Plant-available soil water capacity: estimation methods and implications
Autor(a) principal: | |
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Data de Publicação: | 2014 |
Outros Autores: | , , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Institucional da UFLA |
Texto Completo: | http://repositorio.ufla.br/jspui/handle/1/13089 |
Resumo: | The plant-available water capacity of the soil is defined as the water content between field capacity and wilting point, and has wide practical application in planning the land use. In a representative profile of the Cerrado Oxisol, methods for estimating the wilting point were studied and compared, using a WP4-T psychrometer and Richards chamber for undisturbed and disturbed samples. In addition, the field capacity was estimated by the water content at 6, 10, 33 kPa and by the inflection point of the water retention curve, calculated by the van Genuchten and cubic polynomial models. We found that the field capacity moisture determined at the inflection point was higher than by the other methods, and that even at the inflection point the estimates differed, according to the model used. By the WP4-T psychrometer, the water content was significantly lower found the estimate of the permanent wilting point. We concluded that the estimation of the available water holding capacity is markedly influenced by the estimation methods, which has to be taken into consideration because of the practical importance of this parameter. |
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Plant-available soil water capacity: estimation methods and implicationsCapacidade de água disponível no solo para as plantas: métodos de estimativa e implicaçõesField capacityPermanent wilting pointSoil water retention curve modelingOxisolLand use planningCapacidade de campoPonto de murcha permanenteModelagem da curva de retenção de água do soloLatossolosPlanejamento de uso terraThe plant-available water capacity of the soil is defined as the water content between field capacity and wilting point, and has wide practical application in planning the land use. In a representative profile of the Cerrado Oxisol, methods for estimating the wilting point were studied and compared, using a WP4-T psychrometer and Richards chamber for undisturbed and disturbed samples. In addition, the field capacity was estimated by the water content at 6, 10, 33 kPa and by the inflection point of the water retention curve, calculated by the van Genuchten and cubic polynomial models. We found that the field capacity moisture determined at the inflection point was higher than by the other methods, and that even at the inflection point the estimates differed, according to the model used. By the WP4-T psychrometer, the water content was significantly lower found the estimate of the permanent wilting point. We concluded that the estimation of the available water holding capacity is markedly influenced by the estimation methods, which has to be taken into consideration because of the practical importance of this parameter.A capacidade de água disponível no solo para as plantas é definida como o conteúdo de água entre a capacidade de campo e o ponto de murcha permanente e tem vasta aplicação prática no planejamento do uso da terra. Em um perfil de Latossolo representativo da região do Cerrado, objetivaram-se estudar e comparar métodos de estimativa para o ponto de murcha permanente, empregando os aparelhos de psicrômetro WP4-T e a câmara de Richards, utilizando amostras com e sem preservação da estrutura, bem como para a capacidade de campo, estimando-a pela umidade do solo submetido às tensões 6, 10 e 33 kPa, e pelo ponto de inflexão da curva de retenção de água calculado nos modelos de van Genuchten e polinomial cúbico. Verificou-se que para o Latossolo em estudo a capacidade de campo determinada no ponto de inflexão apresenta maior valor de umidade em comparação aos demais métodos e que mesmo nesse ponto são encontradas diferenças na estimativa em razão do modelo utilizado. Pelo psicrômetro WP4-T, valores significativamente menores de umidade foram encontrados para a estimativa do ponto de murcha permanente. Concluiu-se que a capacidade de água disponível foi influenciada marcantemente pelo método utilizado na estimativa da capacidade de campo e do ponto de murcha permanente, o que precisa ser considerado em virtude da importância prática desse parâmetro.Sociedade Brasileira de Ciência do Solo2017-05-31T19:06:07Z2017-05-31T19:06:07Z2014-03info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfSILVA, B. M. et al. Plant-available soil water capacity: estimation methods and implications. Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 38, n. 2, p. 464-475, Mar./Apr. 2014.http://repositorio.ufla.br/jspui/handle/1/13089Revista Brasileira de Ciência do Soloreponame:Repositório Institucional da UFLAinstname:Universidade Federal de Lavras (UFLA)instacron:UFLASilva, Bruno MontoaniSilva, Érika Andressa daOliveira, Geraldo César deFerreira, Mozart MartinsSerafim, Milson Evaldoinfo:eu-repo/semantics/openAccesseng2017-05-31T19:06:07Zoai:localhost:1/13089Repositório InstitucionalPUBhttp://repositorio.ufla.br/oai/requestnivaldo@ufla.br || repositorio.biblioteca@ufla.bropendoar:2017-05-31T19:06:07Repositório Institucional da UFLA - Universidade Federal de Lavras (UFLA)false |
dc.title.none.fl_str_mv |
Plant-available soil water capacity: estimation methods and implications Capacidade de água disponível no solo para as plantas: métodos de estimativa e implicações |
title |
Plant-available soil water capacity: estimation methods and implications |
spellingShingle |
Plant-available soil water capacity: estimation methods and implications Silva, Bruno Montoani Field capacity Permanent wilting point Soil water retention curve modeling Oxisol Land use planning Capacidade de campo Ponto de murcha permanente Modelagem da curva de retenção de água do solo Latossolos Planejamento de uso terra |
title_short |
Plant-available soil water capacity: estimation methods and implications |
title_full |
Plant-available soil water capacity: estimation methods and implications |
title_fullStr |
Plant-available soil water capacity: estimation methods and implications |
title_full_unstemmed |
Plant-available soil water capacity: estimation methods and implications |
title_sort |
Plant-available soil water capacity: estimation methods and implications |
author |
Silva, Bruno Montoani |
author_facet |
Silva, Bruno Montoani Silva, Érika Andressa da Oliveira, Geraldo César de Ferreira, Mozart Martins Serafim, Milson Evaldo |
author_role |
author |
author2 |
Silva, Érika Andressa da Oliveira, Geraldo César de Ferreira, Mozart Martins Serafim, Milson Evaldo |
author2_role |
author author author author |
dc.contributor.author.fl_str_mv |
Silva, Bruno Montoani Silva, Érika Andressa da Oliveira, Geraldo César de Ferreira, Mozart Martins Serafim, Milson Evaldo |
dc.subject.por.fl_str_mv |
Field capacity Permanent wilting point Soil water retention curve modeling Oxisol Land use planning Capacidade de campo Ponto de murcha permanente Modelagem da curva de retenção de água do solo Latossolos Planejamento de uso terra |
topic |
Field capacity Permanent wilting point Soil water retention curve modeling Oxisol Land use planning Capacidade de campo Ponto de murcha permanente Modelagem da curva de retenção de água do solo Latossolos Planejamento de uso terra |
description |
The plant-available water capacity of the soil is defined as the water content between field capacity and wilting point, and has wide practical application in planning the land use. In a representative profile of the Cerrado Oxisol, methods for estimating the wilting point were studied and compared, using a WP4-T psychrometer and Richards chamber for undisturbed and disturbed samples. In addition, the field capacity was estimated by the water content at 6, 10, 33 kPa and by the inflection point of the water retention curve, calculated by the van Genuchten and cubic polynomial models. We found that the field capacity moisture determined at the inflection point was higher than by the other methods, and that even at the inflection point the estimates differed, according to the model used. By the WP4-T psychrometer, the water content was significantly lower found the estimate of the permanent wilting point. We concluded that the estimation of the available water holding capacity is markedly influenced by the estimation methods, which has to be taken into consideration because of the practical importance of this parameter. |
publishDate |
2014 |
dc.date.none.fl_str_mv |
2014-03 2017-05-31T19:06:07Z 2017-05-31T19:06:07Z |
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 |
SILVA, B. M. et al. Plant-available soil water capacity: estimation methods and implications. Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 38, n. 2, p. 464-475, Mar./Apr. 2014. http://repositorio.ufla.br/jspui/handle/1/13089 |
identifier_str_mv |
SILVA, B. M. et al. Plant-available soil water capacity: estimation methods and implications. Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 38, n. 2, p. 464-475, Mar./Apr. 2014. |
url |
http://repositorio.ufla.br/jspui/handle/1/13089 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
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 |
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 reponame:Repositório Institucional da UFLA instname:Universidade Federal de Lavras (UFLA) instacron:UFLA |
instname_str |
Universidade Federal de Lavras (UFLA) |
instacron_str |
UFLA |
institution |
UFLA |
reponame_str |
Repositório Institucional da UFLA |
collection |
Repositório Institucional da UFLA |
repository.name.fl_str_mv |
Repositório Institucional da UFLA - Universidade Federal de Lavras (UFLA) |
repository.mail.fl_str_mv |
nivaldo@ufla.br || repositorio.biblioteca@ufla.br |
_version_ |
1815439023255060480 |