900 resultados para Ultra high-pressure homogenization (UHPH)


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One of the models proposed for the origin of ultra high energy cosmic rays (UHECR's) suggests that these events are the decay products of relic superheavy metastable particles, which we call S particles. These particles can be produced in the reheating period following the inflationary epoch of the early Universe. We study this possibility and obtain constraints on some parameters such as the lifetime and direct couplings of the X-particle to the inflaton field from the requirement that they are responsible for the observed UHECR flux.

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The Poincar, group generalizes the Galilei group for high-velocity kinematics. The de Sitter group is assumed to go one step further, generalizing Poincar, as the group governing high-energy kinematics. In other words, ordinary special relativity is here replaced by de Sitter relativity. In this theory, the cosmological constant I > is no longer a free parameter, and can be determined in terms of other quantities. When applied to the whole universe, it is able to predict the value of I > and to explain the cosmic coincidence. When applied to the propagation of ultra-high energy photons, it gives a good estimate of the time delay observed in extragalactic gamma-ray flares. It can, for this reason, be considered a new paradigm to approach the quantum gravity problem.

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

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

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

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

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The prevalence of Mycobacterium bovis and other mycobacterial species in livestock specimens and milk was evaluated. An emphasis was placed upon the distribution of these organisms in milk that is readily available to the public that was either untreated, pasteurized, or treated using ultra high temperature. Twenty-two pathologic specimens from livestock (bovine, swine and bubaline) in five Brazilian states and 128 bovine milk samples from retail markets in the State of São Paulo were examined for mycobacteria. Identification was made by classical biochemical tests, thin layer chromatography of mycolic acids and polymerase chain reaction-restriction fragment length polymorphism (PCR-RFLP) analysis. Mycobacteria were isolated from 15 (68.2%) caseous lesions and from 23 (18%) milk samples. Eleven isolates were identified as M. bovis, and the remaining 27 nontuberculous mycobacterial isolates were represented by five species and six unidentified rapidly growing mycobacterial strains. The data demonstrate that animal products in Brazil are frequent reservoirs of mycobacteria and may pose a risk to the public.

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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)