Gibbs Energy of Formation of Ca3Ti8Al12O37 and Phase Relations and Chemical Potentials in the System Al2O3-TiO2-CaO

The quaternary oxide in the system Al2O3-CaO-TiO2 is found to have the composition Ca3Ti8Al12O37 rather than CaTi3Al8O19 as reported in the literature. The standard Gibbs energy of formation of Ca3Ti8Al12O37 from component binary oxides is measured in the temperature range from 900 to 1250 K using a solid-state electrochemical cell incorporating single crystal CaF2 as the solid electrolyte. The results can be represented by the equation: delta G(f(0x))(0) (+/- 70)/J mol(-1) = -248474 - 15.706(T/K). Combining this information with thermodynamic data on calcium aluminates and titanates available in the literature, subsolidus phase relations in the pseudo-ternary system Al2O3-CaO-TiO2 are computed and presented as isothermal sections. The evolution of phase relations with temperature is highlighted. Chemical potential diagrams are computed at 1200 K, showing the stability domains of the various phases in the chemical potential-composition space. In each chemical potential diagram, chemical potential of one component is plotted against the cationic fraction of the other two components. The diagrams are valid at relatively high oxygen potentials where Ti is present in its four-valent state in all the oxide phases.

Preparation of Al2TiO5-Al2O3 and Al2TiO5-Al2O3-TiO2 Ceramics by High-Energy Ball Milling and Sintering

The present work reports on the preparation of Al2O3-TiO2 ceramics by high-energy ball milling and sintering, varying the molar fraction in 1:1 and 3:1. The powder mixtures were processed in a planetary Fritsch P-5 ball mill using silicon nitride balls (10 mm diameter) and vials (225 mL), rotary speed of 250 rpm and a ball-to-powder weight ratio of 5:1. Samples were collected into the vial after different milling times. The milled powders were uniaxially compacted and sintered at 1300 and 1500 degrees C for 4h. The milled and sintered materials were characterized by X-ray diffraction and electron scanning microscopy (SEM). Results indicated that the intensity of Al2O3 and TiO2 peaks were reduced for longer milling times, suggesting that nanosized particles can be achieved. The densification of Al2O3-TiO2 ceramics was higher than 98% over the relative density in samples sintered at 1500 degrees C for 4h, which presented the formation of Al2TiO5.

Desenvolvimento de revestimentos de óxidos mistos nanoestruturados de TiO2/Al2O3 em substratos metálicos de aço AISI 1020 e estudo das propriedades anticorrosivas

Sóis liofilizados precursores de Al2O3/TiO2, foram preparados via tecnologia sol-gel, com diferentes porcentagens de óxido de titânio (5%, 10%, 15% e 20%, em massa). Os sóis liofilizados foram caracterizados por meio de diversas análises, com o intuito de obter informações sobre o comportamento térmico, fases presentes, tamanho de partícula, composição e uniformidade das amostras. Os resultados obtidos indicam que os sóis apresentam as fases boemita e anatase, com partículas de tamanho nanométrico, tem composições muito similares quando analisadas em pontos distintos, átomos bem dispersos e distribuídos. Após esta etapa, amostras de aço AISI 1020 foram recobertas com estes sóis através do método dip-coating, o comportamento corrosivo foi estudado por meio de ensaios eletroquímicos e a morfologia das camadas, analisadas por meio de microscopias. Observou-se que as camadas eram uniformes e recobriam por completo toda a superfície das amostras, os ensaios de polarização indicaram melhorias no potencial eletroquímico para amostras recobertas, em comparação com amostras de aço sem recobrimento. O monitoramento de circuito aberto apresentou bons ajustes, indicando bom comportamento da camada. Notou-se pelas microscopias a presença de pontos de corrosão em algumas amostras antes dos ensaios, suspeitando-se que os resultados obtidos teriam sido melhores, caso houvesse um maior controle do processo de recobrimento.

Caracterização térmica e mecânica de cerâmicas porosas com camadas de TiO2 e Al2O3

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Influence of TiO2 and AI(2)O(3) on the electrical and microstructural properties of SnO2 ceramics obtained by the Pechini method

Tin oxide has wakened up great scientific and technological interest for its potential use in varistors production and as gas sensor. In order to improve the microstructural and electrical properties in SnO2 varistor ceramics, the influence of differents dopants used, like TiO2 and Al2O3, is under research. The effect of TiO2 and Al2O3 on the properties of Sn-Co-Nb varistor systems obtained by the Pechini method has been investigated in this work. Characterization of synthesized raw material was performed by X-Ray Diffraction (XRD) and Scanning Electronic Microscopy (SEM). The microstructural and electrical characterization of sintered samples show that the TiO2 favors the grain growth and the Al2O3 contributes to the decrease it, effect that is manifested in the Sn-Co-Nb varistor systems. Breakdown field increase up to 6300V/cm with increasing Al2O3 content and non-linear coefficients with alpha=22 were obtained.

A Novel Method for the Uniform Incorporation of Grain-Boundary Layer Modifiers in Positive Temperature Coefficient of Resistivity Barium Titanate

The presently developed two-stage process involves diping the prefired porous disks of n-BaTiO3 in nonaqueous solutions containing Al-buty rate, Ti-isopropoxide, and tetraethyl silicate and subsequent sintering. This leads to uniform distribution of the grain-boundary layer (GBL) modifiers (Al2O3+ TiO2+ SiO2) and better control of the grain size as well as the positive temperature coefficient of resistivity characteristics. The technique is particularly suited for GBL modifiers in low concentrations (< 1%).

Broadband near-infrared emission from transparent Ni2+-doped silicate glass ceramics

Transparent Ni2+-doped MgO-Al2O3-TiO2-SiO2 glass ceramics were prepared, and the optical properties of Ni2+-doped glass ceramics were investigated. Broadband emission centered at 1320 nm was observed by 980 nm excitation. The longer wavelength luminescence compared with Ni2+-doped Li2O-Ga2O3-SiO2 glass ceramics is ascribed to the low crystal field hold by Ni2+ in MgO-Al2O3-TiO2-SiO2 glass ceramics. The change in optical signals at the telecommunication bands with or without 980 nm excitation was also measured when the seed beam passes through the bulk gain host.(C) 2007 American Institute of Physics.

Improvement of Pt catalyst for soot oxidation using mixed oxide as a support

Catalytic activity of Pt catalysts for soot oxidation was studied using temperature programmed reactions. The activity of Pt loaded over TiO2-SiO2 (Pt/TiO2-SiO2) showed higher activity than other Pt/MOx systems (MOx = TiO2, ZrO2, SiO2, Al2O3. TiO2-ZrO2. TiO2-Al2O3, ZrO2-SiO2, ZrO2-Al2O3, SiO2-Al2O3). The activity was highest when the molar ratio of TiO2/(TiO2 + SiO2) ranged from 0.4 to 0.7. The effect of pretreatment with a gas containing low SO2 concentrations on the activity was compared for Pt/SiO2, Pt/TiO2 and Pt/TiO2-SiO2. In the case of Pt/TiO2-SiO2, the activity was markedly promoted by the pretreatment whereas no variation in the activity was observed for Pt/SiO2. The difference in the behavior towards the SO, pretreatment was attributed to property difference in the supports for sulfate accumulation. The high activity of Pt/TiO2-SiO2 was also confirmed under practical conditions with a diesel engine exhaust using a catalyst-supported diesel particulate filter (DPF). (C) 2003 Elsevier Science B.V. All rights reserved.

滇东南八布蛇绿岩地球化学特征及构造背景

八布蛇绿岩出露在北西向文山-麻栗坡和富宁走滑断裂之间的断块内，主要由蛇纹岩、辉长岩、玄武岩三个单元组成，彼此间均以断裂相接。地球化学研究表明，蛇纹岩SiO2、Al2O3、TiO2、MgO含量变化较大，依据主、微量元素组成可以分为两类，第一类球粒陨石标准化稀土元素分配模式整体较为平坦，推测原岩为镁铁质堆晶岩；另一类呈U型配分，推断原岩是方辉橄榄岩。玄武岩属拉斑系列，主量元素具有富MgO、TiO2，低Al2O3、K2O、P2O5，并且Na2O〉K2O等特征，类似于MORB型玄武岩；REE配分模式也显示出N-MORB型玄武岩的特征；同时，微量元素普遍具有LILE、Th富集，Nb、Ta、Zr、Hf等元素具明显亏损特征，又暗示源区曾遭受不同程度的俯冲带流体交代作用。综合分析认为，八布蛇绿岩形成于弧后盆地环境，其形成可能是古太平洋从SE至NW向华南大陆俯冲的产物。

Desenvolvimento e caracterização de revestimentos protetores contra carburização em tubos de pirólise de hidrocarbonetos na produção de olefinas

Este trabalho consistiu no desenvolvimento de revestimentos protetores contra carburização em ligas HP-40Nb, utilizadas na em fornos de pirólise para produção de olefinas, e do desenvolvimento de aparatos e técnicas para o teste, avaliação e caracterização destes revestimentos em ambientes fortemente carburizantes. Foram testados vários tipos de revestimentos, podendo estes ser resumidos em três grupos: i) camada de difusão de elementos específicos para o interior do metal (Al, Cu e Sn); ii) recobrimento com liga metálica (Ni-50Cr e Ni-5Al) e iii) recobrimento cerâmico (Al2O3, Cr2O3 e Al2O3 - TiO2). Além de revestimentos e camadas de difusão, um quarto tipo de material foi testado em sua resistência à carburização: ligas do tipo Fe-Cr- Al. A fim de testar os revestimentos e materiais desenvolvidos foram testados vários meios carburizantes. O que se mostrou mais adequado foi a mistura gasosa de hidrogênio e n-hexano, a uma temperatura de 1050°C. Foi construído um aparato exclusivamente para estes ensaios de carburização, o qual também foi utilizado para realizar os tratamentos de difusão necessários para produzir alguns dos revestimentos. A avaliação da resistência a carburização dos revestimentos e materiais foi feita por medição da profundidade de avanço da zona de precipitação de carbetos causada pela carburização, feito com auxílio de microscópio ótico. Os resultados dos ensaios mostraram que as camadas de difusão de alumínio, o revestimento da liga Ni-50Cr, o revestimento cerâmico de Al2O3 e as ligas Fe-Cr-Al tiveram bom ou ótimo desempenho como barreiras contra a carburização. Os outros revestimentos ou permitiram a penetração de carbono no metal base ou causaram uma deposição exagerada de coque na superfície dos corpos de prova.

Characterization of the porosity developed in a new titania-alumina catalyst support prepared by the sol gel route

Titanium oxide (TiO2) is a good candidate for support of hydrotreating catalysts but has the disadvantage of presenting a low surface area and a poor thermal stability when compared with Al2O3. A mixed TiO2-Al2O3 support was proposed as an alternative that is expected to be free from these drawbacks. The variation during firing of the nanoporous texture of supports composed of TiO2-Al2O3, TiO2 and Al2O3 was studied by small angle X-ray scattering (SAXS). The supports were prepared by the sol-gel route using Ti and Al isopropoxides. We have particularly analyzed the effects of acid and basic hydrolysis on the nanostructural features of catalyst supports fired at different temperatures. The nanopore radius distribution functions were determined from SAXS results assuming a simple model of spherical nanopores embedded in a homogeneous solid matrix. The modal pore radius in both pure TiO2 and pure Al2O3 supports grows from 1.3 to 2.2 nm as the firing temperature increases from 673 to 973 K. on the other hand, the modal pore radius in the mixed TiO2-Al2O3 support remains below 1.2 nm over the same range of firing temperatures. These results demonstrate the good thermal stability of the nanoporous texture of mixed TiO2-Al2O3 supports.

Structural and electrical characterization of semiconducting barium-lead-titanate ceramics

BaTiO3 is usually doped to achieve the temperature stability required by device applications, as well as to obtain a large positive temperature coefficient anomaly of resistivity (PTCR). Uniform distribution of dopants among the submicron dielectric particles is the key for optimal control of grain size and microstructure to maintain a high reliability. The system Ba0.84Pb0.16TiO3 was synthesized from high purity BaCO3, TiO2, PbO oxide powders as raw materials. Sb2O3, MnSO4 and ZnO were used as dopants and Al2O3, TiO2 and SiO2 as grain growth controllers. Phase composition was analyzed by using XRD and the microstructure was investigated by SEM. EDS attached to SEM was used to analyze phase composition specially related to abnormal grain growth. Electrical resistivities were measured as a function of temperature and the PTCR effect characterized by an abrupt increase on resistivity.

Caratterizzazione di membrane da nanofiltrazione

Nanofiltration (NF) is a pressure-driven membrane process, intermediate between reverse osmosis and ultrafiltration. Commercially available polymeric membranes have been used in a wide range of applications, such as drinking, process industry and waste water treatment. For all the applications requiring high stability and harsh washing procedures inorganic membranes are preferred due to their high chemical inertia. Typically, γ – Al2O3 as well as TiO2 and ZrO2 selective layers are used; the latter show higher chemical stability in a wide range of pH and temperatures. In this work the experimental characterization of two different type of membrane has been performed in order to investigate permeation properties, separation performance and efficiency with aqueous solutions containing strong inorganic electrolytes. The influence of salt concentration and feed pH as well as the role of concentration polarization and electrolyte type on the membrane behavior are investigated. Experimentation was performed testing a multi–layer structured NF membrane in α-Al2O3, TiO2 and ZrO2, and a polymeric membrane, in polyamide supported on polysulfone, with binary aqueous solutions containing NaCl, Na2SO4 or CaCl2; the effect of salt composition and pH in the feed side was studied both on flux and salt rejection. All the NF experimental data available for the two membranes were used to evaluate the volumetric membrane charge (X) corresponding to each operative conditions investigated, through the Donnan Steric Pore Model and Dielectric Exclusion (DSPM&DE). The results obtained allow to understand which are the main phenomena at the basis of the different behaviors observed.

Caratterizzazione geochimica dei sedimenti nel sito Caretti di Ferrara

Lo studio riguarda la caratterizzazione geochimica dei sedimenti del sito Caretti, situato a est del comune di Ferrara, interessato da un forte caso di contaminazione dovuto alla presenza di due discariche municipali non controllate risalenti agli anni '60-'70. L'obiettivo del lavoro è quello di valutare la geochimica dei sedimenti e delle acque prelevate nel sito al fine di individuare eventuali relazioni tra il chimismo delle due matrici. Inoltre, i dati dell' analisi dei sedimenti sono stati confrontati con quelli di letteratura per delinearne aspetti di provenienza. I dati geochimici dei sedimenti sono stati ottenuti mediante fluorescenza a raggi X (XRF) e sono stati elaborati graficamente e statisticamente, mediante software di analisi statistica (GCDkit). La composizione geochimica delle acque è stata ottenuta mediante tecniche di cromatografia ionica e spettroscopia di assorbimento atomico. La geochimica dei sedimenti ha evidenziato che la composizione chimica mostra associazioni di elementi legate a una componente tessiturale del sedimento. In particolare si rilevano concentrazioni elevate di Fe2O3, Al2O3, TiO2, Cr, Ni, e V in sedimenti a granulometria fine, a differenza delle concentrazioni di SiO2 e Na2O elevate in sedimenti sabbiosi. La distribuzione statistica degli elementi nei sedimenti e nelle acque ha permesso di effettuare una valutazione delle caratteristiche geochimiche dei principali corpi idrogeologici. La caratterizzazione geochimica ha fornito, inoltre, indicazioni sull'origine dei sedimenti. Cromo e Nichel, tra gli elementi in traccia, sono particolarmente efficaci nella valutazione della provenienza permettendo, all'interno del sito Caretti, una distinzione tra popolazioni di provenienza appenninica (bassi valori Cr-Ni) e padana (alti valori Cr-Ni).

Geochemical composition of the Trincheira Complex in the southwestern Amazon craton, Brazil

We document the first-known Mesoproterozoic ophiolite from the southwestern part of the Amazon craton, corresponding to the Trincheira Complex of Calymmian age, and propose a tectonic model that explains many previously enigmatic features of the Precambrian history of this key craton, and discuss its role in the reconstruction of the Columbia supercontinent. The complex comprises extrusive rocks (fine-grained amphibolites derived from massive and pillowed basalts), mafic-ultramafic intrusive rocks, chert, banded iron formation (BIFs), pelites, psammitic and a smaller proportion of calc-silicate rocks. This sequence was deformed, metasomatized and metamorphosed during the development of the Alto Guaporé Belt, a Mesoproterozoic accretionary orogen. The rocks were deformed by a single tectonic event, which included isoclinal folding and metamorphism of the granulite-amphibolite facies. Layered magmatic structures were preserved in areas of low strain, including amygdaloidal and cumulate structures. Metamorphism was pervasive and reached temperatures of 780-853°C in mafic granulites and 680-720°C in amphibolites under an overall pressure of 6.8 kbar. The geochemical composition of the extrusive and intrusive rocks indicates that all noncumulus mafic-ultramafic rocks are tholeiitic basalts. The mafic-ultramafic rocks display moderately to strongly fractionation of light rare earth elements (LREE), near-flat heavy rare earth elements (HREE) patterns and moderate to strong negative high field strength elements (HFSE) anomalies (especially Nb), a geochemical signature typical of subduction zones. The lowest units of mafic granulites and porphyroblastic amphibolites in the Trincheira ophiolite are similar to the modern mid-ocean ridge basalt (MORB), although they locally display small Ta, Ti and Nb negative anomalies, indicating a small subduction influence. This behavior changes to an island arc tholeiites (IAT) signature in the upper units of fine-grained amphibolites and amphibole rich-amphibolites, characterized by progressive depletion in the incompatible elements and more pronounced negative Ta and Nb anomalies, as well as common Ti and Zr negative anomalies. Tectono-magmatic variation diagrams and chondrite-normalized REE and primitive mantle normalized patterns suggest a back-arc to intra-oceanic island arc tectonic regime for the eruption of these rocks. Therefore, the Trincheira ophiolite appears to have originated in an intraoceanic supra-subduction setting composed of an arc-back-arc system. Accordingly, the Trincheira Complex is a record of oceanic crust relics obducted during the collision of the Amazon craton and the Paraguá block during the Middle Mesoproterozoic. Thus, the recognition of the Trincheira ophiolite and suture significantly changes views on the evolution of the southern margin of the Amazon craton, and how it can influence the global tectonics and the reconstruction of the continents.