Dinâmica sazonal de nutrientes nos solos em diferentes fitofisionomias vegetais no Norte do Pantanal Mato-Grossense

Detalhes bibliográficos
Ano de defesa: 2016
Autor(a) principal: Nassarden, Danielle Christine Stenner
Orientador(a): Não Informado pela instituição
Banca de defesa: Não Informado pela instituição
Tipo de documento: Dissertação
Tipo de acesso: Acesso aberto
Idioma: por
Instituição de defesa: Universidade Federal de Mato Grosso
Brasil
Instituto de Física (IF)
UFMT CUC - Cuiabá
Programa de Pós-Graduação em Física Ambiental
Programa de Pós-Graduação: Não Informado pela instituição
Departamento: Não Informado pela instituição
País: Não Informado pela instituição
Palavras-chave em Português:
Link de acesso: http://ri.ufmt.br/handle/1/2323
Resumo: The Pantanal undergoes frequent fluctuations of the flood levels, these in turn, are caused by rainfall variation and changes in the dynamics of sediments over the time. The flood pulse changes the chemical and physical properties of the soil, changing the concentration of nutrients. This regime of flood corroborates to the development of some species of invasive and monodominant vegetation. In this sense, the objective of this study was to understand the dynamics of soil nutrients in different phytophysiognomies, under different hydrological conditions in Northern Pantanal of Mato Grosso. The study was performed at Baía das Pedras Park in the Ecological Resort SESC Pantanal in Poconé / MT. The samples were collected in the soil of 03 phytophysiognomies named Cambará, Flooded Field and Pombeiral, and at each location were removed 03 samples of indeformed soil. The gathering was held in three distinct hydrological periods, been them before the flood (December / 2013), after the flood (July / 2014) and at the dry (October / 2014). There was an increase of organic matter after the flood at Cambara and Pombeiral soils. There was differences in the concentration of soil nutrients according to the type of vegetation and with the hydrological period. There was a change in the pH of the soil after the flood. The concentration of H + interfered in soil acidity, and thus replacing essential elements such as Ca + Mg.