973 resultados para ALUMINA-CERAMICS
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Dissertação de mestrado em Técnicas de Caracterização e Análise Química
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The fundamental goal we set ourselves when developing this study is to try to characterize, both technically and formally, ceramics made in the city of Braga and its territory from the initial moments of the Late Antiquity to the Middle Ages. Thus, we will focus on analyzing some own productions that appear attached to the phases of late antique occupation —ceramics of red engobes and late gray—, as well as in the early medieval containers identified in different archaeological interventions practiced in the Braga environment. Concretely, we will analyze the material from various excavations conducted recently at the Theatre in the solar number 20/28 and 36/56 from the Afonso Henriques Street and the former District Hostel as well as the church of São Martinho de Dume.
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There has been a long-standing debate concerning the extent to which the spread of Neolithic ceramics and Malay-Polynesian languages in Island Southeast Asia (ISEA) were coupled to an agriculturally driven demic dispersal out of Taiwan 4000 years ago (4 ka). We previously addressed this question using founder analysis of mitochondrial DNA (mtDNA) control-region sequences to identify major lineage clusters most likely to have dispersed from Taiwan into ISEA, proposing that the dispersal had a relatively minor impact on the extant genetic structure of ISEA, and that the role of agriculture in the expansion of the Austronesian languages was therefore likely to have been correspondingly minor. Here we test these conclusions by sequencing whole mtDNAs from across Taiwan and ISEA, using their higher chronological precision to resolve the overall proportion that participated in the "out-of-Taiwan" mid-Holocene dispersal as opposed to earlier, postglacial expansions in the Early Holocene. We show that, in total, about 20 % of mtDNA lineages in the modern ISEA pool result from the "out-of-Taiwan" dispersal, with most of the remainder signifying earlier processes, mainly due to sea-level rises after the Last Glacial Maximum. Notably, we show that every one of these founder clusters previously entered Taiwan from China, 6-7 ka, where rice-farming originated, and remained distinct from the indigenous Taiwanese population until after the subsequent dispersal into ISEA.
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Engineering ceramics, indentation methods, crack-resistance, Rayleigh waves, acoustic microscopy, machining parameters, green ceramic bodies, ultrasonic contact impedance, acoustic impedance, residual stress
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Enterobacteria of pathogenic group were isolated directly of superficial waters using Alumina Milk as precipitate, being 23 Salmonella, 19 Shigella and 17 Proteus from 18 samples which were collected in brooks and rivers of São Paulo, Brazil.
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Este trabalho foi realizado com o objetivo de estudar a ocorrência de montmorilonita em solos desenvolvidos do arenito de Botucatu no município de Piracicaba. Tais solos são os seguintes: Regossol (série Ribeirão Claro), Podzólico Vermelho Amarelo-variação Laras (série Ibitiruna) e Regossol "intergrade". para Podzólico Vermelho Amarelo. Foram selecionados cinco perfis, sendo dois pertencentes ao Regossol (perfis P1, e Ρ2), dois ao Podzólico (perfis P3 e P4) e um ao Regossol "intergrade" (perfil Ρ5). As amostras dos cinco perfis, em número de 33, foram tratadas convenientemente para se processar a eliminação de sais solúveis e agentes cimentantes (matéria orgânica, óxidos de ferro livres, etc), e assim facilitar o estudo da fração argila. Nesta fração foram feitas as determinações químicas (% de K2O, silica, alumina e C.T.C.) e mineralógicas (raios X e análise térmica diferencial). Também determinações granulométricas e químicas foram realizadas em todas as amostras. Os perfis Ρ1 e P2, que não apresentaram rocha consolidada, tiveram a caolinita como mineral dominante (acima de 50%). Os perfis Ρ3, Ρ4 e Ρ5, que apresentaram como material de origem a rocha arenítica consolidada, tiveram a montmorilonita como mineral dominante, apresentando todavia, diferenças quanto ao teor desse mineral. Assim, o Podzólico Vermelho Amarelo-variação Laras, que possui o arenito de Botucatu de estratificação plano-paralela como material originário, teve um teor médio de montmorilonita de 35%, enquanto que o Regossol "intergrade" para Podzólico Vermelho Amarelo, com o mesmo arenito, mas de estratificação cruzada como material originário apresentou um teor médio de montmorilonita de 57%. A presença da montmorilonita nestes dois solos se deve a uma herança do material originário e não à formação local, por intemperização. Neste caso, o material originário deve ter tido, em outras épocas, condições favoráveis para a formação deste mineral, ou seja, clima semi-árido, riqueza de Ca, Mg, Na, baixa relação Si/Al e baixo teor de H. Pelos resultados obtidos, os perfis Ρ1 e P2), parecem não pertencer ao arenito de Botucatu. Infelizmente, devido à falta de dados mineralógicos da rocha do arenito de Botucatu de outras regiões do Estado, não foi possível verificar se a ocorrência da montmorilonita é ou não comum neste arenito. Outras pesquisas devem ser executadas visando este objetivo.
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En aplicaciones como la conformación en frío, donde los metales duros recubiertos con películas de naturaleza cerámica son ampliamente empleados, la existencia de un contacto mecánico repetitivo induce tensiones Hertzianas y origina el fallo por fatiga. En este trabajo, se investigan diversos recubrimientos cerámicos depositados por deposición física desde fase vapor sobre calidades diferentes de metal duro y un acero rápido pulvimetalúrgico para evaluar sus respectivas respuesta al contacto y comportamiento a fatiga. El trabajo experimental incluye la caracterización de los sistemas mediante ensayos de rayado y nanoindentación y la evaluación de las curvas tensión-deformación de indentación esférica de los sustratos, tanto desnudos como recubiertos, poniendo especial atención en determinar las tensiones de contacto críticas asociadas a la deformación plástica y a la aparición de grietas circulares en la superficie recubierta. A este estudio, le siguen numerosos ensayos a fatiga a cargas inferiores a aquéllas identificadas como críticas bajo carga monotónica y para un número de ciclos comprendido entre 1.000 y 1.000.000 de ciclos. Los resultados experimentales indican que las películas cerámicas no parecen desempeñar un papel relevante en la aparición de la cedencia plástica, siendo la deformación plástica global controlada por la deformación del sustrato. No obstante, para tensiones elevadas de indentación durante el régimen plástico, existe la aparición de grietas circulares en los recubrimientos cerámicos. Además, la aparición de las mismas es sensible a la fatiga por contacto. Este análisis mecánico se complementa con una inspección detallada del daño generado en profundidad y superficie.
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Informe de investigación realizado a partir de una estancia en el Instituto de Biotecnología Medioambiental de la Universidad Tecnológica de Graz, Austria, entre Julio y Agosto de 2006. Se ha estudiado la decoloración de varios tintes sintéticos de estructuras químicas diferentes (Rojo Congo, Azul de Naftol, Indigo Carmín, Lanaset Gris, Azul de Nilo) por la enzima lacasa inmovilizada. La inmovilización de la enzima lacasa se llevó a cabo sobre esferas de alúmina (Al2O3) de 3 mm de diámetro debido a la resistecia mecánica de este material. La lacasa y la proteína inmovilizada se determinaron como la diferencia entre las concentraciones iniciales y residuales (obtenidas en los lavados). El porcentaje de lacasa inmovilizada fue del 68% y la cantidad de proteína inmovilizada por gramo de soporte de 5,6 mg. La enzima lacasa inmovilizada fue capaz de decolorar tintes de diferente estructura sin la necesidad de añadir mediadores redox, lo cual la hace una enzima muy adecuada para su aplicación en la decoloración de efluentes procedentes de la industria textil. De todas formas, son necesarios más estudios para optimizar la técnica de inmovilización así como el proceso de decoloración. Es interesante destacar que aunque hay muchos estudios basados en la oxidación de tintes textiles por lacasa la mayoría utilizan la enzima libre y hay muy poca información disponible sobre la aplicación de lacasas inmovilizadas, por lo que el presente estudio constituye una aportación muy interesante y novedosa.
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S’ha estudiat la bioacumulació de contaminants orgànics persistents en el múscul d’una espècie de peix en dos punts del litoral català: al Port de Barcelona i a la costa de Blanes. Citharus linguatula ha estat escollida per les seves característiques d’hàbitats (està més exposada a la contaminació al ser una espècie bentònica). La metodologia emprada consisteix en la homogeneïtzació amb sulfat de sodi i una extracció assistida amb microones amb n-hexà-acetona(1:1 v/v) durant 20 minuts. Els extractes es netegen i es fraccionen amb una columna cromatogràfica d’alúmina que permet la separació dels extractes en dos fraccions: un amb la majoria dels compostos organoclorats (hexaclorbenzè, DDTs, ciclodiens clorats i policlorbifenils) i l’altre amb els isòmers hexaclorciclohexans i els PAHs. Aquestes dos fraccions són posteriorment analitzades en el GC-MS. S’ha pogut corroborar l’elevada presència de PCBs a Barcelona, així com que en aquest punt de mostreig les espècies estan més exposades a la contaminació per organoclorats. S’ha identificat la presència de DDTs en els dos llocs estudiats. Pel que fa als PAHs s’ha pogut observar que a Barcelona també hi ha més presència d’aquests. Cal destacar que la concentració obtinguda dels compostos no es pot donar com a vàlida per l’existència d’indicis d’errors experimentals o d’injecció.
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Two contiguous villages in Tracunhaém county (State of Pernambuco), endemic for schistosomiasis, were studied: Itapinassu (138 inhabitants) and São Joaquim (91 inhabitants). Agriculture predominates in the former region while ceramics is the main activity in the latter. Although no statistical difference was found regarding prevalence, severe infection (>400 epg) predominated in Itapinassu, probably related to the kind of occupation. No association was found between parasite burden and severity of disease, in spite of the high infection rates for Schistosoma mansoni in both communities (approx. 60%). Typical epidemiological features of schistosomiasis such as age-related prevalences and intensities of infection (high in children, low in adults) were also mutual characteristics. Nutritional status determined through anthropometric evaluation was carried out by measuring specific anthropometric indicators. A deficit of energy intake, as well as vitamin A and riboflavin deficiencies were detected. The prevalence of moderate or severe undernutrition in patients under 18 years old was 21.9% in Itapinassu and 24.1% in São Joaquim. In this group an association was found between prevalence of schistosomiasis and chronic undernutrition. Similarly, for patients over 18 year old the prevalence of undernutrition was higher than 20%. However, in this case no association between nutritional status and either prevalence of schistosomiasis or parasite burden could be detected. The two communities had not been treated for eight years.
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The origin of andesite is an important issue in petrology because andesite is the main eruptive product at convergent margins, corresponds to the average crustal composition and is often associated with major Cu-Au mineralization. In this study we present petrographic, mineralogical, geochemical and isotopic data for basaltic andesites of the latest Pleistocene Pilavo volcano, one of the most frontal volcanoes of the Ecuadorian Quaternary arc, situated upon thick (30-50 km) mafic crust composed of accreted Cretaceous oceanic plateau rocks and overlying mafic to intermediate Late Cretaceous-Late Tertiary magmatic arcs. The Pilavo rocks are basaltic andesites (54-57 center dot 5 wt % SiO(2)) with a tholeiitic affinity as opposed to the typical calc-alkaline high-silica andesites and dacites (SiO(2) 59-66 wt %) of other frontal arc volcanoes of Ecuador (e.g. Pichincha, Pululahua). They have much higher incompatible element contents (e.g. Sr 650-1350 ppm, Ba 650-1800 ppm, Zr 100-225 ppm, Th 5-25 ppm, La 15-65 ppm) and Th/La ratios (0 center dot 28-0 center dot 36) than Pichincha and Pululahua, and more primitive Sr ((87)Sr/(86)Sr similar to 0 center dot 7038-0 center dot 7039) and Nd (epsilon(Nd) similar to +5 center dot 5 to +6 center dot 1) isotopic signatures. Pilavo andesites have geochemical affinities with modern and recent high-MgO andesites (e.g. low-silica adakites, Setouchi sanukites) and, especially, with Archean sanukitoids, for both of which incompatible element enrichments are believed to result from interactions of slab melts with peridotitic mantle. Petrographic, mineral chemistry, bulk-rock geochemical and isotopic data indicate that the Pilavo magmatic rocks have evolved through three main stages: (1) generation of a basaltic magma in the mantle wedge region by flux melting induced by slab-derived fluids (aqueous, supercritical or melts); (2) high-pressure differentiation of the basaltic melt (at the mantle-crust boundary or at lower crustal levels) through sustained fractionation of olivine and clinopyroxene, leading to hydrous, high-alumina basaltic andesite melts with a tholeiitic affinity, enriched in incompatible elements and strongly impoverished in Ni and Cr; (3) establishment of one or more mid-crustal magma storage reservoirs in which the magmas evolved through dominant amphibole and clinopyroxene (but no plagioclase) fractionation accompanied by assimilation of the modified plutonic roots of the arc and recharge by incoming batches of more primitive magma from depth. The latter process has resulted in strongly increasing incompatible element concentrations in the Pilavo basaltic andesites, coupled with slightly increasing crustal isotopic signatures and a shift towards a more calc-alkaline affinity. Our data show that, although ultimately originating from the slab, incompatible element abundances in arc andesites with primitive isotopic signatures can be significantly enhanced by intra-crustal processes within a thick juvenile mafic crust, thus providing an additional process for the generation of enriched andesites.
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Aquesta és la realització del TFC en l'àrea de .NET de en quant al "Desenvolupament ràpid de llocs web". L'objectiu global del projecte és explorar la tecnologia WebMatrix de Microsoft, proveint una web per la PYME Cerámicas Alba, dedicada a les reformes i la venda al detall de mobiliari i ceràmiques per a banys i cuines. La PYME necessita amb certa urgència una web per publicar d'una manera ràpida informació de l'empresa. La web tindrà dues parts: back-end i el front-end. El back-end pretén permetre al client administrar les parts dinàmiques de la web com ara productes i dades de l'empresa. El front-end serà la part visible per els usuaris d'Internet. Com a proveïdor de la web, és requisit disposar d'eines i un entorn per a generar i publicar la web, WebMatrix és una tecnologia de Microsoft que s'hi ajusta i la definida en el TFC.
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The ceramic shell is a material mainly used for making foundry molds. This research demonstrates that ceramic shell can be used for making sculptures with exceptional definition in its finish. The research has identified a number of advantages of the material to meet the challenges of an artist during the making of a sculpture. The research has been developed in six stages: In the first stage data were collected from the chaff as the process material. This was the starting point for research. In the second stage, we have set the appropriate composition of the slurry, both in percentage and type of binder, and firing curve. To this end, we evaluated the application characteristics, thickness, drying, mechanical strength, the reduction coefficient and porosity. In the third stage it was observed that the husk is suitable for all types of materials acting as support. It was also found that the slurry can be used with various sculptural processes: modeling, molding using silicone or plaster mold, shuttering, with internal metal frame, and so on. In addition, we have established methods to repair and modify the husk by hand and power tools. In the fourth stage we have found ways to modify the surface of the husk with other minerals that affect the structure: introduction of filing of copper, bronze and iron in the slurry ceramics, different staining procedure in hot or cold, by enamel slip, and so on. In the fifth stage sculptures were made using the methods established in the previous stages, to verify this hypothesis. The sixth stage, which is annexed, contains a new method to process the ceramic shell as a mold in casting that emerged from the proven methods in the investigation.
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A problem in the archaeometric classification of Catalan Renaissance pottery is the fact, thatthe clay supply of the pottery workshops was centrally organized by guilds, and thereforeusually all potters of a single production centre produced chemically similar ceramics.However, analysing the glazes of the ware usually a large number of inclusions in the glaze isfound, which reveal technological differences between single workshops. These inclusionshave been used by the potters in order to opacify the transparent glaze and to achieve a whitebackground for further decoration.In order to distinguish different technological preparation procedures of the single workshops,at a Scanning Electron Microscope the chemical composition of those inclusions as well astheir size in the two-dimensional cut is recorded. Based on the latter, a frequency distributionof the apparent diameters is estimated for each sample and type of inclusion.Following an approach by S.D. Wicksell (1925), it is principally possible to transform thedistributions of the apparent 2D-diameters back to those of the true three-dimensional bodies.The applicability of this approach and its practical problems are examined using differentways of kernel density estimation and Monte-Carlo tests of the methodology. Finally, it istested in how far the obtained frequency distributions can be used to classify the pottery
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Here we present a processing route to produce multi-structured ceramic foams based on the combination of particle-stabilized foams with polymeric sponges to produce positive and negative templating structures. Polyester sponges are infiltrated with freshly produced calcium aluminate alumina foams and upon sintering either positive templating structures are produced when wetting the sponges, or negative templating foams with a percolating pore network are obtained when completely filling the sponges. Additionally, by combining different layers of these particle-stabilized foam infiltrated sponges, various different structures can be produced, including sandwich structures, pore size gradients, and ceramic bone-like structures applying to different types of bone. The particle-stabilized foams used were in situ self-hardening calcium aluminate cement enriched alumina foams to obtain crack-free samples with pore interconnections and tailorable pore sizes.