Europium-doped calcium titanate: Optical and structural evaluations

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Geochemistry at DSDP Leg 82 Holes

DSDP Leg 82 drilled nine sites to the southwest of the Azores Islands on the west flank of the Mid-Atlantic Ridge (MAR) in an attempt to determine the temporal and spatial evolution of the Azores "hot-spot" activity. The chemistry of the basalts recovered during Leg 82 is extremely varied: in Holes 558 and 561, both enriched (E-type: CeN/YbN = 1.5 to 2.7; Zr/Nb = 4.5 to 9.6) and depleted (or normal-N-type: CeN/YbN = 0.6 to 0.8; Zr/Nb > 20) mid-ocean ridge basalts (MORB) occur as intercalated lava flows. To the north of the Hayes Fracture Zone, there is little apparent systematic relationship between basalt chemistry and geographic position. However, to the south of the Hayes Fracture Zone, the chemical character of the basalts (N-type MORB) is more uniform. The coexistence of both E-type and N-type MORB in one hole may be explicable in terms of either complex melting/ fractionation processes during basalt genesis or chemically heterogeneous mantle sources. Significant variation in the ratios of strongly incompatible trace elements (e.g., La/Ta; Th/Ta) in the basalts of Holes 558 and 561 are not easily explicable by processes such as dynamic partial melting or open system crystal fractionation. Rather, the trace element data require that the basalts are ultimately derived from at least two chemically distinct mantle sources. The results from Leg 82 are equivocal in terms of the evolution of the Azores "hot spot," but would appear not to be compatible with a simple model of E-type MORB magmatism associated with upwelling mantle "blobs." Models that invoke a locally chemically heterogeneous mantle are best able to account for the small-scale variation in basalt chemistry.

New Catalysts for the Renewable Production of Monomers for Bioplastics

Terephthalic acid (PTA) is one of the monomers used for the synthesis of the polyester, polyethylene terephthalate (PET), that is used for the large-scale manufacture of synthetic fibers and plastic bottles. PTA is largely produced from the liquid-phase oxidation of petroleum-derived p-xylene (PX). However, there are now ongoing worldwide efforts exploring alternative routes for producing PTA from renewable, biomass resources.

In this thesis, I present a new route to PTA starting from the biomass-derived platform chemical, 5-hydroxymethylfurfural (HMF). This route utilizes new, selective Diels-Alder-dehydration reactions involving ethylene and is advantageous over the previously proposed Diels-Alder-dehydration route to PTA from HMF via 2,5-dimethylfuran (DMF) since the H₂ reduction of HMF to DMF is avoided. Specifically, oxidized derivatives of HMF are reacted as is, or after etherification-esterification with methanol, with ethylene over solid Lewis acid catalysts that do not contain strong Brønsted acids in order to synthesize intermediates of PTA and its equally important diester, dimethyl terephthalate (DMT). The partially oxidized HMF, 5-(hydroxymethyl)furoic acid (HMFA) is reacted with high pressure ethylene over a pure-silica molecular sieve catalyst containing framework tin (Sn-Beta) to produce the Diels-Alder-dehydration product, 4-(hydroxymethyl)benzoic acid (HMBA), with ~30% selectivity at ~20% yield. If HMFA is protected with methanol to form methyl 5-(methoxymethyl)furan-2-carboxylate (MMFC), MMFC can react with ethylene in the presence of a pure-silica molecular sieve containing framework zirconium (Zr-Beta) to produce methyl 4-(methoxymethyl)benzenecarboxylate (MMBC) with >70% selectivity at >20% yield. HMBA and MMBC can then be oxidized to produce PTA and DMT, respectively. When Lewis acid containing mesoporous silica (MCM-41) and amorphous silica, or Brønsted acid containing zeolites (Al-Beta), are used as catalysts, a significant decrease in selectivity/yield of the Diels-Alder-dehydration product is observed.

An investigation to elucidate the reaction network and side products in the conversion of MMFC to MMBC was performed, and the main side products are found to be methyl 4-formylcyclohexa-1,3-diene-1-carboxylate and the ethylene Diels-Alder adduct of this cyclohexadiene. These products presumably form by a different dehydration pathway of the MMFC/ethylene Diels-Alder adduct and should be included when determining the overall selectivity to PTA or DMT since, like MMBC, these compounds are precursors to PTA or DMT.

Fundamental physical and chemical information on the ethylene Diels-Alder-dehydration reactions catalyzed by the Lewis acid-containing molecular sieves was obtained. Madon-Boudart experiments using Zr-Beta as catalyst show that the reaction rates are limited by chemical kinetics only (physical transport limitations are not present), all the Zr⁴⁺ centers are incorporated into the framework of the molecular sieve, and the whole molecular sieve crystal is accessible for catalysis. Apparent activation energies using Zr-Beta are low, suggesting that the overall activation energy of the system may be determined by a collection of terms and is not the true activation energy of a single chemical step.

Implicaciones geodinámicas del complejo metamórfico paleozoico de la Sierra Madre Oriental en el Noreste de México

Dataciones geocronológicas U-Pb en circones detríticos, edades 40Ar/ 39Ar en mica blanca, análisis estructurales, texturales, la composición química de elementos mayores, traza y tierras raras (REE) así como la composición química mineral de las rocas metamáficas, metultramáficas y metasedimentarias, fueron determinadas con el fin de determinar las condiciones metamórficas, el ambiente tectónico y la procedencia del Esquisto Granjeno en el noreste de México (Nuevo León y Tamaulipas). En el país existen rocas metamórficas paleozoicas que están relacionados con los procesos que dieron lugar a la colisión entre Laurentia y Gondwana durante la formación Pangea. Vestigios de la configuración continental paleozoica de México se encuentran en el Esquisto Granjeno, que forma parte del basamento metamórfico de la Sierra Madre Oriental. Relaciones de campo y análisis petrográficos indican que el Esquisto Granjeno consiste de rocas metamórficas con protolitos sedimentarios (psamita, pelita, turbidita, conglomerado, lutita negra) e ígneos (toba, flujos de lava, lava meta-almohadillada y cuerpos ultramáficos). El geotermómetro de clorita, el geobarómetro de fengita y la edad 40Ar/ 39Ar calculada indican que el Esquisto Granjeno fue afectado por metamorfismo en facies de sub-esquistos verdes a facies de esquistos verdes-anfibolita, (165-410°C y 2.5-4 kbar ) durante el Carbonífero (330±30 Ma). Las rocas metamáficas del Esquisto Granjeno tienen una afinidad sub-alcalina a alcalina y se caracterizan por un bajo contenido de SiO2 (40-50 wt%), alto contenido de Al2O3 (19 wt%) y #MgO de 48-67. La abundancia de tierras raras (∑REE) varía de 51-167 ppm. Estas rocas presentan patrones de REE normalizados a condrita moderadamente fraccionados, con valores de LaN/YbN 0.74-8.88. La anomalía de europio es variable (Eu/Eu* 0.80- 1.09) y presenta una tendencia ligeramente negativa (Eu/Eu* 0.96). Las rocas metamáficas tienen composiciones correspondientes a basaltos de cresta (MORB) e isla oceánica (OIB), de acuerdo a los valores en las relaciones Zr/Y=6-8 y Zr/Nb=4-9 para OIB y 0.9-3; 14-53 para MORB. Los protolitos de la serpentinita y el metacumulato corresponden a dunita y harzburgita. La serpentina y el metacumulato tienen un contenido de MgO (16-39 wt%), SiO2 (36-45 wt%), FeO (2-11 wt%), Al2O3 (0.76-13 wt%), CaO (< 22wt%) y #MgO (85-98, 69). Las rocas de talco presentan contenido de MgO (26-33wt%), SiO2 (31- 61wt%), FeO (3.7-9.8wt%), Al2O3 (1.2-19wt%), CaO (0.25-2.0wt%), y #Mg (83-93). Los patrones de tierras raras casi horizontals (LaN/YbN=0.51-19.95 y la relación LaN/SmN=0.72-9.08 sugieren un origen vinculado a un ambiente de dorsal oceánica y de suprasubducción para las rocas ultramáficas. Las serpentinitas contienen cromita rica en Al, ferrit-cromita y magnetita. La cromita rica en Al tiene #Cr 0.48-0.55 que indica que este mineral fue formado a partir de una fuente tipo MORB y que fue afectada hasta un 18% fusión parcial durante su formación. La ferritchromita tiene #Cr 0.93-1.00 que indica un origen metamórfico. La composición química de roca total indica que los protolitos de las rocas metasedimentarias consisten de lutita, grauvaca y arenita. La metapelita y metapsamita tienen un contenido de SiO2 (69-78% y 80-96% ) y de Al2O3 (9-13% y 1-8%). La abundancia de ∑REE son variables en los metasedimentos (9-178 ppm). Presentan patrones de REE normalizados a condrita con una tendencia más fraccionada que los de las rocas metamáficas, con valores en las relaciones LaN/YbN de 3-16. Las rocas metasedimentarias tienen anomalías de europio negativa (Eu/Eu* 0.67). Los datos obtenidos sugieren que los protolitos de las rocas metasedimentarias derivan de fuentes mixtas con una composición ígnea félsica-básica. (Ti/Nb 200-400). Según los valores de las relaciones de los elementos traza Th/Sc y Zr/Sc de 0.2-3.6 y 0.2-220, respectivamente se sugiere un ambiente de depósito para los protolitos de margen continental activo.

Microstructures and mechanical properties of as-cast Mg-5Y-3Nd-Zr-xGd (x=0, 2 and 4 wt.%) alloys

Mg-5Y-3Nd-0.6Zr-xGd (x = 0, 2 and 4 wt.%) alloys were prepared by metal mould casting technique, the structures and mechanical properties were investigated. The alloys were mainly composed of alpha-Mg solid solution and beta-phase. With increasing Gd content, Mg5RE phase increased and the grain was refined. The Mg-5Y-3Nd-2Gd-0.6Zr alloy exhibited highest ultimate tensile strength and Mg-5Y-3Nd-0.6Zr alloy showed highest yield strength at room temperature. With increasing amount of Gd, the thermal resistance was improved. The Mg-5Y-3Nd-4Gd-0.6Zr alloy exhibited highest UTS and YS at 250 degrees C, they were about 1.27 times higher than those of Gd-free alloy, which was mainly attributed to the increase of the beta-phase and Mg5RE strengthening phase.

Zr^4＋和Hf^4＋在水合氧化铁上的吸附及其分异的实验研究

本文研究了4价阳离子Zr、Hf在水合氧化铁(HFO)上的吸附及其在胶体／溶液界面的分异行为。研究结果表明：等价元素Zr、Hf在HFO上的吸附是非线性的，在吸附和共沉淀过程中二者发生了分异，Zr的吸附能力要大于Hf；pH<6时，固相中Zr／Hf比值随pH的升高迅速降低，而在天然水体pH范围内(pH≥6)，Zr、Hf的吸附量Q及Zr／Hf比值则不随pH发生变化，显示了Zr、Hf在表生环境中的相对惰性行为。本研究为吸附／解吸或水／粒相互作用导致Zr、Hf在地表环境的分异提供了实验证据。

Studies of the Room-Temperature Multiferroic Pb(Fe0.5Ta0.5)0.4(Zr0.53Ti0.47)0.6O3: Resonant Ultrasound Spectroscopy, Dielectric, and Magnetic Phenomena

Recently, lead iron tantalate/lead zirconium titanate (PZTFT) was demonstrated to possess large, but unreliable, magnetoelectric coupling at room temperature. Such large coupling would be desirable for device applications but reproducibility would also be critical. To better understand the coupling, the properties of all 3 ferroic order parameters, elastic, electric, and magnetic, believed to be present in the material across a range of temperatures, are investigated. In high temperature elastic data, an anomaly is observed at the orthorhombic mm2 to tetragonal 4mm transition, Tot = 475 K, and a softening trend is observed as the temperature is increased toward 1300 K, where the material is known to become cubic. Thermal degradation makes it impos- sible to measure elastic behavior up to this temperature, however. In the low temperature region, there are elastic anomalies near ≈40 K and in the range 160–245 K. The former is interpreted as being due to a magnetic ordering transition and the latter is interpreted as a hysteretic regime of mixed rhom- bohedral and orthorhombic structures. Electrical and magnetic data collected below room temperature show anomalies at remarkably similar temperature ranges to the elastic data. These observations are used to suggest that the three order parameters in PZTFT are strongly coupled.

Electric field gradients in (111)In-doped (Hf/Zr)(3)Al(2) and (Hf/Zr)(4)Al(3) mixed compounds: ab initio calculations, perturbed angular correlation measurements and site preference

The quadrupolar hyperfine interactions of in-diffused (111)In -> (111)Cd probes in polycrystalline isostructural Zr(4)Al(3) and Hf(4)Al(3) samples containing small admixtures of the phases (Zr/Hf)(3)Al(2) were investigated. A strong preference of (111)In solutes for the contaminant (Zr/Hf)(3)Al(2) minority phases was observed. Detailed calculations of the electric field gradient (EFG) at the Cd nucleus using the full-potential augmented plane wave + local orbital formalism allowed us to assign the observed EFG fractions to the various lattice sites in the (Zr/Hf)(3)Al(2) compounds and to understand the preferential site occupation of the minority phases by the (111)In atoms. The effects of the size of the supercell and relaxation around the oversized In and Cd probe atoms were investigated in detail.

Ionized oxygen vacancy-related electrical conductivity in (Pb(1-x)La(x)) (Zr(0.90)Ti(0.10))(1-x/4)O(3) ceramics

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Deformation and crystallization of Zr-based amorphous alloys in homogeneous flow regime

The purpose of this study is to experimentally investigate the interaction of inelastic deformation and microstructural changes of two Zr-based bulk metallic glasses (BMGs): Zr41.25Ti13.75Cu12.5Ni10Be22.5 (commercially designated as Vitreloy 1 or Vit1) and Zr46.75Ti8.25Cu7.5Ni10Be27.5 (Vitreloy 4, Vit4). High-temperature uniaxial compression tests were performed on the two Zr alloys at various strain rates, followed by structural characterization using differential scanning calorimetry (DSC) and transmission electron microscopy (TEM). Two distinct modes of mechanically induced atomic disordering in the two alloys were observed, with Vit1 featuring clear phase separation and crystallization after deformation as observed with TEM, while Vit4 showing only structural relaxation with no crystallization. The influence of the structural changes on the mechanical behaviors of the two materials was further investigated by jump-in-strain-rate tests, and flow softening was observed in Vit4. A free volume theory was applied to explain the deformation behaviors, and the activation volumes were calculated for both alloys.

The influence of Zr layer thickness on contact deformation and fracture in a ZrN-Zr multilayer coating

In order to understand the influence of ductile metal interlayer on the overall deformation behavior of metal/nitride multilayer, different configurations of metal and nitride layers were deposited and tested under indentation loading. To provide insight into the trends in deformation with multilayer spacings, an FEM model with elastic-perfect plastic metal layers alternate with an elastic nitride on top of an elastic-plastic substrate. The strong strain mismatch between the metal and nitride layers significantly alters the stress field under contact loading leading to micro-cracking in the nitride, large tensile stresses immediately below the contact, and a transition from columnar sliding in thin metal films to a more uniform bending and microcracking in thicker coatings.

Structure and Photocatalytic Activity of Ti 1- x M x O 2±δ (M = W, V, Ce, Zr, Fe, and Cu) Synthesized by Solution Combustion Method

The W, V, Ce, Zr, Fe, and Cu metal ion substituted nanocrystalline anatase TiO2 was prepared by solution combustion method and characterized by XRD, Raman, BET, EPR, XPS, IR TGA, UV absorption, and photoluminescence measurements. The structural studies indicate that the solid solution formation was limited to a narrow range of concentrations of the dopant ions. The photocatalytic degradation of 4-nitrophenol under UV and solar exposure was investigated with Ti1-xMxO2±δ. The degradation rates of 4-nitrophenol with these catalysts were lesser than the degradation rates of 4-nitrophenol with undoped TiO2 both with UV exposure and solar radiation. However, the photocatalytic activities of most metal ion doped TiO2 are higher than the activity of the commercial TiO2, Degussa P25. The decrease in photocatalytic activity is correlated with decrease in photoluminescence due to electron states of metal ions within the band gap of TiO2.

Experimental and Theoretical Studies of Unusual Four-Membered Metallacycles from Reactions of Group 4 Metallocene Bis(trimethylsilyl)-acetylene Complexes with the Sulfurdiimide Me3SiN=S=NSiMe3

The use of the sulfurdiimide RN=S=NR' (R = R' = SiMe3, 3) in reactions with group 4 metallocene bis(trimethylsilyl)-acetylene complexes of the type [Cp2M(L (eta(2)-Me3Si-C2SiMe3)] (1: M = Ti, no L; 2: M = Zr, L = pyridine) has led to the formation of four-membered metallacycles 4M containing the group 4 metal, nitrogen and sulfur. DFT calculations performed on compound 4Ti indicate that this complex is best described as a sigma-complex with cyclic delocalisation of the ring electrons. Moreover, pseudo-Jahn-Teller distortion plays a significant role in stabilising this complex.