Atributos físicos e químicos do solo em área sob diferentes usos na Região Norte do Estado do Espírito Santo
Ano de defesa: | 2016 |
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Autor(a) principal: | |
Orientador(a): | |
Banca de defesa: | |
Tipo de documento: | Dissertação |
Tipo de acesso: | Acesso aberto |
Idioma: | por |
Instituição de defesa: |
Universidade Federal do Espírito Santo
BR Mestrado em Agricultura Tropical UFES Programa de Pós-Graduação em Agricultura Tropical |
Programa de Pós-Graduação: |
Não Informado pela instituição
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Departamento: |
Não Informado pela instituição
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País: |
Não Informado pela instituição
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Palavras-chave em Português: | |
Link de acesso: | http://repositorio.ufes.br/handle/10/8254 |
Resumo: | Considering an increasing demand related to Brazil's agricultural production becomes a need for greater and better understanding of how to keep it sustainable, it is important to keep a good soil for future crops have a suitable environment and it has good productivity. Studies about soil physical and chemical attributes allows a good indication of the quality of a given soil. In this sense, it was evaluated in this study changes in physical and chemical properties in areas with different uses within a property located in the city of Jaguaré-ES. The areas studied were under the homogeneous planting conilon coffee (Coffea canephora Pierre ex A. Froehner) (Cc); rubber tree (Hevea brasiliensis L.) (S); consortium with rubber tree and conilon coffee (SCc); consortium with rubber tree and coconut (Cocos nucifera L.) (SCo); consortium with rubber tree, black pepper (Piper nigrum L.) and cocoa (Theobroma cacao L.) (SPCa); and native vegetation (MN). The experiment was carried out by sampling in five installments of 6 x 6 meters on each use system. The chemical attributes were analyzed at 0-10, 10-20 e 20-40cm depths are: soil organic matter (SOM), pH, P, Ca, Mg, Na, K, Al, H + Al, sum of bases (SB), effective CEC (t), potencial CEC (T), base saturation (V) and Al saturation (m). The physical attributes analyzed at 0-10, 10-20 e 20-40cm depths were: texture, particle density, soil density, macro and microporosity and aggregate stability. At 15 and 30cm depths were analyzed hydraulic conductivity and 0-10, 10-20, 20-30 e 30-40cm penetration soil resistance. Data were subjected to variance analysis and treatment means were compared by Tukey test at 5% probability. It used also Tocher grouping method based on the Mahalanobis dispersion. MN had lower penetration soil resistance and soil density and higher macroporosity compared to other areas, probably due to the higher values of soil organic matter. The areas under Cc and agroforestry system SPCa were similar when evaluated particle density, soil density, total porosity, microporosity, microporosity and sand, clay and silt percentage. The covers Cc and MN were similar when was considered the chemistry and analyzed depths. The management adopted in Cc area performed better than adopted in agroforestry viii systems in the upper layers. It worked more effectively, improving the quality of soil chemical properties. The agricultural use of the soil, even in the case of perennial crops, caused changes in soil physical properties and degraded soil organic matter when compared with original condition. |