Desempenho de bovinos jovens das raças Aberdeen Angus e Hereford, confinados e alimentados com dois níveis de energia

Estudou-se o desempenho de bovinos machos não-castrados das raças Aberdeen Angus (AA) e Hereford (HE) em confinamento, submetidos a dois níveis de energia, em esquema fatorial 2 x 2, sendo o menor nível com 3,07 e o maior com 3,18 Mcal/kg de energia digestível (12 e 32% de concentrado na dieta, respectivamente). Foram utilizados oito animais da raça AA e oito HE, com idade inicial de nove meses e peso médio inicial de 220,31 kg, que permaneceram confinados até que o peso da carcaça atingiu o mínimo de 190 kg (estimativa). Os animais da raça AA apresentaram maior consumo de MS, em % PV (2,27 vs 2,10%) e em g/kg0,75 (91,4 vs 86,4 g). Os animais que consumiram o maior nível de energia na dieta apresentaram maiores consumos de MS/dia (6,31 vs 5,71 kg), em PV (2,26 vs 2,11%) e em g/kg0,75 (92,28 vs 85,44 g), de energia digestível (ED), em Mcal/dia (20,58 vs 18,13 Mcal), e de PB, em kg/dia (0,845 vs 0,759 kg), além de maior ganho médio diário de peso (1,409 vs 1,250 kg). Os animais que consumiram o menor nível apresentaram maiores consumos de fibra em detergente neutro (FDN), em kg/dia (2,23 vs 2,07 kg), e de fibra em detergente ácido (FDA), em kg/dia (1,13 vs 1,01 kg). Os consumos de MS/dia, de FDN e de FDA, nos animais que consumiram o menor nível de energia, tiveram comportamento linear e, naqueles que receberam o maior nível, comportamento quadrático, frente aos períodos de confinamento. Para as características consumo de MS, em %PV e em g/kg0,75, nos tratamentos com menor nível de energia, o comportamento foi de forma cúbica e naqueles de maior nível, de forma quadrática. O consumo de ED apresentou, nos períodos, comportamento linear para o menor nível energético e cúbico para o maior nível.

Metal-insulator transition in Nd1-xEuxNiO 3 compounds

Polycrystalline Nd1-xEuxNiO3 (0≤x≤0.5) compounds were synthesized in order to investigate the character of the metal-insulator (MI) phase transition in this series. Samples were prepared through the sol-gel route and subjected to heat treatments at ∼1000 °C under oxygen pressures as high as 80bar. X-ray diffraction (XRD) and neutron powder diffraction (NPD), electrical resistivity ρ(T), and magnetization M(T) measurements were performed on these compounds. The NPD and XRD results indicated that the samples crystallize in an orthorhombic distorted perovskite structure, space group Pbnm. The analysis of the structural parameters revealed a sudden and small expansion of ∼0.2% of the unit cell volume when electronic localization occurs. This expansion was attributed to a small increase of ∼0.003 of the average Ni-O distance and a simultaneous decrease of ∼-0.5° of the Ni-O-Ni superexchange angle. The ρ(T) measurements revealed a MI transition occurring at temperatures ranging from TMI∼193 to 336K for samples with x ≤ 0 and 0.50, respectively. These measurements also show a large thermal hysteresis in NdNiO3 during heating and cooling processes, suggesting a first-order character of the phase transition at TMI. The width of this thermal hysteresis was found to decrease appreciably for the sample Nd 0.7Eu0.3NiO3. The results indicate that cation disorder associated with increasing substitution of Nd by Eu is responsible for changing the first-order character of the transition in NdNiO3. © 2006 IOP Publishing Ltd.

Organic geochemistry of ODP Leg 135 sediment samples

The average total organic carbon (TOC) content obtained after Rock-Eval/TOC analysis of 156 sediment samples from the eight sites cored during Leg 135 is 0.05%. Hence, the TOC content of Leg 135 sediments is extremely low. The organic matter that is present in these samples is probably mostly reworked and oxidized material. Ten sediment samples were selected for extraction and analysis by gas chromatography and gas chromatography-mass spectrometry. Very low amounts of extractable hydrocarbons were obtained and some aspects of the biomarker distributions suggest that these hydrocarbons are not representative of the organic matter indigenous to the samples. A sample of an oil seep from Pili, Tongatapu was also analyzed. The seep is a biodegraded, mature oil that shows many characteristics in common with previously published analyses of oil seeps from Tongatapu. Biomarker evidence indicates that its source is a mature, marine carbonate of probable Late Cretaceous-Early Tertiary age. The source rock responsible for the Tongatapu oil seeps remains unknown.

Sediment organic matter, grain size, and results of prediction models from northern North Atlantic and Arctic Seas

Sediment samples and hydrographic conditions were studied at 28 stations around Iceland. At these sites, Conductivity-Temperature-Depth (CTD) casts were conducted to collect hydrographic data and multicorer casts were conductd to collect data on sediment characteristics including grain size distribution, carbon and nitrogen concentration, and chloroplastic pigment concentration. A total of 14 environmental predictors were used to model sediment characteristics around Iceland on regional geographic space. For these, two approaches were used: Multivariate Adaptation Regression Splines (MARS) and randomForest regression models. RandomForest outperformed MARS in predicting grain size distribution. MARS models had a greater tendency to over- and underpredict sediment values in areas outside the environmental envelope defined by the training dataset. We provide first GIS layers on sediment characteristics around Iceland, that can be used as predictors in future models. Although models performed well, more samples, especially from the shelf areas, will be needed to improve the models in future.

Sediment descriptions, stage, calcium carbonate, organic carbon, delta 13C and geolipids at DSDP Hole 93-603B

Organic matter contents of black shales from the Cretaceous Hatteras and Blake-Bahama formations have been compared to those from surrounding organic-poor strata using C/N ratios, d13C values, and distributions of extractable and nonsolvent-extractable, long-chain hydrocarbons, acids, and alcohols. The proportion of marine and land-derived organic matter varies considerably among all samples, although terrigenous components generally dominate. Most black shales are hydrocarbon-poor relative to their organic-carbon concentrations. Deposition of the black shales in Hole 603B evidently occurred through turbiditic relocation from shallower landward sites and rapid reburial at this outer continental rise location under generally oxygenated bottom-water conditions.