Mineral nitrogen dynamics after flooding in lowland soils of Rio Grande do Sul

Detalhes bibliográficos
Autor(a) principal: da Silva, Leandro Souza
Data de Publicação: 2011
Outros Autores: Pocojeski, Elisandra, Rhoden, Anderson Clayton
Tipo de documento: Artigo
Idioma: por
Título da fonte: Semina. Ciências Agrárias (Online)
Texto Completo: https://ojs.uel.br/revistas/uel/index.php/semagrarias/article/view/3846
Resumo: The present work aims at assessing the releasing of N mineral in the forms of NH4+ e NO3- in a due time after the beginning of the flooding in different lowland soils of RS and correlate the forms of N mineral to the soil characteristics. Samples of 15 lowland soils of RS were collected in 13 cities of flooded rice producing regions. The samples were put into leaching tubes and incubated for 24 weeks. During this period, leaching was carried out and the N-mineral content was determined. The N-NO3- contents decreased after the beginning of the incubation process and nearly disappeared after 8 weeks of incubation. However, the N-NH4+ content increased with the flooding, reaching peaks around 4 to 5 weeks of incubation, showing a decline until the 18th week. The soils present differences concerning the content of cumulated N-NH4+ and it presented a correlation, among others, with the organic C content. The N-NO3- content did not presented a correlation with the evaluated parameters, except with total N content and, the highest peak of N-NH4+ presented a correlation with the organic C content and the cumulated N-NH4+. The lowland soils in RS may present different amounts of N-NO3- before the flooding and if it is not absorbed by the plants, it might be lost. The cumulated N-NH4+ content in lowland soils presented variations related to the soils characteristics, mainly organic C content.
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spelling Mineral nitrogen dynamics after flooding in lowland soils of Rio Grande do SulDinâmica de nitrogênio mineral após alagamento em solos de várzea do Rio Grande do SulAmmoniumNitrateIncubation-leaching.AmônioNitratoIncubação-lixiviação.The present work aims at assessing the releasing of N mineral in the forms of NH4+ e NO3- in a due time after the beginning of the flooding in different lowland soils of RS and correlate the forms of N mineral to the soil characteristics. Samples of 15 lowland soils of RS were collected in 13 cities of flooded rice producing regions. The samples were put into leaching tubes and incubated for 24 weeks. During this period, leaching was carried out and the N-mineral content was determined. The N-NO3- contents decreased after the beginning of the incubation process and nearly disappeared after 8 weeks of incubation. However, the N-NH4+ content increased with the flooding, reaching peaks around 4 to 5 weeks of incubation, showing a decline until the 18th week. The soils present differences concerning the content of cumulated N-NH4+ and it presented a correlation, among others, with the organic C content. The N-NO3- content did not presented a correlation with the evaluated parameters, except with total N content and, the highest peak of N-NH4+ presented a correlation with the organic C content and the cumulated N-NH4+. The lowland soils in RS may present different amounts of N-NO3- before the flooding and if it is not absorbed by the plants, it might be lost. The cumulated N-NH4+ content in lowland soils presented variations related to the soils characteristics, mainly organic C content. O objetivo deste trabalho foi avaliar a liberação de N mineral nas formas de NH4+ e NO3- em função do tempo após o início do alagamento, em diferentes solos de várzea do RS, e correlacionar as formas de N mineral com características dos solos. Amostras de 15 solos de várzea do RS foram coletadas em 13 municípios de regiões produtoras de arroz irrigado, as quais foram acondicionadas em tubos de lixiviação e incubadas durante 24 semanas. Durante esse período, foram realizadas lixiviações e determinado o teor de N-mineral. Os teores de N-NO3- decresceram após o início da incubação e praticamente desapareceram após oito semanas de incubação enquanto o teor de N-NH4+ aumentou com o alagamento, atingindo picos ao redor de quatro a cinco semanas de incubação, com posterior declínio até a 18º semana. Os solos apresentaram diferenças quanto ao teor de N-NH4+ acumulado e este apresentou correlação, entre outros, com o teor de C orgânico. O teor de N-NO3- não apresentou correlação com os parâmetros avaliados, exceto com o teor de N total do solo, e o pico máximo de N-NH4+ apresentou correlação com o teor de C orgânico e com o N-NH4+ acumulado. Os solos de várzea do RS podem apresentar diferentes quantidades de N-NO3- antes do alagamento e se este não for absorvido pelas plantas, poderá ser perdido. O teor de N-NH4+ acumulado nos solos de várzea apresentou variações relacionadas às características dos solos, principalmente ao teor de C orgânico.UEL2011-07-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionAvaliado por paresPesquisa científica de laboratórioapplication/pdfhttps://ojs.uel.br/revistas/uel/index.php/semagrarias/article/view/384610.5433/1679-0359.2011v32n2p583Semina: Ciências Agrárias; Vol. 32 No. 2 (2011); 583-590Semina: Ciências Agrárias; v. 32 n. 2 (2011); 583-5901679-03591676-546Xreponame:Semina. Ciências Agrárias (Online)instname:Universidade Estadual de Londrina (UEL)instacron:UELporhttps://ojs.uel.br/revistas/uel/index.php/semagrarias/article/view/3846/8418da Silva, Leandro SouzaPocojeski, ElisandraRhoden, Anderson Claytoninfo:eu-repo/semantics/openAccess2016-03-09T17:00:24Zoai:ojs.pkp.sfu.ca:article/3846Revistahttp://www.uel.br/revistas/uel/index.php/semagrariasPUBhttps://ojs.uel.br/revistas/uel/index.php/semagrarias/oaisemina.agrarias@uel.br1679-03591676-546Xopendoar:2016-03-09T17:00:24Semina. Ciências Agrárias (Online) - Universidade Estadual de Londrina (UEL)false
dc.title.none.fl_str_mv Mineral nitrogen dynamics after flooding in lowland soils of Rio Grande do Sul
Dinâmica de nitrogênio mineral após alagamento em solos de várzea do Rio Grande do Sul
title Mineral nitrogen dynamics after flooding in lowland soils of Rio Grande do Sul
spellingShingle Mineral nitrogen dynamics after flooding in lowland soils of Rio Grande do Sul
da Silva, Leandro Souza
Ammonium
Nitrate
Incubation-leaching.
Amônio
Nitrato
Incubação-lixiviação.
title_short Mineral nitrogen dynamics after flooding in lowland soils of Rio Grande do Sul
title_full Mineral nitrogen dynamics after flooding in lowland soils of Rio Grande do Sul
title_fullStr Mineral nitrogen dynamics after flooding in lowland soils of Rio Grande do Sul
title_full_unstemmed Mineral nitrogen dynamics after flooding in lowland soils of Rio Grande do Sul
title_sort Mineral nitrogen dynamics after flooding in lowland soils of Rio Grande do Sul
author da Silva, Leandro Souza
author_facet da Silva, Leandro Souza
Pocojeski, Elisandra
Rhoden, Anderson Clayton
author_role author
author2 Pocojeski, Elisandra
Rhoden, Anderson Clayton
author2_role author
author
dc.contributor.author.fl_str_mv da Silva, Leandro Souza
Pocojeski, Elisandra
Rhoden, Anderson Clayton
dc.subject.por.fl_str_mv Ammonium
Nitrate
Incubation-leaching.
Amônio
Nitrato
Incubação-lixiviação.
topic Ammonium
Nitrate
Incubation-leaching.
Amônio
Nitrato
Incubação-lixiviação.
description The present work aims at assessing the releasing of N mineral in the forms of NH4+ e NO3- in a due time after the beginning of the flooding in different lowland soils of RS and correlate the forms of N mineral to the soil characteristics. Samples of 15 lowland soils of RS were collected in 13 cities of flooded rice producing regions. The samples were put into leaching tubes and incubated for 24 weeks. During this period, leaching was carried out and the N-mineral content was determined. The N-NO3- contents decreased after the beginning of the incubation process and nearly disappeared after 8 weeks of incubation. However, the N-NH4+ content increased with the flooding, reaching peaks around 4 to 5 weeks of incubation, showing a decline until the 18th week. The soils present differences concerning the content of cumulated N-NH4+ and it presented a correlation, among others, with the organic C content. The N-NO3- content did not presented a correlation with the evaluated parameters, except with total N content and, the highest peak of N-NH4+ presented a correlation with the organic C content and the cumulated N-NH4+. The lowland soils in RS may present different amounts of N-NO3- before the flooding and if it is not absorbed by the plants, it might be lost. The cumulated N-NH4+ content in lowland soils presented variations related to the soils characteristics, mainly organic C content.
publishDate 2011
dc.date.none.fl_str_mv 2011-07-12
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
Avaliado por pares
Pesquisa científica de laboratório
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv https://ojs.uel.br/revistas/uel/index.php/semagrarias/article/view/3846
10.5433/1679-0359.2011v32n2p583
url https://ojs.uel.br/revistas/uel/index.php/semagrarias/article/view/3846
identifier_str_mv 10.5433/1679-0359.2011v32n2p583
dc.language.iso.fl_str_mv por
language por
dc.relation.none.fl_str_mv https://ojs.uel.br/revistas/uel/index.php/semagrarias/article/view/3846/8418
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 UEL
publisher.none.fl_str_mv UEL
dc.source.none.fl_str_mv Semina: Ciências Agrárias; Vol. 32 No. 2 (2011); 583-590
Semina: Ciências Agrárias; v. 32 n. 2 (2011); 583-590
1679-0359
1676-546X
reponame:Semina. Ciências Agrárias (Online)
instname:Universidade Estadual de Londrina (UEL)
instacron:UEL
instname_str Universidade Estadual de Londrina (UEL)
instacron_str UEL
institution UEL
reponame_str Semina. Ciências Agrárias (Online)
collection Semina. Ciências Agrárias (Online)
repository.name.fl_str_mv Semina. Ciências Agrárias (Online) - Universidade Estadual de Londrina (UEL)
repository.mail.fl_str_mv semina.agrarias@uel.br
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