Submitted by Automa??o e Estat?stica (sst@bczm.ufrn.br) on 2016-05-30T23:14:12Z No. of bitstreams: 1 RomuloAlvesDeOliveira_TESE.pdf: 1869244 bytes, checksum: af0453c8083aee85607b79c3a17c1d4c (MD5) / Approved for entry into archive by Arlan Eloi Leite Silva (eloihistoriador@yahoo.com.br) on 2016-06-01T22:30:48Z (GMT) No. of bitstreams: 1 RomuloAlvesDeOliveira_TESE.pdf: 1869244 bytes, checksum: af0453c8083aee85607b79c3a17c1d4c (MD5) / Made available in DSpace on 2016-06-01T22:30:48Z (GMT). No. of bitstreams: 1 RomuloAlvesDeOliveira_TESE.pdf: 1869244 bytes, checksum: af0453c8083aee85607b79c3a17c1d4c (MD5) Previous issue date: 2015-01-27 / Atualmente os projetos de Ilumina??o P?blica (IP), ou seja, ruas, avenidas, pra?as, estacionamentos e similares s?o realizados com a utiliza??o de softwares comerciais ou livres, em geral, fornecidos por fabricantes ou grupos de fabricantes de produtos de ilumina??o, aplicando o M?todo Ponto a Ponto para o c?lculo dos n?veis de ilumina??o. Outros pontos em comum s?o: a falta de preocupa??o na redu??o dos custos dos projetos e a dificuldade em modificar as estruturas utilizadas, tais como: localiza??o e altura dos postes e lumin?rias, ?ngulo de inclina??o das lumin?rias, quantidade de lumin?rias por poste, entre outros. Qualquer altera??o nas estruturas ter? que ser feita manualmente, geralmente em um ambiente CAD, para depois obter os novos resultados e comparar com os anteriores. Para auxiliar nessa tarefa, ? proposta aqui a utiliza??o da Metaheur?stica Col?nia de Formigas, onde os par?metros e localiza??o das estruturas passam a ser definidos automaticamente, de forma a atender os n?veis de ilumina??o estabelecidos nas normas t?cnicas, al?m de otimizar o custo de material por unidade de ?rea. / The development of public lighting projects in Brazil must meet the standards established in Brazilian standards. Many of these projects is developed through the use of knowledge about "practical rules" practiced by the designers of this area. In some cases are also used computational tools offered, generally, by leading manufacturers of lamps/luminaires. These tools have served only as calculation tools, with some limitations, such as: are not able to verify compliance or not the parameters established by Brazilian standards, most of the luminaires offered in your database are not sold in Brazil, not have no concern about the analysis of the implementation costs of elaborate designs and, finally, present an enormous difficulty in performing tests on a large volume of possible projects. It is the goal of this thesis to develop a methodology and a computational tool for the development of public lighting projects based on genetic algorithm techniques that not only perform the calculations of these projects, but can also test several possible projects using in your database the luminaires marketed in Brazil, providing the user, as a solution, a set of projects that meet the Brazilian standards and classified according the implementation costs of each project. To adjust the proposed algorithm the following performance parameters were modified: number of individuals in the initial population; probability of achievement of the cross-over; probability of achievement of the mutation. A comparison of this method with the projects developed with the use of "practical rules" is performed for various types of existing roads. The results obtained using the proposed methodology and the developed computational tool show that the methodology, including the adjustments in performance parameters, is able to meet the objectives of the work.

Submitted by Automa??o e Estat?stica (sst@bczm.ufrn.br) on 2016-06-10T19:03:35Z No. of bitstreams: 1 BrunoFerreiraAmorim_TESE.pdf: 4546675 bytes, checksum: f3babdd1005205365d367583411ae46c (MD5) / Approved for entry into archive by Arlan Eloi Leite Silva (eloihistoriador@yahoo.com.br) on 2016-06-13T20:09:02Z (GMT) No. of bitstreams: 1 BrunoFerreiraAmorim_TESE.pdf: 4546675 bytes, checksum: f3babdd1005205365d367583411ae46c (MD5) / Made available in DSpace on 2016-06-13T20:09:02Z (GMT). No. of bitstreams: 1 BrunoFerreiraAmorim_TESE.pdf: 4546675 bytes, checksum: f3babdd1005205365d367583411ae46c (MD5) Previous issue date: 2015-12-07 / Coordena??o de Aperfei?oamento de Pessoal de N?vel Superior (CAPES) / Conselho Nacional de Desenvolvimento Cient?fico e Tecnol?gico (CNPq) / As ferritas de cobalto-mangan?s (Co1?xMnxFe2O4 e Co1,2Fe1,8?xMnxO4) possuem uma estrutura do tipo espin?lio mista, e t?m sido consideradas como um das candidatas competitivas para grande variedade de aplica??es em dispositivos, desde a gera??o e detec??o de ultra-som, sensores, transformadores, bem como na ind?stria m?dica. Ferritas de cobaltomangan?s nanoestruturadas foram produzidas via moagem de alta energia, com subsequente tratamento t?rmico, e foram caracterizados por difra??o de raios X, fluoresc?ncia de raios X, microscopia eletr?nica de varredura e magnetiza??o. Amostras do tipo Co1?xMnxFe2O4 e Co1,2Fe1,8?xMnxO4 foram obtidas a partir dos p?s precursores Fe3O4, Co3O4 e Mn3O4, os quais foram estequiometricamente misturados e mo?dos por 10h e tratados termicamente ? 900?C por 2h. A difratometria confirma a forma??o das fases nanocristalinas puras para s?rie Co1,2Fe1,8?xMnxO4 com umdi?metro m?dio de cerca de 94nm. Verificou-se que o par?metro de rede aumenta com a substitui??o do Fe3? pelo Mn3?. A fluoresc?ncia de raios X revelou que as por??es de metais nas amostras estavam pr?xima das composi??es estequiom?tricas nominais. As caracter?sticas microestruturais observadas nas micrografias demonstraram que as part?culas formadas apresentam morfologia e granulometria bastante distintas. As medidas de histerese magn?ticas realizadas em baixa temperatura, mostraram que a magnetiza??o de satura??o e reman?ncia aumentaram com a concentra??o de mangan?s, enquanto que o campo coercivo diminuiu. A constante de anisotropia (Ke f ), foi calculada a partir dos ajustes dos dados pela lei de aproxima??o de satura??o. Verificou-se que a anisotropia diminui substancialmente com a substitui??o do ferro pelomangan?s. / The cobalt-manganese ferrites (Co1?xMnxFe2O4 and Co1,2Fe1,8?xMnxO4) has a mixed structure of spinel type and it has been regarded as one of candidates for petitive wide variety of applications in devices from ultrasonic generation and detection, sensors, transformers, as well as in medical industry. Ferrites cobalt-manganese nanostructured were produced via mechanical alloying with subsequent heat treatment and were characterized by X-ray diffraction, X-ray fluorescence, scanning electron microscopy and magnetization. Samples of Co1?xMnxFe2O4 and Co1,2Fe1,8?xMnxO4 were obtained from the precursor powders Fe3O4, Co3O4 and Mn3O4 which were stoichiometrically mixed and ground by 10h and heat treated at 900?C for 2h. The diffraction confirmed the formation of the pure nanocrystalline phases to series Co1,2Fe1,8?xMnxO4 with an average diameter of about 94nm. It was found that the lattice parameter increases with the substitution of Fe3? by Mn3?. The x-ray fluorescence revealed that the portions of metals in samples were close to the nominal stoichiometric compositions. The microstructural features observed in micrographs showed that the particles formed show very different morphology and particle size. The magnetic hysteresis measurements performed at low temperature showed that the saturation magnetization and remanence increased as the concentration of manganese, while the coercive field decreased. The anisotropy constant (Ke f ), was estimated from the data adjustments the law of approaching saturation. It was found that the anisotropy decreases substantially with the substitution of Fe by Mn.

Submitted by Automa??o e Estat?stica (sst@bczm.ufrn.br) on 2016-07-11T18:12:28Z No. of bitstreams: 1 VirginiaCavalcantiSantos_DISSERT.pdf: 19571261 bytes, checksum: d85bb1e84f493d266a87d1c8c5f7242f (MD5) / Approved for entry into archive by Arlan Eloi Leite Silva (eloihistoriador@yahoo.com.br) on 2016-07-19T21:15:42Z (GMT) No. of bitstreams: 1 VirginiaCavalcantiSantos_DISSERT.pdf: 19571261 bytes, checksum: d85bb1e84f493d266a87d1c8c5f7242f (MD5) / Made available in DSpace on 2016-07-19T21:15:42Z (GMT). No. of bitstreams: 1 VirginiaCavalcantiSantos_DISSERT.pdf: 19571261 bytes, checksum: d85bb1e84f493d266a87d1c8c5f7242f (MD5) Previous issue date: 2015-12-16 / Esta disserta??o sugere ambientes sonoros a partir da proposta de imagens configuradas segundo a descri??o do texto ?A Visagem da Mo?a Caetana? de Ariano Suassuna, a fim de gerar possibilidades sonoras individuais que auxiliem os instrumentistas na interpreta??o da pe?a. O ciclo composto em 1996 - para canto, viola, violoncelo e clarone/clarineta - ? constitu?do por tr?s can??es sem t?tulo. Seu texto foi extra?do do ?Folheto XLIV?, do Romance d?A Pedra do Reino e o pr?ncipe do sangue do vai-e-volta, e descreve uma senten?a de morte ilustrada por s?mbolos do imagin?rio Armorial, usando neologismos e fon?tica peculiar do Sert?o nordestino. Al?m da an?lise das dificuldades t?cnicas de execu??o, este trabalho informa os int?rpretes quanto a timbres e texturas sonoras utilizadas por Nelson Almeida para retratar o tradicional atrav?s da linguagem musical contempor?nea. As met?foras e as transgress?es do racional no texto de Suassuna foram exploradas para esbo?ar tr?s composi??es de imagens que conduzam os int?rpretes ? descri??o sonora dos objetos inanimados e dos afetos a que se refere a poesia, extrapolando as indica??es t?cnico-interpretativas limitadas pela nota??o musical. A pesquisa se valeu da pr?pria partitura, da literatura existente sobre o tema, de discuss?es com os instrumentistas que j? executaram a obra, de entrevistas com o compositor e de depoimentos de outros compositores inseridos nesse contexto. Para ilustrar a teoria, as tr?s imagens gravadas em xilogravura s?o disponibilizadas como na literatura de cordel. / This study suggests sonorous ambiences from the propose of images configured according to the description in ?A Visagem da Mo?a Caetana? by Ariano Suassuna in order to create individual sonorous possibilities that may help musicians to play the piece. The cycle, composed in 1996 (for voice, viola, cello, bass clarinet/clarinet), is formed by three untitled songs. Its text is an excerpt from the ?Folheto XLIV?, from the Romance d?A Pedra do Reino e o pr?ncipe do sangue do vai-e-volta, and describes a sentence of death illustrated by symbols of the Armorial imagery, with neologisms and the peculiar accent from the Sert?o in northeast Brazil. In addition to the analysis of technical difficulties to play, this study informs interpreters of the sonorous timbre and texture used by Nelson Almeida to describe tradition through contemporary musical language. The metaphors and transgressions of reason in Suassuna?s book were explored to create three image compositions so that they may lead interpreters to the sonorous description of the inanimate objects and the affections to which the poetry refers, expanding any technical-interpretative indications limited by musical notation. This research used the Visagem scores, the literature on the theme, discussions with the musicians that played the piece, interviews with Almeida, and composers? reports. To illustrate the theory, the three images are available, printed as woodcut in cordel literature.

Submitted by Automa??o e Estat?stica (sst@bczm.ufrn.br) on 2016-07-25T19:35:27Z No. of bitstreams: 1 AlanPereiraDaCosta_DISSERT.pdf: 24726684 bytes, checksum: 6b4523ea74314d3a8b4944c8fbeef8ad (MD5) / Approved for entry into archive by Arlan Eloi Leite Silva (eloihistoriador@yahoo.com.br) on 2016-07-28T21:11:34Z (GMT) No. of bitstreams: 1 AlanPereiraDaCosta_DISSERT.pdf: 24726684 bytes, checksum: 6b4523ea74314d3a8b4944c8fbeef8ad (MD5) / Made available in DSpace on 2016-07-28T21:11:35Z (GMT). No. of bitstreams: 1 AlanPereiraDaCosta_DISSERT.pdf: 24726684 bytes, checksum: 6b4523ea74314d3a8b4944c8fbeef8ad (MD5) Previous issue date: 2015-04-23 / A atividade plut?nica ediacarana, relacionada a orog?nese Brasiliana/Pan-Africana, constitui uma das mais importantes fei??es geol?gicas na Prov?ncia Borborema, representada em sua extens?o por in?meros bat?litos, stocks e diques. O Pl?ton Gran?tico Serra da Rajada (PGSR), principal objeto desse estudo, situado na por??o central do Dom?nio Rio Piranhas-Serid? representa um exemplo dessa atividade, sendo objeto de estudos cartogr?fico, petrogr?fico, litogeoqu?mico e geocronol?gico. Suas rochas s?o individualizadas em duas f?cies, sendo a f?cies gran?tica descrita como monzogranitos constitu?dos por K-feldspato, plagiocl?sio (oligocl?sico-An23-24%), quartzo e biotita (m?fico principal), tendo como minerais acess?rios opacos, titanita, allanita, apatita e zirc?o. Clorita, mica branca e carbonato s?o minerais de altera??o. A f?cies dior?tica compreende rochas formadas por quartzo diorito contendo plagiocl?sio (fase mineral dominante), quartzo e K-feldspato. Biotita e anfib?lio s?o os minerais m?ficos dominantes, e titanita, minerais opacos, allanita, zirc?o e apatita s?o os acess?rios. Contudo, os trabalhos de cartografia geol?gica tamb?m identificaram na regi?o a presen?a de outras unidades litoestratigr?ficas, descritas como gnaisses e migmatitos indiferenciados com lentes de anfibolitos relacionados ao Complexo Caic? (Paleoproterozoica) e rochas metassedimentares do Grupo Serid? (Neoproterozoico) compostos por paragnaisses com lentes de calciossilic?ticas, muscovita quartzitos e biotita xistos (respectivamente forma??es Jucurutu, Equador e Serid?), os quais s?o as encaixantes para as rochas do PGSR. Ainda foram identificados diques de leucomicrogranito e de pegmatitos, ambos relacionados ao final do magmatismo Ediacarano, bem como dep?sitos col?vio-eluviais e aluvionares relacionados ao Ne?geno e Quatern?rio, respectivamente. Dados litogeoqu?micos, na f?cies gran?tica do PGSR, evidenciam rochas bastante evolu?das (SiO2 69% a 75%), rica em ?lcalis (Na2O+K2O ? 8,0%), empobrecidas em MgO (? 0,45%), CaO (? 1,42%) e TiO2 (? 0,36%) e teores moderados de Fe2O3t (2,16 a 3,53%). Apresentam natureza transicional entre metaluminosa e peraluminosa (predom?nio do ?ltimo) e possuem afinidade subalcalina/monzon?tica (c?lcio-alcalina de alto K). Diagramas de Harker mostram correla??es negativas em Fe2O3t, MgO e CaO, indicando fracionamento de m?ficos e plagiocl?sio. O espectro de ETR mostra enriquecimento dos ETR leves com rela??o aos ETR pesados (LaN/YbN = 23,70 a 0,23), com anomalia negativa no Eu (Eu/Eu* = 0,70 a 0,23), sugerindo fracionamento ou acumula??o na fonte de feldspatos (plagiocl?sio). A integra??o dos dados permite correlacionar ?s rochas do PGSR ?quelas referidas na literatura como Su?te C?lcio-Alcalina de Alto K Equigranular. Considera??es sobre as condi??es de cristaliza??o para as rochas do PGSR foram obtidas a partir da integra??o de dados petrogr?ficos e litogeoqu?micos, os quais indicaram atua??o de condi??es moderadas a elevadas de ?O2 (parag?nese mineral titanita + magnetita + quartzo), magma progenitor saturado em H2O (cristaliza??o precoce das biotitas), atua??o de processos tardi-magm?ticos de fluidos ricos em ?CO2, H2O e O2 causando altera??es em parte da assembleia mineral (carbonata??o e saussuritiza??o dos plagiocl?sio, cloritiza??o das biotitas e esfenitiza??o dos opacos). Condi??es de termobarom?tricas foram estimadas com base em par?metros geoqu?micos (Zr e P2O5), bem como por minerais normativos CIPW, com resultados mostrando temperatura m?nima de liquidus da ordem de 800?C e temperatura de solidus da ordem de 700?C. As press?es final/m?nima de cristaliza??o sugerem ser da ordem de 3 a 5 Kbar. A presen?a de minerais zonados (plagiocl?sio e allanita) associadas a dados litogeoqu?micos diagramas bi-log para Rb vs Ba e Rb vs Sr sugerem a atua??o da cristaliza??o fracionada como processo dominante na evolu??o magm?tica do PGSR. Estudos geocronol?gicos U-Pb e isot?picos Sm-Nd indicam, respectivamente, que o biotita monzogranito possui idade de cristaliza??o de 557?13 Ma, com idade modelo TDM de 2,36 Ga, tendo valor de eNd para a idade de cristaliza??o de -20,10, permitindo inferir fonte crustal paleoproterozoica para o magma. / The ediacaran plutonic activity related to the Brasilian/Pan-African orogeny is one of the most important geological features in the Borborema Province, represented along its extension by numerous batholiths, stocks, and dikes.The object of this study, the Serra Rajada Granitic Pluton (SRGP), located in the central portion of the Piranhas-Serid? River Domain is an example of this activity. This pluton has been the subject of cartographic, petrographic, geochronological and lithogeochemical studies and its rocks were characterized by two facies. First, the granitic facies were described as monzogranites consisting of K-feldspar, plagioclase (oligoclase - An23-24%), quartz and biotite (main mafic) and opaque minerals such as titanite, allanite, apatite, and zircon as accessories. Alteration minerals are chlorite, white mica and carbonate. Second, the dioritic facies consist of rocks formed by quartz diorite containing plagioclase (dominant mineral phase), quartz and K-feldspar. Biotite and amphibole are the dominant mafic minerals; and titanite, opaque minerals, allanite, zircon and apatite are the accessories. However, previous geological mapping work in the region also identified the presence of other lithostratigraphic units. These were described as gneisses and migmatites with undifferentiated amphibolite lenses related to the Caic? Complex (Paleoproterozoic) and metasedimentary rocks of the Serid? Group (Neoproterozoic) composed of paragneiss with calc-silicate lenses, muscovite quartzite and biotite schist (respectively, the Jucurutu formations, Equador and Serid?), the host rocks for the SRGP rocks. Leucomicrogranite and pegmatite dikes have also been identified, both related to the end of the Ediacaran magmatism and colluvial- eluvial and alluvial deposits related to Neogene and Quaternary, respectively. Lithogeochemical data on the SRGP granite facies, highlighted quite evolved rocks (SiO2 69% to 75%), rich in alkalis (Na2O+K2O ? 8.0%), depleted of MgO (? 0.45%), CaO (? 1.42%) and TiO2 (? 0.36%) and moderate levels of Fe2O3t (2.16 to 3.53%). They display transitional nature between metaluminous and peraluminous (predominance of the latter) with sub-alkaline/monzonitic (High K calcium-alkali) affinity. Harker diagrams show negative correlations for Fe2O3t, MgO, and CaO, indicating mafic and plagioclase fractionation. REE spectrum shows enrichment of LREE relative to heavy REE (LaN/YbN = 23.70 to 10.13), with negative anomaly in the Eu (Eu/Eu* = 0.70 to 0.23), suggesting fractionation or accumulation in the feldspars source (plagioclase). Data integration allows to correlate the SRGP rocks with those described as Calcium-Alkaline Suite of equigranular High K. The crystallization conditions of the SRGP rocks were determined from the integration of petrographic and lithogeochemical data. These data indicated intermediate to high conditions of ?O2 (mineral paragenesis titanite + magnetite + quartz), parent magma saturated in H2O (early biotite crystallization), tardi-magmatic processes of fluids rich in ?CO2, H2O and O2 causing part of the mineral assembly to change (plagioclase carbonation and saussuritization, biotite chloritization and opaques Sphenitization). Thermobarometrical conditions were estimated based on geochemical parameters (Zr and P2O5) and CIPW normative minerals, with results showing the liquidus minimum temperature of about800?C and the solidus temperature of approximately 700?C. The final/minimum crystallization pressure are suggested to be between 3 and 5 Kbar. The presence of zoned minerals (plagioclase and allanite) associated with lithogeochemical data in bi-log diagrams for Rb vs. Ba and Rb vs. Sr suggest the role of fractional crystallization as the dominant process in the magmatic evolution of SRGP. U-Pb Geochronological and Sm-Nd isotope studies indicated, respectively, the crystallization age of biotite monzogranite as 557 ? 13 Ma, with TDM model age of 2.36 Ga, and ?Nd value of -20.10 to the crystallization age, allowing to infer paleoproterozoic crustal source for the magma.

Submitted by Automa??o e Estat?stica (sst@bczm.ufrn.br) on 2016-07-25T19:35:25Z No. of bitstreams: 1 RogerioCavalcante_DISSERT.pdf: 19303384 bytes, checksum: fa3e7192e96e5cd761bc77b41b6e499e (MD5) / Approved for entry into archive by Arlan Eloi Leite Silva (eloihistoriador@yahoo.com.br) on 2016-08-01T19:20:01Z (GMT) No. of bitstreams: 1 RogerioCavalcante_DISSERT.pdf: 19303384 bytes, checksum: fa3e7192e96e5cd761bc77b41b6e499e (MD5) / Made available in DSpace on 2016-08-01T19:20:01Z (GMT). No. of bitstreams: 1 RogerioCavalcante_DISSERT.pdf: 19303384 bytes, checksum: fa3e7192e96e5cd761bc77b41b6e499e (MD5) Previous issue date: 2015-01-30 / A presente disserta??o procurou avan?ar no conhecimento geol?gico das rochas do Pl?ton Gran?tico Barcelona (PGB), corpo esse que est? localizado na regi?o que abrange o Dom?nio Rio Grande do Norte (DRN) na sua por??o leste, no denominado Subdom?nio S?o Jos? do Campestre (SJC) (Prov?ncia Borborema, NE do Brasil). O objetivo principal foi compreender a evolu??o geol?gica das rochas desse pl?ton, do ambiente de gera??o do magma at? o ambiente em que o mesmo foi alojado. O Pl?ton Gran?tico Barcelona (PGB) localiza-se na por??o oeste do Subdom?nio S?o Jos? do Campestre, por??o leste do Dom?nio Rio Grande do Norte na Prov?ncia Borborema, possui ?rea aflorante de aproximadamente 260 km2, com idade Ediacarana presumida. O PGB ? formado por tr?s f?cies petrogr?ficas/texturais distintas: (a) granito porfir?tico (biotita monzogranitos) dominante; (b) os diques e sheets de microgranitos (biotita granodioritos); e (c) rochas de composi??o m?fica a intermedi?ria (dior?ticas a quartzo-dior?ticas) que ocorrem essencialmente como enclaves. A f?cies granito porfir?tico possui plagiocl?sio (oligocl?sio com An25-20%), K-feldspato (microclina pert?tica) e quartzo compondo sempre mais de 70% modal. Biotita e anfib?lio s?o os minerais m?ficos dominantes, ep?doto, titanita, allanita, opacos, zirc?o e apatita, os acess?rios. As rochas do PGB possuem as seguintes estruturas: (i) uma trama magm?tica (Smag) dominante com dire??o NE-SW e NW-SE, acompanhado por uma linea??o magm?tica (Lmag) mergulhando suavemente para NE-SW e NW-SE, principalmente. Na por??o sul do PGB, destaca-se padr?o conc?ntrico desta folia??o com caimento m?dio a alto, e (ii) a folia??o de estado s?lido (S3+) possui aspecto milonitizado, localizada principalmente na borda leste do corpo gran?tico, com dire??o NE-SW e caimento suave a moderado para W. A sugest?o do modelo de alojamento das rochas do PGB foi baseada na combina??o do estudo das medidas estruturais de afloramentos e em dados gravim?tricos. O alojamento desse corpo gran?tico ? controlado por sistemas de zonas de cisalhamento transcorrentes, denominadas de ZCLP (Zona de Cisalhamento Lajes Pintadas) e ZCSN (Zona de Cisalhamento S?tio Novo) ambas de cinem?tica dextr?gira e deforma??o em regime transcorrente com a segunda estando relacionada a ascen??o do mesmo. A qu?mica mineral mostra que os anfib?lios da f?cies porfir?tico ? a hastingsita com moderadas raz?es Mg/(Mg+Fe), indicando forma??o em ambiente com moderada a elevada ?O2 e press?es de cristaliza??o da ordem de 5,0-6,0kbar. As biotitas possuem composi??o com leve tend?ncia para o p?lo da annita (Fe), mostram um trend que partem do campo das biotitas prim?rias para o das biotitas prim?rias reequilibradas. Em diagramas discriminantes de s?ries magm?ticas as biotitas se comportam como ?quelas de afinidade subalcalina, coerentes com a afinidade geoqu?mica c?lcio-alcalina pot?ssica/subalcalina da rocha hospedeira (granitos porfir?ticos). Os minerais opacos s?o essencialmente magnetitas, com alguns cristais martitizados para hematita, indicando condi??es relativamente oxidantes durante a evolu??o do magma que originou o PGB. Zona??o em cristais de plagiocl?sio, K-feldspato e allanita, s?o indicativos que o processo de cristaliza??o fracionada. A litogeoqu?mica mostra que as f?cies granito porfir?tico e microgranito plotam na maioria dos diagramas de campo e trend como rochas com afinidades transicionais entre subalcalina e c?lcio-alcalina de alto K, e quanto ao ?ndice de satura??o em alum?nio est?o entre os campos meta a peraluminoso. Os dados de litogeoqu?mica sugerem que as f?cies do PGB estudados tenham uma fonte magm?tica similar, mas com hist?rias evolutivas diferentes (co-magm?ticos). / The Dissertation aimed to advance the geological knowledge of the Barcelona Granitic Pluton (BGP). This body is located in the eastern portion of the Rio Grande do Norte Domain (RND), within the S?o Jos? do Campestre subdomain (SJC), NE of the Borborema Province. The main goal was to understand the geological evolution of the rocks of the pluton and the tectonic setting of magma generation and its emplacement. The BGP has an assumed Ediacaran age and outcropping area of approximately 260 km2, being composed of three varied petrographic/textural facies: (a) porphyritic biotite monzogranite; (b) dykes and sheets of biotite microgranite; (c) dioritic to quartz-dioritic enclaves. The rocks of the BGP have the following structures: (i) a NE-SW and NW-SE directed magmatic fabric (S?), accompanied by a magmatic lineation (L?) with gentle dip to NE-SW and NW-SE. In the southern portion, there is the concentric pattern of this foliation with medium to high dip, and (ii) a solid state foliation, in part mylonitic (S3+), mainly on the eastern edge with slightly plunging to west. The integration of structural and gravity data permitted to interpret the emplacement of the BGP as controlled by the transcurrent shear zones systems Lajes Pintadas (LPSZ) and S?tio Novo (SNSZ), both of dextral strike-slip kinematics. Mineral chemistry data show that the amphibole form the porphyritic biotite monzogranite facies is hastingsite with moderate Mg / (Mg + Fe) ratios, indicating crystallization under moderate to high ?O2 and cristallization pressure of around 5.0-6.0 kbar. The biotite tends to be slightly richer in annite molecule and plots in the transitional field from primary biotite to reequilibrated biotite. In discriminant diagrams of magmatic series, the biotite behave like those of subalkaline affinity, consistent with the potassium calc-alkaline / sub-alkaline geochemical affinity of the hosting rock. The opaque minerals are primarily magnetite, with some crystals martitized to hematite indicating relatively oxidizing conditions during magma evolution that originated the BGP. Zoning in plagioclase, K-feldspar and allanite crystals suggest fractional crystallization process. Lithogeochemical data suggest that the facies described for the BGP have similar magma source, usually plotting in the fields and trends of the subalkaline / high potassium calc-alkaline series.

Submitted by Automa??o e Estat?stica (sst@bczm.ufrn.br) on 2016-07-26T00:34:29Z No. of bitstreams: 1 LaraDeFigueiredoEufrauzino_DISSERT.pdf: 30308301 bytes, checksum: bf514e9dbc21b91c7bbf4d101b49d4ab (MD5) / Approved for entry into archive by Arlan Eloi Leite Silva (eloihistoriador@yahoo.com.br) on 2016-08-08T20:15:54Z (GMT) No. of bitstreams: 1 LaraDeFigueiredoEufrauzino_DISSERT.pdf: 30308301 bytes, checksum: bf514e9dbc21b91c7bbf4d101b49d4ab (MD5) / Made available in DSpace on 2016-08-08T20:15:54Z (GMT). No. of bitstreams: 1 LaraDeFigueiredoEufrauzino_DISSERT.pdf: 30308301 bytes, checksum: bf514e9dbc21b91c7bbf4d101b49d4ab (MD5) Previous issue date: 2015-09-18 / Coordena??o de Aperfei?oamento de Pessoal de N?vel Superior (CAPES) / Este trabalho se prop?e a compreender o processo e as pr?ticas das estrat?gias de marketing pol?tico aplicadas ?s m?dias sociais facebook e twitter de um candidato a governador da Para?ba nas elei??es de 2014. Visando atingir o prop?sito desta pesquisa, foi realizado um estudo de caso tendo como objeto de an?lise a campanha online do candidato a governador da Para?ba, C?ssio Cunha Lima - PSDB, em 2014. O estudo de caso se deu a partir da constru??o de um perfil biogr?fico e pol?tico do candidato. Esta pesquisa tamb?m fez uso da etnografia virtual. Para tanto, foram monitoradas as m?dias sociais facebook e twitter desse pol?tico, com o aux?lio do programa de captura de imagens - Greenshot, atrav?s da cria??o de categorias de an?lise pr?-definidas, como, por exemplo, agenda, prest?gio e apoio, campanha negativa, engajamento, entre outras. O per?odo escolhido para o monitoramento dos perfis oficiais de C?ssio Cunha Lima foi entre os dias 24 de agosto e 28 de outubro de 2014, pois comporta o per?odo pr?, durante e p?s-elei??o onde observou-se maior n?vel de movimenta??o do candidato e de sua equipe de marketing nas m?dias sociais selecionadas para an?lise. / This dissertation aims to analyze and understand the process and practices of political marketing strategies applied to social media facebook and twitter C?ssio Cunha Lima - PSDB candidate for governor of Para?ba, in the 2014 elections The work is divided into three parts . The first two chapters, both of theoretical nature, underlie the discussion about the use of the Internet as a campaign space and political marketing campaign as well as the different communication strategies and electoral marketing already presented in the literature. Following, is dedicated to a topic for the presentation of the methodology and subsequently makes the discussion of empirical data analysis. Finally, we present the conclusions. The analysis takes as its starting point the models Figueiredo et al. (1998) and Albuquerque (1999) to observe the traditional strategies and suggests the inclusion of typically recorded on the Internet strategies. The methodology used for the analysis was the qualitative and quantitative content from variables that we list different campaign strategies. In order to achieve the purpose of this research, we conducted a case study as an analytical object online campaign C?ssio Cunha Lima. The case study took place from the construction of a candidate's biographical and political profile, presented and discussed in the text. This research also made use of virtual ethnography. Therefore, were monitored social media facebook and twitter that political, with the help of image capture program - Greenshot by creating pre-defined categories of analysis, for example, calendar, prestige and support, negative campaign , engagement, among others. The period chosen for monitoring the candidate's official profiles was from 24 August to 28 October 2014, because it holds the pre, during and post-election where there was greater candidate drive level and his team marketing in social media selected for analysis. The results indicate that mobilization strategy (online and offline), merged with the promotion schedule, it is predominant in the social media Cassio. They also indicate that they do not show the failure of the campaign of the candidate in 2014.

Submitted by Automa??o e Estat?stica (sst@bczm.ufrn.br) on 2016-08-09T22:51:26Z No. of bitstreams: 1 GilmaraLinharesDeAraujo_TESE.pdf: 11647948 bytes, checksum: 94a5e966f18f8dd6bfc6646d2519542b (MD5) / Approved for entry into archive by Arlan Eloi Leite Silva (eloihistoriador@yahoo.com.br) on 2016-08-10T23:44:37Z (GMT) No. of bitstreams: 1 GilmaraLinharesDeAraujo_TESE.pdf: 11647948 bytes, checksum: 94a5e966f18f8dd6bfc6646d2519542b (MD5) / Made available in DSpace on 2016-08-10T23:44:37Z (GMT). No. of bitstreams: 1 GilmaraLinharesDeAraujo_TESE.pdf: 11647948 bytes, checksum: 94a5e966f18f8dd6bfc6646d2519542b (MD5) Previous issue date: 2015-12-10 / Coordena??o de Aperfei?oamento de Pessoal de N?vel Superior (CAPES) / Esse trabalho apresenta uma t?cnica h?brida de projeto de superf?cies seletivas em frequ?ncia, sobre uma camada diel?trica isotr?pica, considerando diversas geometrias para os elementos das c?lulas unit?rias. Especificamente, a t?cnica h?brida usa o m?todo do circuito equivalente em conjunto com algoritmos gen?ticos, visando a s?ntese de estruturas com resposta singleband e dual-band. O m?todo do circuito equivalente permite modelar a estrutura por meio de um circuito equivalente e tamb?m a obten??o de circuitos para diferentes geometrias. A partir da obten??o dos par?metros desses circuitos, podem-se obter as caracter?sticas de transmiss?o e de reflex?o das estruturas modeladas. Para obter a otimiza??o das estruturas modeladas, de acordo com a resposta em frequ?ncia desejada, a ferramenta de otimiza??o do Matlab optimtool mostrou-se de f?cil utiliza??o, permitindo explorar resultados importantes na an?lise de otimiza??o. No trabalho, s?o apresentados resultados num?ricos e experimentais para as caracter?sticas de transmiss?o de diferentes geometrias analisadas. Foram efetuadas compara??es com resultados apresentados na literatura, tendo-se observado uma boaconcord?ncia nos casos analisados para estruturas com substratos isotr?picos. / This thesis presents a hybrid technique of frequency selective surfaces project (FSS) on a isotropic dielectric layer, considering various geometries for the elements of the unit cell. Specifically, the hybrid technique uses the equivalent circuit method in conjunction with genetic algorithm, aiming at the synthesis of structures with response single-band and dual-band. The equivalent circuit method allows you to model the structure by using an equivalent circuit and also obtaining circuits for different geometries. From the obtaining of the parameters of these circuits, you can get the transmission and reflection characteristics of patterned structures. For the optimization of patterned structures, according to the desired frequency response, Matlab? optimization tool named optimtool proved to be easy to use, allowing you to explore important results on the optimization analysis. In this thesis, numeric and experimental results are presented for the different characteristics of the analyzed geometries. For this, it was determined a technique to obtain the parameter N, which is based on genetic algorithms and differential geometry, to obtain the algebraic rational models that determine values of N more accurate, facilitating new projects of FSS with these geometries. The optimal results of N are grouped according to the occupancy factor of the cell and the thickness of the dielectric, for modeling of the structures by means of rational algebraic equations. Furthermore, for the proposed hybrid model was developed a fitness function for the purpose of calculating the error occurred in the definitions of FSS bandwidths with transmission features single band and dual band. This thesis deals with the construction of prototypes of FSS with frequency settings and band widths obtained with the use of this function. The FSS were initially reviewed through simulations performed with the commercial software Ansoft Designer ?, followed by simulation with the equivalent circuit method for obtaining a value of N in order to converge the resonance frequency and the bandwidth of the FSS analyzed, then the results obtained were compared. The methodology applied is validated with the construction and measurement of prototypes with different geometries of the cells of the arrays of FSS.

Submitted by Automa??o e Estat?stica (sst@bczm.ufrn.br) on 2016-08-09T23:54:33Z No. of bitstreams: 1 CamilaRodriguesCabral_TESE.pdf: 4270769 bytes, checksum: 1d87d6722008a708e5ed50603d965a96 (MD5) / Approved for entry into archive by Arlan Eloi Leite Silva (eloihistoriador@yahoo.com.br) on 2016-08-15T22:59:31Z (GMT) No. of bitstreams: 1 CamilaRodriguesCabral_TESE.pdf: 4270769 bytes, checksum: 1d87d6722008a708e5ed50603d965a96 (MD5) / Made available in DSpace on 2016-08-15T22:59:31Z (GMT). No. of bitstreams: 1 CamilaRodriguesCabral_TESE.pdf: 4270769 bytes, checksum: 1d87d6722008a708e5ed50603d965a96 (MD5) Previous issue date: 2015-12-11 / Conselho Nacional de Desenvolvimento Cient?fico e Tecnol?gico (CNPq) / Coordena??o de Aperfei?oamento de Pessoal de N?vel Superior (CAPES) / Esse estudo avalia os padr?es de diversidade alfa, diversidade beta e similaridade das comunidades zooplanct?nicas em 100 lagos rasos tropicais. No primeiro cap?tulo, n?s verificamos a riqueza zooplanct?nica entre os habitats limn?tico e litor?neo, se o resultado encontrado foi decorrente da presen?a de macr?fitas no habitat litor?neo ou de condi??es do habitat per se, e quais foram as vari?veis ambientais locais que mais influenciaram nos padr?es de riqueza. Nossas hip?teses eram de que a riqueza seria maior no habitat litor?neo, principalmente para microcrust?ceos, e que esses padr?es seriam determinados pela presen?a de macr?fitas. N?s vimos que o habitat litor?neo com macr?fitas ? detentor de maior riqueza zooplanct?nica, especialmente de esp?cies de rot?feros beneficiadas pelo espectro de recursos providos pelas macr?fitas. A riqueza de microcrust?ceos n?o foi afetada pelas macr?fitas, possivelmente devido ao tamanho reduzido desses organismos e ? baixa preda??o visual e h?bito omn?voro de peixes tropicais. Encontramos rela??o positiva entre a riqueza com a presen?a de macr?fitas e a baixa concentra??o de nitrog?nio. ? poss?vel que, devido ?s consequ?ncias da eutrofiza??o, o aumento dos nutrientes na ?gua determina: o aumento da biomassa algas e a redu??o de macr?fitas, e consequentemente, a redu??o da riqueza zooplanct?nica. J? no segundo cap?tulo,n?s observamos que o efeito combinado da heterogeneidade de habitats (habitat limn?tico ou litor?neo) e a aus?ncia direta de conectividade entre os lagos foram fundamentais no aumento da diversidade beta zooplanct?nica, e que, a complexidade estrutural (presen?a de macr?fitas) exerceu importante papel sobre a diversidade beta em escalas local e regional. A varia??o espacial, como a promovida pela compartimentaliza??o horizontal em lagos e pela presen?a de macr?fitas no habitat litor?neo, foi capaz de produzir mosaicos e gradientes capazes de permitir a coexist?ncia de diferentes esp?cies adaptadas ?s condi??es espec?ficas criadas pela variabilidade dos habitats limn?tico e litor?neo. Dentre esses habitats, o litor?neo constituiu a regi?o mais sujeita a efeitos do filtro ambiental em escala regional, apresentando maior diversidade beta e heterogeneidade ambiental, possivelmente devido ? maior complexidade espacial e temporal de fatores f?sico-qu?mico e biol?gicos. Enquanto que, no terceiro cap?tulo, n?s vimos os padr?es do zoopl?ncton de decaimento da similaridade com a dist?ncia (DDS), considerando o potencial de dispers?o dos organismos e a idade do lagos. Devido ao potencial de dispers?o, n?s esper?vamos que as taxas de DDS fossem maiores para cop?podes, clad?ceros e rot?feros, respectivamente, e que, devido ao maior tempo de exist?ncia dos lagos antigos e ao potencial de dispers?o do zoopl?ncton, as medidas de similaridade inicial fossem maiores e as taxas de DDS menores nos lagos antigos. N?s vimos que dentro de cada conjunto de lagos as taxas de DDS n?o variaram entre os organismos, evidenciando que al?m da habilidade de dispers?o per se, existem outros fatores que contribu?ram para inexist?ncia de decaimento mais r?pidos entre os grupos. As taxas de DDS foram mais evidentes nos lagos mais novos, possivelmente, o tempo tornou os lagos antigos mais complexos e heterog?neos, capazes de agir como filtro ambiental na sele??o de diferentes esp?cies. A DDS significativa do zoopl?ncton em escalas espaciais relativamente pequenas comprova que organismos pequenos podem apresentar padr?es biogeogr?ficos semelhante ao esperado para os macrorganismos. Por fim, os tr?s cap?tulos em conjunto forneceram informa??es importantes sobre os fatores que controlam a riqueza e distribui??o zooplanct?nica no espa?o e no tempo e pode auxiliar-nos na previs?o de respostas ecossist?micas, diante da eutrofiza??o cultural ou das mudan?as clim?ticas globais, e nas a??es de conserva??o e estrat?gias de conserva??o de ecossistemas lacustres.

Made available in DSpace on 2014-12-17T14:55:04Z (GMT). No. of bitstreams: 1 MarceloRBGV.pdf: 514846 bytes, checksum: f54178f2d4a2cb1b74a993d664aad1b3 (MD5) Previous issue date: 2007-12-05 / On this paper, it is made a comparative analysis among a controller fuzzy coupled to a PID neural adjusted by an AGwith several traditional control techniques, all of them applied in a system of tanks (I model of 2nd order non lineal). With the objective of making possible the techniques involved in the comparative analysis and to validate the control to be compared, simulations were accomplished of some control techniques (conventional PID adjusted by GA, Neural PID (PIDN) adjusted by GA, Fuzzy PI, two Fuzzy attached to a PID Neural adjusted by GA and Fuzzy MISO (3 inputs) attached to a PIDN adjusted by GA) to have some comparative effects with the considered controller. After doing, all the tests, some control structures were elected from all the tested techniques on the simulating stage (conventional PID adjusted by GA, Fuzzy PI, two Fuzzy attached to a PIDN adjusted by GA and Fuzzy MISO (3 inputs) attached to a PIDN adjusted by GA), to be implemented at the real system of tanks. These two kinds of operation, both the simulated and the real, were very important to achieve a solid basement in order to establish the comparisons and the possible validations show by the results / Neste trabalho ?realizado uma an?lise comparativa entre um controlador fuzzy acoplado aum PID neural ajustado por um AGcom diversas t?cnicas de controle tradicionais, todas elas aplicadas em um sistema de tanques (modelo de 2a ordem n?o linear). Com o objetivo de viabilizar as t?cnicas envolvidas nas an?lises comparativas e validar o controle a ser comparado, foram realizadas simula??es de algumas t?cnicas de controle (PID convencional ajustado por AG, PID Neural (PIDN) ajustado por AG, Fuzzy PI, Fuzzy cascata acoplado a um PIDN ajustado por AG e Fuzzy MISO (3 entradas) acoplado a um PIDN ajustado por AG) para efeitos comparativos com o controlador proposto. Depois de realizar todos os testes simulados, foram eleitas, dentre as t?cnicas testadas na fase de simula??o, algumas estruturas de controle (PID convencional ajustado por AG, Fuzzy PI, Fuzzy cascata acoplado aum PIDN ajustado por AGeFuzzy MISO (3entradas) acoplado a um PIDN ajustado por AG) para serem implementadas no sistema real de tanques. Esses dois modos de opera??o, tanto o simulado como o real, se fizeram importantes para um embasamento s?lido para fazer as compara??es e valida??es poss?veis mostradas nos resultados

Made available in DSpace on 2014-12-17T14:55:13Z (GMT). No. of bitstreams: 1 JaimeBF_capa_ate_pag_19.pdf: 7962172 bytes, checksum: 45237e67ab4c644a9513e54fd4865fb5 (MD5) Previous issue date: 2002-12-10 / The present work presents an algorithm proposal, which aims for controlling and improving idle time to be applied in oil production wells equipped with beam pump. The algorithm was totally designed based on existing papers and data acquired from two Potiguar Basin pilot wells. Oil engineering concepts such as submergence, pump off, Basic Sediments and Water (BSW), Inflow Performance Relationship (IPR), reservo ir pressure, inflow pressure, among others, were included into the algorithm through a mathematical treatment developed from a typical well and then extended to the general cases. The optimization will increase the well production potential maximum utilization having the smallest number of pumping unit cycles directly reflecting on operational cost and electricity consumption reduction / O presente trabalho apresenta proposta de um algoritmo que objetiva o controle e a otimiza??o do tempo de espera a ser aplicado em po?os de produ??o de petr?leo equipados com bombeio mec?nico. O algoritmo foi totalmente elaborado atrav?s de subs?dios da literatura existente e de dados coletados de dois po?os pilotos de campos de petr?leo da ?rea terrestre da Bacia Potiguar. Conceitos de engenharia de petr?leo tais como submerg?ncia, pancada de fluido, Basic Sediments and Water (BSW), lnflow Performance Relationship (IPR), press?o do reservat?rio, press?o em fluxo, entre outros, foram incorporados ao algoritmo por um tratamento matem?tico desenvolvido a partir de um po?o t?pico, para da? ser estendido aos casos gerais. A otimiza??o favorecer? o aproveitamento m?ximo do potencial de produ??o do po?o com o menor n?mero de ciclos da unidade de bombeio, refletindo diretamente na redu??o de custos operacionais e do consumo de energia el?trica