998 resultados para Strontium stannate


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Electrocerâmicos são uma classe de materiais avançados com propriedades eléctricas valiosas para aplicações. Estas propriedades são geralmente muito dependentes da microestrutura dos materiais. Portanto, o objectivo geral deste trabalho é investigar o desenho da resposta dieléctrica de filmes espessos obtidos por Deposição Electroforética (EPD) e cerâmicos monolíticos, através do controlo da evolução da microestrutura durante a sinterização de electrocerâmicos à base de titanatos. Aplicações sem fios na indústria microelectrónica e de comunicações, em rápido crescimento, tornaram-se um importante mercado para os fabricantes de semicondutores. Devido à constante necessidade de miniaturização, redução de custos e maior funcionalidade e integração, a tecnologia de filmes espessos está a tornar-se uma abordagem de processamento de materiais funcionais cada vez mais importante. Uma técnica adequada neste contexto é EPD. Os filmes espessos resultantes necessitam de um passo subsequente de sinterização que é afectada pelo substrato subjacente, tendo este um forte efeito sobre a evolução da microestrutura. Relacionado com a miniaturização e a discriminação do sinal, materiais dieléctricos usados como componentes operando a frequências das microondas em aplicações na industria microelectrónica de comunicações devem apresentar baixas perdas dieléctricas e elevadas permitividade dieléctrica e estabilidade com a temperatura. Materiais do sistema BaO-Ln2O3- TiO2 (BLnT: Ln = La ou Nd), como BaLa4Ti4O15 (BLT) e Ba4.5Nd9Ti18O54 (BNT), cumprem esses requisitos e são interessantes para aplicações, por exemplo, em estações de base para comunicações móveis ou em ressonadores para telefones móveis, onde a miniaturização dos dispositivos é muito importante. Por sua vez, o titanato de estrôncio (SrTiO3, STO) é um ferroeléctrico incipiente com constante dieléctrica elevada e baixas perdas, que encontra aplicação em, por exemplo, condensadores de camada interna, tirando partido de fronteiras de grão altamente resistivas. A dependência da permitividade dieléctrica do campo eléctrico aplicado torna este material muito interessante para aplicações em dispositivos de microondas sintonizáveis. Materiais à base de STO são também interessantes para aplicações termoeléctricas, que podem contribuir para a redução da actual dependência de combustíveis fósseis por meio da geração de energia a partir de calor desaproveitado. No entanto, as mesmas fronteiras de grão resistivas são um obstáculo relativamente à eficiência do STO para aplicações termoeléctricas. Para além do efeito do substrato durante a sinterização constrangida, outros factores, como a presença de fase líquida, a não-estequiometria ou a temperatura de sinterização, afectam significativamente não apenas a microestrutura dos materiais funcionais, mas também a sua resposta dieléctrica. Se adequadamente compreendidos, estes factores podem ser intencionalmente usados para desenhar a microestrutura dos electrocerâmicos e, desta forma, as suas propriedades dieléctricas. O efeito da não-estequiometria (razão Sr/Ti 0.995-1.02) no crescimento de grão e resposta dieléctrica de cerâmicos de STO foi investigado neste trabalho. A mobilidade das fronteiras de grão aumenta com a diminuição da razão Sr/Ti. A resistividade do interior dos grãos e das fronteiras de grão é sistematicamente diminuída em amostras não-estequiométricas de STO, em comparação com o material estequiométrico. O efeito é muito mais forte para as fronteiras de grão do que para o seu interior. Dependências sistemáticas da não-estequiometria foram também observadas relativamente à dependência da condutividade da temperatura (muito mais afectada no caso da contribuição das fronteiras de grão), à capacitância do interior e fronteiras de grão e à espessura das fronteiras de grão. Uma anomalia no crescimento de grão em cerâmicos de STO ricos em Ti foi também observada e sistematicamente analisada. Foram detectadas três descontinuidades na dependência do tipo Arrhenius do crescimento de grão relativamente à temperatura com diminuições no tamanho de grão a temperaturas em torno de 1500, 1550 e 1605 °C. Além disso, descontinuidades semelhantes foram também observadas na dependência da energia de activação relativamente à condutividade das fronteiras de grão e na espessura das fronteiras de grão, avaliadas por Espectroscopia de Impedância. Estas notáveis coincidências suportam fortemente a formação de diferentes complexos de fronteira de grão com transições entre os regimes de crescimento de grão observados, que podem ser correlacionados com diferentes mobilidades de fronteira de grão e propriedades dieléctricas. Um modelo é sugerido, que se baseia na diminuição da fase líquida localizada nas fronteiras de grão, como o aumento da temperatura de sinterização, um cenário compatível com um fenómeno de solubilidade retrógrada, observado anteriormente em metais e semicondutores, mas não em cerâmicos. A EPD de filmes espessos de STO em substratos de folha de Pt e a sinterização constrangida dos filmes fabricados foram também preliminarmente tratadas. Filmes espessos de STO foram depositados com êxito por EPD sobre substratos de Pt e, depois de sinterizados, atingiram densidades elevadas. Um aumento da densificação e do tamanho de grão assim como o alargamento da distribuição de tamanho do grão foram observados com a diminuição da razão Sr/Ti, tal como anteriormente observado em amostras cerâmicas. Grãos equiaxiados foram observados para todas as composições, mas um certo grau de anisotropia na orientação dos poros foi detectado: os poros revelaram uma orientação vertical preferencial. Este trabalho focou-se também na sinterização constrangida do sistema BLnT (Ln = La ou Nd), nomeadamente de filmes espessos de BLT e BNT sobre substratos de folha de platina, e na relação do desenvolvimento de anisotropia microestrutural com as propriedades dieléctricas. As observações durante a sinterização constrangida foram comparadas com cerâmicos monolíticos equivalentes sinterizados livremente. Filmes espessos de BLnT (Ln = La ou Nd) com elevada densidade foram obtidos por EPD e subsequente sinterização constrangida. A anisometria cristalográfica do material em conjunto com um passo de sinterização constrangida resultou em grãos alongados e microestruturas anisotrópicas. O efeito do stress do substrato durante a sinterização constrangida originou graus mais elevados de anisotropia (grãos e poros alongados e orientação preferencial, bem como textura cristalográfica) nos filmes sinterizados relativamente aos cerâmicos equivalentes sinterizados livremente, não obstante o estado equivalente das amostras em verde. A densificação dos filmes de BLnT (Ln = La ou Nd) é retardada em comparação com os cerâmicos, mas depois de longos tempos de sinterização densidades semelhantes são obtidas. No entanto, em oposição a observações na sinterização constrangida de outros sistemas, o crescimento do grão em filmes de BLnT (Ln = La ou Nd) é favorecido pelo constrangimento causado pelo substrato. Além disso, grãos e poros alongados orientados paralelamente ao substrato foram desenvolvidos durante a sinterização constrangida de filmes espessos. Verificou-se uma forte correlação entre a evolução de grãos e poros, que começou assim que o crescimento do grão se iniciou. Um efeito da tensão do substrato no aumento do crescimento de grão, bem como um forte “Zener pinning”, origina microestruturas altamente texturizadas, o que também é observado a nível cristalográfico. Efeitos marcantes da anisotropia microestrutural foram também detectados nas propriedades dieléctricas dos filmes de BLnT (Ln = La ou Nd). Juntamente com o aumento da razão de aspecto dos grãos, do factor de orientação e do grau de textura cristalográfica, a permitividade relativa é ligeiramente diminuída e o coeficiente de temperatura da permitividade evolui de negativo para positivo com o aumento do tempo isotérmico de sinterização. Este trabalho mostra que a não-estequiometria pode ser usada para controlar a mobilidade das fronteiras de grão e, portanto, desenhar a microestrutura e as propriedades dieléctricas de electrocerâmicos à base de STO, com ênfase nas propriedades das fronteiras de grão. O papel da não-estequiometria no STO e dos complexos de fronteira de grão no desenvolvimento microestrutural é discutido e novas oportunidades para desenhar as propriedades de materiais funcionais são abertas. As observações relativamente à sinterização constrangida apontam para o efeito de tensões mecânicas desenvolvidas devido ao substrato subjacente no desenvolvimento da microestrutura de materiais funcionais. É assim esperado que a escolha adequada de substrato permitia desenhar a microestrutura de filmes espessos funcionais com desempenho optimizado. “Stress Assisted Grain Growth” (SAGG) é então proposto como uma técnica potencial para desenhar a microestrutura de materiais funcionais, originando microestruturas anisotrópicas texturizadas com propriedades desejadas.

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Bioactive glasses and glass-ceramics are a class of third generation biomaterials which elicit a special response on their surface when in contact with biological fluids, leading to strong bonding to living tissues. The purpose of the present study was to develop diopside based alkali-free bioactive glasses in order to achieve good sintering behaviour, high bioactivity, and a dissolution/ degradation rates compatible with the target applications in bone regeneration and tissue engineering. Another aim was to understand the structure-property relationships in the investigated bioactive glasses. In this quest, various glass compositions within the Diopside (CaMgSi2O6) – Fluorapatite (Ca5(PO4)3F) – Tricalcium phosphate (3CaO•P2O5) system have been investigated. All the glasses were prepared by melt-quenching technique and characterized by a wide array of complementary characterization techniques. The glass-ceramics were produced by sintering of glass powders compacts followed by a suitable heat treatment to promote the nucleation and crystallization phenomena. Furthermore, selected parent glass compositions were doped with several functional ions and an attempt to understand their effects on the glass structure, sintering ability and on the in vitro bio-degradation and biomineralization behaviours of the glasses was made. The effects of the same variables on the devitrification (nucleation and crystallization) behaviour of glasses to form bioactive glass-ceramics were also investigated. Some of the glasses exhibited high bio-mineralization rates, expressed by the formation of a surface hydroxyapatite layer within 1–12 h of immersion in a simulated body fluid (SBF) solution. All the glasses showed relatively lower degradation rates in comparison to that of 45S5 Bioglass®. Some of the glasses showed very good in vitro behaviour and the glasses co-doped with zinc and strontium showed an in vitro dose dependent behaviour. The as-designed bioactive glasses and glass–ceramic materials are excellent candidates for applications in bone regeneration and for the fabrication of scaffolds for tissue engineering.

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Tese de doutoramento, Geologia (Metalogenia), Universidade de Lisboa, Faculdade de Ciências, 2014

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The Ajjanahalli gold mine is spatially associated with a Late Archean craton-scale shear zone in the eastern Chitradurga greenstone belt of the Dharwar craton, India. Gold mineralization is hosted by an similar to100-m-wide antiform in a banded iron formation. Original magnetite and siderite are replaced by a peak metamorphic alteration assemblage of chlorite, stilpnomelane, minnesotaite, sericite, ankerite, arsenopyrite, pyrite, pyrrhotite, and gold at ca. 300degrees to 350degreesC. Elements enriched in the banded iron formation include Ca, Mg, C, S, An, As, Bi. Cu, Sb, Zn, Pb, Se, Ag, and Te, whereas in the wall rocks As, Cu, Zn, Bi, Ag, and An are only slightly enriched. Strontium correlates with CaO, MgO, CO2, and As, which indicates cogenetic formation of arsenopyrite and Mg-Ca carbonates. The greater extent of alteration in the Fe-rich banded iron formation layers than in the wall rock reflects the greater reactivity of the banded iron formation layers. The ore fluids, as interpreted from their isotopic composition (delta(18)O = 6.5-8.5parts per thousand; initial Sr-87/Sr-86 = 0.7068-0.7078), formed by metamorphic devolatilization of deeper levels of the Chitradurga greenstone belt. Arsenopyrite, chalcopyrite, and pyrrhotite have delta(34)S values within a narrow range between 2.1 and 2.7 per mil, consistent with a sulfur source in Chitradurga greenstone belt lithologies. Based on spatial and temporal relationships between mineralization, local structure development, and sinistral strike-slip deformation in the shear zone at the eastern contact of the Chitradurga greenstone belt, we suggest that the Ajjanahalli gold mineralization formed by fluid infiltration into a low strain area within the first-order structure. The ore fluids were transported along this shear zone into relatively shallow crustal levels during lateral terrane accretion and a change from thrust to transcurrent tectonics. Based on this model of fluid flow, exploration should focus on similar low strain areas or potentially connected higher order splays of the first-order shear zone.

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Trilobites ¥tere collected from Ordovician and Devonian formations of Ontario} New York} Ohio} Oklahoma} and Indiana. Diversity was generally low} but 19..?telllS and Ph..~tY>ps ¥tere the most abundant species from the Ordovician and Devonian} respectively. Recent marine arthropods ¥tere collected from the Atlantic shore of the middle Florida Keys} and from the Pacific and lagoonal waters at Cape Beale} B. C. Fresh-water arthropods were collected along the shore of the Severn River in northcentral Ontario. Cuticles ¥tere analyzed for major} minor and trace elements, 180 and 13C isotopes, as ¥tell as examined by scanning electron micr?scope to identify original and diagenetic fabrics. Examination of trilobite cuticles by scanning electron microscope revealed several microstructures consistent with those observed in Recent arthropods. Microstructures} such as setae and tegumental gland duct openings} in like sized Lim/IllS and Isoteline trilobites may indicate common ancestral origins for these organisms, or simply parallel cuticle evolutions. The dendritic microstructure, originally' thought to be a diagenetic indicator, was found in Recent specimens and therefore its presence in trilobites may be suggestive of the delicate nature of diagenesis in trilobites. The absence of other primary microstructures in trilobites may indicate alteration, taxonomic control} or that there is some inherent feature of S EM examination which may' not allow detection of some features} while others are apparently visit·le onl~1 under SH.·1. The region of the cuticle sampled for examination is also a major influence in detecting pristine microstructures, as not all areas of trilobite and Recent arthropod cuticles will have microstructures identifiable in a SEM study. Subtleties in the process of alteration, however} ma~·· leave pristine microstructures in cuticles that are partial~/ silicified or do 10m itized, and degree and type of alteration may vary stratigraphically and longitudinally within a unit. The presence of fused matrices, angular calcite rhombs, and pyrite in the cuticle are thought to be indicative of altered cuticles, although pyritization may not affect the entire cuticle. t-~atural processes in Recent arthropods, such as molting, lead to variations in cuticle chemistries, and are thought to reflect the area of concentration of the elements during calcification. The level of sodium in Recent arthropods was found to be higher than that in trilobites, but highly mobile when sUbjected to the actions of VY'€'athering. Less saline water produced lovy'€'r magnesium and higher calcium values in Recent specimens .. and metal variations in pristine Ordovician trilobite cuticle appears to follow the constraints outlined for Recent arthropods, of regulation due to the chemislry of the surrounding medium. In diagenetic analysis, sodium, strontium and magnesium proved most beneficial in separating altered from least altered trilobites. Using this criterion, specimens from shale show the least amount of geochemical alteration, and have an original mineralogy of 1.7 - 2.4 mole % MgC03 (8000 t(> 9500 ppm magnesium) for both /s>..?/e/11S lJA'i.riff!11S and PseIAit'11J17ites I..itmirpin..itl/~ and 2.8 - 3.3 mole % MgC03 (5000 to 7000 ppm magnesium) for Ph.i{).?PS This is Slightly lower than the mineralogy of Recent marine arthropods (4.43 - 12.1 mole % MgC03), and slightly higher than that of fresh-water crayfish (0.96 - 1.82 mole % MgC03). Geochemically pristine trilobites were also found to possess primary microstructures. Stable isotope values and trends support the assertion that marine-meteoriclburial fluids were responsible for the alteration observed in a number of the trilobite specimens. The results of this stUdy suggest that fossil material has to be evaluated separately along taxonomic and lithological lines to arrive at sensible diagenetic and e nvironmenta I interpretations.

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Réalisé en cotutelle avec le Département de Préhistoire du Muséum national d’Histoire naturelle (Paris, France), École doctorale « Sciences de la nature et de l’Homme » (ED 227)

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The present study addresses to understand the sedimentological properties of the coasts of kodungallur and chellanam, central Kerala to bring out the relationship between the textural, mineralogical and geochemical characters with that of the respective environment. The grain size study of the beach ridge sediments from different pits has been investigated at close intervals, which enables to understand the grain size variations with depth. The sediment samples from various pits of the beach ridges indicate that the sediments range primarily from medium to very fine sand, well to moderately sorted, fine to coarse skewed and leptokurtic to platykurtic. The study area is considered as a prograding coast. Variations in grain size down the pit give three phases of beach building activities i.e.; a coarsening upward sequence in the bottom layers, a fining upward in the middle and coarsening upward in the top. Beach ridges are formed by swash built sediments with cross bedding and setting lag type sediments with seaward dipping/horizontal units. Geochemical signatures in the study area have been brought out through the analysis of major and trace elements. Iron is significantly enriched and its control over many trace elements is evident. Copper, chromium, cobalt, lithium, lead and zinc show decreasing trend with depth, while sodium, potassium,strontium,nickel and organic carbon increases. The association of many trace elements with organic carbon has also been established. Dissolution of trace elements in anoxic environment, at depth and reprecipitation in the oxic layers, at near or subsurface, are the major mechanism that brought out the variation of certain environmentally sensitive elements

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The electron donating properties, surface acidity/basicity and catalytic activity of lanthana for various dopant concentrations of strontium are reported at two activation temperatures. The catalytic activity has been correlated with electron donating properties and surface acidity/basicity of the oxide.

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In the present study the preparation and characterisation of rubber ferrite composites (RFC) containing barium ferrite (BaF) and strontium ferrite (SrF) have been dealt with. The incorporation of the hard ferrites into natural and nitrile rubber was carried out according to a specific recipe for various loadings of magnetic fillers. For this, the ferrite materials namely barium ferrite and strontium ferrite having the general formula MO6Fe2O3 have been prepared by the conventional ceramic techniques. After characterisation they were incorporated into the natural and nitrile rubber matrix by mechanical method. Carbon black was also incorporated at different loading into the rubber ferrite composites to study its effect on various properties. The cure characteristics, mechanical, dielectric and magnetic properties of these composites were evaluated. The ac electrical conductivity of both the ceramic ferrites and rubber ferrite composites were also calculated using a simple relation. The investigations revealed that the rubber ferrite composites with the required dielectric and magnetic properties can be obtained by the incorporation of ferrite fillers into the rubber matrix, without compromising much on the processability and mechanical properties.

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This thesis lays importance in the investigation on the multiferroic and thermooelectric properties of selected representatives of low bandwidth and intermediate band width manganites. The first candidate, Strontium doped Gd manganite, is prepared by wet solid state reaction method and the second candidate, Na doped La manganite, by citrate gel method. In addition to the above mentioned properties, magneto resistance and dielectric properties are investigated. Using dielectric spectroscopic the dispersion parameters are correlated to the relaxation mechanisms and an attempt is made to obtain the grain and grain boundary contribution to the impedance of the sample through impedance spectroscopy studies.

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Laser‐induced damage and ablation thresholds of bulk superconducting samples of Bi2(SrCa)xCu3Oy(x=2, 2.2, 2.6, 2.8, 3) and Bi1.6 (Pb)xSr2Ca2Cu3 Oy (x=0, 0.1, 0.2, 0.3, 0.4) for irradiation with a 1.06 μm beam from a Nd‐YAG laser have been determined as a function of x by the pulsed photothermal deflection technique. The threshold values of power density for ablation as well as damage are found to increase with increasing values of x in both systems while in the Pb‐doped system the threshold values decrease above a specific value of x, coinciding with the point at which the Tc also begins to fall.  

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A method of preparation of strontium sulphide phosphors doped with europium is given. Nitrogen laser excited fluorescence emission spectra of these phosphors in the visible region are recorded. A band with line structure in the region 350-430 nm and a new broad band at 460 nm are observed. The splitting pattern for the 6p levels of Eu 2+ are given.

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Artificial neural networks (ANNs) are relatively new computational tools that have found extensive utilization in solving many complex real-world problems. This paper describes how an ANN can be used to identify the spectral lines of elements. The spectral lines of Cadmium (Cd), Calcium (Ca), Iron (Fe), Lithium (Li), Mercury (Hg), Potassium (K) and Strontium (Sr) in the visible range are chosen for the investigation. One of the unique features of this technique is that it uses the whole spectrum in the visible range instead of individual spectral lines. The spectrum of a sample taken with a spectrometer contains both original peaks and spurious peaks. It is a tedious task to identify these peaks to determine the elements present in the sample. ANNs capability of retrieving original data from noisy spectrum is also explored in this paper. The importance of the need of sufficient data for training ANNs to get accurate results is also emphasized. Two networks are examined: one trained in all spectral lines and other with the persistent lines only. The network trained in all spectral lines is found to be superior in analyzing the spectrum even in a noisy environment.

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Previous anthropological investigations at Trentholme Drive, in Roman York identified an unusual amount of cranial variation amongst the inhabitants, with some individuals suggested as having originated from the Middle East or North Africa. The current study investigates the validity of this assessment using modern anthropological methods to assess cranial variation in two groups: The Railway and Trentholme Drive. Strontium and oxygen isotope evidence derived from the dentition of 43 of these individuals was combined with the craniometric data to provide information on possible levels of migration and the range of homelands that may be represented. The results of the craniometric analysis indicated that the majority of the York population had European origins, but that 11% of the Trentholme Drive and 12% of The Railway study samples were likely of African decent. Oxygen analysis identified four incomers, three from areas warmer than the UK and one from a cooler or more continental climate. Although based on a relatively small sample of the overall population at York, this multidisciplinary approach made it possible to identify incomers, both men and women, from across the Empire. Evidence for possible second generation migrants was also suggested. The results confirm the presence of a heterogeneous population resident in York and highlight the diversity, rather than the uniformity, of the population in Roman Britain. Am J Phys Anthropol 140:546-561, 2009. (C) 2009 Wiley-Liss, Inc

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In order to investigate how the population diversity at major Romano-British urban centres compared to small towns and military outposts, we conducted multi-isotope (carbon, nitrogen, oxygen and strontium) analyses of bones (42 individuals) and teeth (26 individuals) of human skeletons from Cataractonium/ Roman Catterick in North Yorkshire (U.K.). The results suggest a markedly less diverse population at Catterick than at the larger towns. Significant differences are observed between burials from the town and fort area and the suburb of Bainesse to the south, and it is suggested that these reflect a shift to more localised recruitment for the Roman army in the Late Roman period. Isotope data for the ‘Bainesse Eunuch’, an unusual 4th century burial that has been interpreted as the remains of a ‘transvestite’ priest of Cybele, are not ultimately conclusive but consistent with origins in Southern Britain or areas with a similar climate abroad. This paper also presents strontium isotope data for modern vegetation samples from 17 sites in the Catterick/northern Vale of York area which contribute to a continuing effort to map the biosphere 87Sr/86Sr variation in Britain.