Aplicação de calcário e seus efeitos no sistema radicular, estado nutricional, produção e qualidade tecnológica de frutos de mangueiras

Pós-graduação em Agronomia - FEIS

Pontos polêmicos acerca do forrageamento de cupins subterrâneos (Isoptera: Rhinotermitidae): consumo de alimentos similares, reutilização de iscas e tunelamento em solos não uniformes

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Influência da acidez da suspensão coloidal para a geração de defeitos pontuais e emissão no infra vermelho em SnO2 dopado com Er

Pós-graduação em Ciência e Tecnologia de Materiais - FC

Implantação da cultura de cana-de-açúcar em argissolo vermelho do noroeste paulista: preparo do solo e uso de gesso

Pós-graduação em Agronomia - FEIS

COMPORTAMENTO FÍSICO-HÍDRICO DOS SOLOS DO PERÍMETRO IRRIGADO CURAÇÁ EM JUAZEIRO/BA

O objetivo desse trabalho foi avaliar o comportamento físico-hídrico dos solos do Perímetro Irrigado Curaçá, no município de Juazeiro–BA, que possam ser utilizados como base para definir práticas de manejo de solo e da irrigação. Foram coletadas amostras em 10 lotes agrícolas em duas profundidades (0-0,30m e 0,30-0,60m) de diferentes perfis de solos cultivados com várias culturas, determinando-se a granulometria, densidade, porosidade, curva de retenção de água no solo, água disponível e disponibilidade total de água no solo. Verificou-se que os solos amostrados possuem textura areia franca em 45% das amostras estudadas, seguida de franca arenosa, em 35%, apresentando reduzido armazenamento de água. A média da densidade do solo foi de 2,06 e 1,94 Mg.m-3 nas duas profundidades, indicando compactação em 100% na superfície e 87,5% na camada sub-superficial dos solos. Concluiu-se que os solos analisados apresentam textura arenosa e, assim, naturalmente propensos a uma reduzida retenção da água no solo. Possuem, ainda, problemas de compactação, ao longo do perfil do solo.

Dependência Espacial de Atributos Diagnósticos para Delimitação de Classes de Solos

Os solos são classificados por seus horizontes e atributos diagnósticos para que possam ser agrupados por semelhanças e fornecer informações relativas a sua utilização. Conhecer a variabilidade espacial dos atributos diagnósticos utilizados na classificação do solo é importante na definição do manejo do solo. O objetivo desse trabalho foi verificar a dependência espacial dos atributos diagnósticos na classificação de solos (índice de avermelhamento, gradiente textural e V%) e identificar os limites entre classes de solos. O índice de avermelhamento, gradiente textural e V% do solo foram determinados nos horizontes A e B de uma grade amostral de 65 pontos coletados no Horto da cidade de Mogi-Guaçu, SP. A análise da variabilidade espacial dos atributos estudados foi realizada por meio da geoestatística, considerando a dependência espacial no intervalo de amostragem. Todos os atributos do Horto de Mogi-Guaçu apresentaram dependência espacial e foram interpolados pela krigagem ordinária para obtenção dos mapas temáticos. Com base nos mapas de índice de avermelhamento, gradiente textural e V% foi possível gerar o mapa de classes de solos. Na área de estudo houve maior ocorrência de solos Vermelho Amarelo sem migração de argila do horizonte A para o B e Distrófico.

Nutrição mineral e escleromorfismo foliar de grupos funcionais e comunidades vegetais savânicas

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Caracterização potenciométrica de substâncias húmicas extraídas de solos da Antártica Marítima

Monitoring of soil carbon storage may indicate possible effects of climate change on the terrestrial environment and it is therefore necessary to understand the influence of redox potential and chemical characteristics of humic substances (HS) of Antarctic soil. Five soils from King George Island were used. HS were extracted, quantified and characterized by potentiometry and the content of total carbon and nitrogen determined. HS of these soils had greater aliphatic character, low content of phenolic groups, lower acidity and lower formal standard electrode potential, compared to HS of soils from other regions, suggesting they are more likely to be oxidized.

Chemical and biological properties of phosphorus-fertilized soil under legume and grass cover (Cerrado region, Brazil)

The use of cover crops has been suggested as an effective method to maintain and/or increase the organic matter content, while maintaining and/or enhancing the soil physical, chemical and biological properties. The fertility of Cerrado soils is low and, consequently, phosphorus levels as well. Phosphorus is required at every metabolic stage of the plant, as it plays a role in the processes of protein and energy synthesis and influences the photosynthetic process. This study evaluated the influence of cover crops and phosphorus rates on soil chemical and biological properties after two consecutive years of common bean. The study analyzed an Oxisol in Selvíria (Mato Grosso do Sul, Brazil), in a randomized block, split plot design, in a total of 24 treatments with three replications. The plot treatments consisted of cover crops (millet, pigeon pea, crotalaria, velvet bean, millet + pigeon pea, millet + crotalaria, and millet + velvet bean) and one plot was left fallow. The subplots were represented by phosphorus rates applied as monoammonium phosphate (0, 60 and 90 kg ha-1 P2O5). In August 2011, the soil chemical properties were evaluated (pH, organic matter, phosphorus, potential acidity, cation exchange capacity, and base saturation) as well as biological variables (carbon of released CO2, microbial carbon, metabolic quotient and microbial quotient). After two years of cover crops in rotation with common bean, the cover crop biomass had not altered the soil chemical properties and barely influenced the microbial activity. The biomass production of millet and crotalaria (monoculture or intercropped) was highest. The biological variables were sensitive and responded to increasing phosphorus rates with increases in microbial carbon and reduction of the metabolic quotient.

Absorção de nutrientes e alterações químicas em Latossolos cultivados com plantas de cobertura em rotação com soja e milho

The effects on soil chemical properties brought about by cover crops vary considerably. This study was conducted to evaluate nutrient uptake by five cover crops used for grain, seed and forage production at different seed densities per hectare, as well as uptake by spontaneous vegetation, and their effect on the chemical properties of two Oxisols when grown in rotation with soybean and corn. The experiments were set up in Votuporanga, SP, Brazil and Selvíria, MS, Brazil in March 2008 after conventional soil tillage. A randomized complete block experimental design was used with four replications with the following cover crops at different seed densities: Sorghum bicolor at 6, 7 and 8 kg ha-1; Pennisetum americanum at 10, 15 and 20 kg ha-1; Sorghum sudanense at 12, 15 and 18 kg ha-1; hybrid of Sorghum bicolor with Sorghum sudanense at 8, 9 and 10 kg ha-1; and Urochloa ruziziensis at 8, 12 and 16 kg ha-1. We also used a spontaneous vegetation control. After management of the cover crops, in the first year of study, soybean was sown in no-tillage system and, in the second year, corn was sown, also in a no-tillage system. We evaluated the dry matter yield of different cover crops, nutrient uptake by the cover crops, and the chemical changes in the soil. It was found that in clayey soils with high aluminum content, as in Selvíria, sudan grass at a seed density of 18 kg ha-1, and sorghum at a seed density of 6 kg ha-1, in combination with liming, contributed to reduction of aluminum content and high potential acidity and an increase in base saturation. The different seed densities of each cover crop did not affect the dry matter yield of the cover crop itself, but affected nitrogen uptake of the hybrid Sorghum bicolor with Sorghum sudanense at a seed density of 10 kg ha-1, with lower uptake than at a seed density of 8 kg ha-1. Seed density also affected the organic matter content in the soil with sudan grass, with the seed density of 15 kg ha-1 providing more organic matter content than a seed density of 18 kg ha-1.

Determination of reactivity rates of silicate particle-size fractions

The efficiency of sources used for soil acidity correction depends on reactivity rate (RR) and neutralization power (NP), indicated by effective calcium carbonate (ECC). Few studies establish relative efficiency of reactivity (RER) for silicate particle-size fractions, therefore, the RER applied for lime are used. This study aimed to evaluate the reactivity of silicate materials affected by particle size throughout incubation periods in comparison to lime, and to calculate the RER for silicate particle-size fractions. Six correction sources were evaluated: three slags from distinct origins, dolomitic and calcitic lime separated into four particle-size fractions (2, 0.84, 0.30 and <0.30-mm sieves), and wollastonite, as an additional treatment. The treatments were applied to three soils with different texture classes. The dose of neutralizing material (calcium and magnesium oxides) was applied at equal quantities, and the only variation was the particle-size material. After a 90-day incubation period, the RER was calculated for each particle-size fraction, as well as the RR and ECC of each source. The neutralization of soil acidity of the same particle-size fraction for different sources showed distinct solubility and a distinct reaction between silicates and lime. The RER for slag were higher than the limits established by Brazilian legislation, indicating that the method used for limes should not be used for the slags studied here.

Resistência de união ao microcisalhamento de sistemas adesivos autocondicionates com graus de acidez distintos: efeito de diferentes tratamentos em substrato dentinário normal e hipermineralizado artificialmente

Pós-graduação em Ciências Odontológicas - FOAR

Influência da vinhaça e da palhada de cana-de-açúcar na sorção de herbicidas aplicados em diferentes solos

Pós-graduação em Agronomia (Agricultura) - FCA

Balanço de potássio no sistema solo-planta influenciado pela textura e adubação potássica em solos tropicais

Pós-graduação em Agronomia (Agricultura) - FCA