Effect of crops residues used as soil surface mulching to control water direct evaporation - DOI: 10.4025/actasciagron.v26i2.1882

Detalhes bibliográficos
Autor(a) principal: Freitas, Paulo Sergio Lourenço de
Data de Publicação: 2008
Outros Autores: Mantovani, Everardo C., Sediyama, Gilberto C., Costa, Luiz Claudio
Tipo de documento: Artigo
Idioma: por
Título da fonte: Acta Scientiarum. Agronomy (Online)
Texto Completo: http://www.periodicos.uem.br/ojs/index.php/ActaSciAgron/article/view/1882
Resumo: The influence of corn, bean and wheat crops residues used as soil surface mulching to control the water evaporation demands, for two soils textural classes, was analyzed in the present work. The treatments consisted of three layers of crop residues, corresponding to 0, 50 and 100% of dry matter produced by irrigated cropping systems, and three water evaporative demands of 3, 6 and 8mm d-1, for two soil textural classes, silty sand and heavy loamy soils, with 84% of sand and 76% of clay, respectively. The experiment was carried out in laboratory, with the soil sample conditioned in a 45-cm high and 20-cm nominal diameter PVC pipes columns. The water evaporation rate from the bare soil column presented different behavior for the three water evaporation demands tested. For water evaporative demand of approximately 3mm d-1, the treatments with corn and wheat crops residues, which represented mulching layer of 50 and 100% of dry matter, the water evaporation rate reached only the first evaporation stage. For treatment with 50% of dry matter with residues produced by bean crop, the evaporation stage moved beyond the first evaporation stage. Finally, for mulching with 100% of bean crop dry matter, the rate of soil water evaporation was influenced by the evaporative demand tested. The relationship among evaporation rate for treatment with 100% of dry matter and the water evaporative demands of 7,0, 5,0 and 2,5mm d-1 were 46, 41 and 47%, respectively
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spelling Effect of crops residues used as soil surface mulching to control water direct evaporation - DOI: 10.4025/actasciagron.v26i2.1882Efeito da cobertura de resíduos de culturas na evaporação direta da água do solo - DOI: 10.4025/actasciagron.v26i2.1882demanda evaporativaevaporaçãotextura do solo5.00.00.00-4 Ciências AgráriasThe influence of corn, bean and wheat crops residues used as soil surface mulching to control the water evaporation demands, for two soils textural classes, was analyzed in the present work. The treatments consisted of three layers of crop residues, corresponding to 0, 50 and 100% of dry matter produced by irrigated cropping systems, and three water evaporative demands of 3, 6 and 8mm d-1, for two soil textural classes, silty sand and heavy loamy soils, with 84% of sand and 76% of clay, respectively. The experiment was carried out in laboratory, with the soil sample conditioned in a 45-cm high and 20-cm nominal diameter PVC pipes columns. The water evaporation rate from the bare soil column presented different behavior for the three water evaporation demands tested. For water evaporative demand of approximately 3mm d-1, the treatments with corn and wheat crops residues, which represented mulching layer of 50 and 100% of dry matter, the water evaporation rate reached only the first evaporation stage. For treatment with 50% of dry matter with residues produced by bean crop, the evaporation stage moved beyond the first evaporation stage. Finally, for mulching with 100% of bean crop dry matter, the rate of soil water evaporation was influenced by the evaporative demand tested. The relationship among evaporation rate for treatment with 100% of dry matter and the water evaporative demands of 7,0, 5,0 and 2,5mm d-1 were 46, 41 and 47%, respectivelyNo presente trabalho analisou-se a influência dos resíduos das culturas do milho, feijoeiro e trigo nas demandas evaporativas e duas classes texturais de solos. Os tratamentos constaram de três taxas de resíduos de culturas, 0, 50 e 100% da matéria seca produzida pelas culturas em sistemas irrigados; e três demandas evaporativas de 3, 6 e 8mm d-1 e duas classes texturais de solos, areia franca e muito argiloso, contendo 84% de areia e 76% de argila respectivamente. O experimento foi conduzido em laboratório, com o solo acondicionado em colunas. A taxa de evaporação da água do solo descoberto apresentou comportamento distinto para as três demandas evaporativas utilizadas. Para a demanda evaporativa de aproximadamente 3mm d-1 em tratamentos com resíduos da cultura do milho e do trigo para as taxas de 50 e 100% de matéria seca permaneceram no primeiro estádio de evaporação, enquanto para o tratamento com 50% de matéria seca produzida pela cultura do feijoeiro isto não ocorreu. Para a taxa de resíduos de 100% da matéria seca, para a cultura do feijoeiro, a demanda evaporativa influenciou a taxa de evaporação da água do solo, e a relação entre a evaporação para o tratamento com 100% de matéria seca e as demandas evaporativas de 7,0, 5,0 e 2,5mm d-1 foi de 46, 41 e 47%, respectivamenteUniversidade Estadual de Maringá2008-04-11info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttp://www.periodicos.uem.br/ojs/index.php/ActaSciAgron/article/view/188210.4025/actasciagron.v26i2.1882Acta Scientiarum. Agronomy; Vol 26 No 2 (2004); 193-201Acta Scientiarum. Agronomy; v. 26 n. 2 (2004); 193-2011807-86211679-9275reponame:Acta Scientiarum. Agronomy (Online)instname:Universidade Estadual de Maringá (UEM)instacron:UEMporhttp://www.periodicos.uem.br/ojs/index.php/ActaSciAgron/article/view/1882/1295Freitas, Paulo Sergio Lourenço deMantovani, Everardo C.Sediyama, Gilberto C.Costa, Luiz Claudioinfo:eu-repo/semantics/openAccess2022-11-23T18:37:35Zoai:periodicos.uem.br/ojs:article/1882Revistahttp://www.periodicos.uem.br/ojs/index.php/ActaSciAgronPUBhttp://www.periodicos.uem.br/ojs/index.php/ActaSciAgron/oaiactaagron@uem.br||actaagron@uem.br|| edamasio@uem.br1807-86211679-9275opendoar:2022-11-23T18:37:35Acta Scientiarum. Agronomy (Online) - Universidade Estadual de Maringá (UEM)false
dc.title.none.fl_str_mv Effect of crops residues used as soil surface mulching to control water direct evaporation - DOI: 10.4025/actasciagron.v26i2.1882
Efeito da cobertura de resíduos de culturas na evaporação direta da água do solo - DOI: 10.4025/actasciagron.v26i2.1882
title Effect of crops residues used as soil surface mulching to control water direct evaporation - DOI: 10.4025/actasciagron.v26i2.1882
spellingShingle Effect of crops residues used as soil surface mulching to control water direct evaporation - DOI: 10.4025/actasciagron.v26i2.1882
Freitas, Paulo Sergio Lourenço de
demanda evaporativa
evaporação
textura do solo
5.00.00.00-4 Ciências Agrárias
title_short Effect of crops residues used as soil surface mulching to control water direct evaporation - DOI: 10.4025/actasciagron.v26i2.1882
title_full Effect of crops residues used as soil surface mulching to control water direct evaporation - DOI: 10.4025/actasciagron.v26i2.1882
title_fullStr Effect of crops residues used as soil surface mulching to control water direct evaporation - DOI: 10.4025/actasciagron.v26i2.1882
title_full_unstemmed Effect of crops residues used as soil surface mulching to control water direct evaporation - DOI: 10.4025/actasciagron.v26i2.1882
title_sort Effect of crops residues used as soil surface mulching to control water direct evaporation - DOI: 10.4025/actasciagron.v26i2.1882
author Freitas, Paulo Sergio Lourenço de
author_facet Freitas, Paulo Sergio Lourenço de
Mantovani, Everardo C.
Sediyama, Gilberto C.
Costa, Luiz Claudio
author_role author
author2 Mantovani, Everardo C.
Sediyama, Gilberto C.
Costa, Luiz Claudio
author2_role author
author
author
dc.contributor.author.fl_str_mv Freitas, Paulo Sergio Lourenço de
Mantovani, Everardo C.
Sediyama, Gilberto C.
Costa, Luiz Claudio
dc.subject.por.fl_str_mv demanda evaporativa
evaporação
textura do solo
5.00.00.00-4 Ciências Agrárias
topic demanda evaporativa
evaporação
textura do solo
5.00.00.00-4 Ciências Agrárias
description The influence of corn, bean and wheat crops residues used as soil surface mulching to control the water evaporation demands, for two soils textural classes, was analyzed in the present work. The treatments consisted of three layers of crop residues, corresponding to 0, 50 and 100% of dry matter produced by irrigated cropping systems, and three water evaporative demands of 3, 6 and 8mm d-1, for two soil textural classes, silty sand and heavy loamy soils, with 84% of sand and 76% of clay, respectively. The experiment was carried out in laboratory, with the soil sample conditioned in a 45-cm high and 20-cm nominal diameter PVC pipes columns. The water evaporation rate from the bare soil column presented different behavior for the three water evaporation demands tested. For water evaporative demand of approximately 3mm d-1, the treatments with corn and wheat crops residues, which represented mulching layer of 50 and 100% of dry matter, the water evaporation rate reached only the first evaporation stage. For treatment with 50% of dry matter with residues produced by bean crop, the evaporation stage moved beyond the first evaporation stage. Finally, for mulching with 100% of bean crop dry matter, the rate of soil water evaporation was influenced by the evaporative demand tested. The relationship among evaporation rate for treatment with 100% of dry matter and the water evaporative demands of 7,0, 5,0 and 2,5mm d-1 were 46, 41 and 47%, respectively
publishDate 2008
dc.date.none.fl_str_mv 2008-04-11
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 http://www.periodicos.uem.br/ojs/index.php/ActaSciAgron/article/view/1882
10.4025/actasciagron.v26i2.1882
url http://www.periodicos.uem.br/ojs/index.php/ActaSciAgron/article/view/1882
identifier_str_mv 10.4025/actasciagron.v26i2.1882
dc.language.iso.fl_str_mv por
language por
dc.relation.none.fl_str_mv http://www.periodicos.uem.br/ojs/index.php/ActaSciAgron/article/view/1882/1295
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 Universidade Estadual de Maringá
publisher.none.fl_str_mv Universidade Estadual de Maringá
dc.source.none.fl_str_mv Acta Scientiarum. Agronomy; Vol 26 No 2 (2004); 193-201
Acta Scientiarum. Agronomy; v. 26 n. 2 (2004); 193-201
1807-8621
1679-9275
reponame:Acta Scientiarum. Agronomy (Online)
instname:Universidade Estadual de Maringá (UEM)
instacron:UEM
instname_str Universidade Estadual de Maringá (UEM)
instacron_str UEM
institution UEM
reponame_str Acta Scientiarum. Agronomy (Online)
collection Acta Scientiarum. Agronomy (Online)
repository.name.fl_str_mv Acta Scientiarum. Agronomy (Online) - Universidade Estadual de Maringá (UEM)
repository.mail.fl_str_mv actaagron@uem.br||actaagron@uem.br|| edamasio@uem.br
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