Nitrate movement on surface and subsurface horizons of Udox and Udult soils with variable charges
Autor(a) principal: | |
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Data de Publicação: | 2011 |
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/1723 |
Resumo: | The objective of this work was to evaluate nitrate movement on soil columns considering mainly, total amount recovered, fit among experimental and model‑predicted transposition curves, and model‑obtained retardation factors. Samples of A and B horizons of Udox and Udult soils were used. A leaching experiment was carried out considering the miscible displacement theory, using 100 mL of a 10-mmol L-1 KNO3 solution as pulse. The amounts of nitrate leached and recovered in the columns for Udox and Udult soils in horizons A and B varied from 0.405 to 1.432 mmol L-1. There was significant (p<0.05) correlation between experimental and model-predicted curves for columns Udult-A, Udult-B and Udox-B. The mathematical model used is suitable for predicting nitrate lixiviation in B-horizon columns in Udox and Udult soils. The retardation factor was greater than 1.0 in the soil columns with good fit among experimental and predicted data, which indicates that the nitrate movement is delayed in comparison to the advance of the soil wetting front. |
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Nitrate movement on surface and subsurface horizons of Udox and Udult soils with variable chargesMovimentação de nitrato em horizonte superficial e subsuperficial de Latossolo e Nitossolo com cargas variáveisretardation factor; mathematical model; tropical soilsfator de retardamento; modelo matemático; solos tropicaisThe objective of this work was to evaluate nitrate movement on soil columns considering mainly, total amount recovered, fit among experimental and model‑predicted transposition curves, and model‑obtained retardation factors. Samples of A and B horizons of Udox and Udult soils were used. A leaching experiment was carried out considering the miscible displacement theory, using 100 mL of a 10-mmol L-1 KNO3 solution as pulse. The amounts of nitrate leached and recovered in the columns for Udox and Udult soils in horizons A and B varied from 0.405 to 1.432 mmol L-1. There was significant (p<0.05) correlation between experimental and model-predicted curves for columns Udult-A, Udult-B and Udox-B. The mathematical model used is suitable for predicting nitrate lixiviation in B-horizon columns in Udox and Udult soils. The retardation factor was greater than 1.0 in the soil columns with good fit among experimental and predicted data, which indicates that the nitrate movement is delayed in comparison to the advance of the soil wetting front.O objetivo deste trabalho foi avaliar a movimentação de nitrato em colunas de solo considerando-se, principalmente, a quantidade total recuperada, o ajuste entre as curvas de transposição experimental e predita por um modelo matemático e os fatores de retardamento obtidos pelo modelo. Foram utilizadas amostras dos horizontes A e B de um Latossolo Vermelho acriférrico e de um Nitossolo Vermelho eutrófico (LV‑A, LV‑B, NV-A e NV-B). O experimento de lixiviação foi conduzido tendo em vista a teoria do deslocamento miscível, utilizando como pulso 100 mL de KNO3 10 mmol L-1. As quantidades lixiviadas de nitrato e recuperadas nas colunas, para os solos NV e LV nos horizontes A e B, variaram de 0,405 a 1,432 mmol L-1. Houve correlação significativa (p<0,05) entre as curvas experimentais e as ajustadas pelo modelo para as colunas NV‑A, NV‑B e LV-B. O modelo matemático utilizado é adequado para prever a lixiviação de nitrato em colunas do horizonte B dos solos Nitossolo Vermelho Eutrófico e Latossolo Vermelho Acriférrico. Nas colunas dos solos com bom ajuste entre dados experimentais e preditos, o fator de retardamento é maior do que 1, o que indica que a movimentação do nitrato é retardada em relação ao avanço da frente de molhamento do solo.Pesquisa Agropecuaria BrasileiraPesquisa Agropecuária BrasileiraFapesp, CNPqAlcântara, Marco Aurélio Kondracki deCamargo, Otávio Antonio de2011-01-18info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://seer.sct.embrapa.br/index.php/pab/article/view/1723Pesquisa Agropecuaria Brasileira; v.45, n.1, jan. 2010; 81-88Pesquisa Agropecuária Brasileira; v.45, n.1, jan. 2010; 81-881678-39210100-104xreponame:Pesquisa Agropecuária Brasileira (Online)instname:Empresa Brasileira de Pesquisa Agropecuária (Embrapa)instacron:EMBRAPAporhttps://seer.sct.embrapa.br/index.php/pab/article/view/1723/5950https://seer.sct.embrapa.br/index.php/pab/article/downloadSuppFile/1723/1125info:eu-repo/semantics/openAccess2014-10-15T20:54:18Zoai:ojs.seer.sct.embrapa.br:article/1723Revistahttp://seer.sct.embrapa.br/index.php/pabPRIhttps://old.scielo.br/oai/scielo-oai.phppab@sct.embrapa.br || sct.pab@embrapa.br1678-39210100-204Xopendoar:2014-10-15T20:54:18Pesquisa Agropecuária Brasileira (Online) - Empresa Brasileira de Pesquisa Agropecuária (Embrapa)false |
dc.title.none.fl_str_mv |
Nitrate movement on surface and subsurface horizons of Udox and Udult soils with variable charges Movimentação de nitrato em horizonte superficial e subsuperficial de Latossolo e Nitossolo com cargas variáveis |
title |
Nitrate movement on surface and subsurface horizons of Udox and Udult soils with variable charges |
spellingShingle |
Nitrate movement on surface and subsurface horizons of Udox and Udult soils with variable charges Alcântara, Marco Aurélio Kondracki de retardation factor; mathematical model; tropical soils fator de retardamento; modelo matemático; solos tropicais |
title_short |
Nitrate movement on surface and subsurface horizons of Udox and Udult soils with variable charges |
title_full |
Nitrate movement on surface and subsurface horizons of Udox and Udult soils with variable charges |
title_fullStr |
Nitrate movement on surface and subsurface horizons of Udox and Udult soils with variable charges |
title_full_unstemmed |
Nitrate movement on surface and subsurface horizons of Udox and Udult soils with variable charges |
title_sort |
Nitrate movement on surface and subsurface horizons of Udox and Udult soils with variable charges |
author |
Alcântara, Marco Aurélio Kondracki de |
author_facet |
Alcântara, Marco Aurélio Kondracki de Camargo, Otávio Antonio de |
author_role |
author |
author2 |
Camargo, Otávio Antonio de |
author2_role |
author |
dc.contributor.none.fl_str_mv |
Fapesp, CNPq |
dc.contributor.author.fl_str_mv |
Alcântara, Marco Aurélio Kondracki de Camargo, Otávio Antonio de |
dc.subject.por.fl_str_mv |
retardation factor; mathematical model; tropical soils fator de retardamento; modelo matemático; solos tropicais |
topic |
retardation factor; mathematical model; tropical soils fator de retardamento; modelo matemático; solos tropicais |
description |
The objective of this work was to evaluate nitrate movement on soil columns considering mainly, total amount recovered, fit among experimental and model‑predicted transposition curves, and model‑obtained retardation factors. Samples of A and B horizons of Udox and Udult soils were used. A leaching experiment was carried out considering the miscible displacement theory, using 100 mL of a 10-mmol L-1 KNO3 solution as pulse. The amounts of nitrate leached and recovered in the columns for Udox and Udult soils in horizons A and B varied from 0.405 to 1.432 mmol L-1. There was significant (p<0.05) correlation between experimental and model-predicted curves for columns Udult-A, Udult-B and Udox-B. The mathematical model used is suitable for predicting nitrate lixiviation in B-horizon columns in Udox and Udult soils. The retardation factor was greater than 1.0 in the soil columns with good fit among experimental and predicted data, which indicates that the nitrate movement is delayed in comparison to the advance of the soil wetting front. |
publishDate |
2011 |
dc.date.none.fl_str_mv |
2011-01-18 |
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/1723 |
url |
https://seer.sct.embrapa.br/index.php/pab/article/view/1723 |
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/1723/5950 https://seer.sct.embrapa.br/index.php/pab/article/downloadSuppFile/1723/1125 |
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.45, n.1, jan. 2010; 81-88 Pesquisa Agropecuária Brasileira; v.45, n.1, jan. 2010; 81-88 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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1793416662208217088 |