Relationship between acidity and chemical properties of brazilian soils

In soils of tropical climate regions the high acidity and the presence of exchangeable aluminum (Al3+), associated to low fertility, are the main restrainting factors for agricultural production. A laboratory experiment was conducted using 26 soils of different Brazilian regions, to investigate soil acidity components, giving emphasis to Al and their relations with chemical properties. The pH correlated positively with P, Ca, Mg, K, BS, CEC and V% values, and negatively with Al saturation. The Al3+ was the predominant exchangeable cation in 32% of the soils with pH below 5.6. The KCl titratable H+ represents the hydroxi-Al(OH)x complex with low stability and the Wolf-Morgan extracted Al corresponds to the exchangeable + non-exchangeable Al species. The Al3+ and low stability hydroxi-Al decreased quickly with increasing pH up to 5.5. The non-exchangeable Al increased up to pH 4.5, then decreased to pH 5.5 and had a small increment from 7.0 to 7.5.

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Main Authors: Abreu Jr.,Cássio Hamilton, Muraoka,Takashi, Lavorante,André Fernando
Format: Digital revista
Language:English
Published: Escola Superior de Agricultura "Luiz de Queiroz" 2003
Online Access:http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0103-90162003000200019
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spelling oai:scielo:S0103-901620030002000192003-05-15Relationship between acidity and chemical properties of brazilian soilsAbreu Jr.,Cássio HamiltonMuraoka,TakashiLavorante,André Fernando total acidity exchangeable acidity pH aluminum in soil In soils of tropical climate regions the high acidity and the presence of exchangeable aluminum (Al3+), associated to low fertility, are the main restrainting factors for agricultural production. A laboratory experiment was conducted using 26 soils of different Brazilian regions, to investigate soil acidity components, giving emphasis to Al and their relations with chemical properties. The pH correlated positively with P, Ca, Mg, K, BS, CEC and V% values, and negatively with Al saturation. The Al3+ was the predominant exchangeable cation in 32% of the soils with pH below 5.6. The KCl titratable H+ represents the hydroxi-Al(OH)x complex with low stability and the Wolf-Morgan extracted Al corresponds to the exchangeable + non-exchangeable Al species. The Al3+ and low stability hydroxi-Al decreased quickly with increasing pH up to 5.5. The non-exchangeable Al increased up to pH 4.5, then decreased to pH 5.5 and had a small increment from 7.0 to 7.5.info:eu-repo/semantics/openAccessEscola Superior de Agricultura "Luiz de Queiroz"Scientia Agricola v.60 n.2 20032003-01-01info:eu-repo/semantics/articletext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0103-90162003000200019en10.1590/S0103-90162003000200019
institution SCIELO
collection OJS
country Brasil
countrycode BR
component Revista
access En linea
databasecode rev-scielo-br
tag revista
region America del Sur
libraryname SciELO
language English
format Digital
author Abreu Jr.,Cássio Hamilton
Muraoka,Takashi
Lavorante,André Fernando
spellingShingle Abreu Jr.,Cássio Hamilton
Muraoka,Takashi
Lavorante,André Fernando
Relationship between acidity and chemical properties of brazilian soils
author_facet Abreu Jr.,Cássio Hamilton
Muraoka,Takashi
Lavorante,André Fernando
author_sort Abreu Jr.,Cássio Hamilton
title Relationship between acidity and chemical properties of brazilian soils
title_short Relationship between acidity and chemical properties of brazilian soils
title_full Relationship between acidity and chemical properties of brazilian soils
title_fullStr Relationship between acidity and chemical properties of brazilian soils
title_full_unstemmed Relationship between acidity and chemical properties of brazilian soils
title_sort relationship between acidity and chemical properties of brazilian soils
description In soils of tropical climate regions the high acidity and the presence of exchangeable aluminum (Al3+), associated to low fertility, are the main restrainting factors for agricultural production. A laboratory experiment was conducted using 26 soils of different Brazilian regions, to investigate soil acidity components, giving emphasis to Al and their relations with chemical properties. The pH correlated positively with P, Ca, Mg, K, BS, CEC and V% values, and negatively with Al saturation. The Al3+ was the predominant exchangeable cation in 32% of the soils with pH below 5.6. The KCl titratable H+ represents the hydroxi-Al(OH)x complex with low stability and the Wolf-Morgan extracted Al corresponds to the exchangeable + non-exchangeable Al species. The Al3+ and low stability hydroxi-Al decreased quickly with increasing pH up to 5.5. The non-exchangeable Al increased up to pH 4.5, then decreased to pH 5.5 and had a small increment from 7.0 to 7.5.
publisher Escola Superior de Agricultura "Luiz de Queiroz"
publishDate 2003
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0103-90162003000200019
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