Abstract We present our experimental setup to produce ultracold strongly correlated fermionic superfluids made of a two-component spin-mixture of 6Li atoms. Employing standard cooling techniques, we achieve quantum degeneracy in a single-beam optical dipole trap. Our setup is capable of generating spin-balanced samples at temperatures as low as T/T F = 0.1 containing up to 5 x 104 atomic pairs. We can access different superfluid regimes by tuning the interparticle interactions close to a broad magnetic Feshbach resonance. In particular, we are able to explore the crossover from the molecular Bose-Einstein condensate (BEC) to the Bardeen-Cooper-Schrieffer (BCS) superfluid regimes.

O objetivo deste trabalho foi avaliar as propriedades físicas e carbono orgânico de um Argissolo Vermelho, em Pelotas (RS), submetido a sistemas de manejo numa propriedade agrícola. Avaliaram-se densidade do solo, porosidade total, macro e microporosidade, granulometria, argila dispersa em água, diâmetro médio ponderado de agregados e infiltração de água, bem como carbono orgânico. Foram estudados os sistemas: plantio direto com três anos de condução, com aveia + ervilhaca no inverno e milho no verão; sistema convencional (uma aração e uma gradagem) com aveia como cobertura de inverno e milho no verão; sistema convencional, com ervilhaca + aveia no inverno e milho no verão, e campo nativo. Observou-se que o solo sob os sistemas convencionais apresentou maior porosidade total e macroporosidade na profundidade de 0,0-0,10 m e maior microporosidade na profundidade de 0,10-0,20 m. Os maiores valores de densidade do solo na profundidade de 0,0-0,10 m foi no solo sob plantio direto. Houve aumento do teor de carbono orgânico do solo no sistema plantio direto na camada de 0,0-0,10 m em relação aos outros sistemas avaliados, não resultando em aumento no diâmetro médio ponderado dos agregados.

The objective of this research was to evaluate the physical properties and organic carbon of a Typic Hapludalf in Pelotas, State of Rio Grande do Sul, Brazil, under different soil management systems on a farm. The assessed physical attributes were: soil bulk density, total porosity, macro and microporosity, particle size distribution, water dispersed clay, mean weight diameter of water-stable aggregates, and soil water infiltration, as well as organic carbon, in a factorial scheme in a completely randomized design with six replications. The management systems were studied for three years: no-tillage system with oats + vetch in winter and corn in summer; conventional tillage system with oat winter covering and corn in summer; conventional tillage (once plowing and once disking) with oats + vetch in winter and corn in summer; and native grassland. It was observed that soil under conventional tillage systems presented a higher total porosity and macroporosity in the 0.0-0.10 m, but higher microporosity in the 0.10-0.20 m layer; the no-tillage system presented the greatest values of soil bulk density in the 0.0-0.10 m layer. There was an increase in the soil organic carbon content for the no-tillage system, which was not reflected in an increase in the mean weight diameter of the water-stable aggregates.