Structural changes in latosols of the cerrado region: I - relationships between soil physical properties and least limiting water range
Autor(a) principal: | |
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Data de Publicação: | 2011 |
Outros Autores: | , , , , |
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=S0100-06832011000300013 |
Resumo: | The agricultural potential of Latosols of the Brazilian Cerrado region is high, but when intensively cultivated under inappropriate management systems, the porosity can be seriously reduced, leading to rapid soil degradation. Consequently, accelerated erosion and sedimentation of springs and creeks have been observed. Therefore, the objective of this study was to evaluate structural changes of Latosols in Rio Verde, Goiás, based on the Least Limiting Water Range (LLWR), and relationships between LLWR and other physical properties. Soil samples were collected from the B horizons of five oxidic Latosols representing the textural variability of the Latosols of the Cerrado biome. LLWR and other soil physical properties were determined at various soil compaction degrees induced by uniaxial compression. Soil compaction caused effects varying from enhanced plant growth due to higher water retention, to severe restriction of edaphic functions. Also, inverse relationships were observed between clay content and bulk density values (Bd) under different structural conditions. Bd values corresponding to critical soil macroporosity (BdcMAC) were more restrictive to a sustainable use of the studied Latosols than the critical Bd corresponding to LLWR (BdcLLWR). The high tolerable compression potential of these oxidic Latosols was related to the high aeration porosity associated to the granular structure. |
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Structural changes in latosols of the cerrado region: I - relationships between soil physical properties and least limiting water rangesoil compactiondegradation of agricultural soilssoil penetration resistancewater availabilitysoil textureThe agricultural potential of Latosols of the Brazilian Cerrado region is high, but when intensively cultivated under inappropriate management systems, the porosity can be seriously reduced, leading to rapid soil degradation. Consequently, accelerated erosion and sedimentation of springs and creeks have been observed. Therefore, the objective of this study was to evaluate structural changes of Latosols in Rio Verde, Goiás, based on the Least Limiting Water Range (LLWR), and relationships between LLWR and other physical properties. Soil samples were collected from the B horizons of five oxidic Latosols representing the textural variability of the Latosols of the Cerrado biome. LLWR and other soil physical properties were determined at various soil compaction degrees induced by uniaxial compression. Soil compaction caused effects varying from enhanced plant growth due to higher water retention, to severe restriction of edaphic functions. Also, inverse relationships were observed between clay content and bulk density values (Bd) under different structural conditions. Bd values corresponding to critical soil macroporosity (BdcMAC) were more restrictive to a sustainable use of the studied Latosols than the critical Bd corresponding to LLWR (BdcLLWR). The high tolerable compression potential of these oxidic Latosols was related to the high aeration porosity associated to the granular structure.Sociedade Brasileira de Ciência do Solo2011-06-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832011000300013Revista Brasileira de Ciência do Solo v.35 n.3 2011reponame:Revista Brasileira de Ciência do Solo (Online)instname:Sociedade Brasileira de Ciência do Solo (SBCS)instacron:SBCS10.1590/S0100-06832011000300013info:eu-repo/semantics/openAccessSeveriano,Eduardo da CostaOliveira,Geraldo César deDias Júnior,Moacir de SouzaCosta,Katia Aparecida de PinhoSilva,Fabiano GuimarãesFerreira Filho,Silvio Marcoseng2011-09-27T00:00:00Zoai:scielo:S0100-06832011000300013Revistahttp://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:2011-09-27T00:00Revista Brasileira de Ciência do Solo (Online) - Sociedade Brasileira de Ciência do Solo (SBCS)false |
dc.title.none.fl_str_mv |
Structural changes in latosols of the cerrado region: I - relationships between soil physical properties and least limiting water range |
title |
Structural changes in latosols of the cerrado region: I - relationships between soil physical properties and least limiting water range |
spellingShingle |
Structural changes in latosols of the cerrado region: I - relationships between soil physical properties and least limiting water range Severiano,Eduardo da Costa soil compaction degradation of agricultural soils soil penetration resistance water availability soil texture |
title_short |
Structural changes in latosols of the cerrado region: I - relationships between soil physical properties and least limiting water range |
title_full |
Structural changes in latosols of the cerrado region: I - relationships between soil physical properties and least limiting water range |
title_fullStr |
Structural changes in latosols of the cerrado region: I - relationships between soil physical properties and least limiting water range |
title_full_unstemmed |
Structural changes in latosols of the cerrado region: I - relationships between soil physical properties and least limiting water range |
title_sort |
Structural changes in latosols of the cerrado region: I - relationships between soil physical properties and least limiting water range |
author |
Severiano,Eduardo da Costa |
author_facet |
Severiano,Eduardo da Costa Oliveira,Geraldo César de Dias Júnior,Moacir de Souza Costa,Katia Aparecida de Pinho Silva,Fabiano Guimarães Ferreira Filho,Silvio Marcos |
author_role |
author |
author2 |
Oliveira,Geraldo César de Dias Júnior,Moacir de Souza Costa,Katia Aparecida de Pinho Silva,Fabiano Guimarães Ferreira Filho,Silvio Marcos |
author2_role |
author author author author author |
dc.contributor.author.fl_str_mv |
Severiano,Eduardo da Costa Oliveira,Geraldo César de Dias Júnior,Moacir de Souza Costa,Katia Aparecida de Pinho Silva,Fabiano Guimarães Ferreira Filho,Silvio Marcos |
dc.subject.por.fl_str_mv |
soil compaction degradation of agricultural soils soil penetration resistance water availability soil texture |
topic |
soil compaction degradation of agricultural soils soil penetration resistance water availability soil texture |
description |
The agricultural potential of Latosols of the Brazilian Cerrado region is high, but when intensively cultivated under inappropriate management systems, the porosity can be seriously reduced, leading to rapid soil degradation. Consequently, accelerated erosion and sedimentation of springs and creeks have been observed. Therefore, the objective of this study was to evaluate structural changes of Latosols in Rio Verde, Goiás, based on the Least Limiting Water Range (LLWR), and relationships between LLWR and other physical properties. Soil samples were collected from the B horizons of five oxidic Latosols representing the textural variability of the Latosols of the Cerrado biome. LLWR and other soil physical properties were determined at various soil compaction degrees induced by uniaxial compression. Soil compaction caused effects varying from enhanced plant growth due to higher water retention, to severe restriction of edaphic functions. Also, inverse relationships were observed between clay content and bulk density values (Bd) under different structural conditions. Bd values corresponding to critical soil macroporosity (BdcMAC) were more restrictive to a sustainable use of the studied Latosols than the critical Bd corresponding to LLWR (BdcLLWR). The high tolerable compression potential of these oxidic Latosols was related to the high aeration porosity associated to the granular structure. |
publishDate |
2011 |
dc.date.none.fl_str_mv |
2011-06-01 |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832011000300013 |
url |
http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832011000300013 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
10.1590/S0100-06832011000300013 |
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.35 n.3 2011 reponame:Revista Brasileira de Ciência do Solo (Online) instname:Sociedade Brasileira de Ciência do Solo (SBCS) instacron:SBCS |
instname_str |
Sociedade Brasileira de Ciência do Solo (SBCS) |
instacron_str |
SBCS |
institution |
SBCS |
reponame_str |
Revista Brasileira de Ciência do Solo (Online) |
collection |
Revista Brasileira de Ciência do Solo (Online) |
repository.name.fl_str_mv |
Revista Brasileira de Ciência do Solo (Online) - Sociedade Brasileira de Ciência do Solo (SBCS) |
repository.mail.fl_str_mv |
||sbcs@ufv.br |
_version_ |
1752126517040644096 |