Sistema de tratamento anaeróbio, aeróbio e anóxico para águas residuárias de suinocultura: remoção de matéria orgânica, de nutrientes e de coliformes

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Fontes de matéria orgânica para inibição de fitopatógenos habitantes do solo

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

Substâncias húmicas aquáticas: caracterização e interação com íons crômio e proposta de um indicador de matéria orgânica lábil

Pós-graduação em Química - IBILCE

Avaliação da remoção de matéria orgânica carbonácea e nitrogenada de águas residuárias utilizando biorreator de membranas

Pós-graduação em Engenharia Civil - FEIS

Correlação entre a produtividade e teor de proteína bruta do capim-Marandu com atributos físicos e químicos de um latossolo do cerrado brasileiro

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Rotação de culturas e propriedades físicas e matéria orgânica de um latossolo

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

Substâncias húmicas e fontes de fósforo: teor de fósforo disponível em solos e absorção pela cana-de-açúcar

Pós-graduação em Agronomia (Ciência do Solo) - FCAV

Adubação orgânica e nitrogenada em videira cv. syrah no vale do submédio São Francisco

Pós-graduação em Agronomia (Irrigação e Drenagem) - FCA

Formulações de fungos nematófagos associadas ao controle químico e matéria orgânica no manejo dos nematoides dos citros (Tylenchulus semipenetrans e Pratylenchus jaehni)

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Utilização da ultrafiltração em fluxo tangencial como nova metodologia para determinação da capacidade de complexação e constantes de equilíbrio de íons 'Cu'(II) complexados por matéria orgânica natural

Pós-graduação em Química - IQ

Interações entre espécies de arsênio e matéria orgânica natural: Lílian Karla de Oliveira. -

Pós-graduação em Química - IQ

Teores e estoque de carbono em frações lábeis e recalcitrantes da matéria orgânica do solo sob integração lavoura-pecuária no bioma Cerrado

The study of organic matter and its compartments and their relationship with management, aims to develop strategies for increasing their levels in soils and better understanding of its dynamics. This work aimed to evaluate the fractions of soil organic matter and their carbon stocks in different soil cover system in crop-livestock integration and native Cerrado vegetation. The study was conducted at the farm Cabeceira, Maracaju-MS, sample area have the following history: soybean/corn + brachiaria/cotton/oat + pasture/soybean/formation of pasture/grazing, sampling was carried out in two seasons, dry (May/2009) and rainy (March 2010), in the dry season, crops present were: pasture, corn and cotton + brachiaria and in the rainy season were corn, cotton and soybeans, so the areas in the two evaluation periods were: pasture / maize + brachiaria / cotton, cotton / soybean area and a native of Savanna. Was performed to determine the exchangeable cations, particle size analysis, bulk density, organic carbon, particle size fractionation of organic matter of the soil with the quantification of particulate organic carbon (POC) and organic carbon associated with minerals (OCam). Was also quantified the carbon stock and size fractions. The area of pasture / maize showed higher carbon stock in the particulate fraction in the topsoil. The area of cotton / soy due to its lower clay, showed the greatest loss of carbon. Because of the areas have the same history, the stock of more recalcitrant fraction was not sensitive to variations in coverage. The POC fraction appears more sensitive to different soil covers and seasonality.

Atributos químicos e matéria orgânica em complexos florestais periodicamente inundados na restinga da marambaia - RJ

This study aimed to evaluate and characterize the chemical properties of soil organic matter under two periodically flooded forest formations on the island of Marambaia, Rio de Janeiro. These formations differ on the degree of soil water saturation, caused by the influence of water table, and in the (F1) formation presents the water table nearer the surface compared to the (F2) formation. Samples were collected in layers from 0.00 to 0.05, 0.05-0.10 and 0.10-0.20 m. The soil properties evaluated were: pH, H+ + Al+ 3, Ca+2, Mg+2, Na+, K+, P, N, total organic carbon (TOC) and base saturation (V%), humin carbon fraction (C-HUM), carbon of humic acid fraction (HAF-C) and fulvic acid fraction carbon (FAF-C). Statistically higher pH values were observed for F1. In F2 there are higher values of Mg+2, P, N and V% value. Correlation was found between the concentrations of Mg+2, N, humic acid and fulvic acid with water table in F1, and water table in F2 with Na+ and K+. Fraction C-HUM was more representative of the total organic carbon, followed by C-HAF and C-FAF. The TOC levels were higher in F1. The C /N ratio was lower in F2, with values ranging between 9 and 12, and F1 were found higher values of this relationship, ranging from 9 to 15. Among the pathways of formation of organic soils in both areas it appears that the major route for organic matter accumulation is the inheritance route.

Teores de nitrogênio no solo e nas frações da matéria orgânica sob diferentes sistemas de produção de milho

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

Dependência espacial da estabilidade de agregados e matéria orgânica do solo em cambissolo sob cultivo de cana de açucar

The soil management system can modify the natural distribution of the soil attributes and, consequently, the variability of the soil aggregation and organic matter content. Thus, the aim of this work was to evaluate the aggregate stability and organic matter content spatial distribution on a Haplic Cambisol under sugar cane cultivation in the Southern Amazonas State, Brazil. A 70 x 70 m square mesh, with regular 10 meters intervals, was designed over the cultivation area, resulting in 64 sample points. Soil blocks with preserved structure were collected at 0.0-0.2 m depth in order to analyze the aggregate stability and organic matter content. The data were submitted to the descriptive and geostatistical analysis. The soil attributes presented a spatial dependence structure and the greater range was observed for the mean weighted diameter and aggregate class <1.00 mm. Also, there is a spatial relation among the mean geometric diameter, mean weighted diameter and aggregate classes (>2.00 and 2.00-1.00 mm).