For years, the alloy of choice for electroplating electronic components has been tin-lead (Sn-Pb) alloy. However, the legislation established in Europe on July 1, 2006, required significant lead (Pb) content reductions from electronic hardware due to its toxic nature. A popular alternative for coating electronic components is pure tin (Sn). However, pure tin has the tendency to spontaneously grow electrically conductive Sn whisker during storage. Sn whisker is usually a pure single crystal tin with filament or hair-like structures grown directly from the electroplated surfaces. Sn whisker is highly conductive, and can cause short circuits in electronic components, which is a very significant reliability problem. The damages caused by Sn whisker growth are reported in very critical applications such as aircraft, spacecraft, satellites, and military weapons systems. They are also naturally very strong and are believed to grow from compressive stresses developed in the Sn coating during deposition or over time. The new directive, even though environmentally friendly, has placed all lead-free electronic devices at risk because of whisker growth in pure tin. Additionally, interest has occurred about studying the nature of other metal whiskers such as zinc (Zn) whiskers and comparing their behavior to that of Sn whiskers. Zn whiskers can be found in flooring of data centers which can get inside electronic systems during equipment reorganization and movement and can also cause systems failure.Even though the topic of metal whiskers as reliability failure has been around for several decades to date, there is no successful method that can eliminate their growth. This thesis will give further insights towards the nature and behavior of Sn and Zn whiskers growth, and recommend a novel manufacturing technique that has potential to mitigate metal whiskers growth and extend life of many electronic devices.

Made available in DSpace on 2014-06-11T19:22:18Z (GMT). No. of bitstreams: 0 Previous issue date: 2011-02-28Bitstream added on 2014-06-13T18:08:00Z : No. of bitstreams: 1 oliveira_el_me_sjrp.pdf: 531004 bytes, checksum: 26290057a6f49446476e6e8192925843 (MD5) / Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES) / Neste trabalho, descrevemos cíclicas de reticulados algébricos Zn-rotacionados de dimensão ímpar. Essas construções são obtidas através da imersão Rn, via homomorfismo canônico, de determinados Z-módulos livres de posto finito contidos em subcorpos de extensões ciclotômicas do tipo Q(ζp), Q(ζp2), Q(ζpq)e Q(ζpq2), com p e q primos ímpares. Caracterizamos os reticulados e apresentamos propriedades e aplicações na Teoria da Informação. / In this work we describe cyclic constructions of odd dimension. These constructions are obtained by immersion in Rn via the canonical homomorphism, of certain Z-free modules of finite rank contained in subfield cyclotomic extensions of type Q(ζp), Q(ζp2), Q(ζpq)e Q(ζpq2), com p e q odd prime. Featuring the obtained lattices and presenting properties and applications in Information Theory.

O conteúdo de zinco (Zn) reativo cerebral é importante para o equilíbrio da sinaptofisiologia neural. A prova disto é que um aumento nos seus níveis, após evento hipóxico-isquêmico, resulta em neurotoxicidade, o que tem estimulado o tratamento desta disfunção cerebral com quelantes de Zn, tal como o dietilditiocarabamato (DEDTC). No caso do DEDTC, o uso deste composto sobre esta disfunção deve ser analisado com cuidado, pois ele também apresenta muitos efeitos colaterais sobre o sistema nervoso central. Desta forma, para atender este propósito, é necessário antes obter uma concentração de DEDTC com menores efeitos colaterais. Por esta razão, no presente trabalho, nós decidimos usar um modelo vertebrado mais simples, tal como o peixe-zebra, o qual permitiria a triagem, em larga escala, dos efeitos de DEDTC sobre o Zn reativo. Entretanto, jamais foi mostrada a presença de Zn reativo no cérebro de peixe-zebra. Com isto, através de marcações histológicas, nós conseguimos mostrar pela primeira vez a distribuição citoarquitectônica de Zn reativo em neurônios glutamatérgicos, bem como o número desses neurônios contendo Zn no cérebro de peixe-zebra. Isto nos permitiu avaliar o efeito de diferentes concentrações de DEDTC sobre o conteúdo de Zn cerebral do peixe-zebra, o qual foi intensamente quelado por elevadas quantidades do composto, induzindo comportamentos tipo-crise. Neste mesmo estudo nós obtemos também uma concentração de DEDTC com poucos efeitos colaterais que poderia exercer neuroproteção sobre o aumento de Zn reativo induzido pela hipóxia-isquemia. Assim, após a padronização de um modelo de hipóxia em peixe-zebra, que demonstra danos relacionados à isquemia, nós testamos se essa concentração de DEDTC poderia ser neuroprotetora sobre este modelo. Contudo, DEDTC apresentou efeitos pró-oxidantes, embora ele tenha atenuado o elevado conteúdo de Zn reativo induzido pela hipóxia. Portanto, mesmo que o DEDTC tenha falhado, este modelo, agora, está apto para a triagem de outros fármacos com potencial ação sobre o alterado conteúdo de Zn reativo que ocorre em eventos hipóxicos-isquêmicos. / The content of brain reactive zinc (Zn) is important for the synaptophysiology in the central nervous system (CNS). This is evidenced in hypoxic-ischemic events, when an increase in their levels results in neurotoxicity. Consequently, this has stimulated the treatment of cerebral ischemia with Zn chelators, such as diethyldithiocarbamate (DEDTC). In the case of DEDTC, the use of this compound in this dysfunction should be examined carefully, because it also has many side effects on the (CNS). Thus, to meet this, it is necessary first to obtain a concentration of DEDTC with negligible side effects. Here, we decided to use a simpler vertebrate model, such as zebrafish, which would allow large-scale screening of DEDTC effects on reactive Zn. However, the presence of reactive Zn has never been shown in zebrafish brain. Then, using histological markers, we were able to show for the first time the cytoarchitectonic distribution of reactive Zn in glutamatergic neurons as well as the number of these neurons containing Zn in the zebrafish brain. This allowed us to evaluate the effect of different DEDTC concentrations on the brain content of Zn in zebrafish. As a result, high levels of the compound did strongly chelate the metal, inducing seizure-like behaviors. In this study we also obtained a DEDTC concentration with few side effects that could exert neuroprotection on the increased reactive Zn induced by hypoxia-ischemia. Then, after the standardization of an ischemic-sensitive model of hypoxia in zebrafish, we tested if this DEDTC concentration could be neuroprotective on this model. Nevertheless, DEDTC showed pro-oxidant effects, though it had mitigated the elevated content of reactive Zn induced hypoxia. Therefore, despite the DEDTC have failed as neuroprotective drug, this model enables the screening of other chemical agents with potential action on the increased content of reactive Zn that occurs in hypoxic-ischemic events.

This work represents the most recent development of Zn isotopic measurements, and the first identification of Zn isotopic fractionation in natural materials using Thermal Ionisation Mass Spectrometry (TIMS). The procedures developed in this research systematically evaluates and solves several critical analytical issues involved in TIMS Zn isotopic measurements such as, reducing the size of sample needed to perform an accurate and precise measurement, minimizing the effect of interferences on the Zn fractionation, reducing the blank associated with the analyses, dissolution and purification of different natural samples, and the generally ignored issue of the effect of the ion exchange chemistry (Zn separation) to the fractionation of Zn. These procedures have allowed sub-permil fractionations in the isotopic composition of Zn to be revealed in small Zn sample (1µg), and the determination of low level (ng) elemental abundance of Zn in samples to be measured accurately by the means of isotope dilution mass spectrometry IDMS. This thesis uses the rigorous double spike technique to measure fractionation, relative to the internationally proposed absolute Zn isotopic reference material (δ zero), based on a high purity Alfa Aesar 10759, now available to the international isotope community. All the isotopic measurements in natural materials were performed on bulk samples purified by ion exchange chemistry. / The isotopic composition of the Zn minerals and igneous rocks agreed with that of the absolute reference material, which makes it possible to consider this reference material as being representative of “bulk Earth” Zn. Significant and consistent fractionation of ~+0.3 ‰ per amu were found in 5 sediments from a range of localities. The consistency of this is attributed to conveyor type oceanic circulations effects. The results from the two metamorphic samples indicate that the fractionation of Zn in these rocks is the same as found in igneous rocks but are different from the Zn found in sedimentary rocks. This supports the widely held assumption that high temperature and pressure processes do not fractionate the isotopic composition of chalcophile elements, such as has been found for Cd. Clay sample TILL-3 appears to exhibit a consistently slightly positive Zn fractionation of +0.12 ± 0.10 ‰ amu-1, although inside the uncertainties of both igneous and sedimentary rocks, which is not surprising since Till is thought to be a formed from a range of mixed glacial sediments The isotopic composition of Zn was measured in two plants and one animal sample. The fractionation of (-0.088 ± 0.070 ‰ amu-1) of Zn in the Rice (a C3 type plant material) sample suggested that Zn may be used to study Zn systematics in plants. The result obtained for MURST-Iss-A2 (Antarctic Krill) was +0.21 ± 0.11 ‰ amu-1 relative to the laboratory standard which is similar to the average Zn fractionation results of +0.281 ± 0.083 ‰ amu-1 obtained for marine sediments. / In this work, the isotopic composition of Zn was measured in five stone and two iron meteorites. The range of Zn fractionation in stone meteorites was between -0.287 ± 0.098 and + 0.38 ± 0.16 ‰ amu-1, and was consistent with previous work, although more measurements would be needed to generalize this to all stone meteorites. In iron meteorites; Canyon Diablo was found to have the greatest fractionation of +1.11 ± 0.11 ‰ amu-1 relative to the laboratory standard. Of all the meteorites studied, Redfields clearly showed an anomalous isotopic composition indicating that this meteorite possesses a significantly different Zn isotopic composition compared to all of the other natural materials measured. Using 64Zn as a reference isotope, significant differences relative to the laboratory standard were found of +5.6 ± 0.4‰, +4.4 ± 3.6 ‰, and +21.0± 0.9 ‰ and +27.4 ± 18.8 ‰ on 66Zn and 67Zn, 68Zn and 70Zn respectively. These significant “Redfields anomalies” can be interpreted in a number of ways in relation to their nucleosynthetic production. Whether Redfields is a primitive type of iron meteorite or not, the Redfields anomaly strongly suggests wide spread isotopic heterogeneity of at least one part of the Solar System and does not support the suggestion that “Zn was derived from an initially single homogeneous reservoir in the early Solar System”. A pilot study to determine the concentration and the isotopic composition of Zn in River and tap water was performed. / The concentration of Zn in River water averaged 6.9 ± 0.8 ngg-1, while for tap water it ranged from 13.1 ngg-1 to 5.2 μgg-1. River water was fractionated by -1.09 ± 0.70 ‰ amu-1, while restrained tap water yielded the maximum fractionation of -6.39 ± 0.62 ‰ amu-1 relative to the laboratory standard. The Zn fractionation of tap water is much larger than all other natural samples, although the uncertainty is also significantly greater due to the use of the less precise Daly detector used for these preliminary experimental measurements. The fractionation of Zn in seven ultra pure Zn standard materials was measured relative to the laboratory standard and found to range from -5.11 ± 0.36 ‰ amu-1 for AE 10760 to +0.12 ± 0.16 ‰ amu-1 for Zn IRMM 10440. There appears to be some evidence for a relationship between Zn fractionation and its purity. As well as natural materials, the fractionation of Zn was measured in a number of processed materials. None of these results or those obtained for natural materials impact on the currently IUPAC accepted value for the atomic weight of Zn. Along with fractionation determinations, the concentration of Zn was also measured by Isotope Dilution Mass Spectrometry in all of the samples. The concentration of Zn in five stony meteorites ranged from 26 ± 13 to 302 ± 14 μgg-1 for Plainview and Orgueil respectively. For ordinary Chondrites, the concentration of Zn in the three samples analysed ranged from 26 ± 13 to 64 ± 34 μgg-1 for Plainview and Brownfield 1937 respectively. / The concentration of Zn was measured in two metamorphic rocks standard materials; the maximum concentration was 101.5 ± 1.7 µgg-1 in SDC-1. The concentration of Zn present in plant samples studied in this research was 22.15 ± 0.42, 14.62 ± 0.27 µgg-1 for Rice IMEP-19 and Sargasso NIES-Number 9 respectively which is within the normal range of Zn concentrations. Except for meteorites, the final uncertainties consistently cover the ranges of individual concentration measurements and indicate the homogeneity of the samples, including samples from different bottles where available. The final fractional uncertainties obtained for SRMs were all less than 2.8 %, demonstrating the high level of precision possible using IDMS.

An acid rock drainage (ARD) stream emanating from the Zn-Pb XY-deposit in the Yukon Territory was examined in order to evaluate the physico-chemical and geochemical processes governing the distribution of dissolved elements from the creek. The creek showed very high concentrations of metals (300 mg/L Fe, 500 mg/L Zn, 15 000 µg/L Ni, 1300 µg/L Cu and 4500 µg/L Cd), low water temperatures (1 – 12°C) and was acidic to moderately acidic (pH 3.1 – 5.0). It was found that this stream experienced a strong seasonal evolution, with increased sulphate and metal concentrations and decreased pH over the course of the summer. The mineral precipitates that formed under low pH conditions were a mixture of schwertmannite, goethite, jarosite and barite, while those that formed under moderately acidic conditions were a mixture of jurbanite, hydrobasaluminite, gibbsite and an X-ray amorphous Al-sulphate phase. Most of the mineral precipitates were of inorganic origin, although microbes may have played a role in mineral formation and trace metal sequestration in some of the precipitates. All of the mineral precipitates contained anomalous concentrations of trace elements (up to 1.5 % wt Zn) and showed a seasonal evolution in their mineralogy, both of which were determined to be a function of the pH and prevailing geochemical conditions. The geochemistry of the ARD creek draining the XY-deposit was compared to another ARD creek in the area that was likely draining shales. The two creeks were compared in order to determine if ARD geochemical characteristics can be used as a tool for the mineral exploration industry.

The West Ansil deposit was the first Cu discovery in 25 years in the Noranda Central Camp. It has a combined indicated and inferred resource of ~1.2 Mt. Grades for the indicated resource are 3.4% Cu, 0.4% Zn, 1.4 g/t Au and 9.2 g/t Ag. The bulk of the resource is located in three massive sulphide lenses (Upper, Middle and Lower) that are entirely within the Rusty Ridge Formation above the Lewis exhalite. The mineralization in all three ore lenses consists of massive pyrrhotite + chalcopyrite + magnetite. Semi-massive sphalerite is restricted to the upper and lower parts of the Middle lens. Massive magnetite occurs at the center of the Upper and Middle lenses, where it replaces massive pyrrhotite. A striking feature of West Ansil is the presence of abundant colloform and nodular pyrite (+marcasite) in the massive sulphides. Late-stage replacement of massive pyrrhotite by colloform pyrite and marcasite, occurs mostly along the upper and lower contacts of the lenses.

An acid rock drainage (ARD) stream emanating from the Zn-Pb XY-deposit in the Yukon Territory was examined in order to evaluate the physico-chemical and geochemical processes governing the distribution of dissolved elements from the creek. The creek showed very high concentrations of metals (300 mg/L Fe, 500 mg/L Zn, 15 000 µg/L Ni, 1300 µg/L Cu and 4500 µg/L Cd), low water temperatures (1 – 12°C) and was acidic to moderately acidic (pH 3.1 – 5.0). It was found that this stream experienced a strong seasonal evolution, with increased sulphate and metal concentrations and decreased pH over the course of the summer. The mineral precipitates that formed under low pH conditions were a mixture of schwertmannite, goethite, jarosite and barite, while those that formed under moderately acidic conditions were a mixture of jurbanite, hydrobasaluminite, gibbsite and an X-ray amorphous Al-sulphate phase. Most of the mineral precipitates were of inorganic origin, although microbes may have played a role in mineral formation and trace metal sequestration in some of the precipitates. All of the mineral precipitates contained anomalous concentrations of trace elements (up to 1.5 % wt Zn) and showed a seasonal evolution in their mineralogy, both of which were determined to be a function of the pH and prevailing geochemical conditions. The geochemistry of the ARD creek draining the XY-deposit was compared to another ARD creek in the area that was likely draining shales. The two creeks were compared in order to determine if ARD geochemical characteristics can be used as a tool for the mineral exploration industry.

The West Ansil deposit was the first Cu discovery in 25 years in the Noranda Central Camp. It has a combined indicated and inferred resource of ~1.2 Mt. Grades for the indicated resource are 3.4% Cu, 0.4% Zn, 1.4 g/t Au and 9.2 g/t Ag. The bulk of the resource is located in three massive sulphide lenses (Upper, Middle and Lower) that are entirely within the Rusty Ridge Formation above the Lewis exhalite. The mineralization in all three ore lenses consists of massive pyrrhotite + chalcopyrite + magnetite. Semi-massive sphalerite is restricted to the upper and lower parts of the Middle lens. Massive magnetite occurs at the center of the Upper and Middle lenses, where it replaces massive pyrrhotite. A striking feature of West Ansil is the presence of abundant colloform and nodular pyrite (+marcasite) in the massive sulphides. Late-stage replacement of massive pyrrhotite by colloform pyrite and marcasite, occurs mostly along the upper and lower contacts of the lenses.

This report describes the successful application of a combinatorial chemistry approach to the evaluation of the amorphous transparent oxide semiconductor Al-In-Zn-O, a-AIZO, for use as channel layers in thin film transistors, TFTs. Many technologies, such as computing and electronic displays, rely on the use of the transistor. In particular, for flat panel displays, the development of new TFTs for the control electronics are necessary for thinner displays with better resolution. In addition, transparent materials deposited at low temperatures would enable a new range of applications. To accomplish this, new materials for the TFT channel layer are needed. Transparent oxide semiconductors (TOS) are one alternative the silicon based materials currently in use and the first TOS, amorphous In-Ga-Zn-O, has just gone into production. However, despite its good properties, it suffers from the disadvantage of containing the scarce and expensive metals In and Ga. Several attempts have been made to replace Ga with Al but no systematic study of a-AIZO has been reported. This report describes such a study, using a method known as combinatorial chemistry. Initially, a-AIZO thin films with composition gradients were deposited by DC/RF magnetron sputtering and, following characterization, TFTs with a variety of a-AIZO channel layer composition were manufactured and investigated. Two different compositional areas were found to yield TFTs with good characteristics.

The deformation mechanism of an ultrafine grained (UFG) Al-Zn alloy has been studied. In this work, Al-15wt%Zn alloy was processed by equal channel angular extrusion (ECAE) route A at 100oC to achieve UFG structure. The deformation mechanism was studied by performing tensile test with various strain rates. Scanning electron microscopy and transmission electron microscopy were used to investigate the microstructure evolution in Al-15wt%Zn alloy with increasing ECAE passes. The observation indicated that the super saturated Al-Zn alloy would decompose and precipitate Zn particles during ECAE process. Increasing ECAE passes, the aluminum grain size was reduced, but the size of Zn particles was increased. However, the net effect of increasing ECAE passes is softening of this Al-Zn alloy. The tensile properties of the UFG Al-Zn alloy can be summarized as follows. (1)The UFG Al-Zn alloy possesses higher tensile strength and elongation as compared to commercial purity Al (AA1050). (2)The strain rate sensitivity of the UFG Al-Zn alloy increases significantly with increasing number of ECAE pass, which might be related to the refined aluminum grain size. After processed by 4-16 ECAE passes, the activation volume of the UFG Al-Zn alloy falls in the range of 25 b3~40 b3, which remains nearly constant value with increasing tensile strain. It is suggested that the controlling mechanism responsible for the tensile deformation of the UFG Al-Zn alloy might be related to a grain boundary mediated mechanism. (3)With increasing ECAE passes, the total tensile elongation of the UFG Al-Zn alloy increases but the uniform elongation show little change. This indicates that the increase in total elongation is mainly due to the contribution from an enhanced post-uniform elongation (PUE). It is suggested that the enhanced PUE might be related to the increase in strain rate sensitivity, which is resulted from the refinement of grain size. More detailed studies are needed to understand the deformation mechanism.