CHEMICAL AND PHYSICAL ATTRIBUTES OF SOIL, AND CARBON AND NITROGEN STOCK AND HUMIC FRACTIONS IN DIFFERENT PLANT FORMATIONS
Autor(a) principal: | |
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Data de Publicação: | 2015 |
Outros Autores: | , , |
Tipo de documento: | Artigo |
Idioma: | por |
Título da fonte: | Ciência Florestal (Online) |
Texto Completo: | https://periodicos.ufsm.br/cienciaflorestal/article/view/19613 |
Resumo: | Cerrado biome is the second largest Brazilian biome, where different phyto-physiognomical features are observed, which may be influenced by soil factors. Thus, this study aimed to evaluate soil physical and fertility properties (particle size analysis, bulk density - BD and total pore volume - TPV), carbon and nitrogen stocks and chemical fractions of soil organic matter (SOM ) in areas of mesophytic forest, Cerrado and Cerrado sensu stricto in the ecological station of Pirapitinga, Minas Gerais state. The soil was classified as Oxisol and soil samples were collected from the layers 0-0.05, 0.5-0.1, 0.1-0.2, and 0.2-0.4 m. The experimental design was completely randomized. Areas of mesophytic forest and cerrado grow in soil with higher clay compared to the Cerrado sensu stricto, indicating that possibly more clayey soils have higher water holding capacity and nutrient supply to attend the demand more appropriately with larger vegetations. The mesophytic forest area by presenting high waste disposal of plant and be in the clayey soil is in some layers providing higher levels of soil organic C and humic substances, triggering lower values of bulk density, greater total porosity and availability of P in relation to other vegetation types studied. However, the closed areas and Cerrado sensu stricto have higher amounts of Mg, K, and lower pH, H + Al and Al compared to mesophitic forest area, which may suggest that these phytophysiognomies settle preferentially in the most fertile soils of Cerrado biome. The relationship between the humic acid and fulvic acid fraction indicates that the forest vegetation Mesophytic presents for vegetation of Cerrado and Cerado sensu stricto soil organic matter of great quality, which allows the establishment of physical and chemical attributes favorable to the development of the plant. The largest stocks of carbon are verified in larger vegetation, cerrado and mesophytic forest. However, the higher grade and stock soil nitrogen occur in Cerrado sensu stricto. |
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CHEMICAL AND PHYSICAL ATTRIBUTES OF SOIL, AND CARBON AND NITROGEN STOCK AND HUMIC FRACTIONS IN DIFFERENT PLANT FORMATIONSATRIBUTOS QUÍMICOS E FÍSICOS DO SOLO, ESTOQUES DE CARBONO E NITROGÊNIO E FRAÇÕES HÚMICAS EM DIFERENTES FORMAÇÕES VEGETAISPhysiognomies of Cerrado biomesoil fertilityorganic matter.Fitofisionomias do bioma Cerradofertilidade do solomatéria orgânicaCerrado biome is the second largest Brazilian biome, where different phyto-physiognomical features are observed, which may be influenced by soil factors. Thus, this study aimed to evaluate soil physical and fertility properties (particle size analysis, bulk density - BD and total pore volume - TPV), carbon and nitrogen stocks and chemical fractions of soil organic matter (SOM ) in areas of mesophytic forest, Cerrado and Cerrado sensu stricto in the ecological station of Pirapitinga, Minas Gerais state. The soil was classified as Oxisol and soil samples were collected from the layers 0-0.05, 0.5-0.1, 0.1-0.2, and 0.2-0.4 m. The experimental design was completely randomized. Areas of mesophytic forest and cerrado grow in soil with higher clay compared to the Cerrado sensu stricto, indicating that possibly more clayey soils have higher water holding capacity and nutrient supply to attend the demand more appropriately with larger vegetations. The mesophytic forest area by presenting high waste disposal of plant and be in the clayey soil is in some layers providing higher levels of soil organic C and humic substances, triggering lower values of bulk density, greater total porosity and availability of P in relation to other vegetation types studied. However, the closed areas and Cerrado sensu stricto have higher amounts of Mg, K, and lower pH, H + Al and Al compared to mesophitic forest area, which may suggest that these phytophysiognomies settle preferentially in the most fertile soils of Cerrado biome. The relationship between the humic acid and fulvic acid fraction indicates that the forest vegetation Mesophytic presents for vegetation of Cerrado and Cerado sensu stricto soil organic matter of great quality, which allows the establishment of physical and chemical attributes favorable to the development of the plant. The largest stocks of carbon are verified in larger vegetation, cerrado and mesophytic forest. However, the higher grade and stock soil nitrogen occur in Cerrado sensu stricto.http://dx.doi.org/10.5902/1980509819613O Cerrado é o segundo maior bioma brasileiro, no qual são observadas diferentes feições fitofisionômicas, que podem ser influenciadas por fatores edáficos. Desta forma, este estudo objetivou avaliar a fertilidade e os atributos físicos do solo (análise granulométrica, densidade do solo - Ds e volume total de poros – VTP), os estoques de carbono e nitrogênio e as frações químicas da matéria orgânica do solo (MOS) em áreas de mata mesofítica, cerradão e cerrado sensu stricto na estação ecológica de Pirapitinga - MG. O solo das áreas de estudo foi classificado como Latossolo Vermelho. Em cada uma das áreas avaliadas foram coletadas amostras nas camadas de 0-0,05; 0,5-0,1; 0,1-0,2 e 0,2-0,4 m. O delineamento utilizado foi inteiramente casualizado. As áreas de mata mesofítica e cerradão desenvolvem-se em solo com maiores teores de argila em comparação à área de cerrado sensu stricto, indicando que possivelmente solos mais argilosos têm maior capacidade de retenção de água e fornecimento de nutrientes para atender mais adequadamente à demanda dessas vegetações com maior porte. A área de mata mesofítica por apresentar maior deposição de resíduos vegetais e estar em solo de textura argilosa está proporcionando em algumas camadas do solo maiores teores de C orgânico e substâncias húmicas, desencadeando menores valores de densidade do solo, maior volume total de poros e maior disponibilidade de P em relação às demais fitofisionomias estudadas. No entanto, as áreas de cerradão e cerrado sensu stricto apresentam maiores valores de Mg, K, pH e menores valores de H+Al e Al em comparação à área de mata mesofítica, o que pode sugerir que estas fitofisionomias se estabelecem preferencialmente nos solos mais férteis do bioma Cerrado. A relação entre a fração ácido húmico e fração ácido fúlvico indica que a vegetação de mata mesofítica apresenta em relação à vegetação de cerradão e cerrado sensu stricto matéria orgânica do solo de melhor qualidade, que permite o estabelecimento de atributos físicos e químicos favoráveis ao desenvolvimento de plantas. Os maiores estoques de carbono são verificados nas vegetações de maior porte, cerradão e mata mesofítica. Entretanto, o maior teor e estoque de nitrogênio do solo ocorrem na área de cerrado sensu stricto. Universidade Federal de Santa Maria2015-09-30info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://periodicos.ufsm.br/cienciaflorestal/article/view/1961310.5902/1980509819613Ciência Florestal; Vol. 25 No. 3 (2015); 617-631Ciência Florestal; v. 25 n. 3 (2015); 617-6311980-50980103-9954reponame:Ciência Florestal (Online)instname:Universidade Federal de Santa Maria (UFSM)instacron:UFSMporhttps://periodicos.ufsm.br/cienciaflorestal/article/view/19613/11608Giácomo, Romulo GuimarãesPereira, Marcos GervasioGuareschi, Roni FernandesMachado, Deivid Lopesinfo:eu-repo/semantics/openAccess2017-04-10T17:37:23Zoai:ojs.pkp.sfu.ca:article/19613Revistahttp://www.ufsm.br/cienciaflorestal/ONGhttps://old.scielo.br/oai/scielo-oai.php||cienciaflorestal@ufsm.br|| cienciaflorestal@gmail.com|| cf@smail.ufsm.br1980-50980103-9954opendoar:2017-04-10T17:37:23Ciência Florestal (Online) - Universidade Federal de Santa Maria (UFSM)false |
dc.title.none.fl_str_mv |
CHEMICAL AND PHYSICAL ATTRIBUTES OF SOIL, AND CARBON AND NITROGEN STOCK AND HUMIC FRACTIONS IN DIFFERENT PLANT FORMATIONS ATRIBUTOS QUÍMICOS E FÍSICOS DO SOLO, ESTOQUES DE CARBONO E NITROGÊNIO E FRAÇÕES HÚMICAS EM DIFERENTES FORMAÇÕES VEGETAIS |
title |
CHEMICAL AND PHYSICAL ATTRIBUTES OF SOIL, AND CARBON AND NITROGEN STOCK AND HUMIC FRACTIONS IN DIFFERENT PLANT FORMATIONS |
spellingShingle |
CHEMICAL AND PHYSICAL ATTRIBUTES OF SOIL, AND CARBON AND NITROGEN STOCK AND HUMIC FRACTIONS IN DIFFERENT PLANT FORMATIONS Giácomo, Romulo Guimarães Physiognomies of Cerrado biome soil fertility organic matter. Fitofisionomias do bioma Cerrado fertilidade do solo matéria orgânica |
title_short |
CHEMICAL AND PHYSICAL ATTRIBUTES OF SOIL, AND CARBON AND NITROGEN STOCK AND HUMIC FRACTIONS IN DIFFERENT PLANT FORMATIONS |
title_full |
CHEMICAL AND PHYSICAL ATTRIBUTES OF SOIL, AND CARBON AND NITROGEN STOCK AND HUMIC FRACTIONS IN DIFFERENT PLANT FORMATIONS |
title_fullStr |
CHEMICAL AND PHYSICAL ATTRIBUTES OF SOIL, AND CARBON AND NITROGEN STOCK AND HUMIC FRACTIONS IN DIFFERENT PLANT FORMATIONS |
title_full_unstemmed |
CHEMICAL AND PHYSICAL ATTRIBUTES OF SOIL, AND CARBON AND NITROGEN STOCK AND HUMIC FRACTIONS IN DIFFERENT PLANT FORMATIONS |
title_sort |
CHEMICAL AND PHYSICAL ATTRIBUTES OF SOIL, AND CARBON AND NITROGEN STOCK AND HUMIC FRACTIONS IN DIFFERENT PLANT FORMATIONS |
author |
Giácomo, Romulo Guimarães |
author_facet |
Giácomo, Romulo Guimarães Pereira, Marcos Gervasio Guareschi, Roni Fernandes Machado, Deivid Lopes |
author_role |
author |
author2 |
Pereira, Marcos Gervasio Guareschi, Roni Fernandes Machado, Deivid Lopes |
author2_role |
author author author |
dc.contributor.author.fl_str_mv |
Giácomo, Romulo Guimarães Pereira, Marcos Gervasio Guareschi, Roni Fernandes Machado, Deivid Lopes |
dc.subject.por.fl_str_mv |
Physiognomies of Cerrado biome soil fertility organic matter. Fitofisionomias do bioma Cerrado fertilidade do solo matéria orgânica |
topic |
Physiognomies of Cerrado biome soil fertility organic matter. Fitofisionomias do bioma Cerrado fertilidade do solo matéria orgânica |
description |
Cerrado biome is the second largest Brazilian biome, where different phyto-physiognomical features are observed, which may be influenced by soil factors. Thus, this study aimed to evaluate soil physical and fertility properties (particle size analysis, bulk density - BD and total pore volume - TPV), carbon and nitrogen stocks and chemical fractions of soil organic matter (SOM ) in areas of mesophytic forest, Cerrado and Cerrado sensu stricto in the ecological station of Pirapitinga, Minas Gerais state. The soil was classified as Oxisol and soil samples were collected from the layers 0-0.05, 0.5-0.1, 0.1-0.2, and 0.2-0.4 m. The experimental design was completely randomized. Areas of mesophytic forest and cerrado grow in soil with higher clay compared to the Cerrado sensu stricto, indicating that possibly more clayey soils have higher water holding capacity and nutrient supply to attend the demand more appropriately with larger vegetations. The mesophytic forest area by presenting high waste disposal of plant and be in the clayey soil is in some layers providing higher levels of soil organic C and humic substances, triggering lower values of bulk density, greater total porosity and availability of P in relation to other vegetation types studied. However, the closed areas and Cerrado sensu stricto have higher amounts of Mg, K, and lower pH, H + Al and Al compared to mesophitic forest area, which may suggest that these phytophysiognomies settle preferentially in the most fertile soils of Cerrado biome. The relationship between the humic acid and fulvic acid fraction indicates that the forest vegetation Mesophytic presents for vegetation of Cerrado and Cerado sensu stricto soil organic matter of great quality, which allows the establishment of physical and chemical attributes favorable to the development of the plant. The largest stocks of carbon are verified in larger vegetation, cerrado and mesophytic forest. However, the higher grade and stock soil nitrogen occur in Cerrado sensu stricto. |
publishDate |
2015 |
dc.date.none.fl_str_mv |
2015-09-30 |
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://periodicos.ufsm.br/cienciaflorestal/article/view/19613 10.5902/1980509819613 |
url |
https://periodicos.ufsm.br/cienciaflorestal/article/view/19613 |
identifier_str_mv |
10.5902/1980509819613 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
https://periodicos.ufsm.br/cienciaflorestal/article/view/19613/11608 |
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 Federal de Santa Maria |
publisher.none.fl_str_mv |
Universidade Federal de Santa Maria |
dc.source.none.fl_str_mv |
Ciência Florestal; Vol. 25 No. 3 (2015); 617-631 Ciência Florestal; v. 25 n. 3 (2015); 617-631 1980-5098 0103-9954 reponame:Ciência Florestal (Online) instname:Universidade Federal de Santa Maria (UFSM) instacron:UFSM |
instname_str |
Universidade Federal de Santa Maria (UFSM) |
instacron_str |
UFSM |
institution |
UFSM |
reponame_str |
Ciência Florestal (Online) |
collection |
Ciência Florestal (Online) |
repository.name.fl_str_mv |
Ciência Florestal (Online) - Universidade Federal de Santa Maria (UFSM) |
repository.mail.fl_str_mv |
||cienciaflorestal@ufsm.br|| cienciaflorestal@gmail.com|| cf@smail.ufsm.br |
_version_ |
1799944130389868544 |