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Geology, mineralogy, and geochemistry of the Vazante Northern Extension zinc silicate deposit, Minas Gerais, BrazilSLEZAK, PAUL 01 March 2012 (has links)
The Vazante Northern Extension is a continuation of the structurally controlled, hypogene nonsulfide zinc deposit from the Vazante Mine, Minas Gerais, Brazil. The deposit is hosted in Neoproterozoic carbonates of the Serra do Poço Verde Formation located in the Brasília Fold Belt along the western margin of the São Francisco Craton. The Northern Extension deposit is hosted within a shear zone that strikes 200 to 225 and dips 30º-70º NW and is associated with substantial folding that occurred in the same deformation (D2) event and later transcurrent faulting. The shear zone is composed of a tectonic-hydrothermal breccia that can be subdivided into four types: Type 1 Breccia– distally located from the willemite (Zn2SiO4) ore, weakly brecciated dolostone with some Fe-carbonate alteration; Type 2 Breccia–Strong Fe-carbonate alteration, intense brecciation; Type 3 Breccia–hematite replacement breccia, usually proximal to the Type 4 Breccia; Type 4 Breccia–willemite ore breccia, containing three generations of hypogene willemite (Zn2SiO4) as well as hematite (Fe2O3), and franklinite (ZnFe2O4). In the southern part of the deposit, late sulfide-rich veinlets are observed cutting the hypogene zinc silicate mineralization, and contain galena, sphalerite, native silver, covellite, and stromeyerite (Cu1-xAg1-xS). Geochemical studies conducted on the tectonic-hydrothermal breccia showed a strong regional signature enriched in Ag, Cd, Pb, and Zn. The presence of willemite as opposed to sphalerite and the ubiquity of hematite suggest that the zinc silicate mineralization has formed from the mixing between a low sulfur, acid, oxidizing metalliferous basinal brine similar to the fluids found in MVT deposits with a cooler, more oxidizing, meteoric fluid. / Thesis (Master, Geological Sciences & Geological Engineering) -- Queen's University, 2012-02-29 16:45:36.41
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THE INTEGRATION OF PHYSICAL ROCK PROPERTIES, MINERALOGY AND GEOCHEMISTRY FOR THE EXPLORATION OF LARGE HYPOGENE ZINC SILICATE DEPOSITS: A CASE STUDY OF THE VAZANTE ZINC DEPOSITS, MINAS GERAIS, BRAZILMCGLADREY, ALEXANDRA JANE 27 March 2014 (has links)
Exploration for large zinc silicate deposits is more challenging than zinc sulfide deposits, as they do not exhibit similar geophysical anomalies. The Vazante deposit, which is the world’s largest zinc silicate deposit, occurs in brecciated dolomite and comprises mainly willemite with various proportions of hematite, and minor franklinite and sphalerite. In the Vazante region, the exploration challenge is enhanced as outcrops are rare, bedrock generally sits below 10s of metres of laterite cover and barren hematite-rich breccias have a similar geophysical signature to willemite ore bodies. In order to evaluate the applications of geophysical surveys in the exploration of this type of deposit, data from 475 samples were investigated from drill holes representative of the various types of ore, host rocks and zones of known geophysical anomalies in the Vazante District. Geochemical (ICP-MS and XRF) and mineralogical (optical, EMPA, SEM and MLA) data were integrated with physical rock properties (density, magnetic susceptibility and K-U-Th gamma ray spectrometry) to assist in finding new ore zones. The most distinct physical property of the ore is density (3.0-4.3 g/cm3), compared with the host rocks (2.7-3.0 g/cm3). This is due to high proportion of denser minerals (hematite and willemite) in the ore. However, barren hematite breccias also have high densities (3.0-4.5 g/cm3). The zinc ore and hematite breccias yielded higher magnetic susceptibilities (0.1-38 x10-3 SI) than the surrounding host rocks, with the highest values associated with greater proportions of franklinite and magnetite (7-38 x10-3 SI). The zinc ore has an elevated U concentration (up to 33ppm) relative to the various host rocks (up to 7 ppm), yielding higher gamma spectrometric values. The results of this investigation indicate that an integration of magnetic, gravimetric and radiometric surveys would be required to identify zinc silicate ore zones and potentially differentiate them from barren hematite breccias and host rocks. / Thesis (Master, Geological Sciences & Geological Engineering) -- Queen's University, 2014-03-27 13:32:54.132
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Zinc Silicate Based Pigments for Corrosion Inhibition of Cold Rolled SteelPemmaraju, Prajyula January 2018 (has links)
No description available.
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Síntese e caracterização de silicato de zinco dopado com manganês /Porcel, Henrique Reatto. January 2019 (has links)
Orientador: Alexandre Mesquita / Resumo: Os materiais nanoestruturados vêm sendo extensivamente estudados, não somente pelas novas propriedades e suas possíveis aplicações tecnológicas, mas também pela busca de uma melhor compreensão dos aspectos físicos e químicos. Em relação a materiais semicondutores, estudos da estrutura em escala nanométrica tem recebido considerável interesse em razão do efeito de tamanho que exibem. Semicondutores nanocristalinos apresentam propriedades eletrônicas intermediárias entre aqueles de estrutura molecular e sólidos macrocristalinos e são objeto de intensa pesquisa, apresentando uma grande diversidade de aplicações quando na forma nanoestruturada. Dentre esses materiais, o silicato de zinco (Zn2SiO4) puro ou dopado tem recebido atenção em razão de notáveis propriedades fundamentais, versatilidade e potencial para diversas aplicações tecnológicas. Nesse contexto, essa dissertação teve como objetivo realizar a síntese e a caracterização de Zn2SiO4 puro e dopado com átomos de manganês e sua correlação com propriedades fotoluminescentes. Neste trabalho, foi utilizado o método químico de preparação conhecido por co-preciptação. Deste modo, a caracterização morfológica foi realizada através da técnica de microscopia eletrônica de varredura de alta resolução (FEG-MEV), a qual demonstra um aglomerado de grãos, tornando a determinação do tamanho do mesmo difícil. As propriedades estruturais das nanopartículas, bem como suas propriedades físicas e químicas, foram determinadas através das técn... (Resumo completo, clicar acesso eletrônico abaixo) / Abstract: Nanostructured materials have been extensively studied, not only for new properties and their possible technological applications, but also for a better understanding of the physical and chemical aspects. With regard to semiconductor materials, nanoscale structure studies have received considerable interest because of the size effect they exhibit. Nanocrystalline semiconductors have intermediate electronic properties between those of molecular structure and macrocrystalline solids and are the subject of intense research, presenting a great diversity of applications when in nanostructured form. Among these materials, pure or doped zinc silicate (Zn2SiO4) has received attention because of its remarkable fundamental properties, versatility and potential for various technological applications. In this context, this dissertation aimed to synthesize and characterize pure and doped Zn2SiO4 with manganese atoms and its correlation with photoluminescent properties. In this work, the chemical preparation method known as co-precipitation was used. Thus, the morphological characterization was performed by the high resolution scanning electron microscopy (FEG-SEM) technique, which demonstrates a grain cluster, making the size determination difficult. The structural properties of nanoparticles, as well as their physical and chemical properties, were determined by X-ray diffraction, Raman spectroscopy and photoluminescence techniques, with which it is possible to observe the formation of na... (Complete abstract click electronic access below) / Mestre
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Síntese e caracterização de materiais do sistema ternário SiO2-ZnO-TiO2 obtido por sol-gel/Pechini / Synthesis and characterization of materials from SiO2-ZnOTiO2 ternary system obtained by sol-gel/PechiniFógia, Michelly Patrícia Santana de Almeida 24 September 2014 (has links)
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Previous issue date: 2014-09-24 / In this work the structural and optical properties of SiO2-ZnO-TiO2 system
doped with of Eu3+ (1% in mol) or Er3+ ions (0,2% to 2,0% in mol) were
investigated. The compositions xSiO2-([100-x]/2)ZnO-([100-x]/2)TiO2 with x
ranging from 40 to 80 were synthesized and studied. A mixed methodology
using the traditional sol-gel process and Pechini method was employed to
prepare stable and transparent sols, homogeneous gels, powders and
transparent thin films without cracks. The prepared powders were heat treated
from 100°C to 1100°C. The optical “band gap” values, the lifetime of Eu3+ 5D0
level, the R/O ratio of Eu3+ emissions and refractive index are dependent on the
composition and thermal treatment of the powders. Multilayered thin films were
deposited onto silica substrates using the “spin coating” technique. Afterwards,
the as-prepared thin films were calcined at 500°C followed by annealings from
700°C to 1000°C. The X-ray diffraction of powders showed that the
crystallization starts at 800°C with a mixture of zinc titanate phases (ZnTiO3,
Zn2TiO4) and titanium rutile (TiO2). In compositions with low silica content (x =
40 or 50) the formation of zinc silicate (Zn2SiO4) occurs at high temperatures.
The optical properties were evaluated for both powders and thin films.
Particularly, thin films exhibit transmittance above 80% in the visible region. The
refractive index at 632.8 nm and thickness of thin films were estimated using
the envelope method and m-Line spectrocopy. Furthermore, morphological
analysis of the thin films surface was performed by scanning electron
microscopy. The characteristic emission peaks of Er3+ or Eu3+ doped powders
and thin films were measured. The photoluminescent emission of Eu3+ ions,
obtained the highest intensities for the powders treated at 800°C, for films
treated at 700°C, under excitation at 394 nm, where the system remains
primarily amorphous. The photoluminescent emission of the Er3+ ions was more
intense for the powders treated at 1100°C under excitation at 980 nm, mainly
due to reduction of hydroxyl groups which act as photoluminescence
quenchers. In the film the highest intensity occurred at a temperature of 700°C
under excitation at 378 nm and showing only one guided mode. Thus, the
obtained thin films can be suitable for application as waveguides in integrated
optical systems. Moreover, the Eu and Er doped powders can be used as
phosphors in displays. / Este trabalho avalia as propriedades estruturais e ópticas do sistema ternário
SiO2-ZnO-TiO2 dopado com íons Eu3+ (1% em mol) ou Er3+ (0,2% a 2,0% em
mol). As composições xSiO2-([100-x]/2)ZnO-([100-x]/2)TiO2, com x = 40, 50, 60,
70 e 80 foram estudadas. Através de metodologia mista do processo sol-gel
com o método Pechini foi possível obter sóis estáveis e transparentes, géis
homogêneos, pós tratados termicamente de 100ºC a 1100°C e filmes finos
transparentes e sem trincas. Filmes finos multicamadas foram depositados
sobre substratos de sílica usando “spin coating” e calcinados a 500°C, seguido
de um tratamento térmico entre 700°C e 1000°C. Por fotoluminescência foram
observadas as transições de emissão características de íons Er3+ e Eu3+. A
caracterização por difração de raios X dos pós mostrou que a cristalização tem
início a partir de 800°C, com uma mistura de fases de titanatos de zinco
(ZnTiO3, Zn2TiO4) e segregação de titânio rutilo (TiO2). Em composições com
menores proporções de sílica (x= 40 ou 50) também ocorreu a formação de
silicato de zinco (Zn2SiO4) em temperaturas mais elevadas. Os espectros de
transmissão dos filmes apresentaram transmitância superior a 80%. Os valores
de “band gap” óptico, o tempo de vida, as razões R/O e o índice de refração
são dependentes do tratamento térmico e da composição dos pós. Usando o
método da envoltória, pôde-se calcular o índice de refração a 632,8 nm e a
espessura dos filmes finos, sendo que esta também foi estimada por
microscopia eletrônica de varredura (MEV) e espectroscopia m-Line. A emissão
fotoluminescente dos íons Eu3+ tem maior intensidade nos pós tratados à
800°C e nos filmes tratados à 700°C, sob excitação a 394 nm. Nestas
temperaturas o sistema permanece predominantemente amorfo. A emissão
fotoluminescente dos íons Er3+ foi mais intensa para os pós tratados a 1100°C,
sob excitação a 980 nm, devido à eliminação de grupos OH supressores das
emissões de Er3+. Nos filmes a maior intensidade se deu à temperatura de
700°C, sob excitação a 378 nm. Os filmes apresentaram apenas um modo
guiado, sendo o mais apropriado para uso como guia de onda e os pós são
indicados como fósforos podendo ser aplicados em “displays".
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