Do Aggregate Size Classes of the Subsurface Soil Horizon Have Different Chemical/Mineralogical Properties?

Detalhes bibliográficos
Autor(a) principal: Mitton,Rolff Vladimir
Data de Publicação: 2019
Outros Autores: Melo,Vander Freitas, Pauletti,Volnei
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Revista Brasileira de Ciência do Solo (Online)
Texto Completo: http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832019000100401
Resumo: ABSTRACT Variations in chemical and mineralogical properties of a soil can occur at short vertical and horizontal distances. The objective of the present study was to evaluate the chemical and mineralogical soil properties of different aggregate classes from young (Ustrochrept) and highly weathered (Acrustox) soils from the state of Paraná, Brazil. Undisturbed blocks (0.20 ×0.20 ×0.20 m) of soils were separated into aggregate classes: Acrustox – 8.0-4.0 mm; 4-2 mm; 2.0-0.5 mm; 0.5-0.2 mm; and <0.2 mm; and Ustrochrept – 8.0-4.0 mm; 4.0-2.0 mm; 2.0-0.5 mm; and 0.5-0.2 mm. The exchangeable K contents showed an opposite behavior for the two soils: higher contents in the Acrustox for the larger aggregate classes and higher contents in the Ustrochrept for the smaller aggregate classes. The crystallographic characteristics of hematite and goethite were variable according to the aggregate class. The goethite in the 2-4-mm aggregate class is expected to exhibit the highest reactivity for the Ustrochrept: lower growth and a more elongated form of the crystals. The smallest aggregate class presented the lowest contents of kaolinite and gibbsite in the clay fraction. Gibbsite and kaolinite in the intermediate classes presented higher growth in both soils. The studied soils present different side-by-side environments (aggregate classes) for the exploration by the root system. This means that for the precise identification of the environments explored by the roots of a single plant, field sampling should consider the aggregate class, obtained from an undisturbed soil sample. However, this is impractical in agricultural practice.
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spelling Do Aggregate Size Classes of the Subsurface Soil Horizon Have Different Chemical/Mineralogical Properties?kaolinitehematitegoethitegibbsiteK reserveABSTRACT Variations in chemical and mineralogical properties of a soil can occur at short vertical and horizontal distances. The objective of the present study was to evaluate the chemical and mineralogical soil properties of different aggregate classes from young (Ustrochrept) and highly weathered (Acrustox) soils from the state of Paraná, Brazil. Undisturbed blocks (0.20 ×0.20 ×0.20 m) of soils were separated into aggregate classes: Acrustox – 8.0-4.0 mm; 4-2 mm; 2.0-0.5 mm; 0.5-0.2 mm; and <0.2 mm; and Ustrochrept – 8.0-4.0 mm; 4.0-2.0 mm; 2.0-0.5 mm; and 0.5-0.2 mm. The exchangeable K contents showed an opposite behavior for the two soils: higher contents in the Acrustox for the larger aggregate classes and higher contents in the Ustrochrept for the smaller aggregate classes. The crystallographic characteristics of hematite and goethite were variable according to the aggregate class. The goethite in the 2-4-mm aggregate class is expected to exhibit the highest reactivity for the Ustrochrept: lower growth and a more elongated form of the crystals. The smallest aggregate class presented the lowest contents of kaolinite and gibbsite in the clay fraction. Gibbsite and kaolinite in the intermediate classes presented higher growth in both soils. The studied soils present different side-by-side environments (aggregate classes) for the exploration by the root system. This means that for the precise identification of the environments explored by the roots of a single plant, field sampling should consider the aggregate class, obtained from an undisturbed soil sample. However, this is impractical in agricultural practice.Sociedade Brasileira de Ciência do Solo2019-01-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832019000100401Revista Brasileira de Ciência do Solo v.43 2019reponame:Revista Brasileira de Ciência do Solo (Online)instname:Sociedade Brasileira de Ciência do Solo (SBCS)instacron:SBCS10.1590/18069657rbcs20180041info:eu-repo/semantics/openAccessMitton,Rolff VladimirMelo,Vander FreitasPauletti,Volneieng2019-08-13T00:00:00Zoai:scielo:S0100-06832019000100401Revistahttp://www.scielo.br/scielo.php?script=sci_serial&pid=0100-0683&lng=es&nrm=isohttps://old.scielo.br/oai/scielo-oai.php||sbcs@ufv.br1806-96570100-0683opendoar:2019-08-13T00:00Revista Brasileira de Ciência do Solo (Online) - Sociedade Brasileira de Ciência do Solo (SBCS)false
dc.title.none.fl_str_mv Do Aggregate Size Classes of the Subsurface Soil Horizon Have Different Chemical/Mineralogical Properties?
title Do Aggregate Size Classes of the Subsurface Soil Horizon Have Different Chemical/Mineralogical Properties?
spellingShingle Do Aggregate Size Classes of the Subsurface Soil Horizon Have Different Chemical/Mineralogical Properties?
Mitton,Rolff Vladimir
kaolinite
hematite
goethite
gibbsite
K reserve
title_short Do Aggregate Size Classes of the Subsurface Soil Horizon Have Different Chemical/Mineralogical Properties?
title_full Do Aggregate Size Classes of the Subsurface Soil Horizon Have Different Chemical/Mineralogical Properties?
title_fullStr Do Aggregate Size Classes of the Subsurface Soil Horizon Have Different Chemical/Mineralogical Properties?
title_full_unstemmed Do Aggregate Size Classes of the Subsurface Soil Horizon Have Different Chemical/Mineralogical Properties?
title_sort Do Aggregate Size Classes of the Subsurface Soil Horizon Have Different Chemical/Mineralogical Properties?
author Mitton,Rolff Vladimir
author_facet Mitton,Rolff Vladimir
Melo,Vander Freitas
Pauletti,Volnei
author_role author
author2 Melo,Vander Freitas
Pauletti,Volnei
author2_role author
author
dc.contributor.author.fl_str_mv Mitton,Rolff Vladimir
Melo,Vander Freitas
Pauletti,Volnei
dc.subject.por.fl_str_mv kaolinite
hematite
goethite
gibbsite
K reserve
topic kaolinite
hematite
goethite
gibbsite
K reserve
description ABSTRACT Variations in chemical and mineralogical properties of a soil can occur at short vertical and horizontal distances. The objective of the present study was to evaluate the chemical and mineralogical soil properties of different aggregate classes from young (Ustrochrept) and highly weathered (Acrustox) soils from the state of Paraná, Brazil. Undisturbed blocks (0.20 ×0.20 ×0.20 m) of soils were separated into aggregate classes: Acrustox – 8.0-4.0 mm; 4-2 mm; 2.0-0.5 mm; 0.5-0.2 mm; and <0.2 mm; and Ustrochrept – 8.0-4.0 mm; 4.0-2.0 mm; 2.0-0.5 mm; and 0.5-0.2 mm. The exchangeable K contents showed an opposite behavior for the two soils: higher contents in the Acrustox for the larger aggregate classes and higher contents in the Ustrochrept for the smaller aggregate classes. The crystallographic characteristics of hematite and goethite were variable according to the aggregate class. The goethite in the 2-4-mm aggregate class is expected to exhibit the highest reactivity for the Ustrochrept: lower growth and a more elongated form of the crystals. The smallest aggregate class presented the lowest contents of kaolinite and gibbsite in the clay fraction. Gibbsite and kaolinite in the intermediate classes presented higher growth in both soils. The studied soils present different side-by-side environments (aggregate classes) for the exploration by the root system. This means that for the precise identification of the environments explored by the roots of a single plant, field sampling should consider the aggregate class, obtained from an undisturbed soil sample. However, this is impractical in agricultural practice.
publishDate 2019
dc.date.none.fl_str_mv 2019-01-01
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
format article
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dc.identifier.uri.fl_str_mv http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832019000100401
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832019000100401
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 10.1590/18069657rbcs20180041
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv text/html
dc.publisher.none.fl_str_mv Sociedade Brasileira de Ciência do Solo
publisher.none.fl_str_mv Sociedade Brasileira de Ciência do Solo
dc.source.none.fl_str_mv Revista Brasileira de Ciência do Solo v.43 2019
reponame:Revista Brasileira de Ciência do Solo (Online)
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instname_str Sociedade Brasileira de Ciência do Solo (SBCS)
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reponame_str Revista Brasileira de Ciência do Solo (Online)
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repository.name.fl_str_mv Revista Brasileira de Ciência do Solo (Online) - Sociedade Brasileira de Ciência do Solo (SBCS)
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