910 resultados para High-pressure processing
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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
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Biodiesel is a fuel made up by mono-alkyl-esters of long chain fatty acids, derived from vegetable oils or animal fat. This fuel can be used in compression ignition engines for automotive propulsion or energy generation, as a partial or total substitute of fossil diesel fuel. Biodiesel can be processed from different mechanisms. Transesterification is the most common process for obtaining biodiesel, in which an ester compound reacts with an alcohol to form a new ester and a new alcohol. These reactions are normally catalyzed by the addition of an acid or a base. Initially sunflower, castor and soybean oil physicochemical properties are determined according to standard test methods, to evaluate if they had favorable conditions for use as raw material in the transesterification reaction. Sunflower, castor and soybean biodiesel were obtained by the methylic transesterification route in the presence of KOH and presented a yield above 93% m/m. The sunflower/castor and soybean/castor blends were studied with the aim of evaluating the thermal and oxidative stability of the biofuels. The biodiesel and blends were characterized by acid value, iodine value, density, flash point, sulfur content, and content of methanol and esters by gas chromatography (GC). Also studies of thermal and oxidative stability by Thermogravimetry (TG), Differential Scanning Calorimetry High Pressure (P-DSC) and dynamic method exothermic and Rancimat were carried out. Biodiesel sunflower and soybean are presented according to the specifications established by the Resolution ANP no 7/2008. Biodiesel from castor oil, as expected, showed a high density and kinematic viscosity. For the blends studied, the concentration of castor biodiesel to increased the density, kinematic viscosity and flash point. The addition of castor biodiesel as antioxidant in sunflower and soybean biodiesels is promising, for a significant improvement in resistance to autoxidation and therefore on its oxidative stability. The blends showed that compliance with the requirements of the ANP have been included in the range of 20-40%. This form may be used as a partial substitute of fossil diesel
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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
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A hemoglobina fetal - Hb F, formada por duas cadeias gama e duas cadeias alfa, é característica do período fetal do desenvolvimento, tendo sua síntese diminuída no período pós-natal. em algumas alterações hereditárias, a Hb F permanece aumentada, como nas delta-beta talassemia, beta talassemia e persistência hereditária de Hb F (PHHF). A síntese da globina gama também pode ser estimulada por fatores externos como leucemias, transplantes de medula óssea, induções químicas, dentre outros. Através da observação de Hb F aumentada em doadores de sangue por procedimentos eletroforéticos objetivou-se avaliar a quantidade de Hb F em amostras de sangue de candidatos à doação, visando estabelecer seus limites de normalidade na população de São José do Rio Preto e região, por meio de desnaturação alcalina e cromatografia líquida de alta pressão (HPLC), comparar as metodologias aplicadas e, nos indivíduos com Hb F aumentada, realizar estudos moleculares para identificar as mutações que alteram a expressão dos genes gama. Foram analisadas 208 amostras de sangue, sendo 119 de candidatos à doação e 89 de indivíduos sem sintomas de anemia ou achados hematológicos e com Hb F aumentada como grupo comparativo. Das 119 amostras de candidatos à doação, 110 foram utilizadas para traçar o perfil de normalidade de Hb F, comparando-se as metodologias de desnaturação alcalina e HPLC, onde se obteve a média de 1,48% e de 0,6%, respectivamente. A análise estatística por regressão linear mostrou diferença significativa na comparação entre as duas metodologias aplicadas, sendo a HPLC mais precisa para a quantificação de Hb F. Foram observados nos testes de rastreamento de hemoglobinas anormais nestas 110 amostras de sangue: 16,4% de alfa talassemia, 0,9% com Hb F aumentada, 0,9% com beta talassemia e 0,9% com hemoglobina variante de cadeia delta. Os outros nove doadores de sangue apresentaram Hb F acima de 10% em eletroforese e observou-se média de 32,28% para desnaturação alcalina e de 26,4% para HPLC. As análises moleculares por PCR-ASO foram realizadas na tentativa de se identificar um defeito genético que pudesse explicar o aumento de Hb F, pelo rastreamento de 16 mutações que originam talassemias do tipo beta. Encontraram-se 5,3% de heterozigotos para mutação CD6-A e 1,75% para as mutações CD 39, IVS1:6, -87 e IVS2:654, todas em heterozigose. Os resultados encontrados neste estudo evidenciam a necessidade de melhor caracterização dos perfis de hemoglobina obtidos pelos métodos clássicos e a importância de sua caracterização molecular.
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New structural data from Elephant Island and adjacent islands are presented with the objective to improve the understanding of subduction kinematics in the area northeast of the Antarctic Peninsula. on the island, a first deformation phase, D-1, produced a strong SL fabric with steep stretching and mineral lineations, partly defined by relatively high pressure minerals, such as crossite and glaucophane. D-1 is interpreted to record southward subduction along an E-W trench with respect to the present position of the island. A second phase, D-2, led to intense folding with steep E-W-trending axial surfaces. The local presence of sinistral C'-type sheer bands related to this phase and the oblique inclination of the L-2 stretching lineations are the main arguments to interpret this phase as representing oblique sinistral transpressive shear along steep, approximately E-W-trending shear zones, with the northern (Pacific) block going down with respect to the southern (Antarctic Peninsula) block. The sinistral strike-slip component may represent a trench-linked strike-slip movement as a consequence of oblique subduction. Lithostatic pressure decreased and temperature increased to peak values during D-2, interpreted to represent the collision of thickened oceanic crust with the active continental margin. The last deformation phase, D-3, is characterised by post-metamorphic kink bands, partially forming conjugate sets consistent with E-W shortening and N-S extension. The rock units that underlie the island probably rotated during D-3, in Cenozoic times, together with the trench, from an NE-SW to the present ENE-WSW position, during the progressive opening of the Scotia Sea. The similarity between the strain orientation of D-3 and that of the sinistral NE-SW Shackleton Fracture Zone is consistent with this interpretation. (C) 2000 Elsevier B.V. B.V. All rights reserved.
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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
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Embora espalhantes-adesivos sejam considerados importantes em pulverizações, existem dúvidas quanto à sua utilidade em pulverizações a alto volume quando o escorrimento é maior, como nas aplicações com equipamentos tipo pistola, para o controle de Brevipalpus phoenicis (Geijskes). Dois ensaios de campo foram conduzidos, em 1991 e 1994, em pomar de citros cv. Natal. As pulverizações foram realizadas com pulverizador tratorizado equipado com pistolas de alta pressão usando 18 l e 11 l de calda/planta, respectivamente. Efeitos dos espalhante-adesivo foi avaliado contando-se o número de ácaros antes e após a aplicação. Não se verificaram diferenças sensíveis na retenção do líquido pulverizado nas folhas de citros quando se adicionou o espalhante-adesivo à calda com propargite. Redução de até 95,6% na população do ácaro foi obsevada com o aumento na dosagem do propargite e de até 98,9% em relação de menor dosagem para o cyhexatin. Constatou-se que o espalhante-adesivo não melhorou a eficiência do cyhexatin, embora a somatória dos totais de ácaros, independentemente da dosagem e da formulação, tenha sido 50,1% menor com o uso de espalhante-adesivo.
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O objetivo deste trabalho foi testar duas formas de hidrólise do bagaço de cana (com [17kgf/cm²]e sem [4kgf/cm²] rápida descompressão pós-hidrólise) e dois níveis de concentrado (25 e 45% MS) no desempenho e na composição corporal de novilhas em crescimento sob regime confinado durante 112 dias. Vinte e quatro novilhas Nelore e 12 Canchim foram distribuídas em delineamento de blocos casualizados em arranjo fatorial 2x2. Os resultados demonstraram que a omissão da explosão pós-hidrólise e o uso de níveis mais elevados de concentrado aumentaram o ganho de peso e o consumo de alimentos. Os resultados para ganho de peso e consumo de matéria seca, respectivamente, para tratamento sem vs com descompressão e 45 vs 25% de concentrado, foram 0,76 vs 0,67 e 0,76 vs 0,66 kg/d e 6,7 vs 5,8 e 6,8 vs 5,7 kg/dia. Entretanto, não houve diferença entre os tratamentos para conversão alimentar. Não foram observadas diferenças entre os tratamentos quanto à composição corporal determinada por meio do espaço de deutério ao final do período de confinamento, embora a taxa estimada de deposição de lipídios tenha sido maior para o tratamento sem explosão (216 vs 175 g/d) e o tratamento com 45% de concentrado (225 vs 166 g/d). Não foram observadas vantagens na descompressão rápida pós-hidrólise em alta pressão na eficiência de conversão de alimentos. Os resultados demonstram que animais alimentados com bagaço hidrolisado em níveis altos de ingestão (2,9% PV) e proporções baixas de concentrado apresentaram eficiência de utilização da dieta semelhante a dietas com níveis mais altos de concentrado.
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The Eastern Blue Ridge Province of the southern Appalachians contains, in part, remnants of an Ordovician accretionary wedge complex formed during subduction of an oceanic tract before mid-Ordovician accretion with Laurentia. The Eastern Blue Ridge Province consists of metapelite and amphibolite intruded by low-K plutons, high-temperature (T > 750 degrees C) Ordovician eclogite, and other high-pressure metamafic and meta-ultramatic rocks. Felsic plutons in the Eastern Blue Ridge Province are important time markers for regional-scale tectonics, deformation, and metamorphism. Plutons were thought to be related to either Taconian (Ordovician) or Acadian (Devonian-Silurian) tectonothermal events.We dated five plutonic or metaplutonic rocks to constrain pluton crystallization ages better and thus the timing of tectonism. The Persimmon Creek gneiss yielded a protolith crystallization age of 455.7 +/- 2.1 Ma, Chalk Mountain 377.7 +/- 2.5 Ma, Mt. Airy 334 +/- 3 Ma, Stone Mountain 335.6 +/- 1.0 Ma, and Rabun 335.1 +/- 2.8 Ma. The latter four plutons were thought to be part of the Acadian Spruce Pine Suite, but instead our new ages indicate that Alleghanian (Carboniferous-Permian) plutonism is widespread and voluminous in the Eastern Blue Ridge Province. The Chattahoochee fault, which was considered an Acadian structure, cuts the Rabun pluton and thus must have been active during the Alleghanian orogeny. The new ages indicate that Persimmon Creek crystallized less than 3 m.y. after zircon crystallization in Eastern Blue Ridge eclogite and is nearly synchronous with nearby high-grade metamorphism and migmatization. The three phases of plutonism in the Eastern Blue Ridge Province correspond with established metamorphic ages for each of the three major orogenic pulses along the western flank of the southern Appalachians.
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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
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In this work, the performance of a-C: H films produced by the hybrid Plasma Immersion Ion Implantation and Deposition technique as lubricating layers for a steel forming tool has been investigated. Hardened steel (AISI M2, 64 HRC) plates coated with a commercial TiN layer were used as substrates and the films were deposited in a vacuum chamber fitted with two parallel-plate electrodes. The discharges were generated in atmospheres composed of 91% C2H2 and 9% Ar by the application of radiofrequency power (13.56 MHz, 100 W) to the upper electrode while the lower one, also used as the sample holder, was biased with high voltage negative pulses (3.6 kV, 30 mu s, 300 Hz). A deposition time of 840 s was used. The effects of the gas pressure, p, on thickness, molecular structure, wettability, surface morphology and topography, hardness and friction coefficient of the films lwere investigated. Film thickness increased from 0.3 to 0.5 mu m when p was increased from 2.7 to 16.5 Pa. Generally, the films were slightly hydrophilic, with contact angles of around 84 degrees, and the deposition decreased the roughness of the steel. A polymer-like structure was detected in high pressure depositions and an amorphous carbon structure derived from the low pressure procedures. Hardness decreased from 8.2 to 7.0 GPa with increasing p. Improvement in tribological performance was indicated by the fall in the friction coefficient from 0.5 to 0.2 as the deposition pressure was reduced. Operating at the latter value (of mu) would lead to a significant reduction in wear and hence to significant economy in diverse industrial applications.
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The influence of parietal cell vagotomy (PCV) on esophagogastric high pressure zone (HPZ) (pressure and length) was studied in 30 dogs. The animals were divided in 3 groups: group 1, 10 dogs submitted to PCV with gastric denervation until the esophagogastric junction; group 2, 10 dogs submitted to PCV with gastric denervation into esophagogastric junction and 3 cm above this; group 3 (control), 10 dogs submitted to laparotomy only. In the postoperative period (immediate and later) it wasn't observed any alteration of pressure and length of esophagogastric HPZ in three studied groups.
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The Araguaia-Tocantins geosuture, which separates the Araguaia Fold Belt (AFB) from the Archean Amazonian Craton, was active in the late Middle Proterozoic. The Baixo Araguaia Supergroup was deposited, consisting of the Estrondo Group (lower quartzites with intercalated schists), Xambioá Formation (schists), and Canto da Vazante Formation (upper feldspathic schists); and the Tocantins Group consisting of the Couto Magalhaës Formation (phyllites, quartzites, slates, limestones, and metacherts) and Pequizeiro Formation (upper chlorite schists); and associated mafic-ultramafic bodies. The deformational history includes four regional phases of deformation within this supracrustal sequence: recumbent folds with vergence to the west; refolding with a N-S trend; an intense crenulation episode; and late thrusting from east to west. Metamorphism is of intermediate or intermediate-high pressure type with garnet, biotite, chlorite, and sericite isograds succeeded by a slightly or non-metamorphosed zone, from east to west. Rocks surrounding sparse gneissic-cored domes contain isograds of staurolite, kyanite, and fibrolite. These isograds are believed to be associated with the 1100 Ma Uruaçuano event. The Brasiliano Orogeny strongly affected the AFB with displacements due to transcurrent reactivation of great and old faults of the basement, slight folding in the supracrustal sequence, intrusion of small granite bodies, and development of domes with associated normal faults. The area underlain by the Estrondo Group was uplifted at this time, causing the deposition of the Rio das Barreiras polymictic conglomerate of the central area. K-Ar and Rb-Sr analyses date this thermo-tectonic event at 550 ± 100 Ma. The Archean basement is exposed in the cores of domes as a granite-gneiss association, the Colméia complex, which shows thermo-tectonic features that may be interpreted as polycyclic imprints (Jequié, Transamazonian?, Uruaçuano, and Brasiliano Events). © 1989.