963 resultados para atmosfera de forno
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A anchoita foi capturada e acondicionada a bordo sob-resfriamento a 0°C com gelo em escamas. Após o recebimento, o pescado foi processado na forma salgado-maturado. Após a maturação foram processadas e embaladas em sacos de polietileno e armazenadas sob-refrigeração a 5°C durante 84 dias. As amostras foram divididas grupos: (1) sob pressão atmosfera normal, (2) vácuo, (3) atmosfera modificada com 50% CO2 + 20% O2 + 30% N2 e (4) 60% CO2 + 10% O2 + 30% N2, em embalagens de polietileno e aluminizadas, termo-seladas e armazenadas sob-refrigeração a 5°C. Os valores de textura tiveram uma redução de 2277,8 N (Kg.m/s2 ) para 821,90 N (Kg.m/s2 ) para o tratamento controle. A qualidade inicial do pescado atendeu aos padrões legais vigentes, apresentando ausência Salmonella sp e enumerações aceitáveis aos padrões de Staphylococcus coagulase positiva, Clostridium sulfito redutores, coliforme totais e a 45ºC. Com relação ao pH, houve diferenças significativas durante o tempo de processamento (p<0,05), o valor passou de 6,3 (início) para 6,4 (final). Com relação aos resultados correspondentes aos parâmetros L*, a* e b* (cor), em todos os tratamentos e ao longo do tempo de processamento (ambas as embalagens), ocorreram diferenças significativas (p<0,05). Os valores de L* variaram de 34,80 para 18,00 (controle) 23,00 (vácuo), 20,21 (T3) e 22,00 (T4) embalagens de polietileno. Nas embalagens de alumínio os valores de L* variaram de 34,00 para 25,00 (controle), 29,00(vácuo), 22,10 (T3) e 26,00 (T4).
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Tese submetida à Universidade de Coimbra, Faculdade de Ciências e Tecnologia e aprovada em provas públicas para a obtenção do Grau de Doutor em Engenharia Mecânica (especialidade de Ciência dos Materiais)
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A injecção de Zamak em Portugal é uma actividade corrente, sendo usada na produção de inúmeras peças de pequena dimensão, nomeadamente em acessórios de vestuário, no fabrico de cablagens metálicas para a indústria automóvel, no fabrico de placas indicativas de marcas nos mais diversos produtos, entre muitas outras aplicações. Quando a quantidade de Zamak injectada em cada ciclo é relativamente baixa, o tempo que demora a consumir um lingote é bastante longo, pelo que não se justifica que o forno esteja equipado com um sistema de alimentação automática de lingotes. No entanto, quando as peças injectadas possuem uma maior massa ou o número de cavidades por molde é maior, um lingote pode ser consumido num período de tempo suficientemente curto para ser necessário um operário permanentemente atento à alimentação do forno. Neste caso, justifica-se a inclusão de um sistema automático que vá descarregando lingotes à medida que aquele que está a abastecer o forno é consumido. O presente trabalho foi elaborado com base na necessidade de uma empresa fabricante de máquinas para a injecção de Zamak, a qual pretendia dotar alguns dos seus modelos com este sistema, indo de encontro às necessidades dos seus clientes e ampliando a gama de acessórios que passa a poder disponibilizar em torno de cada equipamento.
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This work a studied the high energy milling effect in microstructure and magnetic properties of the WC-10wt.%Co composite. The composite powders were prepared by mechanical mixed and milled at 2 hours, 100 hours, 200 hours and 300 hours in planetary milling. After this process the composite were compacted in stainless steel die with cylindrical county of 10 mm of diameter, at pressure 200 Mpa and sintered in a resistive furnace in argon atmosphere at 1400 oC for 5 min. The sintered composite were cutted, inlaid, sandpapered, and polished. The microestrutural parameters of the composite was analyzed by X-ray diffraction, scanning electronic microscopy, optical microscopy, hardness, magnetic propriety and Rietveld method analyze. The results shows, with milling time increase the particle size decrease, it possibility minor temperature of sintering. The increase of milling time caused allotropic transformation in cobalt phase and cold welding between particles. The cold welding caused the formation of the particle composite. The X-ray diffraction pattern of composite powders shows the WC peaks intensity decrease with the milling time increase. The X-ray diffraction pattern of the composite sintered samples shows the other phases. The magnetic measurements detected a significant increase in the coercitive field and a decrease in the saturation magnetization with milling time increase. The increase coercitive field it was also verified with decrease grain size with milling time increase. For the composite powders the increase coercitive field it was verified with particle size reduction and saturation magnetization variation is relate with the variation of free cobalt. The Rietveld method analyze shows at milling time increase the mean crystalline size of WC, and Co-cfc phases in composite sintered sample are higher than in composite powders. The mean crystallite size of Co-hc phase in composite powders is higher than in composite sintered sample. The mean lattice strains of WC, Co-hc and Co-cfc phases in composite powders are higher than in composite sintered samples. The cells parameters of the composite powder decrease at milling time increase this effect came from the particle size reduction at milling time increase. In sintered composite the cells parameters is constant with milling time increase
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Microalloyed steels constitute a specific class of steel with low amount of carbon and microalloying elements such as Vanadium (V), Niobium (Nb) and Titanium (Ti). The development and application of microalloyed steels and steels in general are limited to the handling of powders with particles of submicron or nanometer dimensions. Therefore, this work presents an alternative in order to construction of microalloyed steels utilizing the deposition by magnetron sputtering technique as a microalloying element addiction in which Ti nanoparticles are dispersed in an iron matrix. The advantage of that technique in relation to the conventional metallurgical processes is the possibility of uniformly disperse the microalloying elements in the iron matrix. It was carried out deposition of Ti onto Fe powder in high CH4, H2, Ar plasma atmosphere, with two deposition times. After the deposition, the iron powder with nanoparticles of Ti dispersed distributed, were compacted and sintered at 1120 ° C in resistive furnace. Characterization techniques utilized in the samples of powder before and after deposition of Ti were Granulometry, Scanning Electron Microscopy (SEM), energy-dispersive X-ray spectroscopy (EDX) and X-ray diffraction (DRX). In the case of sintered samples, it was carried out characterization by SEM and Vickers Microhardness assays. The results show which the deposition technique by magnetron sputtering is practicable in the dispersion of particles in iron matrix. The EDX microanalysis detected higher percentages of Ti when the deposition were carried out with the inert gas and when the deposition process was carried out with reactive gas. The presence of titanium in iron matrix was also evidenced by the results of X-ray diffraction peaks that showed shifts in the network matrix. Given these results it can be said that the technique of magnetron sputtering deposition is feasible in the dispersion of nanoparticles of iron matrix in Ti.
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For the chemical method of synthesis of co-precipitation were produced ferrite powders manganese-cobalt equal stoichiometric formula Mn (1-x) Co (x) Fe2O4, for 0 < x < 1, first reagent element using as the hydroxide ammonium and second time using sodium hydroxide. The obtained powders were calcined at 400 ° C, 650 ° C, 900 ° C and 1150 ° C in a conventional oven type furnace with an air atmosphere for a period of 240 minutes. Other samples were calcined at a temperature of 900 ° C in a controlled atmosphere of argon, to evaluate the possible influence of the atmosphere on the final results the structure and morphology. The samples were also calcined in a microwave oven at 400 ° C and 650 ° C for a period of 45 minutes possible to evaluate the performance of this type of heat treatment furnace. It was successfully tested the ability of this group include isomorphic ferrite with the inclusion of nickel cations in order to evaluate the occurrence of disorder in the crystalline structures and their changes in magnetic characteristics.To identify the structural, morphological, chemical composition and proportions, as well as their magnetic characteristics were performed characterization tests of X-ray diffraction (XRD), scanning electron microscopy (SEM), transmission electron microscopy (TEM), energy dispersive spectroscopy (EDX), thermogravimetric (TG), vibrating sample magnetometry (MAV) and Mössbauer spectroscopy. These tests revealed the occurrence of distortion in the crystal lattice, changes in magnetic response, occurrence of nanosized particles and superparamagnetism
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2015
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Il presente lavoro di tesi riguarda lo studio di un modello di stima delle emissioni per la previsione della contaminazione ambientale in aria. Il lavoro è stato svolto all’interno del DICAM dell’Università di Bologna attraverso il supporto del relatore Giacomo Antonioni e dei correlatori Ada Saracino e Gigliola Spadoni. L’applicazione modellistica, attraverso l’uso del software CALPUFF, ha trattato le emissioni del camino E312 della sezione Agglomerazione dello stabilimento siderurgico ILVA di Taranto nell’anno 2015. Gli inquinanti simulati sono quelli per i quali lo SME fornisce il flusso di massa: SO2, NOx, PM. Le polveri sono state considerate completamente costituite da polveri PM10 e per esse si è calcolata la concentrazione al suolo e la deposizione. A partire dai risultati per le polveri, ipotizzando che siano in parte veicolati da esse, sono state valutate anche le concentrazioni e le deposizioni di Diossine. Della configurazione modellistica “ottimale” sono stati presentati: ▪ Per i macroinquinanti le medie annue di concentrazione al suolo, e quindi, la dispersione degli inquinanti. ▪ Per i microinquinanti i valori massimi di concentrazione annua e di deposizione ottenuti nell’area di studio. Nel caso in esame, lo studio è stato riferito alla rete deposimetrica di gestione ILVA (per mancanza di dati deposimetrici della rete di gestione ARPA). In particolare è stato preso in considerazione il deposimetro del quartiere Tamburi a fronte delle criticità rilevate nei mesi di Novembre 2014 e Febbraio 2015, tale per cui, visti gli elevatissimi valori di deposizione, vista la notevole importanza che i dati deposimetrici hanno rispetto al rischio sanitario per ingestione, è stata aperta un’indagine della procura che ha affidato l’analisi a ARPA PUGLIA congiunta con l’ISPRA (che ne ha mandato ministeriale) e la Regione Puglia. A fronte di tali episodi, il seguente studio ha voluto fornire un resoconto deposimetrico per l’anno 2015.
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A motivação que deu início a este projeto foi a necessidade da empresa Bollinghaus querer alcançar novos mercados, em especial o mercado da indústria petrolífera norueguesa, regida pelas normas NORSOK, aumentar a qualidade do produto e reduzir o tempo de entrega. Para dar resposta a esta necessidade, foi formado um grupo de 5 pessoas que iriam acompanhar e gerir este projeto, tendo como objetivo final a implementação de um forno de tratamento térmico de acordo com a norma NORSOK M650 e que obtenha resultados de propriedades mecânicas iguais ou superiores àqueles obtidos até ao momento nos fornos existentes na empresa. Foram definidas as especificações técnicas do forno e equipamentos envolventes, modificados e/ou instalados os equipamentos necessários e por último, foi feito um controlo às propriedades mecânicas do produto final para garantir a sua conformidade. No final, conclui-se que o forno respeita os requisitos definidos pela empresa, embora os resultados das propriedades mecânicas não estejam completamente de acordo com o que a empresa pretendia.
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Este relatório técnico tem como objetivo descrever o modo como os registos das amostras de dados, i.e., medições das grandezas meteorológicas fornecidas pelo Instituto Português do Mar e da Atmosfera (IPMA), ilha da Madeira, foram tratadas. Foram utilizados registos de oito estações meteorológicas distribuídas pela ilha. No relatório técnico estão descritos os processos de filtragem das medições de radiação solar global e radiação solar difusa, de temperatura máxima e mínima do ar, a correção da radiação solar difusa, o preenchimento de lacunas nas medições e a dimensão da amostra de dados utilizada em cada estação. Este relatório também descreve os métodos utilizados para preencher as lacunas nas séries de dados originais, bem como os métodos utilizados na construção do ano médio e do ano meteorológico típico. O ano meteorológico típico será posteriormente usado na simulação da produção de energia solar através de sistemas fotovoltaicos instalados na ilha da Madeira.
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NEW DATA ON THE CHRONOLOGY OF THE VALE DO FORNO SEDIMENTARY SEQUENCE (LOWER TAGUS RIVER TERRACE STAIRCASE) AND ITS RELEVANCE AS FLUVIAL ARCHIVE OF THE MIDDLE PLEISTOCENE IN WESTERN IBERIA Pedro P. Cunha 1, António A. Martins 2, Jan-Pieter Buylaert 3,4, Andrew S. Murray 4, Luis Raposo 5, Paolo Mozzi 6, Martin Stokes 7 1 MARE - Marine and Environmental Sciences Centre, Department of Earth Sciences, University of Coimbra, Portugal: pcunha@dct.uc.pt 2 MARE - Marine and Environmental Sciences Centre, Dep. Geociências, University of Évora, Portugal; aam@uevora.pt 3 Centre for Nuclear Technologies, Technical University of Denmark, Risø Campus, Denmark; jabu@dtu.dk 4 Nordic Laboratory for Luminescence Dating, Aarhus University, Risø DTU, Denmark; anmu@dtu.dk 5 Museu Nacional de Arqueologia, Lisboa, Portugal; 3raposos@sapo.pt 6 Department of Geosciences, University of Padova, Italy; paolo.mozzi@unipd.it 7 School of Geography, Earth and Environmental Sciences, University of Plymouth, UK; m.stokes@plymouth.ac.uk The stratigraphic units that record the evolution of the Tagus River in Portugal (study area between Vila Velha de Ródão and Porto Alto villages; Fig. 1) have different sedimentary characteristics and lithic industries (Cunha et al., 2012): - a culminant sedimentary unit (the ancestral Tagus, before the drainage network entrenchment) – SLD13 (+142 to 262 m above river bed – a.r.b.; with probable age ca. 3,6 to 1,8 Ma), without artefacts; - T1 terrace (+84 to 180 m; ca. 1000? to 900 ka), without artefacts; - T2 terrace (+57 to 150 m; top deposits with a probable age ca. 600 ka), without artefacts; - T3 terrace (+43 to 113 m; ca. 460 to 360? ka), without artefacts; - T4 terrace (+26 to 55 m; ca. 335 a 155 ka), Lower Paleolithic (Acheulian) at basal and middle levels but early Middle Paleolithic at top levels; - T5 terrace (+5 to 34 m; 135 to 73 ka), Middle Paleolithic (Mousterian; Levallois technique); - T6 terrace (+3 to 14 m; 62 to 32 ka), late Middle Paleolithic (late Mousterian); - Carregueira Sands (aeolian sands) and colluvium (+3 a ca. 100 m; 32 to 12 ka), Upper Paleolithic to Epipaleolithic; - alluvial plain (+0 to 8 m; ca. 12 ka to present), Mesolithic and more recent industries. The differences in elevation (a.r.b.) of the several terrace staircases results from differential uplift due to active faults. Longitudinal correlation with the terrace levels indicates that a graded profile ca. 200 km long was achieved during terrace formation periods and a strong control by sea base level was determinant for terrace formation. The Neogene sedimentary units constituted the main source of sediments for the fluvial terraces (Fig. 2). Geomorphological mapping, coupled with lithostratigraphy, sedimentology and luminescence dating (quartz-OSL and K-feldspar post-IRIR290) were used in this study focused on the T4 terrace, which comprises a Lower Gravels (LG) unit and an Upper Sand (US) unit. The thick, coarse and dominantly massive gravels of the LG unit indicate deposition by a coarse bed-load braided river, with strong sediment supply, high gradient and fluvial competence, during conditions of rapidly rising sea level. Luminescence dating only provided minimum ages but it is probable that the LG unit corresponds to the earlier part of the MIS9 (ca. 335 to 325 ka), immediately postdating the incision promoted by the very low sea level (reaching ca. -140 m) during MIS10 (362 to 337 ka), a period of relatively cold climate conditions with weak vegetation cover on slopes and low sea level. Fig. 1. Main Portuguese reaches in which the Tagus River can be divided (Lower Tagus Basin): I – from the Spanish border to Arneiro (a general E–W trend, mainly consisting of polygonal segments); II – from Arneiro to Gavião (NE–SW); III – from Gavião to Arripiado (E–W); IV – from Arripiado to Vila Franca de Xira (NNE-SSW); V – from Vila Franca de Xira to the Atlantic shoreline. The faults considered to be the limit of the referred fluvial sectors are: F1 – Ponsul-Arneiro fault (WSW-ENE); F2 – Gavião fault (NW-SE); F3 – Ortiga fault (NW-SE); F4 – Vila Nova da Barquinha fault (W-E); F5 – Arripiado-Chamusca fault (NNE-SSW). 1 – estuary; 2 – terraces; 3 – faults; 4 – Tagus main channel. The main Iberian drainage basins are also represented (inset). The lower and middle parts of the US unit, comprising an alternation of clayish silts with paleosols and minor sands to the east (flood-plain deposits) and sand deposits to the west (channel belt), have a probable age of ca. 325 to 200 ka. This points to formation during MIS9 to MIS7, under conditions of high to medium sea levels and warm to mild conditions. The upper part of the US unit, dominated by sand facies and with OSL ages of ca. 200 to 154 ka, correlates with the early part of the MIS6. During this period, progradation resulted from climate deterioration and relative depletion of vegetation that promoted enhanced sediment production in the catchment, coupled with initiation of sea-level lowering that increased the longitudinal slope. The Vale do Forno and Vale da Atela archaeological sites (Alpiarça, central Portugal) document the earliest human occupation in the Lower Tagus River, well established in geomorphological and environmental terms, within the Middle Pleistocene. The Lower Palaeolithic sites were found on the T4 terrace (+26 m, a.r.b.). The oldest artefacts previously found in the LG unit, display crude bifacial forms that can be attributed to the Acheulian, with a probable age of ca. 335 to 325 ka. The T4 US unit has archaeological sites stratigraphically documenting successive phases of an evolved Acheulian, that probably date ca. 325 to 300 ka. Notably, these Lower Palaeolithic artisans were able to produce tools with different sophistication levels, simply by applying different strategies: more elaborated reduction sequences in case of bifaces and simple reduction sequences to obtain cleavers. Fig. 2. . Simplified geologic map of the Lower Tagus Cenozoic basin, adapted from the Carta Geológica de Portugal, 1/500000, 1992). The study area (comprising the Vale do Forno and Vale de Atela sites) is located on the more upstream sector of the Lower Tagus River reach IV, between Arripiado and Chamusca villages. 1 – alluvium (Holocene); 2 – terraces (Pleistocene); 3 – sands, silts and gravels (Paleogene to Pliocene); 4 – Sintra Massif (Cretaceous); 5 – limestones, marls, silts and sandstones (Mesozoic); 6 – quartzites (Ordovician); 7 – basement (Proterozoic to Palaeozoic); 8 – main fault. The main Portuguese reaches of the Tagus River are identified (I to V). The VF3 site (Milharós), containing a Final Acheulian industry, with fine and elaborated bifaces) found in a stratigraphic level located between the T4 terrace deposits and a colluvium associated with Late Pleistocene aeolian sands (32 to 12 ka), has an age younger than ca. 154 ka but much older than 32 ka. In the study area, the sedimentary units of the T4 terrace seem to record the river response to sea-level changes and climatically-driven fluctuations in sediment supply. REFERENCES Cunha P. P., Almeida N. A. C., Aubry T., Martins A. A., Murray A. S., Buylaert J.-P., Sohbati R., Raposo L., Rocha L., 2012, Records of human occupation from Pleistocene river terrace and aeolian sediments in the Arneiro depression (Lower Tejo River, central eastern Portugal). Geomorphology, vol. 165-166, pp. 78-90.
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The exchanges between lakes and the atmosphere at Alqueva reservoir, Southeast Portugal, are the object of a 2014 Summer experiment described in this work, with special attention to above water, air-water interface and below water measurements. Air-water interface momentum, heat and mass (H 2 O and CO 2 ) fluxes are obtained with the new Campbell Scientific’s IRGASON Integrated Open-Path CO 2 /H 2 O Gas Analyser and 3D Sonic Anemometer with a unique design that contains no special displacement between the sample volumes of the gas analyser and the sonic anemometer. The radiative balance, both in short and long wave, is assessed with an albedometer and a pirradiometer. Water temperature profile is also continuously recorded. In-water solar spectral downwelling irradiance profiles are measured which enable the computation of the attenuation coefficient of light in the water column. Thus, with detailed information of the Lake-Atmosphere interactions, it is possible to determine the energy and mass balance of the lake.
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Maçãs cv. Gala são conhecidas por apresentarem bom potencial de armazenamento em atmosfera controlada (AC) associada a refrigeração. Condições de 1% de O2; 2% de CO2; 0°C ± 0,5; 90% UR ± 5% são relatadas por preservarem a firmeza de polpa por até nove meses. Entretanto, logo após a saída da AC, uma perda da firmeza é observada, resultando em perdas na qualidade dos frutos durante o transporte e comercialização. Desse modo, o 1-metilciclopropeno (1-MCP) é utilizado com sucesso em conjunto com a AC, por ser capaz de manter a firmeza de polpa de maçãs mesmo após a saída do armazenamento. O objetivo do trabalho foi elucidar mecanismos pelo qual o 1-MCP preserva a firmeza de polpa da maçã armazenada em AC.