PHOSPHORUS ADSORPTION IN SOILS OF TROPICAL REGIONS

Detalhes bibliográficos
Autor(a) principal: Vinha, Ana Paula Carrara
Data de Publicação: 2023
Outros Autores: Carrara, Bruna Helena, Souza, Emanuella Farias Santos, Santos, Jussane Antunes Fogaça dos, Arantes, Sayonara Andrade C.Moreno
Tipo de documento: Artigo
Idioma: por
Título da fonte: Nativa (Sinop)
Texto Completo: https://periodicoscientificos.ufmt.br/ojs/index.php/nativa/article/view/10973
Resumo: Phosphorus (P) is the most limiting nutrient for cultivation in tropical soils, as they generally have high phosphorus adsorption capacity. Some chemical and physical attributes of soil such as clay content, pH, effective cation exchange capacity (ECEC) and organic matter influence the adsorption dynamics. The objective of this study was to evaluate the behaviour of the phosphorus adsorption process in a Red-Yellow Oxisol and a Typic Quartzipisamment from the Cerrado-Amazon transition region, and to evaluate the soil attributes that influence the adsorption dynamics of the soil of the phosphorus. Chemical and physical characterization and Langmuir isotherm construction were performed by the “Bach” method. From the Langmuir linearized equation, the maximum P adsorption capacity (MPAC), the constant with the binding energy (KB) and the maximum capacity factor (PCFmax) were selected. There was a difference in MPAC, KB and PCFmax of the studied soils, and the highest values ​​were found in the Red-Yellow Oxisol, mainly due to the higher clay content in relation to theTypic Quartzipisamment. Organic matter was one of the few attributes that had a negative correlation with the adsorption attributes, highlighting (emphasizing) it’s importance in (soil) management to increase the efficiency of phosphate fertilization.
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spelling PHOSPHORUS ADSORPTION IN SOILS OF TROPICAL REGIONS ADSORÇÃO DE FÓSFORO EM SOLOS DE REGIÕES TROPICAIS Latossolo Vermelho AmareloNeossolo Quartzarênico Isotermas de adsorçãoPhosphorus (P) is the most limiting nutrient for cultivation in tropical soils, as they generally have high phosphorus adsorption capacity. Some chemical and physical attributes of soil such as clay content, pH, effective cation exchange capacity (ECEC) and organic matter influence the adsorption dynamics. The objective of this study was to evaluate the behaviour of the phosphorus adsorption process in a Red-Yellow Oxisol and a Typic Quartzipisamment from the Cerrado-Amazon transition region, and to evaluate the soil attributes that influence the adsorption dynamics of the soil of the phosphorus. Chemical and physical characterization and Langmuir isotherm construction were performed by the “Bach” method. From the Langmuir linearized equation, the maximum P adsorption capacity (MPAC), the constant with the binding energy (KB) and the maximum capacity factor (PCFmax) were selected. There was a difference in MPAC, KB and PCFmax of the studied soils, and the highest values ​​were found in the Red-Yellow Oxisol, mainly due to the higher clay content in relation to theTypic Quartzipisamment. Organic matter was one of the few attributes that had a negative correlation with the adsorption attributes, highlighting (emphasizing) it’s importance in (soil) management to increase the efficiency of phosphate fertilization.O fósforo (P) é o nutriente mais limitante ao cultivo nos solos tropicais, que, geralmente, apresentam alta capacidade de adsorção de P. Alguns atributos químicos e físicos do solo como o teor de argila, pH, CTC efetiva e matéria orgânica influenciam na dinâmica de adsorção. O objetivo deste estudo foi avaliar o processo de adsorção do fósforo em um Latossolo Vermelho Amarelo (LVA) e um Neossolo Quartzarênico (RQ) da região de transição Cerrado-Amazônia, e avaliar os atributos dos solos que influenciam na dinâmica de adsorção do P. Os ensaios de sorção foram realizados pelo método “Batch” ou em batelada e à partir dos dados obtidos foram construídas curvas obtendo a equação linearizada de Langmuir, com as quais foram determinados os valores de capacidade máxima de adsorção de P (CMAP), a constante relacionada com a energia de ligação (KL) e o fator capacidade de P máximo (FCPmáx). Houve diferença na CMAP, KL e FCPmáx dos solos estudados, sendo que os maiores valores foram encontrados no LVA, devido principalmente ao maior teor de argila em relação ao RQ. A matéria orgânica foi um dos poucos atributos que tiveram correlação negativa com os atributos de adsorção, ressaltando sua importância no manejo para aumentar a eficiência da adubação fosfatada. Palavras-chave: Latossolo Vermelho Amarelo; Neossolo Quartzarênico; Isotermas de adsorção.   Phosphorus adsorption in soils of tropical regions   ABSTRACT: Phosphorus (P) is the most limiting nutrient for cultivation in tropical soils, as they generally have high P adsorption capacity. Some chemical and physical attributes of soil such as clay content, pH, effective cation exchange capacity (ECEC) and organic matter influence the adsorption dynamics. The objective of this study was to evaluate the behaviour of the phosphorus adsorption process in a Red-Yellow Latosol and a Quartzarenic Neosol from the Cerrado-Amazon transition region, and to evaluate the soil attributes that influence the adsorption dynamics of the soil of the phosphorus. Sorption tests were performed using the “Bach” method, from the Langmuir linearized equation, the maximum P adsorption capacity (MPAC), the constant with the binding energy (KB) and the maximum capacity factor (PCFmax) were selected. There was a difference in MPAC, KB and PCFmax of the studied soils, and the highest values ​​were found in the Red-Yellow Oxisol, mainly due to the higher clay content in relation to theTypic Quartzipisamment. Organic matter was one of the few attributes that had a negative correlation with the adsorption attributes, highlighting (emphasizing) it’s importance in (soil) management to increase the efficiency of phosphate fertilization. Keywords: Red-Yellow Latosol; Quartzarenic Neosol; adsorption isotherms.Universidade Federal de Mato Grosso2023-09-29info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdftext/htmlhttps://periodicoscientificos.ufmt.br/ojs/index.php/nativa/article/view/1097310.31413/nativa.v9i1.10973Nativa; v. 9 n. 1 (2021); 30-35Nativa; Vol. 9 Núm. 1 (2021); 30-35Nativa; Vol. 9 No. 1 (2021); 30-352318-7670reponame:Nativa (Sinop)instname:Universidade Federal de Mato Grosso (UFMT)instacron:UFMTporhttps://periodicoscientificos.ufmt.br/ojs/index.php/nativa/article/view/10973/12684https://periodicoscientificos.ufmt.br/ojs/index.php/nativa/article/view/10973/12685Copyright (c) 2021 Nativahttps://creativecommons.org/licenses/by-nc/4.0info:eu-repo/semantics/openAccessVinha, Ana Paula CarraraCarrara, Bruna HelenaSouza, Emanuella Farias SantosSantos, Jussane Antunes Fogaça dosArantes, Sayonara Andrade C.Moreno2021-03-05T18:23:57Zoai:periodicoscientificos.ufmt.br:article/10973Revistahttps://periodicoscientificos.ufmt.br/ojs/index.php/nativaPUBhttps://periodicoscientificos.ufmt.br/ojs/index.php/nativa/oai||rrmelo2@yahoo.com.br2318-76702318-7670opendoar:2021-03-05T18:23:57Nativa (Sinop) - Universidade Federal de Mato Grosso (UFMT)false
dc.title.none.fl_str_mv PHOSPHORUS ADSORPTION IN SOILS OF TROPICAL REGIONS
ADSORÇÃO DE FÓSFORO EM SOLOS DE REGIÕES TROPICAIS
title PHOSPHORUS ADSORPTION IN SOILS OF TROPICAL REGIONS
spellingShingle PHOSPHORUS ADSORPTION IN SOILS OF TROPICAL REGIONS
Vinha, Ana Paula Carrara
Latossolo Vermelho Amarelo
Neossolo Quartzarênico
Isotermas de adsorção
title_short PHOSPHORUS ADSORPTION IN SOILS OF TROPICAL REGIONS
title_full PHOSPHORUS ADSORPTION IN SOILS OF TROPICAL REGIONS
title_fullStr PHOSPHORUS ADSORPTION IN SOILS OF TROPICAL REGIONS
title_full_unstemmed PHOSPHORUS ADSORPTION IN SOILS OF TROPICAL REGIONS
title_sort PHOSPHORUS ADSORPTION IN SOILS OF TROPICAL REGIONS
author Vinha, Ana Paula Carrara
author_facet Vinha, Ana Paula Carrara
Carrara, Bruna Helena
Souza, Emanuella Farias Santos
Santos, Jussane Antunes Fogaça dos
Arantes, Sayonara Andrade C.Moreno
author_role author
author2 Carrara, Bruna Helena
Souza, Emanuella Farias Santos
Santos, Jussane Antunes Fogaça dos
Arantes, Sayonara Andrade C.Moreno
author2_role author
author
author
author
dc.contributor.author.fl_str_mv Vinha, Ana Paula Carrara
Carrara, Bruna Helena
Souza, Emanuella Farias Santos
Santos, Jussane Antunes Fogaça dos
Arantes, Sayonara Andrade C.Moreno
dc.subject.por.fl_str_mv Latossolo Vermelho Amarelo
Neossolo Quartzarênico
Isotermas de adsorção
topic Latossolo Vermelho Amarelo
Neossolo Quartzarênico
Isotermas de adsorção
description Phosphorus (P) is the most limiting nutrient for cultivation in tropical soils, as they generally have high phosphorus adsorption capacity. Some chemical and physical attributes of soil such as clay content, pH, effective cation exchange capacity (ECEC) and organic matter influence the adsorption dynamics. The objective of this study was to evaluate the behaviour of the phosphorus adsorption process in a Red-Yellow Oxisol and a Typic Quartzipisamment from the Cerrado-Amazon transition region, and to evaluate the soil attributes that influence the adsorption dynamics of the soil of the phosphorus. Chemical and physical characterization and Langmuir isotherm construction were performed by the “Bach” method. From the Langmuir linearized equation, the maximum P adsorption capacity (MPAC), the constant with the binding energy (KB) and the maximum capacity factor (PCFmax) were selected. There was a difference in MPAC, KB and PCFmax of the studied soils, and the highest values ​​were found in the Red-Yellow Oxisol, mainly due to the higher clay content in relation to theTypic Quartzipisamment. Organic matter was one of the few attributes that had a negative correlation with the adsorption attributes, highlighting (emphasizing) it’s importance in (soil) management to increase the efficiency of phosphate fertilization.
publishDate 2023
dc.date.none.fl_str_mv 2023-09-29
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://periodicoscientificos.ufmt.br/ojs/index.php/nativa/article/view/10973
10.31413/nativa.v9i1.10973
url https://periodicoscientificos.ufmt.br/ojs/index.php/nativa/article/view/10973
identifier_str_mv 10.31413/nativa.v9i1.10973
dc.language.iso.fl_str_mv por
language por
dc.relation.none.fl_str_mv https://periodicoscientificos.ufmt.br/ojs/index.php/nativa/article/view/10973/12684
https://periodicoscientificos.ufmt.br/ojs/index.php/nativa/article/view/10973/12685
dc.rights.driver.fl_str_mv Copyright (c) 2021 Nativa
https://creativecommons.org/licenses/by-nc/4.0
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Copyright (c) 2021 Nativa
https://creativecommons.org/licenses/by-nc/4.0
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
text/html
dc.publisher.none.fl_str_mv Universidade Federal de Mato Grosso
publisher.none.fl_str_mv Universidade Federal de Mato Grosso
dc.source.none.fl_str_mv Nativa; v. 9 n. 1 (2021); 30-35
Nativa; Vol. 9 Núm. 1 (2021); 30-35
Nativa; Vol. 9 No. 1 (2021); 30-35
2318-7670
reponame:Nativa (Sinop)
instname:Universidade Federal de Mato Grosso (UFMT)
instacron:UFMT
instname_str Universidade Federal de Mato Grosso (UFMT)
instacron_str UFMT
institution UFMT
reponame_str Nativa (Sinop)
collection Nativa (Sinop)
repository.name.fl_str_mv Nativa (Sinop) - Universidade Federal de Mato Grosso (UFMT)
repository.mail.fl_str_mv ||rrmelo2@yahoo.com.br
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