Effect of crops residues used as soil surface mulching to control water direct evaporation - DOI: 10.4025/actasciagron.v26i2.1882
Autor(a) principal: | |
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Data de Publicação: | 2008 |
Outros Autores: | , , |
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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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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1799305904572596224 |