Frações Nitrogenadas, Glicídicas e Amônia Liberada pela Cama de Frangos de Corte em Diferentes Densidades e Tempos de Confinamento

O presente trabalho foi conduzido com o objetivo de estudar a liberação de amônia pela cama de frangos de corte, bem como o teor de umidade e de compostos glicídicos (carboidratos redutores) e nitrogenados (nitrogênio total, nitrogênio solúvel total e nitrato) presentes na mesma, em função da densidade populacional, tempo de confinamento e sexo das aves. Realizou-se o experimento em delineamento inteiramente casualizado. A cama de frango foi submetida às densidades de 10; 14; 18 e 22 aves/m² de piso, para ambos os sexos, e analisada em três épocas diferentes (24, 38 e 42 dias de idade das aves), utilizando-se de esquema fatorial 4x2x3 (densidades x sexos x épocas). de modo geral, observou-se que o sexo não influenciou o comportamento das variáveis estudadas. O aumento da densidade e o avanço da época de amostragem induziram a aumentos da quantidade de amônia liberada, do teor de umidade e dos teores de nitrogênio total e de nitrogênio solúvel, bem como diminuição do teor de carboidratos redutores. Estes resultados sugerem a necessidade de um controle rigoroso da amônia no ar dos galpões, principalmente em densidades elevadas e no período final de criação.

Análise dos compostos flavorizantes da cana-de-açúcar e otimização da aplicação de extratos ricos em β-glicosidases para liberação de aroma na produção de aguardente de cana

Pós-graduação em Química - IBILCE

Distribuição espacial e raio de agregação de cancro cítrico definidos por geoestatística

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Epidemiologia espacial e sorológica da hanseníase no estado do Pará

Mais de 80.000 casos de hanseníase foram diagnosticados nos últimos 20 anos no Pará e, ainda hoje, com um coeficiente de detecção anual de 50/100.000 habitantes (três vezes superior à média nacional) a doença permanece como um grave problema de saúde pública neste Estado. O objetivo geral deste estudo foi desenvolver um método integrando a epidemiologia espacial e sorológica como ferramenta de combate à hanseníase no Pará. Inicialmente, foram realizadas visitas domiciliares a famílias de pessoas afetadas pela hanseníase, diagnosticadas nos últimos cinco a seis anos, em oito municípios de diferentes regiões do Estado. A equipe de pesquisadores com experiência no manejo da hanseníase, composta por médicos dermatologistas, enfermeiros, fisioterapeutas e técnicos de laboratório, realizou exame clínico dermatoneurológico em 1.945 contatos intradomiciliares de 531 casos notificados e coletou amostra de sangue para pesquisa sorológica de anticorpos IgM anti-PGL-I. Além disso, 1.592 estudantes de 37 escolas públicas do ensino fundamental e médio, com idade entre 6 e 20 anos, também foram selecionados aleatoriamente para serem submetidos à mesma avaliação. As residências dos casos notificados, bem como a dos estudantes incluídos no estudo foram georreferenciadas para a análise da distribuição espacial da hanseníase. Dois anos mais tarde, com base na informação sorológica prévia, a equipe de pesquisadores retornou a dois municípios para reavaliar os indivíduos incluídos no estudo. Adicionalmente, duas novas escolas públicas localizadas em áreas de alto risco de hanseníase, determinadas pela análise da distribuição espacial da doença em um dos municípios, foram selecionadas para avaliar-se a importância da informação geográfica na detecção de casos novos. Na avaliação inicial, 156 (8%) contatos e 63 (4%) estudantes foram diagnosticados como casos novos de hanseníase; 806 (41,4%) contatos e 777 (48,8%) estudantes foram soropositivos para anti-PGL-I. A análise da distribuição espacial dos casos registrados da doença em um dos municípios selecionados indicou que a hanseníase apresenta um padrão heterogêneo, com clusters de alta e baixa taxa de detecção anual em áreas específicas da cidade (p < 0,01), e que 94,7% dos estudantes examinados residiam a menos de 200 metros de um caso registrado durante os seis anos anteriores ao estudo. No seguimento, a incidência de hanseníase foi significativamente maior entre os indivíduos soropositivos (22,3%) quando comparados aos soronegativos (9.4%) (OR = 2,7; IC95% = 1,29 – 5,87; p = 0,01); também foi significativamente mais alta entre moradores de residências com pelo menos um sujeito soropositivo (17,4%), comparada aos de residências sem nenhum morador soropositivo (7,4%) (OR = 2,6; IC95% = 1,18 – 5,91; p = 0,02). A seleção de escolas localizadas em áreas de maior risco dentro do município aumentou significativamente a eficiência na detecção de casos novos entre escolares (8,2%), quando comparada aos resultados obtidos em escolas selecionadas aleatoriamente (4%) (p = 0,04). Os dados mostram alta taxa de prevalência oculta de hanseníase e de infecção subclínica pelo M. leprae no Pará. A epidemiologia espacial e sorológica são ferramentas eficazes para aumentar a detecção precoce de casos novos e deveriam ser utilizadas pelos municípios do Pará para que o Estado possa finalmente alcançar as metas de controle da hanseníase.

A new biomimetic sensor based on molecularly imprinted polymers for highly sensitive and selective determination of hexazinone herbicide

A new selective sensor based on molecularly imprinted polymers (MIPs) was developed for the determination of hexazinone (HXZ) in environmental samples. MIPs were synthesized using a non-covalent approach, and selection of the monomers employed in the polymerization reaction was carried out by molecular modeling. Three functional monomers with high (2-vinylpyridine (MP17)) and intermediate (methacrylic acid (MP12) and acrylamide (MP5)) energies of binding to the template (HXZ) were selected for preparation of the MIPs, in order to conduct comparative studies and validate the theoretical data. For sensor construction, carbon pastes were modified with each MIP or NIP (non-imprinted polymer), and HXZ determination was performed using differential pulse adsorptive cathodic stripping voltammetry (DPAdCSV). All parameters affecting the sensor response were optimized. In HCl at pH 2.5, the sensor prepared with MP17 (5% w/w in the paste) showed a dynamic linear range between 1.9 × 10−11 and 1.1 × 10−10 mol L−1, and a detection limit of 2.6 × 10−12 mol L−1, under the following conditions: accumulation time of 200 s at a potential of −0.5V, scan rate of 50 mVs−1, pulse amplitude of 60 mV, and pulse width of 50 ms. The sensor was selective in the presence of other similar compounds, and was successfully applied to the analysis of HXZ in river water samples.

Detection of several carbohydrates using boron-doped diamond electrodes modified with nickel hydroxide nanoparticles

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

Messung der semileptonischen Ξ°-Zerfälle mit dem NA48/1-Detektor

Im Jahre 2002 wurde mit dem NA48/1-Detektor eine Datennahme mit hoher Intensität von K_S-Mesonen und neutralen Hyperonen durchgeführt, bei der unter anderem etwa 10^9 Xi^0-Zerfallskandidaten aufgezeichnet wurden. Im Rahmen dieser Arbeit wurden aus diesem Datensatz 6657 Xi^0 -> Sigma^+ e^- Anti-nü und 581 Anti-Xi^0 -> Anti-Sigma^+ e^+ nü-Ereignisse ausgewählt und damit die Verzweigungsverhältnisse BR1(Gamma(Xi^0 -> Sigma^+ e^- Anti-nü)/Gamma(Xi^0 total))=( 2.533 +-0.032(stat) -0.076+0.089(syst) )10^-4 und BR2(Gamma(Anti-Xi^0 -> Anti-Sigma^+ e^+ nü)/Gamma(Anti-Xi^0 total))= ( 2.57 +-0.12(stat) -0.09+0.10(syst) )10^-4 bestimmt. Dieses Ergebnis für BR1 ist etwa 3.5-mal genauer als die bisher veröffentlichte Messung. Die Analyse der Anti-Xi^0-Beta-Zerfälle stellt die erste Messung von BR2 dar. Beide Ergebnisse stimmen mit der theoretischen Vorhersage von 2.6*10^-4 überein. Aus dem Xi^0-Beta-Verzweigungsverhältnis folgt unter Verwendung des experimentellen Wertes des Formfaktorverhältnisses g1/f1 für das CKM-Matrixelement |Vus| = 0.209 +- 0.004(exp) +- 0.026(syst), wobei die dominierende Unsicherheit von g1/f1 herrührt. Außerdem wurden in dieser Arbeit 99 Xi^0 -> Sigma^+ mu^- Anti-nü Zerfallskandidaten mit einem abgeschätzten Untergrund von 30 Ereignissen rekonstruiert und daraus ebenfalls das Verzweigungsverhältnis extrahiert: BR3(Gamma(Xi^0 -> Sigma^+ mu^- Anti-nü)/Gamma(Xi^0 total)) = ( 2.11 +- 0.31(stat) +- 0.15(syst) )10^-6.

Development and characterization of chemical cochleostomy in the Guinea pig

OBJECTIVES Creation of an atraumatic, hearing-preservation cochleostomy is integral to the future of minimally invasive inner ear surgery. The goal of this study was to develop and characterize a novel chemical approach to cochleostomy. STUDY DESIGN Prospective animal study. SETTING Laboratory. METHODS Experimental animal study in which phosphoric acid gel (PAG) was used to decalcify the otic capsule in 25 Hartley guinea pigs. Five animals in each of 5 surgical groups were studied: (1) mechanically opening the auditory bulla alone, (2) PAG thinning of the basal turn otic capsule, leaving endosteum covered by a layer of bone, (3) micro-pick manual cochleostomy, (4) PAG chemical cochleostomy, exposing the endosteum, and (5) combined PAG/micro-pick cochleostomy, with initial chemical thinning and subsequent manual removal of the last osseous layer. Preoperative and postoperative auditory brainstem responses and otoacoustic emissions were obtained at 2, 6, 10, and 16 kHz. Hematoxylin and eosin-stained paraffin sections were compared. RESULTS Surgical and histologic findings confirmed that application of PAG provided reproducible local bone removal, and cochlear access was enabled. Statistically significant auditory threshold shifts were observed at 10 kHz (P = .048) and 16 kHz (P = .0013) following cochleostomy using PAG alone (group 4) and at 16 kHz using manual cochleostomy (group 3) (P = .028). No statistically significant, postoperative auditory threshold shifts were observed in the other groups, including PAG thinning with manual completion cochleostomy (group 5). CONCLUSION Hearing preservation cochleostomy can be performed in an animal model using a novel technique of thinning cochlear bone with PAG and manually completing cochleostomy.

Chemical and isotopic analysis of bulk organic matter and hydrocarbon biomarkers from IODP Holes 311-U1327C, 311-U1328B and 311-U1328C

The chemical and isotopic compositions of sedimentary organic matter (SOM) from two mid-slope sites of the northern Cascadia margin were investigated during Integrated Ocean Drilling Program (IODP) Expedition 311 to elucidate the organic matter origins and identify potential microbial contributions to SOM. Gas hydrate is present at both locations (IODP Sites U1327 and U1328), with distinct patterns of near-seafloor structural accumulations at the cold seep Site U1328 and deeper stratigraphic accumulations at the slope-basin Site U1327. Source characterization and evidence that some components of the organic matter have been diagenetically altered are determined from the concentrations and isotopic compositions of hydrocarbon biomarkers, total organic carbon (TOC), total nitrogen (TN) and total sulfur (TS). The carbon isotopic compositions of TOC (d13C TOC = -26 to -22 per mil) and long-chain n-alkanes (C27, C29 and C31, d13C = -34 to -29 per mil) suggest the organic matter at both sites is a mixture of 1) terrestrial plants that employ the C3 photosynthetic pathway and 2) marine algae. In contrast, the d15N TN values of the bulk sediment (+4 to +8 per mil) are consistent with a predominantly marine source, but these values most likely have been modified during microbial organic matter degradation. The d13C values of archaeal biomarker pentamethylicosane (PMI) (-46.4 per mil) and bacterial-sourced hopenes, diploptene and hop-21-ene (-40.9 to -34.7 per mil) indicate a partial contribution from methane carbon or a chemoautotrophic pathway. Our multi-isotope and biomarker-based conclusions are consistent with previous studies, based only on the elemental composition of bulk sediments, that suggested a mixed marine-terrestrial organic matter origin for these mid-slope sites of the northern Cascadia margin.

Organic carbon, age, lithology, and CPI-alkenes at DSDP Sites 57-440 and 56-436

"Bound" and "free" solvent-extractable lipids have been examined from Sections 440A-7-6, 440B-3-5, 440B-8-4, 440B-68-2, and 436-11-4. The compound classes studied include aliphatic and aromatic hydrocarbons, ketones, alcohols, and carboxylic acids. Carotenoids and humic acids have also been examined. The quantitative results are considered in terms of input indicators, diagenesis parameters, and structural classes. A difference in input is deduced across the Japan Trench, with a higher proportion of autochthonous components on the western inner trench slope compared with the more easterly, outer trench, wall and greater input in the early Pleistocene than in the Miocene. A variety of diagenetic transformations is observed at Site 440 as sample depth increases. Results are compared with those of samples from Atlantic Cretaceous sediments and from the Walvis Bay high productivity area.

(Appendix) Petrographic information, trace element and Sr isotope ratios of Pito Deep samples

Fluid flow through the axial hydrothermal system at fast spreading ridges is investigated using the Sr-isotopic composition of upper crustal samples recovered from a tectonic window at Pito Deep (NE Easter microplate). Samples from the sheeted dike complex collected away from macroscopic evidence of channelized fluid flow, such as faults and centimeter-scale hydrothermal veins, show a range of 87Sr/86Sr from 0.7025 to 0.7030 averaging 0.70276 relative to a protolith with 87Sr/86Sr of ~0.7024. There is no systematic variation in 87Sr/86Sr with depth in the sheeted dike complex. Comparison of these new data with the two other localities that similar data sets exist for (ODP Hole 504B and the Hess Deep tectonic window) reveals that the extent of Sr-isotope exchange is similar in all of these locations. Models that assume that fluid-rock reaction occurs during one-dimensional (recharge) flow lead to significant decreases in the predicted extent of isotopic modification of the rock with depth in the crust. These model results show systematic misfits when compared with the data that can only be avoided if the fluid flow is assumed to be focused in isolated channels with very slow fluid-rock exchange. In this scenario the fluid at the base of the crust is little modified in 87Sr/86Sr from seawater and thus unlike vent fluids. Additionally, this model predicts that some rocks should show no change from the fresh-rock 87Sr/86Sr, but this is not observed. Alternatively, models in which fluid-rock reaction occurs during upflow (discharge) as well as downflow, or in which fluids are recirculated within the hydrothermal system, can reproduce the observed lack of variation in 87Sr/86Sr with depth in the crust. Minimum time-integrated fluid fluxes, calculated from mass balance, are between 1.5 and 2.6 * 10**6 kg/m**2 for all areas studied to date. However, new evidence from both the rocks and a compilation of vent fluid compositions demonstrates that some Sr is leached from the crust. Because this leaching lowers the fluid 87Sr/86Sr without changing the rock 87Sr/86Sr, these mass balance models must underestimate the time-integrated fluid flux. Additionally, these values do not account for fluid flow that is channelized within the crust.