrato junto com P reduziu a sorção do P aplicado para 25,8 % no LVA_arg e 16,7 % no LVA_med, em relação à aplicação de P sem citrato. No segundo ensaio foi avaliado o efeito da aplicação de P na sorção de citrato. Os tratamentos foram definidos segundo o fatorial 2 x 2, sendo dois solos e duas formas de aplicação de P e citrato no solo (apenas citrato, citrato e P juntos), com três repetições em blocos casualizados. O valor máximo da sorção de citrato no LVA_arg e LVA_med ocorreu no tratamento sem adição de P, correspondendo a 32,0 e 30,2 % do citrato aplicado, respectivamente. Com aplicação de P a sorção de citrato reduziu para 26,4 e 19,7 % do citrato aplicado no LVA_arg e LVA_med, respectivamente. No terceiro ensaio foi avaliada a dessorção de P do solo com o tempo de incubação e adição de citrato. Cada solo recebeu uma dose de P (LVA_arg= 0,545 mg g-1 e LVA_med= 0,2 mg g-1) correspondente a 50 % da Capacidade Máxima de Sorção de P (CMSP) de cada solo e foram deixados incubados por 0, 6, 24, 240, 480 e 960 h. Os tratamentos foram definidos segundo vium fatorial 2 x 2 x 6, sendo dois solos, dois extratores (citrato e água) e os seis períodos de incubação. A dessorção de P foi maior com a utilização do citrato. A dessorção com citrato e água foi inicialmente superior (até 24 h de incubação de P) no LVA_arg e LVA_med, caracterizando uma fase inicialmente rápida, seguida de uma fase lenta, sugerindo que dependendo do tempo de contato do P com os colóides do solo, o P previamente sorvido pode ser liberado para a solução se ligantes competitivos como o citrato estiverem presente.Coordenação de Aperfeiçoamento de Pessoal de Nível Superiorapplication/pdfporUniversidade Federal de ViçosaMestrado em Solos e Nutrição de PlantasUFVBRFertilidade do solo e nutrição de plantas; Gênese, Morfologia e Classificação, Mineralogia, Química,FósforoCitratoSolosPhosphorusCitrateSoilsCNPQ::CIENCIAS AGRARIAS::AGRONOMIA::CIENCIA DO SOLOSorção e dessorção competitiva de fósforo e citrato em solos de textura muito argilosa e médiaCompetitive sorption and desorption of phosphate and citrate in clayey and sandy loam soilsinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesisinfo:eu-repo/semantics/openAccessreponame:LOCUS Repositório Institucional da UFVinstname:Universidade Federal de Viçosa (UFV)instacron:UFVORIGINALtexto completo.pdfapplication/pdf212741https://locus.ufv.br//bitstream/123456789/5504/1/texto%20completo.pdfc4f8787588d283bb7abde30d023405ddMD51TEXTtexto completo.pdf.txttexto completo.pdf.txtExtracted texttext/plain55388https://locus.ufv.br//bitstream/123456789/5504/2/texto%20completo.pdf.txt02b199d422e6fc452553ed66a97f913aMD52THUMBNAILtexto completo.pdf.jpgtexto completo.pdf.jpgIM Thumbnailimage/jpeg3555https://locus.ufv.br//bitstream/123456789/5504/3/texto%20completo.pdf.jpgda5b5e313264b0634033160954053659MD53123456789/55042016-04-11 23:04:30.133oai:locus.ufv.br:123456789/5504Repositório InstitucionalPUBhttps://www.locus.ufv.br/oai/requestfabiojreis@ufv.bropendoar:21452016-04-12T02:04:30LOCUS Repositório Institucional da UFV - Universidade Federal de Viçosa (UFV)false
dc.title.por.fl_str_mv Sorção e dessorção competitiva de fósforo e citrato em solos de textura muito argilosa e média
dc.title.alternative.eng.fl_str_mv Competitive sorption and desorption of phosphate and citrate in clayey and sandy loam soils
title Sorção e dessorção competitiva de fósforo e citrato em solos de textura muito argilosa e média
spellingShingle Sorção e dessorção competitiva de fósforo e citrato em solos de textura muito argilosa e média
Souza, Matheus Fonseca de
Fósforo
Citrato
Solos
Phosphorus
Citrate
Soils
CNPQ::CIENCIAS AGRARIAS::AGRONOMIA::CIENCIA DO SOLO
title_short Sorção e dessorção competitiva de fósforo e citrato em solos de textura muito argilosa e média
title_full Sorção e dessorção competitiva de fósforo e citrato em solos de textura muito argilosa e média
title_fullStr Sorção e dessorção competitiva de fósforo e citrato em solos de textura muito argilosa e média
title_full_unstemmed Sorção e dessorção competitiva de fósforo e citrato em solos de textura muito argilosa e média
title_sort Sorção e dessorção competitiva de fósforo e citrato em solos de textura muito argilosa e média
author Souza, Matheus Fonseca de
author_facet Souza, Matheus Fonseca de
author_role author
dc.contributor.authorLattes.por.fl_str_mv http://lattes.cnpq.br/5534798832058753
dc.contributor.author.fl_str_mv Souza, Matheus Fonseca de
dc.contributor.advisor-co1.fl_str_mv Silva, Ivo Ribeiro da
dc.contributor.advisor-co1Lattes.fl_str_mv http://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4799432D0
dc.contributor.advisor1.fl_str_mv Soares, Emanuelle Mercês Barros
dc.contributor.advisor1Lattes.fl_str_mv http://lattes.cnpq.br/2680869902625278
dc.contributor.referee1.fl_str_mv Villani, Ecila Mercês de Albuquerque
dc.contributor.referee1Lattes.fl_str_mv http://lattes.cnpq.br/3982959345685556
dc.contributor.referee2.fl_str_mv Novais, Roberto Ferreira de
dc.contributor.referee2Lattes.fl_str_mv http://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4783732H4
contributor_str_mv Silva, Ivo Ribeiro da
Soares, Emanuelle Mercês Barros
Villani, Ecila Mercês de Albuquerque
Novais, Roberto Ferreira de
dc.subject.por.fl_str_mv Fósforo
Citrato
Solos
topic Fósforo
Citrato
Solos
Phosphorus
Citrate
Soils
CNPQ::CIENCIAS AGRARIAS::AGRONOMIA::CIENCIA DO SOLO
dc.subject.eng.fl_str_mv Phosphorus
Citrate
Soils
dc.subject.cnpq.fl_str_mv CNPQ::CIENCIAS AGRARIAS::AGRONOMIA::CIENCIA DO SOLO
description Phosphorus (P) is one of the nutrients that often limit plant growth, mainly in highly weathered soils, such as Oxisols. However, low molecular weight organic acids can reduce P sorption in these soils. The aim of the study was to evaluate the P and citrate competitive sorption in clayey and sandy loamy soils using a stirred-flow system. Experiments were performed with soil samples (0-20 cm layer) from clayey (RYL_clay) and sandy loam (RYL_sand_loam) Red-Yellow Latosols (Oxisols). In the first study citrate effect on the P sorption was evaluated. Treatments were set up according to a 2 x 5 factorial, with two soils types and five forms of P application (only P, P and citrate, and citrate addition 7, 22, 52 min before P addition), three replicates in a completely randomized block design. The highest P sorption in the RYL_clay and RYL_sand_loam corresponding to 44.1 e 25.2 % of P added, respectively, was found with no citrate application. In the presence of citrate, P sorption was lower for all treatments evaluated. Citrate and P together reduced the sorption of P initially added to 25.8 % in RYL_clay and 16.7 % in RYL_sand_loam, in comparison to P application only. In the second assay was evaluated the P application effect on the citrate sorption. Treatments were defined according to a 2 x 2 factorial, with two soils two forms of P and citrate application (only citrate, citrate and P) in three replications in randomized blocks. The highest citrate sorption in RYL_clay and RYL_sand_loam occurred when there was no P application, corresponding to 32.0 and 30.2 % of citrate applied, respectively. With P application citrate sorption was reduced to 26.4 and 19.7 % of citrate initially added in RYL_clay and RYL_sand_loam, respectively. In the study assay it was evaluated the kinetics of desorption of previously adsorbed as affected by citrate addition. Each soil received a P dose (RYL_clay = 0.545 mg g-1 and RYL_sand_loam = 0.2 mg g-1) corresponding to 50 % of P sorption maximum capacity (PSMC) and they were incubated for 0, 6, 24, 240, 480 and 960 h before evaluating the kinetics of P desorption. Treatments were defined according to a 2 x 2 x 6 factorial scheme, with two soils, two extractors (citrate and water) and six incubation times. The P viiidesorption was greater when citrate was use as extractor. P desorption with citrate and water was initially higher (up to 24 h incubation of P) in the RYL_clay and RYL_sand_loam, consisting in an initially rapid phase, followed by a slow release phase, suggesting that depending on the time of contact of P with the soil colloids the previously adsorbed P may be released to the soil solution if effectively competing ligands such as citrates are present.
publishDate 2013
dc.date.available.fl_str_mv 2013-06-26
2015-03-26T13:53:28Z
dc.date.issued.fl_str_mv 2013-02-28
dc.date.accessioned.fl_str_mv 2015-03-26T13:53:28Z
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dc.identifier.citation.fl_str_mv SOUZA, Matheus Fonseca de. Competitive sorption and desorption of phosphate and citrate in clayey and sandy loam soils. 2013. 32 f. Dissertação (Mestrado em Fertilidade do solo e nutrição de plantas; Gênese, Morfologia e Classificação, Mineralogia, Química,) - Universidade Federal de Viçosa, Viçosa, 2013.
dc.identifier.uri.fl_str_mv http://locus.ufv.br/handle/123456789/5504
identifier_str_mv SOUZA, Matheus Fonseca de. Competitive sorption and desorption of phosphate and citrate in clayey and sandy loam soils. 2013. 32 f. Dissertação (Mestrado em Fertilidade do solo e nutrição de plantas; Gênese, Morfologia e Classificação, Mineralogia, Química,) - Universidade Federal de Viçosa, Viçosa, 2013.
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dc.publisher.department.fl_str_mv Fertilidade do solo e nutrição de plantas; Gênese, Morfologia e Classificação, Mineralogia, Química,
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