Sintesi e caratterizzazione di cluster Ag-Cu-Fe, Au-Cu-Fe e Ni-Pd

Durante il mio periodo di tirocinio mi sono occupato della sintesi e caratterizzazione di cluster carbonilici eterometallici, ed in particolare di cluster Ag-Cu-Fe, Au-Cu-Fe, e Ni-Pd. In un primo momento il lavoro si è concentrato sullo studio della reazione tra cluster Cu-Fe e sali di Ag e Au, con lo scopo di ottenere specie Ag-Cu-Fe, e Au-Cu-Fe. Nella seconda parte l’attività è stata incentrata sulla sintesi di cluster Ni-Pd ad elevata nuclearità, attraverso reazioni tra [Ni6(CO)12]2- e composti di Pd(II). In entrambi i casi le sintesi sono state condotte variando i rapporti stechiometrici dei reagenti e i solventi, permettendo l’ottenimento di specie, caratterizzate spettroscopicamente mediante tecnica IR. In alcuni casi è stato anche possibile ottenere cristalli caratterizzati strutturalmente tramite diffrattometria a raggi X. Le reazioni di [Cu3Fe3(CO)12]3- con quantità crescenti di M=Ag, Au danno luogo alla formazione in sequenza di [Cu5Fe4(CO)16]3-, [MxCu5-xFe4(CO)16]3- (x = 0-5), [M5Fe4(CO)16]3-, [M6Fe4(CO)16]2-. Successivamente, nel caso in cui M= Ag, un ulteriore aggiunta di sali di M+ porta alla formazione di [Ag13Fe8(CO)32]3-, mentre se M= Au si formano i cosiddetti “bruni d’oro” e alla fine, [AuFe4(CO)16]-. Le specie [MxCu5-xFe4(CO)16]3- risultano particolarmente interessanti dato che possono essere viste come leghe molecolari M/Cu, che mostrano disordine sia sostituzionale che composizionale. Per quanto riguarda i cluster Ni-Pd sono state ottenute tre nuove specie carboniliche ad elevata nuclearità, ovvero [Ni37-xPd7+x(CO)48]6- (x= 0,69), [HNi37-xPd7+x(CO)48]5- (x= 0,53) and [Ni22-xPd20+x(CO)48]6- (x = 0.63). In tutte queste strutture il Pd tende ad occupare posizioni che minimizzano le interazioni Pd-CO massimizzando le interazioni M-M, mentre l’opposto risulta per il Ni. Ciò si traduce in una parziale segregazione dei due metalli, anche se alcuni fenomeni di disordine (sostituzionale e composizionale) sono presenti in tali strutture.

Interazione di cluster carbonilici FE-CU con complessi di metalli di transizione e leganti azotati

Nel corso di questa Tesi sono state studiate reazioni di cluster carburo-carbonilici Fe/Cu con composti azotati di varia natura: complessi fosforescenti di metalli di transizione, 1-10 fenantrolina, L-amminoacidi e Chinolina. In particolare la reazione tra Fe4C(CO)12Cu2(CH3CN)2 e [Ru(tpy)(bpy)(N4C-C6H4-CN)]+ ha portato alla sintesi dell’addotto Fe4C(CO)12{Cu2Cl[Ru(tpy)(bpy)(N4C-C6H4-CN)]}, sul quale sono state condotte misure di luminescenza (emissione, eccitazione e misura dei tempi di vita degli stati eccitati). Per confronto degli spettri registrati su campioni di adotto in soluzione con quelli del complesso cationico di Ru(II), si è ipotizzato che l’addotto sintetizzato in soluzione dia origine ad un sistema in equilibrio tra le specie legate e dissociate. Le reazioni di Fe4C(CO)12Cu2(CH3CN)2 e [NEt4][Fe5C(CO)14Cu(CH3CN)] con 1-10 fenantrolina hanno permesso di isolare le nuove specie [Fe4C(CO)12(Cuphen)]–, [Fe4C(CO)12(Cuphen)] e [Fe5C(CO)14(Cuphen)]–, sottoforma dei loro sali [Cu(phen)2][Fe4C(CO)12(Cuphen)], [NEt4] [Fe4C(CO)12(Cuphen)], [Fe4C(CO)12(Cuphen)], [NEt4][Fe5C(CO)14(Cuphen)]• CH2Cl2 e [NEt4][Fe5C(CO)14(Cuphen)]•THF. In tali cluster si nota come la natura bidentata di phen e il suo ingombro sterico abbiano causato notevoli riarrangiamenti strutturali rispetto alle specie iniziali contenenti acetonitrile. La sintesi di Fe4C(CO)12(CuQ)2 e [NEt4][Fe5C(CO)14(CuQ)] è avvenuta inaspettatamente a partire dalle reazioni condotte tra Fe4C(CO)12Cu2(CH3CN)2 e [NEt4][Fe5C(CO)14Cu(CH3CN)] con le molecole L-prolina, L-metionina e guanina, a causa della chinolina contenuta come impurezza nei reagenti di partenza. L’esito di questa reazione ha comunque mostrato l’elevata affinità dei cluster per il legante chinolina, sebbene presente in ambiente di reazione in misura sensibilmente inferiore rispetto agli altri reagenti. Tutte le nuove specie sintetizzate sono stati caratterizzate mediante spettroscopia IR e le strutture molecolari sono state determinate mediante diffrazione di raggi X su cristallo singolo.

Mineral zoning and geochemistry of epithermal polymetallic Zn-Pb-Ag-Cu-Bi mineralization at Cerro de Pasco, Peru

The large Cerro de Pasco Cordilleran base metal deposit in central Peru is located on the eastern margin of a middle Miocene diatreme-dome complex and comprises two mineralization stages. The first stage consists of a large pyrite-quartz body replacing Lower Mesozoic Pucara carbonate rocks and, to a lesser extent, diatreme breccia. This body is composed of pyrite with pyrrhotite inclusions, quartz, and black and red chalcedony (containing hypogene hematite). At the contact with the pyrite-quartz body, the diatreme breccia is altered to pyrite-quartz-sericite-pyrite. This body was, in part, replaced by pipelike pyrrhotite bodies zoned outward to carbonate-replacement Zn-Pb ores hearing Fe-rich sphalerite (up to 24 mol % Fes). The second mineralization stage is partly superimposed on the first and consists of zoned east-west-trending Cu-Ag-(Au-Zn-Pb) enargite-pyrite veins hosted in the diatreme breccia in the western part of the deposit and well-zoned Zn-Pb-(Bi-Ag-Cu) carbonate-replacement orebodies; in both cases, sphalerite is Fe poor and the inner parts of the orebodies show typically advanced argillic alteration assemblages, including aluminum phosphate Sulfate (APS) minerals. The zoned enargite-pyrite veins display mineral zoning, from a core of enargite-pyrite +/- alunite with traces of Au, through an intermediate zone of tennantite, chalcopyrite, and Bi minerals to a poorly developed Outer zone hearing sphalerite-galena +/- kaolinite. The carbonate-hosted replacement ores are controlled along N 35 degrees E, N 90 degrees E, N 120 degrees E, and N 170 degrees E faults. They form well-zoned upward-flaring pipelike orebodies with a core of famatinite-pyrite and alunite, an intermediate zone with tetrahedrite-pyrite, chalcopyrite, matildite, cuprobismutite, emplectite, and other Bi minerals accompanied by APS minerals, kaolinite, and dickite, and an outer zone composed of Fe-poor sphalerite (in the range of 0.05-3.5 mol % Fes) and galena. The outermost zone consists of hematite, magnetite, and Fe-Mn-Zn-Ca-Mg carbonates. Most of the second-stage carbonate-replacement orebodies plunge between 25 degrees and 60 degrees to the west, suggesting that the hydrothermal fluids ascended from deeper levels and that no lateral feeding from the veins to the carbonate-replacement orebodies took place. In the Venencocha and Santa Rosa areas, located 2.5 km northwest of the Cerro de Pasco open pit and in the southern part of the deposit, respectively, advanced argillic altered dacitic domes and oxidized veins with advanced argillic alteration halos occur. The latter veins are possibly the oxidized equivalent of the second-stage enargite-pyrite veins located in the western part of the deposit. The alteration assemblage quartz-muscovite-pyrite associated with the pyrite-quartz body suggests that the first stage precipitated at slightly, acidic fin. The sulfide mineral assemblages define an evolutionary path close to the pyrite-pyrrhotite boundary and are characteristic of low-sulfidation states; they suggest that the oxidizing slightly acidic hydrothermal fluid was buffered by phyllite, shale, and carbonate host rock. However, the presence in the pyrite-quartz body of hematite within quartz suggests that, locally, the fluids were less buffered by the host rock. The mineral assemblages of the second mineralization stage are characteristic of high- to intermediate-sulfidation states. High-sulfidation states and oxidizing conditions were achieved and maintained in the cores of the second-stage orebodies, even in those replacing carbonate rocks. The observation that, in places, second-stage mineral assemblages are found in the inner and outer zones is explained in terms of the hydrothermal fluid advancing and waning. Microthermometric data from fluid inclusions in quartz indicate that the different ores of the first mineralization stage formed at similar temperatures and moderate salinities (200 degrees-275 degrees C and 0.2-6.8 wt % NaCl equiv in the pyrite-quartz body; 192 degrees-250 degrees C and 1.1-4.3 wt % NaCl equiv in the pyrrhotite bodies; and 183 degrees-212 degrees C and 3.2-4.0 wt % NaCl equiv in the Zn-Pb ores). These values are similar to those obtained for fluid inclusions in quartz and sphalerite from the second-stage ores (187 degrees-293 degrees C and 0.2-5.2 wt % NaCl equiv in the enargite-pyrite veins: 178 degrees-265 degrees C and 0.2-7.5 wt % NaCl equiv in quartz of carbonate-replacement orebodies; 168 degrees-999 degrees C and 3-11.8 wt % NaCl equiv in sphalerite of carbonate-replacement orebodies; and 245 degrees-261 degrees C and 3.2-7.7 wt % NaCl equiv in quartz from Venencocha). Oxygen and hydrogen isotope compositions oil kaolinite from carbonate-replacement orebodies (delta(18)O = 5.3-11.5%o, delta D = -82 to -114%o) and on alunite from the Venencocha and Santa Rosa areas (delta(18)O = 1.9-6.9%o, delta D = -56 to -73%o). Oxygen isotope compositions of quartz from the first and second stages have 6180 values from 9.1 to 1.7.8 per mil. Calculated fluids in equilibrium with kaolinite have delta(18)O values of 2.0 to 8.2 and delta D values of -69 to -97 per mil; values in equilibrium with alunite are -1.4 to -6.4 and -62 to -79 per mil. Sulfur isotope compositions of sulfides from both stages have a narrow range of delta(34)S values, between -3.7 and +4.2 per mil; values for sulfates from the second stage are between 4.2 and 31.2 per mil. These results define two mixing trends for the ore-forming fluids. The first trend reflects mixing between a moderately saline (similar to 10 wt % NaCl equiv) magmatic end member that had degassed (as indicated by the low delta D values) and meteoric water. The second mixing indicates condensation of magmatic vapor with HCl and SO(2) into meteoric water, which formed alunite. The hydrothermal system at Cerro de Pasco was emplaced at a shallow depth (similar to 500 m) in the epithermal and upper part of a porphyry environment. The similar temperatures and salinities obtained for the first stage and second stages, together with the stable isotope data, indicate that both stages are linked and represent successive stages of epithermal polymetallic mineralization in the upper part of a porphyry system.

Comparativa de equipos de síntesis mecánica : aleaciones de base Al-Cu y Fe-Ni

La síntesis mecánica es un proceso basado en la molturación de una mezcla de polvosometida a altas energías que se producen por los choques entre las partículas y lasbolas de un micromolino, entre las partículas y las paredes del recipiente y entre lasmismas partículas. Los dos procesos involucrados en el proceso de síntesis mecánicason la soldadura en frío y la fractura.El proyecto que se presenta es una continuación de los diferentes estudios realizadosen el departamento de Recerca de Materials i Termodinàmica de la Universidad deGirona sobre el proceso de aleado mecánico, en especial del proyecto de Ivan Darnés(Abril 2005) donde se realizaba un estudio comparativo de los micromolinosPulverisette 7 (P7) y SPEX8000 a partir de dos aleaciones en polvo de base Fe.El presente proyecto tiene como objetivo principal realizar nuevamente unacomparación de los equipos P7 y SPEX8000, pero utilizando otras mezclas de polvoiniciales y modificando los parámetros del proceso. Para tal comparación se estudiaránlas muestras obtenidas a nivel estructural, térmico y morfológico

Nanoparticles of octakis [3-(3-amino-1,2,4-triazole)propyl] octasilsesquioxane as ligands for Cu(II), Ni(II), Cd(II), Zn(II), and Fe(III) in aqueous solution

Nanoparticles of octakis[3-(3-amino-1,2,4-triazole)propyl]octasilsesquioxane (ATZ-SSQ) were tested as ligands, for transition-metal ions in aqueous solution with a special attention to sorption isotherms, ligand-metal interaction, and determination of metal ions in natural waters. The adsorption potential of the material ATZ-SSQ was compared with related [3(3-amino-1,2,4-triazole)propyl]silica gel (ATZ-SG). The adsorption was performed using a batchwise process and both organofunctionalized surfaces showed the ability to adsorb the metal ions from aqueous solution. The Langmuir model was used to simulate the sorption isotherms. The results suggest that the sorption of these metals on ATZ-SSQ and ATZ-SG occurs mainly by surface complexation. The equilibrium condition is reached at time lower than 3 min for ATZ-SSQ, while for ATZ-SG is only reached at time of 25 min. The maximum metal ion uptake values for ATZ-SSQ were higher than the corresponding values achieved with the ATZ-SG. In order to obtain more information on the ligand-metal interaction of the complexes on the surface of the ATZ-SSQ nanomaterial, ESR study with various degrees of copper loadings was carried out. The ATZ-SSQ was tested for the determination (in flow using a column technique) of the metal ions present in natural waters. (C) 2007 Elsevier B.V. All rights reserved.

Application of cellulose modified with p-aminobenzoic groups in preconcentration system for determination of Cu, Fe, Ni, and Zn in fuel ethanol samples by flame atomic absorption spectrometry

Cellulose chemically modified with p-aminobenzoic groups, abbreviated as Cel-PAB, was used for preconcentration of copper, iron, nickel, and zinc from ethanol fuel, normally used in Brazil as engine fuel. The surface characteristics and the surface area of the cellulose were obtained before and after chemical modification using FT-IR, elemental analysis, and surface area analysis (B.E.T.). The retention and recovery of the analyte elements were studied by applying batch and column techniques.

Simultaneous Determination of Ba, Cr, Mo (Group 1), and Cu, Fe, Ni, and Pb (Group 2) in Commercial Fuel Ethanol by Graphite Furnace AAS

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

Different lubricating oil treatments for the determination of Cu, Cr, Fe, Ni, Sb, Pb, and Zn by HR-CS FAAS

Microwave-assisted acid decomposition, direct dilution in kerosene, and oil-in-water emulsion were evaluated as lubricating oil pretreatment procedures for Cu, Cr, Fe, Ni, Pb, Sb, and Zn determination by High-Resolution Continuum Source Flame Atomic Absorption Spectrometry (HR-CS FAAS). For wet digestion, results were compared with those obtained by Flame Atomic Absorption Spectrometry (FAAS). The ultrasound probe used in emulsions sonication contaminated samples with Cr, although better results have been observed for the other six elements in this condition. In general, recovery percentages ranging from 81-106%(Cu), 80-107%(Cr), 85-114%(Fe), 82-116%(Ni), 86-117%(Pb), 85-115%(Sb), and 81-114%(Zn) were obtained. The HR-CS FAAS showed to be faster and more sensitive than FAAS.

Simultaneous determination of Cr, Fe, Ni and V in crude oil by emulsion sampling graphite furnace atomic absorption spectrometry

In this work a simple and reliable method for the simultaneous determination of Cr, Fe, Ni and V in crude oil, using emulsion sampling graphite furnace atomic absorption spectrometry is proposed. Under the best conditions, sample masses around 50 mg were weighed in polypropylene tubes and emulsified in a mixture of 0.5% (v v(-1)) hexane + 6% (m v(-1)) Triton X-100 (R). Considering the compromised conditions, the pyrolysis an atomization temperatures for the simultaneous determination of Cr, Fe, Ni and V were 1400 degrees C and 2500 degrees C, respectively. Aliquots of 20 mu L of reference solution and sample emulsion were co-injected into the graphite tube with 10 mu L of 1.0 g L(-1) Mg(NO(3))(2) as chemical modifier. The detection limits (n = 10, 3 sigma) and characteristic masses were, respectively: 0.07 mu g g(-1) and 19 pg for Cr; 2.15 mu g g(-1) and 31 pg for Fe; 1.25 mu g g(-1) and 44 pg for Ni; and 1.15 mu g g(-1) and 149 pg for V. The reliability of the proposed method was checked by fuel oil Standard Reference Material (SRMTriton X-100 (R) 1634c - NIST) analysis. The concentrations found presented no statistical differences compared to the certified values at 95% confidence level.

Magnetic microstructures from magnetic force microscopy and Monte Carlo simulation in CoFe-Ag-Cu granular films

CoFe-Ag-Cu granular films, prepared by rf sputtering, displayed magnetic domain microstructures for ferromagnetic concentrations above about 32% at, and below the percolation threshold. All samples have a fcc structure with an (111) texture perpendicular to the film plane. Magnetic force microscopy (MFM) showed a variety of magnetic domain microstructures, extremely sensitive to the magnetic history of the sample, which arise from the balance of the ferromagnetic exchange, the dipolar interactions and perpendicular magnetocrystalline anisotropy, MFM images indicate that in virgin samples, magnetic bubble domains with an out-of-plane component of the magnetization are surrounded by a quasicontinuous background of opposite magnetization domains. The application of a magnetic field in different geometries drastically modifies the microstructure of the system in the remanent state: i) for an in-plane field, the MFM images show that most of the magnetic moments are aligned along the film plane, ii) for an out-of-plane field, the MFM signal increases about one order of magnitude, and out-of-plane striped domains with alternating up and down magnetization are stabilized. Numerical simulations show that a variety of metastable domain structures (similar to those observed experimentally) can be reached, depending on magnetic history, in systems with competing perpendicular anisotropy, exchange and dipolar interactions.

0 AND 02 ADSORPTION ON Ag/Cu[100]

In this work the adsorption mechanisms of atomic and molecular oxygen on Cu(100) surface are studied using ab initio simulation methods. Through the atomistic scale under-standing of the elementary oxidation processes we can further understand the large-scale oxidation. Copper is a material widely used in industry which makes it an interesting subject, and also understanding the oxidation of copper helps us understand the oxidation mechanism of other metals. First we have a look on some theory on surface alloys in general and behaviour of Ag on Cu(100) surface. After that the physical background there is behind the methods of density functional calculations are discussed, and some methods, namely potential energy surfaces and molecular dynamics, are introduced. Then there is a brief look on the numerical details used in the calculations, and after that, the results of the simulations are exhibited.

Mechanical Characterization of Lead-Free Sn-Ag-Cu Solder Joints by High-Temperature Nanoindentation

The reliability of Pb-free solder joints is controlled by their microstructural constituents. Therefore, knowledge of the solder microconstituents’ mechanical properties as a function of temperature is required. Sn-Ag-Cu lead-free solder alloy contains three phases: a Sn-rich phase, and the intermetallic compounds (IMCs) Cu6Sn5 and Ag3Sn. Typically, the Sn-rich phase is surrounded by a eutectic mixture of β-Sn, Cu6Sn5, and Ag3Sn. In this paper, we report on the Young’s modulus and hardness of the Cu6Sn5 and Cu3Sn IMCs, the β-Sn phase, and the eutectic compound, as measured by nanoindentation at elevated temperatures. For both the β-Sn phase and the eutectic compound, the hardness and Young’s modulus exhibited strong temperature dependence. In the case of the intermetallics, this temperature dependence is observed for Cu6Sn5, but the mechanical properties of Cu3Sn are more stable up to 200°C.