Poole-Frenkel effect in amorphous poly(p-phenylene sulfide)

The conductivity of poly(p-phenylene sulfide) (PPS) amorphous samples sandwiched between metallic electrodes has been studied as a function of applied voltage, temperature, and electrode material. The voltage (U) dependence of the currents for electric fields within the range 10(3)-10(6) V/cm exhibits exp beta U-1/2 behavior with beta = beta(Schottky) below the glass transition temperature (T-g congruent to 90 degrees C), and beta = beta(Poole-Frenkel) above T-g. Coordinated temperature measurements of de currents with different metallic contacts and thermally stimulated currents (TSC) indicate, however, that the conductivity at T < T-g is consistent with the so-called ''anomalous'' Poole-Frenkel effect rather than the Schottky effect. Consequently, the p-type conductivity in amorphous PPS is proposed to be a bulk-limited process due to ionization of two different types of acceptor centers in the presence of neutral hole traps. (C) 1996 John Wiley & Sons, Inc.

Geothermal investigations in an area of induced seismic activity, northern São Paulo State, Brazil

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Permanent Magnet Hall Thruster for satellite orbit raising with low power energy consumption

Electric propulsion is now a succeful method for primary propulsion of deep space long duration missions and for geosyncronous satellite attitude control. Closed Drift Thruster, so called Hall Thruster or SPT (Stationary Plasma Thruster), was primarily conceived in USSR (the ancient Soviet Union) and, since then, it has been developed by space agencies, space research institutes and industries in several countries such as France, USA, Israel, Russian Federation and Brazil. In this work we present the main features of the Permanent Magnet Hall Thruster (PMHT) developed at the Plasma Laboratory of the University of Brasilia. The idea of using an array of permanent magnets, instead of an electromagnet, to produce a radial magnetic field inside the plasma channel of the thruster is very significant. It allows the development of a Hall Thruster with power consumption low enough to be used in small and medium size satellites. Description of a new vacuum chamber used to test the second prototype of the PMHT (PHALL II) will be given. PHALL II has an aluminum plasma chamber and is smaller with 15 cm diameter and will contain rare earth magnets. We will show plasma density and temperature space profiles inside and outside the thruster channel. Ion temperature measurements based on Doppler broadening of spectral lines and ion energy measurements are also shown. Based on the measured plasma parameters we constructed an aptitude figure of the PMHT. It contains the specific impulse, total thrust, propellant flow rate and power consumption necessary for orbit raising of satellites. Based on previous studies of geosyncronous satellite orbit positioning we perform numerical simulations of satellite orbit raising from an altitude of 700 km to 36000 km using a PMHT operating in the 100 mN - 500 mN thrust range. In order to perform these calculations integration techniques were used. The main simulation paraters were orbit raising time, fuel mass, total satellite mass, thrust and exaust velocity. We conclude comparing our results with results obtainned with known space missions performed with Hall Thrusters. © 2008 by the American Institute of Aeronautics and Astronautics, Inc.

Programação, conexão e avaliação de psicrômetro aspirado de termopar de baixo custo em micrologger para estudos agrometeorológicos

As the psychrometric method is considered standard for the measurement of relative humidity, many studies have used aspirated thermocouple psychrometers connected to microloggers but, however, they do not detail how the aspiration of the air stream is done. However, one of the major difficulties of aspirated thermocouple psychrometers is to program and to connect it in micrologger, because specific programming and connection are requires, and still some skills in getting accurate measurements. This work aimed to provide the programming and the connection of the aspirated thermocouple psychrometer type T for the CR10X microloggers and CR23X of Campbell Scientific, evaluating the quality of measurements of temperature and air relative humidity in relation the a sensor Vaisala HMP50. The non-continuous measurements were made in the period 2006/09/04 to 2007/07/11 at Jaboticabal, SP. The air temperature measurements were similar between the Vaisala sensors and aspirated thermocouple psychrometer, but the relative humidity measurements were significantly different. The measurements obtained by the aspirated thermocouple psychrometer connected to CR10X micrologger were the most accurate. Using the programming and connection of a micro-fan to suck in the dry and moist bulbs of aspirated thermocouple psychrometer in microloggers models CR10X and CR23X, it is possible to obtain measurements of air temperature with good precision and accuracy, and measurements of air relative humidity with good precision, but accuracy is not always attainable due to the difficulties inherent to the physical processes that occur in the wet bulb, the skill in the use and maintenance of this equipment and the reservoir protection against radiative effects.

Análise experimental e numérica de convecção forçada em arranjo de obstáculos dentro de canal

Pós-graduação em Engenharia Mecânica - FEIS

Avaliação da eficácia do firocoxib em comparação à fenilbutazona na sinovite induzida por lipopolissacarídeo em equinos

Pós-graduação em Medicina Veterinária - FCAV

Transferência de calor em leitos fixos com aplicação em reatores de fermentação em estado sólido

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Estimulação tátil em coelhos do grupo genético Botucatu e seus efeitos no desempenho, temperamento e reprodução

Pós-graduação em Zootecnia - FCAV

Investigação de contatos elétricos e propriedades de filmes finos de SnO2 dopados com os íons terras raras Eu3+ e Ce3+

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Dinâmica do carbono dissolvido no Rio Acre: variações espaciais e sazonais

Este trabalho teve como principal objetivo estudar a dinâmica do carbono dissolvido ao longo de um trecho do rio Acre, avaliando a influência da área urbana da cidade de Rio Branco, e da descarga de três de seus tributários (Riozinho do Rola, igarapé Judia, igarapé São Francisco), bem como a influência das mudanças hidrológicas sazonais. Foram realizadas campanhas de campo mensais, entre dezembro de 2006 e setembro de 2007, em cinco sítios no rio Acre e um sítio na foz de cada um dos três tributários. A cada amostragem 1 litro de amostra de água era submetida a filtração e dividida em alíquotas para as análises de carbono orgânico dissolvido (COO), carbono inorgânico dissolvido (CIO) e íons maiores (Ca² + , Mg² + , K + , Na + , NH 4 + , HCO 3 -, Cl¯, SO 4 ²¯, NO 3 - , NO 2 - , e PO 4 3-) . Além das coletas foram medidos in situ os parâmetros físico-químicos pH, condutividade elétrica, oxigênio dissolvido e temperatura da água. O pH médio anual no rio Acre variou de 6,46 a 6,54 entre os sítios e a condutividade elétrica apresentou valores médios anuais entre os sítios que variam de 69,93 a 77,84 µS cm¯¹. Nos tributários, os valores médios anuais de pH variaram de 6,10 a 6,51 e a condutividade elétrica apresentou valores médios anuais que variaram entre 54,08 e 153,03 S cm¯¹. Os cátions predominantes no rio Acre e nos tributários foram o Na + e o Ca 2+ e os ânions foram o cr e o sol-. A concentração média anual de COD no rio Acre variou de 4,62 a 5,17 mg l¯¹, sem diferenças significativas entre os sítios de amostragem. Nos tributários as médias anuais, de COD variaram de 3,55 a 6,55 mg r1. As concentrações foram, significativamente maiores no período de cheia, com médias que variaram de 6,26 a 6,39 mg l¯¹ nos sítios do rio Acre. O igarapé São Francisco foi o único tributário que não apresentou diferenças entre os períodos sazonais. O CID teve uma concentração média anual no rio Acre que variou de 527,91 a 598,18 µM, sem diferenças significativas entre os sítios de amostragem. As maiores concentrações foram observada na seca, quando as concentrações médias variaram de 816,31 a 998,52 µM. Nos tributários as concentrações médias anuais de CID variaram de 248,54 a 986,50 µM.Quanto a pressão parcial do CO2 (pCO 2 ) , os sítios no rio Acre apresentam valores médios anuais variando entre 3559 e 4059 ppm, sem diferenças entre os sítios e com os maiores valores ocorrendo no período de cheia. Com base nos resultados, pode-se concluir que a dinâmica do carbono dissolvido no rio Acre não apresenta variações significativas decorrentes das descargas dos tributários nem do lançamento de esgotos. Por outro lado, as mudanças hidrológicas sazonais são os maiores responsáveis pelas alterações nesta dinâmica.

Geotermia rasa em Belém

Um estudo detalhado de geotermia rasa foi realizado no intervalo de profundidade de 0,02 a 210,0 m, na região metropolitana de Belém. As medidas de temperatura foram efetuadas com o uso de termômetros de mercúrio e termistor, enquanto as medidas de condutividade térmica foram feitas em testemunhos de sondagem, utilizando-se o aparato tipo agulha. O fluxo de radiação solar incidente foi registrado com um actinógrafo do tipo Robitzech. O gradiente geotérmico médio obtido na região metropolitana de Belém foi de 0,0254 ± 0,0007 °C.m^-1. O valor médio de condutividade térmica dos testemunhos de sondagem coletados nesta região foi de 1,66 ± 0,52 W.m^-1.°C^-1. Por sua vez, o fluxo geotermal médio na região estudada é de 42,16 ± 1,14 mW.m^-2. A 1,0 m de profundidade ocorrem mudanças temporais nos valores de temperatura, as quais não podem ser consideradas como desprezíveis. Estas, mudanças estão diretamente relacionadas com as variações do fluxo de radiação solar incidente na superfície. O maior incremento deste fluxo, observado de um dia para o outro, foi de cerca de 30 W.m^-2, o que correspondeu a um aumento de temperatura a 1,0 m de profundidade da ordem de 0,22° C. Os perfis de temperatura obtidos durante este trabalho apresentaram deriva em sentidos alternados, durante o ciclo de período de um ano. Os perfis geotérmicos rasos são caracterizados por uma zona de fluxo de calor nulo, denominada "cotovelo", a partir da qual os valores de temperatura crescem com o aumento da profundidade. A profundidade do cotovelo é fundamentalmente influenciada pelo fluxo de calor gerado pela radiação solar incidente na superfície da área em estudo. Elaborou-se um modelo de evolução temporal o qual representa a estrutura térmica e suas variações, da zona compreendida de 0,02 a 10,0 m de profundidade. Os resultados oriundos deste modelo de transferência de calor por condução foram comparados com os obtidos em trabalhos de campo. Observa-se uma boa concordância entre esses resultados. Porém, o ajuste numérico é mais evidente para o período de setembro a fevereiro. Este modelamento poderá ser utilizado também para previsões de deriva dos perfis geotérmicos, desde que sejam conhecidos, a priori, os valores correspondentes às temperaturas médias mensais na superfície, o gradiente geotérmico regional e um dado perfil geotérmico. Este trabalho comprova que o fluxo de radiação solar incidente na superfície é a principal fonte de influência sobre os perfis geotérmicos rasos. A profundidade máxima dessa influência depende principalmente da magnitude desse fluxo, do grau de proteção superficial à incidência direta da radiação e da litologia do local em estudo.

Considerações gerais sobre a aplicação de esterco no processo de compostagem dos resíduos de poda e capina

In the category of the solid waste, are included the yard solid waste, this kind of solid waste are noble raw material and uncontaminated being recycled through the composting processing. Inside this context, it was studied the influence of horse manure in yard solid waste composting process, analyze the viability to compost the yard solid waste in UNESP Bela Vista. It was made four piles of composting, two of them are composed only by yard solid waste and the others are composed by horse manure and yard solid waste. The experiments were operated during 45 days. The evaluation of the process was made through temperature measurements of the piles daily during the test period. On the contrary of the piles with horse manure, the piles with no horse manure didn’t undergo complete maturation in the end of the experiment. Through the results obtained concluded that it was important to use manure horse in yard solid waste composting process to accelerate this process, because the piles without horse manure didn’t reach temperatures that characterize the composting process.

Compostagem dos Resíduos da FCT/UNESP de Presidente Prudente –SP

The present work aimed to study the composting process using two methods of treatment, conventional and mechanized for the treatment of pruning/weeding waste and organic waste generated in the canteens of the FCT/UNESP. For this work, it was quantified the generation of the waste However, of the tests with pure organic compound, which had the best result was T1 - 70% RPC / 30% ROC, again indicating the feasibility of applying this condition in scales at the campus. The conventional treatment by composting was carried out on manual aerated piles: 70% residue pruning/weeding (RPC) and 30% organic waste from the canteen (ROC); 50% RPC / 50% ROC, 30% RPC / 70% ROC. The mechanized system consisted of a reactor of 190 liters – 50% RPC / 50% ROC, with air injection from a compressor for 15 minutes daily. The parameters characterized and monitored were pH, organic matter, organic carbon, ash, nitrogen kjedahl and phosphorus. The temperature measurements were taken daily by a digital thermocouple (top, middle and base of the piles and reactor)... (Completo abstract click electronic access below)

Nanopartículas magnéticas como suporte para imobilização de lipases

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Dynamics of the cold surface layer of polythermal Storglaciären, Sweden

Polythermal glaciers, i.e. glaciers with a combination of ice at and below the freezing point, are widespread in arctic and subarctic environments. The polythermal structure has major implications for glacier hydrology, ice flow and glacial erosion. However, the interplay of factors governing its spatial and temporal variations such as net mass balance, ice advection and water content in the ice is poorly investigated and as yet not fully understood. This study deals with a thorough investigation of the polythermal regime on Storglaciären, northern Sweden, a small valley glacier with a cold surface layer in the ablation area. Extensive field work was performed including mapping of the cold surface layer using ground-penetrating radar, ice temperature measurements, mass balance and ice velocity measurements. Analyses of these data combined with numerical modelling were used specifically to investigate the spatial and temporal variability of the cold surface layer, the spatial distribution of the water content just below the cold surface layer transition, the effect of radar frequency on the detection of the surface layer, and the sensitivity of the cold surface layer to changes in forcing. A comparison between direct temperature measurements in boreholes and ground-penetrating surveys shows that the radar-inferred cold-temperate transition depth is within ±1 m from the melting point of ice at frequencies above ~300 MHz. At frequencies below ~155 MHz, the accuracy degrades because of reduced scattering efficiency that occurs when the scatterers become much smaller compared to the wavelength. The mapped spatial pattern of the englacial cold-temperate transition boundary is complex. This pattern reflects the observed spatial variation in net loss of ice at the surface by ablation and vertical advection of ice, which is suggested to provide the predominant forcing of the cold surface layer thickness pattern. This is further supported by thermomechanical modeling of the cold surface layer, which indicates high sensitivity of the cold surface layer thickness to changes in vertical advection rates. The water content is the least investigated quantity that is relevant for the thermal regime of glaciers, but also the most difficult to assess. Spatial variability of absolute water content in the temperate ice immediately below the cold surface layer on Storglaciären was determined by combining relative estimates of water content from ground-penetrating radar data with absolute determination from temperature measurements and the thermal boundary condition at the freezing front. These measurements indicate large-scale spatial variability in the water content, which seems to arise from variations in entrapment of water at the firn-ice transition. However, this variability cannot alone explain the spatial pattern in the thermal regime on Storglaciären. Repeated surveys of the cold surface layer show a 22% average thinning of the cold surface layer on Storglaciären between 1989 and 2001. Transient thermomechanical modeling results suggest that the cold surface layer adapts to new equilibrium conditions in only a few decades after a perturbation in the forcing is introduced. An increased winter air temperature since mid-1980s seems to be the cause of the observed thinning of the cold surface layer. Over the last decades, mass balance measurements indicate that the glacier has been close to a steady state. The quasi-steady state situation is also reflected in the vertical advection, which shows no significant changes during the last decades. Increased winter temperatures at the ice surface would result in a slow-down of the formation of cold ice at the base of the cold surface layer and lead to a larger imbalance between net loss of ice at the surface and freezing of temperate ice at the cold-temperate transition.