Least limiting water range in soil under crop rotations and chiseling

Detalhes bibliográficos
Autor(a) principal: Calonego, Juliano Carlos [UNESP]
Data de Publicação: 2011
Outros Autores: Rosolem, Ciro Antonio [UNESP]
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UNESP
Texto Completo: http://dx.doi.org/10.1590/S0100-06832011000300012
http://hdl.handle.net/11449/5522
Resumo: Soil water availability to plants is affected by soil compaction and other variables. The Least Limiting Water Range (LLWR) comprises soil physical variables affecting root growth and soil water availability, and can be managed by either mechanical or biological methods. There is evidence that effects of crop rotations could last longer than chiseling, so the objective of this study was to assess the effect of soil chiseling or growing cover crops under no-till (NT) on the LLWR. Crop rotations involving triticale (X Triticosecale) and sunflower (Helianthus annuus) in the fall-winter associated with millet (Pennisetum glaucum), sorghum (Sorghum bicolor) and sunn hemp (Crotalariajuncea) as cover crops preceding soybean (Glycine max) were repeated for three consecutive years. In the treatment with chiseling (performed. only in the first year), the area was left fallow between the fall-winter and summer crops. The experiment was carried out in Botucatu, São Paulo State, Brazil, from 2003 to 2006 on a Typic Rhodudalf. The LLWR was determined in soil samples taken from the layers 0-20 cm and 20-40 cm, after chemical desiccation of the cover crops in December of the first and third year of the experiment. Chiseling decreases soil bulk density in the 0-20 cm soil layer, increasing the LLWR magnitude by lowering the soil water content at which penetration resistance reaches 2.0 MPa; this effect is present up to the third year after chiseling and can reach to a depth of 0.40 in. Crop rotations involving sunflower + sunn hemp, triticale + millet and triticale + sunn hemp for three years prevented soil bulk density from exceeding the critical soil bulk density in the 0-0.20 in layer. This effect was observed to a depth of 0.40 m after three years of chiseling under crop rotations involving forage sorghum. Hence, chiseling and some crop rotations under no tillage are effective in increasing soil quality assessed by the LLWR.
id UNSP_fd1f92be09017aff6310fd92ca519ed8
oai_identifier_str oai:repositorio.unesp.br:11449/5522
network_acronym_str UNSP
network_name_str Repositório Institucional da UNESP
repository_id_str 2946
spelling Least limiting water range in soil under crop rotations and chiselingIntervalo hídrico ótimo em solo sob rotação de culturas e escarificaçãocover cropscrop rotationsoil compactionno tillsoil waterSoil water availability to plants is affected by soil compaction and other variables. The Least Limiting Water Range (LLWR) comprises soil physical variables affecting root growth and soil water availability, and can be managed by either mechanical or biological methods. There is evidence that effects of crop rotations could last longer than chiseling, so the objective of this study was to assess the effect of soil chiseling or growing cover crops under no-till (NT) on the LLWR. Crop rotations involving triticale (X Triticosecale) and sunflower (Helianthus annuus) in the fall-winter associated with millet (Pennisetum glaucum), sorghum (Sorghum bicolor) and sunn hemp (Crotalariajuncea) as cover crops preceding soybean (Glycine max) were repeated for three consecutive years. In the treatment with chiseling (performed. only in the first year), the area was left fallow between the fall-winter and summer crops. The experiment was carried out in Botucatu, São Paulo State, Brazil, from 2003 to 2006 on a Typic Rhodudalf. The LLWR was determined in soil samples taken from the layers 0-20 cm and 20-40 cm, after chemical desiccation of the cover crops in December of the first and third year of the experiment. Chiseling decreases soil bulk density in the 0-20 cm soil layer, increasing the LLWR magnitude by lowering the soil water content at which penetration resistance reaches 2.0 MPa; this effect is present up to the third year after chiseling and can reach to a depth of 0.40 in. Crop rotations involving sunflower + sunn hemp, triticale + millet and triticale + sunn hemp for three years prevented soil bulk density from exceeding the critical soil bulk density in the 0-0.20 in layer. This effect was observed to a depth of 0.40 m after three years of chiseling under crop rotations involving forage sorghum. Hence, chiseling and some crop rotations under no tillage are effective in increasing soil quality assessed by the LLWR.A disponibilidade de água às plantas é alterada pela compactação do solo e outras variáveis. O Intervalo Hídrico Ótimo (IHO) integra variáveis físicas do solo que alteram o crescimento radicular e a disponibilidade de água e pode ser manejado por métodos mecânicos ou biológicos. Há evidências de que os efeitos da rotação de culturas são mais duradouros que os da escarificação. O objetivo deste trabalho foi avaliar o efeito da escarificação e, ou, rotação de culturas em sistema de semeadura direta (SSD) no IHO. Rotações envolvendo triticale (X Triticosecale) e girassol (Helianthus annuus) no outono-inverno e milheto (Pennisetum glaucum), sorgo (Sorghum bicolor) e crotalária (Crotalaria juncea) com plantas de cobertura precedendo a soja (Glycine max) foram repetidas por três anos. No tratamento com escarificação, a área foi deixada em pousio entre as culturas de outono-inverno e verão. O experimento foi conduzido em Botucatu, São Paulo, Brasil, de 2003 a 2006 em um Nitossolo Vermelho. O IHO foi determinado em amostras de solo das profundidades de 0-20 e 20-40 cm, logo após a dessecação química das plantas de cobertura, em dezembro do primeiro e do terceiro ano do experimento. A escarificação diminui a densidade do solo na camada de 0-20 cm, aumentando o IHO por meio da redução da umidade do solo em que a resistência à penetração atinge 2,0 MPa; esse efeito mantém-se até o terceiro ano após a escarificação, podendo chegar a até 40 cm de profundidade. As rotações de culturas envolvendo girassol + crotalária, triticale + milheto e triticale + crotalária por três anos ajudaram a prevenir o aumento na densidade do solo acima do valor crítico na camada de 0-20 cm. Esse efeito é observado na camada de 20- 40 cm após três anos da escarificação e com rotações de culturas envolvendo sorgo. Assim, a escarificação e algumas rotações de culturas em sistema de semeadura direta são eficientes em melhorar a qualidade do solo avaliada pelo IHO.Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)São Paulo State Univ, Coll Agr Sci, Dept Crop Sci, Botucatu, SP, BrazilUniv Oeste Paulista, Ctr Agr Sci, BR-19067175 Presidente Prudente, SP, BrazilSão Paulo State Univ, Coll Agr Sci, Dept Crop Sci, Botucatu, SP, BrazilSociedade Brasileira de Ciência do SoloUniversidade Estadual Paulista (Unesp)Universidade do Oeste Paulista (UNOESTE)Calonego, Juliano Carlos [UNESP]Rosolem, Ciro Antonio [UNESP]2014-05-20T13:20:09Z2014-05-20T13:20:09Z2011-05-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/article759-771application/pdfhttp://dx.doi.org/10.1590/S0100-06832011000300012Revista Brasileira de Ciência do Solo. Vicosa: Soc Brasileira de Ciência do Solo, v. 35, n. 3, p. 759-771, 2011.0100-0683http://hdl.handle.net/11449/5522S0100-06832011000300012WOS:000293039600012S0100-06832011000300012-en.pdf57207758732595280000-0003-2001-0874Web of Sciencereponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengRevista Brasileira de Ciência do Solo0.7990,679info:eu-repo/semantics/openAccess2024-04-30T15:57:56Zoai:repositorio.unesp.br:11449/5522Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462024-04-30T15:57:56Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false
dc.title.none.fl_str_mv Least limiting water range in soil under crop rotations and chiseling
Intervalo hídrico ótimo em solo sob rotação de culturas e escarificação
title Least limiting water range in soil under crop rotations and chiseling
spellingShingle Least limiting water range in soil under crop rotations and chiseling
Calonego, Juliano Carlos [UNESP]
cover crops
crop rotation
soil compaction
no till
soil water
title_short Least limiting water range in soil under crop rotations and chiseling
title_full Least limiting water range in soil under crop rotations and chiseling
title_fullStr Least limiting water range in soil under crop rotations and chiseling
title_full_unstemmed Least limiting water range in soil under crop rotations and chiseling
title_sort Least limiting water range in soil under crop rotations and chiseling
author Calonego, Juliano Carlos [UNESP]
author_facet Calonego, Juliano Carlos [UNESP]
Rosolem, Ciro Antonio [UNESP]
author_role author
author2 Rosolem, Ciro Antonio [UNESP]
author2_role author
dc.contributor.none.fl_str_mv Universidade Estadual Paulista (Unesp)
Universidade do Oeste Paulista (UNOESTE)
dc.contributor.author.fl_str_mv Calonego, Juliano Carlos [UNESP]
Rosolem, Ciro Antonio [UNESP]
dc.subject.por.fl_str_mv cover crops
crop rotation
soil compaction
no till
soil water
topic cover crops
crop rotation
soil compaction
no till
soil water
description Soil water availability to plants is affected by soil compaction and other variables. The Least Limiting Water Range (LLWR) comprises soil physical variables affecting root growth and soil water availability, and can be managed by either mechanical or biological methods. There is evidence that effects of crop rotations could last longer than chiseling, so the objective of this study was to assess the effect of soil chiseling or growing cover crops under no-till (NT) on the LLWR. Crop rotations involving triticale (X Triticosecale) and sunflower (Helianthus annuus) in the fall-winter associated with millet (Pennisetum glaucum), sorghum (Sorghum bicolor) and sunn hemp (Crotalariajuncea) as cover crops preceding soybean (Glycine max) were repeated for three consecutive years. In the treatment with chiseling (performed. only in the first year), the area was left fallow between the fall-winter and summer crops. The experiment was carried out in Botucatu, São Paulo State, Brazil, from 2003 to 2006 on a Typic Rhodudalf. The LLWR was determined in soil samples taken from the layers 0-20 cm and 20-40 cm, after chemical desiccation of the cover crops in December of the first and third year of the experiment. Chiseling decreases soil bulk density in the 0-20 cm soil layer, increasing the LLWR magnitude by lowering the soil water content at which penetration resistance reaches 2.0 MPa; this effect is present up to the third year after chiseling and can reach to a depth of 0.40 in. Crop rotations involving sunflower + sunn hemp, triticale + millet and triticale + sunn hemp for three years prevented soil bulk density from exceeding the critical soil bulk density in the 0-0.20 in layer. This effect was observed to a depth of 0.40 m after three years of chiseling under crop rotations involving forage sorghum. Hence, chiseling and some crop rotations under no tillage are effective in increasing soil quality assessed by the LLWR.
publishDate 2011
dc.date.none.fl_str_mv 2011-05-01
2014-05-20T13:20:09Z
2014-05-20T13:20:09Z
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/10.1590/S0100-06832011000300012
Revista Brasileira de Ciência do Solo. Vicosa: Soc Brasileira de Ciência do Solo, v. 35, n. 3, p. 759-771, 2011.
0100-0683
http://hdl.handle.net/11449/5522
S0100-06832011000300012
WOS:000293039600012
S0100-06832011000300012-en.pdf
5720775873259528
0000-0003-2001-0874
url http://dx.doi.org/10.1590/S0100-06832011000300012
http://hdl.handle.net/11449/5522
identifier_str_mv Revista Brasileira de Ciência do Solo. Vicosa: Soc Brasileira de Ciência do Solo, v. 35, n. 3, p. 759-771, 2011.
0100-0683
S0100-06832011000300012
WOS:000293039600012
S0100-06832011000300012-en.pdf
5720775873259528
0000-0003-2001-0874
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv Revista Brasileira de Ciência do Solo
0.799
0,679
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv 759-771
application/pdf
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 Web of Science
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
_version_ 1799965300297302016