Critical Limits for Soybean and Black Bean Root Growth, Based on Macroporosity and Penetrability, for Soils with Distinct Texture and Management Systems

Detalhes bibliográficos
Autor(a) principal: Suzuki, Luis Eduardo Akiyoshi Sanches
Data de Publicação: 2022
Outros Autores: Reinert, Dalvan José, Alves, Marlene Cristina [UNESP], Reichert, José Miguel
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UNESP
Texto Completo: http://dx.doi.org/10.3390/su14052958
http://hdl.handle.net/11449/234259
Resumo: Soil compaction is a worldwide problem in agricultural areas, and it is important to define soil properties and reference values that allow knowledge of the compaction level for decision making. The objective of this study was to define the critical values of physical properties associated with the compaction of soils. Three Ultisols and two Oxisols, under different management systems, were collected at different depths for an evaluation of particle size, volumetric moisture, bulk density, and porosity. In the field, soil resistance to penetration and the root length of the soybean and edible black bean crop were measured. The soil profiles presented horizontal layers with similar resistance, but in some cases, there is discontinuity of these layers, which allows the roots to use the zones of lower resistance to deepen in the profile. The values of bulk density and resistance to penetration critical to soybean and edible black bean (only in sandy loam soil) root growth, according to soil textural class, are: sandy loam = 1.66 Mg m−3 and 1.5 to 2 MPa; loam and clay loam = 1.52 Mg m−3 and 1 to 1.5 MPa; silty clay loam and silty clay = 1.32 Mg m−3 and 1.5 to 2 MPa; and clay = 1.33 to 1.36 Mg m−3 and 2 to 3.5 MPa.
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spelling Critical Limits for Soybean and Black Bean Root Growth, Based on Macroporosity and Penetrability, for Soils with Distinct Texture and Management SystemsChiselingCritical bulk densityCritical macroporosityNo-tillageProfile of soil resistance to penetrationSoil compactionSoil managementSoil compaction is a worldwide problem in agricultural areas, and it is important to define soil properties and reference values that allow knowledge of the compaction level for decision making. The objective of this study was to define the critical values of physical properties associated with the compaction of soils. Three Ultisols and two Oxisols, under different management systems, were collected at different depths for an evaluation of particle size, volumetric moisture, bulk density, and porosity. In the field, soil resistance to penetration and the root length of the soybean and edible black bean crop were measured. The soil profiles presented horizontal layers with similar resistance, but in some cases, there is discontinuity of these layers, which allows the roots to use the zones of lower resistance to deepen in the profile. The values of bulk density and resistance to penetration critical to soybean and edible black bean (only in sandy loam soil) root growth, according to soil textural class, are: sandy loam = 1.66 Mg m−3 and 1.5 to 2 MPa; loam and clay loam = 1.52 Mg m−3 and 1 to 1.5 MPa; silty clay loam and silty clay = 1.32 Mg m−3 and 1.5 to 2 MPa; and clay = 1.33 to 1.36 Mg m−3 and 2 to 3.5 MPa.Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)Center of Technology Development Federal University of Pelotas, Rio Grande do Sul StateSoils Department Federal University of Santa Maria (Universidade Federal de Santa Maria—UFSM), Rio Grande do Sul StateFaculty of Engineering São Paulo State University, São Paulo StateFaculty of Engineering São Paulo State University, São Paulo StateFederal University of PelotasUniversidade Federal de Sergipe (UFS)Universidade Estadual Paulista (UNESP)Suzuki, Luis Eduardo Akiyoshi SanchesReinert, Dalvan JoséAlves, Marlene Cristina [UNESP]Reichert, José Miguel2022-05-01T15:13:41Z2022-05-01T15:13:41Z2022-03-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://dx.doi.org/10.3390/su14052958Sustainability (Switzerland), v. 14, n. 5, 2022.2071-1050http://hdl.handle.net/11449/23425910.3390/su140529582-s2.0-85126349973Scopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengSustainability (Switzerland)info:eu-repo/semantics/openAccess2024-07-05T18:12:56Zoai:repositorio.unesp.br:11449/234259Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462024-08-05T16:52:04.050489Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false
dc.title.none.fl_str_mv Critical Limits for Soybean and Black Bean Root Growth, Based on Macroporosity and Penetrability, for Soils with Distinct Texture and Management Systems
title Critical Limits for Soybean and Black Bean Root Growth, Based on Macroporosity and Penetrability, for Soils with Distinct Texture and Management Systems
spellingShingle Critical Limits for Soybean and Black Bean Root Growth, Based on Macroporosity and Penetrability, for Soils with Distinct Texture and Management Systems
Suzuki, Luis Eduardo Akiyoshi Sanches
Chiseling
Critical bulk density
Critical macroporosity
No-tillage
Profile of soil resistance to penetration
Soil compaction
Soil management
title_short Critical Limits for Soybean and Black Bean Root Growth, Based on Macroporosity and Penetrability, for Soils with Distinct Texture and Management Systems
title_full Critical Limits for Soybean and Black Bean Root Growth, Based on Macroporosity and Penetrability, for Soils with Distinct Texture and Management Systems
title_fullStr Critical Limits for Soybean and Black Bean Root Growth, Based on Macroporosity and Penetrability, for Soils with Distinct Texture and Management Systems
title_full_unstemmed Critical Limits for Soybean and Black Bean Root Growth, Based on Macroporosity and Penetrability, for Soils with Distinct Texture and Management Systems
title_sort Critical Limits for Soybean and Black Bean Root Growth, Based on Macroporosity and Penetrability, for Soils with Distinct Texture and Management Systems
author Suzuki, Luis Eduardo Akiyoshi Sanches
author_facet Suzuki, Luis Eduardo Akiyoshi Sanches
Reinert, Dalvan José
Alves, Marlene Cristina [UNESP]
Reichert, José Miguel
author_role author
author2 Reinert, Dalvan José
Alves, Marlene Cristina [UNESP]
Reichert, José Miguel
author2_role author
author
author
dc.contributor.none.fl_str_mv Federal University of Pelotas
Universidade Federal de Sergipe (UFS)
Universidade Estadual Paulista (UNESP)
dc.contributor.author.fl_str_mv Suzuki, Luis Eduardo Akiyoshi Sanches
Reinert, Dalvan José
Alves, Marlene Cristina [UNESP]
Reichert, José Miguel
dc.subject.por.fl_str_mv Chiseling
Critical bulk density
Critical macroporosity
No-tillage
Profile of soil resistance to penetration
Soil compaction
Soil management
topic Chiseling
Critical bulk density
Critical macroporosity
No-tillage
Profile of soil resistance to penetration
Soil compaction
Soil management
description Soil compaction is a worldwide problem in agricultural areas, and it is important to define soil properties and reference values that allow knowledge of the compaction level for decision making. The objective of this study was to define the critical values of physical properties associated with the compaction of soils. Three Ultisols and two Oxisols, under different management systems, were collected at different depths for an evaluation of particle size, volumetric moisture, bulk density, and porosity. In the field, soil resistance to penetration and the root length of the soybean and edible black bean crop were measured. The soil profiles presented horizontal layers with similar resistance, but in some cases, there is discontinuity of these layers, which allows the roots to use the zones of lower resistance to deepen in the profile. The values of bulk density and resistance to penetration critical to soybean and edible black bean (only in sandy loam soil) root growth, according to soil textural class, are: sandy loam = 1.66 Mg m−3 and 1.5 to 2 MPa; loam and clay loam = 1.52 Mg m−3 and 1 to 1.5 MPa; silty clay loam and silty clay = 1.32 Mg m−3 and 1.5 to 2 MPa; and clay = 1.33 to 1.36 Mg m−3 and 2 to 3.5 MPa.
publishDate 2022
dc.date.none.fl_str_mv 2022-05-01T15:13:41Z
2022-05-01T15:13:41Z
2022-03-01
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://dx.doi.org/10.3390/su14052958
Sustainability (Switzerland), v. 14, n. 5, 2022.
2071-1050
http://hdl.handle.net/11449/234259
10.3390/su14052958
2-s2.0-85126349973
url http://dx.doi.org/10.3390/su14052958
http://hdl.handle.net/11449/234259
identifier_str_mv Sustainability (Switzerland), v. 14, n. 5, 2022.
2071-1050
10.3390/su14052958
2-s2.0-85126349973
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv Sustainability (Switzerland)
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.source.none.fl_str_mv Scopus
reponame:Repositório Institucional da UNESP
instname:Universidade Estadual Paulista (UNESP)
instacron:UNESP
instname_str Universidade Estadual Paulista (UNESP)
instacron_str UNESP
institution UNESP
reponame_str Repositório Institucional da UNESP
collection Repositório Institucional da UNESP
repository.name.fl_str_mv Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)
repository.mail.fl_str_mv
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