Effect of water content and soil compaction in soybean production
Autor(a) principal: | |
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Data de Publicação: | 2003 |
Outros Autores: | |
Tipo de documento: | Artigo |
Idioma: | por |
Título da fonte: | Pesquisa Agropecuária Brasileira (Online) |
Texto Completo: | https://seer.sct.embrapa.br/index.php/pab/article/view/6645 |
Resumo: | Soil compaction has been limiting physical factor to plants growth. This work aimed to evaluate the production of soybean (Glycine max cv. EMBRAPA 48) as affected by water content and soil compaction. The experimental design was completely randomized, in a factorial scheme 4x2, i.e., four levels of resistance to penetration (between 0.27 and 4.32 MPa) and two levels of soil water retention (0.05 and 0.01 MPa). Samples of Red Latossol medium texture and Red Latossol clayey were collected in 0-20 cm depth, sieved in mesh of 0.4 cm and compacted in layers of 3 cm in pots of 20 cm height and 25 cm of diameter (9.82 L). The levels of resistance to penetration were determined with dynamometric ring penetrometer. The critical level of soil resistance to penetration, in relation to grains production, was 1.66 and 2.22 MPa, in Red Latossol medium texture, and 3.05 and 2.81 MPa, in Red Latossol clayey, for the water content in tension of 0.05 and 0.01 MPa, respectively. The higher grains production was obtained in tension of 0.01 MPa. Soybean production is affected by levels of soil resistance to penetration superior to 2 MPa in latossols under tension of 0.01 MPa. |
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Effect of water content and soil compaction in soybean productionEfeito do conteúdo de água e da compactação do solo na produção de sojaGlycine max; soil strength; soil moisture; soil density; soil managementGlycine max; resistência do solo; umidade do solo; densidade do solo; manejo do soloSoil compaction has been limiting physical factor to plants growth. This work aimed to evaluate the production of soybean (Glycine max cv. EMBRAPA 48) as affected by water content and soil compaction. The experimental design was completely randomized, in a factorial scheme 4x2, i.e., four levels of resistance to penetration (between 0.27 and 4.32 MPa) and two levels of soil water retention (0.05 and 0.01 MPa). Samples of Red Latossol medium texture and Red Latossol clayey were collected in 0-20 cm depth, sieved in mesh of 0.4 cm and compacted in layers of 3 cm in pots of 20 cm height and 25 cm of diameter (9.82 L). The levels of resistance to penetration were determined with dynamometric ring penetrometer. The critical level of soil resistance to penetration, in relation to grains production, was 1.66 and 2.22 MPa, in Red Latossol medium texture, and 3.05 and 2.81 MPa, in Red Latossol clayey, for the water content in tension of 0.05 and 0.01 MPa, respectively. The higher grains production was obtained in tension of 0.01 MPa. Soybean production is affected by levels of soil resistance to penetration superior to 2 MPa in latossols under tension of 0.01 MPa.A compactação do solo tem sido fator físico limitante ao crescimento das plantas. Este trabalho objetivou avaliar a produção de soja (Glycine max cv. EMBRAPA 48) em razão do conteúdo de água e da compactação do solo. Usou-se o delineamento inteiramente casualizado, em esquema fatorial 4x2, ou seja, quatro níveis de resistência à penetração (entre 0,27 e 4,32 MPa) e dois níveis de retenção de água pelo solo (0,05 e 0,01 MPa). Foram utilizadas amostras de Latossolo Vermelho textura média (LVd) e Latossolo Vermelho textura argilosa (LVef), coletadas na profundidade de 0-20 cm, passadas em peneira de 0,4 cm e compactadas em camadas de 3 cm, em vasos de 20 cm de altura e 25 cm de diâmetro (9,82 L). Os níveis de resistência à penetração foram determinados com o penetrômetro de anel dinamométrico. O nível crítico de resistência do solo à penetração, em relação à produção de grãos, foi de 1,66 e 2,22 MPa, no LVd, e 3,05 e 2,81 MPa, no LVef, para o conteúdo de água retida na tensão de 0,05 e 0,01 MPa, respectivamente. A maior produção de grãos foi obtida na tensão de 0,01 MPa. A produção de grãos de soja é afetada em níveis críticos de resistência do solo à penetração superiores a 2 MPa em latossolos com conteúdo de água retida na tensão de 0,01 MPa.Pesquisa Agropecuaria BrasileiraPesquisa Agropecuária BrasileiraBeutler, Amauri NelsonCenturion, José Frederico2003-07-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://seer.sct.embrapa.br/index.php/pab/article/view/6645Pesquisa Agropecuaria Brasileira; v.38, n.7, jul. 2003; 849-856Pesquisa Agropecuária Brasileira; v.38, n.7, jul. 2003; 849-8561678-39210100-104xreponame:Pesquisa Agropecuária Brasileira (Online)instname:Empresa Brasileira de Pesquisa Agropecuária (Embrapa)instacron:EMBRAPAporhttps://seer.sct.embrapa.br/index.php/pab/article/view/6645/3702info:eu-repo/semantics/openAccess2014-08-11T19:19:22Zoai:ojs.seer.sct.embrapa.br:article/6645Revistahttp://seer.sct.embrapa.br/index.php/pabPRIhttps://old.scielo.br/oai/scielo-oai.phppab@sct.embrapa.br || sct.pab@embrapa.br1678-39210100-204Xopendoar:2014-08-11T19:19:22Pesquisa Agropecuária Brasileira (Online) - Empresa Brasileira de Pesquisa Agropecuária (Embrapa)false |
dc.title.none.fl_str_mv |
Effect of water content and soil compaction in soybean production Efeito do conteúdo de água e da compactação do solo na produção de soja |
title |
Effect of water content and soil compaction in soybean production |
spellingShingle |
Effect of water content and soil compaction in soybean production Beutler, Amauri Nelson Glycine max; soil strength; soil moisture; soil density; soil management Glycine max; resistência do solo; umidade do solo; densidade do solo; manejo do solo |
title_short |
Effect of water content and soil compaction in soybean production |
title_full |
Effect of water content and soil compaction in soybean production |
title_fullStr |
Effect of water content and soil compaction in soybean production |
title_full_unstemmed |
Effect of water content and soil compaction in soybean production |
title_sort |
Effect of water content and soil compaction in soybean production |
author |
Beutler, Amauri Nelson |
author_facet |
Beutler, Amauri Nelson Centurion, José Frederico |
author_role |
author |
author2 |
Centurion, José Frederico |
author2_role |
author |
dc.contributor.none.fl_str_mv |
|
dc.contributor.author.fl_str_mv |
Beutler, Amauri Nelson Centurion, José Frederico |
dc.subject.por.fl_str_mv |
Glycine max; soil strength; soil moisture; soil density; soil management Glycine max; resistência do solo; umidade do solo; densidade do solo; manejo do solo |
topic |
Glycine max; soil strength; soil moisture; soil density; soil management Glycine max; resistência do solo; umidade do solo; densidade do solo; manejo do solo |
description |
Soil compaction has been limiting physical factor to plants growth. This work aimed to evaluate the production of soybean (Glycine max cv. EMBRAPA 48) as affected by water content and soil compaction. The experimental design was completely randomized, in a factorial scheme 4x2, i.e., four levels of resistance to penetration (between 0.27 and 4.32 MPa) and two levels of soil water retention (0.05 and 0.01 MPa). Samples of Red Latossol medium texture and Red Latossol clayey were collected in 0-20 cm depth, sieved in mesh of 0.4 cm and compacted in layers of 3 cm in pots of 20 cm height and 25 cm of diameter (9.82 L). The levels of resistance to penetration were determined with dynamometric ring penetrometer. The critical level of soil resistance to penetration, in relation to grains production, was 1.66 and 2.22 MPa, in Red Latossol medium texture, and 3.05 and 2.81 MPa, in Red Latossol clayey, for the water content in tension of 0.05 and 0.01 MPa, respectively. The higher grains production was obtained in tension of 0.01 MPa. Soybean production is affected by levels of soil resistance to penetration superior to 2 MPa in latossols under tension of 0.01 MPa. |
publishDate |
2003 |
dc.date.none.fl_str_mv |
2003-07-01 |
dc.type.none.fl_str_mv |
|
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://seer.sct.embrapa.br/index.php/pab/article/view/6645 |
url |
https://seer.sct.embrapa.br/index.php/pab/article/view/6645 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
https://seer.sct.embrapa.br/index.php/pab/article/view/6645/3702 |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Pesquisa Agropecuaria Brasileira Pesquisa Agropecuária Brasileira |
publisher.none.fl_str_mv |
Pesquisa Agropecuaria Brasileira Pesquisa Agropecuária Brasileira |
dc.source.none.fl_str_mv |
Pesquisa Agropecuaria Brasileira; v.38, n.7, jul. 2003; 849-856 Pesquisa Agropecuária Brasileira; v.38, n.7, jul. 2003; 849-856 1678-3921 0100-104x reponame:Pesquisa Agropecuária Brasileira (Online) instname:Empresa Brasileira de Pesquisa Agropecuária (Embrapa) instacron:EMBRAPA |
instname_str |
Empresa Brasileira de Pesquisa Agropecuária (Embrapa) |
instacron_str |
EMBRAPA |
institution |
EMBRAPA |
reponame_str |
Pesquisa Agropecuária Brasileira (Online) |
collection |
Pesquisa Agropecuária Brasileira (Online) |
repository.name.fl_str_mv |
Pesquisa Agropecuária Brasileira (Online) - Empresa Brasileira de Pesquisa Agropecuária (Embrapa) |
repository.mail.fl_str_mv |
pab@sct.embrapa.br || sct.pab@embrapa.br |
_version_ |
1793416711258505216 |