Physical characteristics of a Dark-Red Latosol (Oxisol) of the Brazilian Savannas ("Cerrados") of Planaltina under fire action
Autor(a) principal: | |
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Data de Publicação: | 2000 |
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/5963 |
Resumo: | The main effects of fire on the soil are related to biological and chemical alterations. Fire can also change the soil moisture as a consequence of alterations in infiltration rates, transpiration rates, porosity, and water repellence. The objective of this work was to evaluate physical characteristics of a heavy clayer Dark Red Latosol (Oxisol) submitted to fire treatments. The selected area of restrict sense Cerrado covers 2.5 ha which have been protected against fire since 1979, despite its use as native pasture during 20 years. The area was divided into two, half of it protected against fire and the other half submitted to fire every two years. Fire has caused no large variations on the physical characteristics of the soil. The non-burnt area has presented an increase on soil moisture. A slight increase of microporosity appeared on the burnt area throughout the period. This could be caused by the rain drops action against the bare soil. Fire every two years was not enough to cause significant degradation on the soil. |
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Physical characteristics of a Dark-Red Latosol (Oxisol) of the Brazilian Savannas ("Cerrados") of Planaltina under fire actionCaracterísticas físicas de um Latossolo Vermelho-Escuro no Cerrado de Planaltina, DF, submetido à ação do fogoburning; soil density; soil water retention; porosity; moisture contentqueimada; densidade do solo; retenção de água no solo; porosidade; teor de umidadeThe main effects of fire on the soil are related to biological and chemical alterations. Fire can also change the soil moisture as a consequence of alterations in infiltration rates, transpiration rates, porosity, and water repellence. The objective of this work was to evaluate physical characteristics of a heavy clayer Dark Red Latosol (Oxisol) submitted to fire treatments. The selected area of restrict sense Cerrado covers 2.5 ha which have been protected against fire since 1979, despite its use as native pasture during 20 years. The area was divided into two, half of it protected against fire and the other half submitted to fire every two years. Fire has caused no large variations on the physical characteristics of the soil. The non-burnt area has presented an increase on soil moisture. A slight increase of microporosity appeared on the burnt area throughout the period. This could be caused by the rain drops action against the bare soil. Fire every two years was not enough to cause significant degradation on the soil.Os principais efeitos do fogo como manejo de solo estão relacionados a alterações biológicas e químicas do solo. A queima pode ainda alterar a umidade do solo em razão de mudanças na taxa de infiltração, na taxa de transpiração, na porosidade e na repelência do solo à água. O objetivo deste trabalho foi avaliar as características físicas de um Latossolo Vermelho-Escuro muito argiloso, plano, fase campo cerrado, submetido à ação do fogo, após ser utilizado durante 20 anos em pastagem nativa sem queima. Uma área de 1,25 ha foi submetida à ação bienal do fogo, e uma área adjacente, do mesmo tamanho, foi mantida protegida da ação do fogo. Após seis anos, não houve variações marcantes nas características físicas do solo induzidas pelo fogo, exceto no aumento da umidade do solo nas parcelas não queimadas. Nas parcelas onde se aplicou o fogo, observou-se tendência para o aumento da microporosidade, que pode ser atribuída à compactação promovida pelo impacto das gotas de chuva no solo desnudado pelo fogo. Conclui-se, entretanto, que a queima bienal não foi suficiente para provocar degradação no período estudado.Pesquisa Agropecuaria BrasileiraPesquisa Agropecuária BrasileiraSpera, Silvio TulioReatto, AdrianaCorreia, João RobertoSilva, José Carlos Sousa2000-09-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://seer.sct.embrapa.br/index.php/pab/article/view/5963Pesquisa Agropecuaria Brasileira; v.35, n.9, set. 2000; 1817-1824Pesquisa Agropecuária Brasileira; v.35, n.9, set. 2000; 1817-18241678-39210100-104xreponame:Pesquisa Agropecuária Brasileira (Online)instname:Empresa Brasileira de Pesquisa Agropecuária (Embrapa)instacron:EMBRAPAporhttps://seer.sct.embrapa.br/index.php/pab/article/view/5963/3067info:eu-repo/semantics/openAccess2010-07-22T16:46:21Zoai:ojs.seer.sct.embrapa.br:article/5963Revistahttp://seer.sct.embrapa.br/index.php/pabPRIhttps://old.scielo.br/oai/scielo-oai.phppab@sct.embrapa.br || sct.pab@embrapa.br1678-39210100-204Xopendoar:2010-07-22T16:46:21Pesquisa Agropecuária Brasileira (Online) - Empresa Brasileira de Pesquisa Agropecuária (Embrapa)false |
dc.title.none.fl_str_mv |
Physical characteristics of a Dark-Red Latosol (Oxisol) of the Brazilian Savannas ("Cerrados") of Planaltina under fire action Características físicas de um Latossolo Vermelho-Escuro no Cerrado de Planaltina, DF, submetido à ação do fogo |
title |
Physical characteristics of a Dark-Red Latosol (Oxisol) of the Brazilian Savannas ("Cerrados") of Planaltina under fire action |
spellingShingle |
Physical characteristics of a Dark-Red Latosol (Oxisol) of the Brazilian Savannas ("Cerrados") of Planaltina under fire action Spera, Silvio Tulio burning; soil density; soil water retention; porosity; moisture content queimada; densidade do solo; retenção de água no solo; porosidade; teor de umidade |
title_short |
Physical characteristics of a Dark-Red Latosol (Oxisol) of the Brazilian Savannas ("Cerrados") of Planaltina under fire action |
title_full |
Physical characteristics of a Dark-Red Latosol (Oxisol) of the Brazilian Savannas ("Cerrados") of Planaltina under fire action |
title_fullStr |
Physical characteristics of a Dark-Red Latosol (Oxisol) of the Brazilian Savannas ("Cerrados") of Planaltina under fire action |
title_full_unstemmed |
Physical characteristics of a Dark-Red Latosol (Oxisol) of the Brazilian Savannas ("Cerrados") of Planaltina under fire action |
title_sort |
Physical characteristics of a Dark-Red Latosol (Oxisol) of the Brazilian Savannas ("Cerrados") of Planaltina under fire action |
author |
Spera, Silvio Tulio |
author_facet |
Spera, Silvio Tulio Reatto, Adriana Correia, João Roberto Silva, José Carlos Sousa |
author_role |
author |
author2 |
Reatto, Adriana Correia, João Roberto Silva, José Carlos Sousa |
author2_role |
author author author |
dc.contributor.none.fl_str_mv |
|
dc.contributor.author.fl_str_mv |
Spera, Silvio Tulio Reatto, Adriana Correia, João Roberto Silva, José Carlos Sousa |
dc.subject.por.fl_str_mv |
burning; soil density; soil water retention; porosity; moisture content queimada; densidade do solo; retenção de água no solo; porosidade; teor de umidade |
topic |
burning; soil density; soil water retention; porosity; moisture content queimada; densidade do solo; retenção de água no solo; porosidade; teor de umidade |
description |
The main effects of fire on the soil are related to biological and chemical alterations. Fire can also change the soil moisture as a consequence of alterations in infiltration rates, transpiration rates, porosity, and water repellence. The objective of this work was to evaluate physical characteristics of a heavy clayer Dark Red Latosol (Oxisol) submitted to fire treatments. The selected area of restrict sense Cerrado covers 2.5 ha which have been protected against fire since 1979, despite its use as native pasture during 20 years. The area was divided into two, half of it protected against fire and the other half submitted to fire every two years. Fire has caused no large variations on the physical characteristics of the soil. The non-burnt area has presented an increase on soil moisture. A slight increase of microporosity appeared on the burnt area throughout the period. This could be caused by the rain drops action against the bare soil. Fire every two years was not enough to cause significant degradation on the soil. |
publishDate |
2000 |
dc.date.none.fl_str_mv |
2000-09-01 |
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/5963 |
url |
https://seer.sct.embrapa.br/index.php/pab/article/view/5963 |
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/5963/3067 |
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.35, n.9, set. 2000; 1817-1824 Pesquisa Agropecuária Brasileira; v.35, n.9, set. 2000; 1817-1824 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 |
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1793416700381626368 |