Experiments in Neutrino Mass and Mixing: Part I - New Limits on Heavy Neutrino Emission in Nuclear Beta Decay. Part II - Fast Neutron Backgrounds for the San Onofre Neutrino Detector

In Part I of this thesis, a new magnetic spectrometer experiment which measured the β spectrum of ^(35)S is described. New limits on heavy neutrino emission in nuclear β decay were set, for a heavy neutrino mass range between 12 and 22 keV. In particular, this measurement rejects the hypothesis that a 17 keV neutrino is emitted, with sin^2 θ = 0.0085, at the 6δ statistical level. In addition, an auxiliary experiment was performed, in which an artificial kink was induced in the β spectrum by means of an absorber foil which masked a fraction of the source area. In this measurement, the sensitivity of the magnetic spectrometer to the spectral features of heavy neutrino emission was demonstrated.

In Part II, a measurement of the neutron spallation yield and multiplicity by the Cosmic-ray Underground Background Experiment is described. The production of fast neutrons by muons was investigated at an underground depth of 20 meters water equivalent, with a 200 liter detector filled with 0.09% Gd-loaded liquid scintillator. We measured a neutron production yield of (3.4 ± 0.7) x 10^(-5) neutrons per muon-g/cm^2, in agreement with other experiments. A single-to-double neutron multiplicity ratio of 4:1 was observed. In addition, stopped π^+ decays to µ^+ and then e^+ were observed as was the associated production of pions and neutrons, by the muon spallation interaction. It was seen that practically all of the π^+ produced by muons were also accompanied by at least one neutron. These measurements serve as the basis for neutron background estimates for the San Onofre neutrino detector.

[A_Ribera_SanEsteban] Modelo virtual de la iglesia de San Esteban de Ribera de Valderejo (Álava)

[ES] Ribera es un pueblo abandonado dentro del parque natural de Valderejo, el único edificio que queda en pie es la antigua iglesia. La razón por la que este edificio no fue derribado es la presencia de un conjunto de pinturas murales de época medieval. Por lo demás, el edificio (de unos 25 x 12 metros en planta) se encontraba en un mal estado de conservación (de hecho, un par de años más tarde de la realización de este trabajo se derrumbó la sacristía).

El caso del colegio "San Martín" de Donostia

Nivel educativo: Grado. Duración (en horas): De 41 a 50 horas

Part I. A study of the velocity structure of the earth by the use of core phases. Part II. The 1971 San Fernando earthquake series focal mechanisms and tectonics

The initial objective of Part I was to determine the nature of upper mantle discontinuities, the average velocities through the mantle, and differences between mantle structure under continents and oceans by the use of P'dP', the seismic core phase P'P' (PKPPKP) that reflects at depth d in the mantle. In order to accomplish this, it was found necessary to also investigate core phases themselves and their inferences on core structure. P'dP' at both single stations and at the LASA array in Montana indicates that the following zones are candidates for discontinuities with varying degrees of confidence: 800-950 km, weak; 630-670 km, strongest; 500-600 km, strong but interpretation in doubt; 350-415 km, fair; 280-300 km, strong, varying in depth; 100-200 km, strong, varying in depth, may be the bottom of the low-velocity zone. It is estimated that a single station cannot easily discriminate between asymmetric P'P' and P'dP' for lead times of about 30 sec from the main P'P' phase, but the LASA array reduces this uncertainty range to less than 10 sec. The problems of scatter of P'P' main-phase times, mainly due to asymmetric P'P', incorrect identification of the branch, and lack of the proper velocity structure at the velocity point, are avoided and the analysis shows that one-way travel of P waves through oceanic mantle is delayed by 0.65 to 0.95 sec relative to United States mid-continental mantle.

A new P-wave velocity core model is constructed from observed times, dt/dΔ's, and relative amplitudes of P'; the observed times of SKS, SKKS, and PKiKP; and a new mantle-velocity determination by Jordan and Anderson. The new core model is smooth except for a discontinuity at the inner-core boundary determined to be at a radius of 1215 km. Short-period amplitude data do not require the inner core Q to be significantly lower than that of the outer core. Several lines of evidence show that most, if not all, of the arrivals preceding the DF branch of P' at distances shorter than 143° are due to scattering as proposed by Haddon and not due to spherically symmetric discontinuities just above the inner core as previously believed. Calculation of the travel-time distribution of scattered phases and comparison with published data show that the strongest scattering takes place at or near the core-mantle boundary close to the seismic station.

In Part II, the largest events in the San Fernando earthquake series, initiated by the main shock at 14 00 41.8 GMT on February 9, 1971, were chosen for analysis from the first three months of activity, 87 events in all. The initial rupture location coincides with the lower, northernmost edge of the main north-dipping thrust fault and the aftershock distribution. The best focal mechanism fit to the main shock P-wave first motions constrains the fault plane parameters to: strike, N 67° (± 6°) W; dip, 52° (± 3°) NE; rake, 72° (67°-95°) left lateral. Focal mechanisms of the aftershocks clearly outline a downstep of the western edge of the main thrust fault surface along a northeast-trending flexure. Faulting on this downstep is left-lateral strike-slip and dominates the strain release of the aftershock series, which indicates that the downstep limited the main event rupture on the west. The main thrust fault surface dips at about 35° to the northeast at shallow depths and probably steepens to 50° below a depth of 8 km. This steep dip at depth is a characteristic of other thrust faults in the Transverse Ranges and indicates the presence at depth of laterally-varying vertical forces that are probably due to buckling or overriding that causes some upward redirection of a dominant north-south horizontal compression. Two sets of events exhibit normal dip-slip motion with shallow hypocenters and correlate with areas of ground subsidence deduced from gravity data. Several lines of evidence indicate that a horizontal compressional stress in a north or north-northwest direction was added to the stresses in the aftershock area 12 days after the main shock. After this change, events were contained in bursts along the downstep and sequencing within the bursts provides evidence for an earthquake-triggering phenomenon that propagates with speeds of 5 to 15 km/day. Seismicity before the San Fernando series and the mapped structure of the area suggest that the downstep of the main fault surface is not a localized discontinuity but is part of a zone of weakness extending from Point Dume, near Malibu, to Palmdale on the San Andreas fault. This zone is interpreted as a decoupling boundary between crustal blocks that permits them to deform separately in the prevalent crustal-shortening mode of the Transverse Ranges region.

^(18)O/^(16)O and D/H studies on the interactions between heated meteoric ground waters and igneous intrusions: Western San Juan Mountains, Colorado and the Isle of Skye, Scotland

Detailed oxygen, hydrogen and carbon isotope studies have been carried out on igneous and metamorphic rocks of the Stony Mountain complex, Colorado, and the Isle of Skye, Scotland, in order to better understand the problems of hydrothermal meteoric water-rock interaction.

The Tertiary Stony Mountain stock (~1.3 km in diameter), is composed of an outer diorite, a main mass of biotite gabbro, and an inner diorite. The entire complex and most of the surrounding country rocks have experienced various degrees of ¹⁸O depletion (up to 10 per mil) due to interaction with heated meteoric waters. The inner diorite apparently formed from a low-¹⁸O magma with δ¹⁸O ≃ +2.5, but most of the isotopic effects are a result of exchange between H₂O and solidified igneous rocks. The low-¹⁸O inner diorite magma was probably produced by massive assimilation and/or melting of hydrothermally altered country rocks. The δ¹⁸O values of the rocks generally increase with increasing grain size, except that quartz typically has δ¹⁸O = +6 to +8, and is more resistant to hydrothermal exchange than any other mineral studied. Based on atom % oxygen, the outer diorites, gabbros, and volcanic rocks exhibit integrated water/rock ratios of 0.3 ± 0.2, 0.15 ± 0.1, and 0.2 ± 0.1, respectively. Locally, water/rock ratios attain values greater than 1.0. Hydrogen isotopic analyses of sericites, chlorites, biotites, and amphiboles range from -117 to -150. δD in biotites varies inversely with Fe/Fe+Mg, as predicted by Suzuoki and Epstein (1974), and positively with elevation, over a range of 600 m. The calculated δD of the mid-to-late-Tertiary meteoric waters is about -100. Carbonate δ¹³C values average -5.5 (PDB), within the generally accepted range for deep-seated carbon.

Almost all the rocks within 4 km of the central Tertiary intrusive complex of Skye are depleted in ¹⁸O. Whole-rock δ¹⁸O values of basalts (-7. 1 to +8.4), Mesozoic shales (-0.6 to + 12.4), and Precambrian sandstones (-6.2 to + 10.8) systematically decrease inward towards the center of the complex. The Cuillin gabbro may have formed from a ¹⁸O-depleted magma (depleted by about 2 per mil); δ¹⁸O of plagioclase (-7.1 to + 2.5) and pyroxene (-0.5 to + 3.2) decrease outward toward the margins of the pluton. The Red Hills epigranite plutons have δ¹⁸O quartz (-2.7 to + 7.6) and feldspar (-6.7 to + 6.0) that suggest about 3/4 of the exchange took place at subsolidus temperatures; profound disequilibrium quartz-feldspar fractionations (up to 12) are characteristic. The early epigranites were intruded as low-¹⁸O melts (depletions of up to 3 per mil) with δ¹⁸O of the primary, igneous quartz decreasing progressively with time. The Southern Porphyritic Epigranite was apparently intruded as a low-¹⁸O magma with δ¹⁸O ≃ -2.6. A good correlation exists between grain size and δ¹⁸O for the unique, high-¹⁸O Beinn an Dubhaich granite which intrudes limestone having a δ¹⁸O range of +0.5 to +20.8, and δ¹³C of -4.9 to -1.0. The δD values of sericites (-104 to -107), and amphiboles, chlorites, and biotites (-105 to -128) from the igneous rocks , indicate that Eocene surface waters at Skye had δD ≃ -90. The average water/rock ratio for the Skye hydrothermal system is approximately one; at least 2000 km³ of heated meteoric waters were cycled through these rocks.

Thus these detailed isotopic studies of two widely separated areas indicate that (1) ¹⁸O-depleted magmas are commonly produced in volcanic terranes invaded by epizonal intrusions; (2) most of the ¹⁸O-depletion in such areas are a result of subsolidus exchange (particularly of feldspars); however correlation of δ¹⁸O with grain size is generally preserved only for systems that have undergone relatively minor meteoric hydrothermal exchange; (3) feldspar and calcite are the minerals mos t susceptible to oxygen isotopic exchange, whereas quartz is very resistant to oxygen isotope exchange; biotite, magnetite, and pyroxene have intermediate susceptibilities; and (4) basaltic country rocks are much more permeable to the hydrothermal convective system than shale, sandstone, or the crystalline basement complex.

Structural geology of the region between Pacoima and Little Tujunga Canyons, San Gabriel Mountains, California

An area of about 25 square miles in the western part of the San Gabriel Mountains was mapped on a scale of 1000 feet to the inch. Special attention was given to the structural geology, particularly the relations between the different systems of faults, of which the San Gabriel fault system and the Sierra Madre fault system are the most important ones. The present distribution and relations of the rocks suggests that the southern block has tilted northward against a more stable mass of old rocks which was raised up during a Pliocene or post-Pliocene orogeny. It is suggested that this northward tilting of the block resulted in the group of thrust faults which comprise the Sierra Madre fault system. It is show that this hypothesis fits the present distribution of the rocks and occupies a logical place in the geologic history of the region as well or better than any other hypothesis previously offered to explain the geology of the region.

O tema do excesso sexual em Gilberto Freyre : Casa Grande & Senzala e Sobrados e Mucambos

Esta dissertação tem por objeto a imagem da sexualidade excessiva do brasileiro, como um dos elementos de caracterização da identidade nacional. Toma as obras CasaGrande & Senzala, e Sobrados e Mocambos de Gilberto Freyre como centrais para a difusão dessa crença. A narrativa freyriana combina de forma já observada por diversos críticos, uma alternância entre ênfases mais naturalizantes e outras enraizadas na esfera cultural. No primeiro caso, por exemplo, estabelece nexos entre raça, sexo e clima. No segundo caso, valoriza o papel da escravidão para caracterizar aspectos da miscigenação e da sexualidade, presentes na sociedade brasileira. Salienta-se o modo como o autor construiu seu discurso sobre as relações entre homens e mulheres, negros, índios, mulatos e brancos. Estas são fundadas em categorias opositivas que revelam uma constante na atribuição de predicados que conectam sexo e gênero, raça e etnia, a partir de um viés assimétrico. Tal procedimento analítico sugere um persistente idioma de gênero.

Programación y mecanizado del escudo del Athletic de Bilbao

[ES]El proyecto ha consistido en el diseño y fabricación de un molde del escudo del Athletic Club de Bilbao que se utilizara posteriormente para plasmar escudos del Athletic en camisetas, barriles y que podría adaptarse a otras aplicaciones como la de fabricar escudos de plástico por inyección. La razón fundamental para el desarrollo del mismo es la cantidad de objetos de plástico que se comercializan en Bilbao y alrededores en los que aparece el escudo del equipo de casa, tales como juguetes para niños, recreaciones a escala del nuevo estadio, etc. El proyecto se ha llevado a cabo en la Escuela Técnica Superior de Ingeniería de Bilbao, más concretamente en su Departamento de Ingeniería Mecánica, y bajo la supervisión de un tutor, en este caso Naiara Ortega. Para la realización del proyecto se han utilizado varios programas muy utilizados actualmente en materia de diseño y fabricación. En primer lugar se ha utilizado el programa Solid Edge para crear un modelo inicial en tres dimensiones de la pieza a que finalmente se va a mecanizar. En segundo lugar, se importara dicho modelo al programa Surfcam para finalizar el diseño y generar las estrategias y trayectorias de mecanizado que ejecutará el centro de mecanizado CNC. En tercer lugar, y por último, se llevará el diseño final con sus correspondientes trayectorias al centro de mecanizado CNC de la Escuela, en donde se mecanizará. Finalmente, tras la realización del trabajo se da cuenta de la importancia de los nuevos programas de diseño y generación de trayectorias para los sistemas de fabricación, que reducen de manera considerable los costes y tiempos de producción, y aumentan significativamente la productividad de las empresas que los utilizan.

De volta para casa: do professor eterno ao complexo docente

Este trabalho apresenta o processo de investigação da pesquisa De volta para casa: do professor eterno ao complexo docente, cujo objetivo ímpar foi analisar o desejo realizado de um grupo específico do magistério: o de retornar como docente da escola em que estudaram. O trabalho adotou o estudo de viés analítico sobre a pesquisa de Sobreira (2008), destacando principalmente o conceito de professor eterno avançando para uma outra perspectiva: o complexo docente. A questão central da pesquisa foi descobrir como os desejos/vontades/sonhos docentes interferem em suas escolhas pedagógicas e profissionais. O trabalho considerou importante a análise conjuntural da escola e, consequentemente, do Curso Normal em relação ao que denominou-se supereu educacional e supereu cultural (FREUD, 2006, 1997a, 1997b; SAFATLE, 2007). Realizou-se uma pesquisa de campo em duas escolas estaduais com Curso Normal de Nível Médio. Portanto, discorre através da análise das entrevistas realizadas com trinta docentes que realizaram esse sonho/desejo, procurando escavar em seus relatos os sentimentos em relação ao retorno, suas recordações da época estudantil e do professor admirado (SOBREIRA, 2008). Os principais referenciais teóricos utilizados foram Adorno, Deleuze e Guattari, adicionando aos estudos o diálogo e a aproximação entre seus conceitos de formação e devir, respectivamente. Destaca-se o posicionamento da pesquisa em relacionar esses dois autores, de correntes filosóficas distintas, num ponto de convergência imbricado com a perspectiva freudiana a respeito das três tarefas impossíveis (governar, psicanalisar e educar). Assim como nestas tarefas, os conceitos de formação e devir estão prenhes da impossibilidade de determinação apriorística de resultados. Nestes termos, aventa-se o imperativo de repensar o currículo da formação docente, a partir do envolvimento dos sentimentos e desejos presentes no magistério, numa construção emancipatória das relações pedagógicas.

Os africanos livres na Casa de Correção: política e direito como disciplinarização

O presente trabalho analisa os africanos livres durante a construção da Casa de Correção da Corte. Para conhecer esse caminho, a investigação começa com a lei de 7 de novembro de 1831 e termina com a inauguração da primeira prisão com trabalho do país, em 1850. A dissertação tem como fio condutor o estudo da produção jurídica sobre os africanos livres e para isso, levam-se em consideração três eixos documentais: as leis brasileiras, os relatórios ministeriais e os despachos burocráticos relativos à administração da casa. O exame dessa material possibilita a operacionalização da noção de disciplinarização e como ela construiu a identidade dos africanos livres como trabalhadores. A disciplina como instrumento de formação de trabalhadores foi o meio de viabilizar a utilização dessa mão de obra. Esse estudo, ao problematizar aos africanos livres na condição de trabalhadores debate as formas de trabalho no Império do Brasil, colocando em pauta as experiências da escravidão e as expectativas do trabalho livre. E nessa análise, o sentido político das enunciações jurídicas foi o cerne para entendimentos desses agentes históricos. Dessa forma, eles foram instruídos e capacitados em diferentes ofícios, na qual recebiam salário e pagavam por sua subsistência. Nesse sentido, a dissertação se estrutura na relação da produção jurídica com a experimentação do trabalho livre.

San Gabriel Valley sewerage system

The disposal of sewage is the most important item in public sanitation. It is the most important present day problem in every city whether large or small. The direct cause of the majority of epidemics is the contamination of the water supply of the city by the excreta of man or animal. Public health varies directly as public sanitation, and if the public sanitation be good, the liability of sickness caused by contamination of the water supply is greatly lessened. When a city outgrows its sewerage system the public health becomes endangered. There are two causes for the increased amount of sewerage, increase in population and increase in industrial and manufacturing wastes. The main problem in this connection is the ultimate disposal of the matter which reaches the sewers.

San Francisco : a city reinvented by creative innovation

The aim of this paper is to analyse the recent evolution of the city of San Francisco to outline the major features that have made it possible this continuing process of creative innovation in the city. In order to meet this objective, the project is framed around answering two key research questions: (1) what are the main economic and social elements that characterise urban change in the city of San Francisco and (2) which is the role of public strategies in the continuing economic success of San Francisco. The paper concludes that the successful performance of San Francisco is the result of the actions taken by many agents in the city, but the role of public authorities, especially the City and County, must be stressed, both through direct intervention and by coordinating, fostering and supporting the private and non-profit sectors. This is especially relevant in a country like the US where private initiative has been seen in many occasions as the greatest driver of economic and social success. Yet, the performance of San Francisco City cannot be explained without the role played by the public sector, in coordination with the civil society

Reposición de la Red Básica Municipal de Donostia/San Sebastián

En el presente Trabajo Fin de Grado, se trabajará sobre la Red Básica Municipal de Donostia/San Sebastián, donde el autor ha sido partícipe en la campaña de reposición de la Red. Nos remontaremos a los orígenes de la Red, explicando cómo nació la Red Básica Municipal de Donostia/San Sebastián y la metodología que se usó para los trabajos previos a su implantación. A lo largo del trabajo, se explicará la metodología de observación y cálculo que se ha empleado en la actual reposición de la Red, el cual ha sido desarrollado por la empresa Geograma S.L. para el Ayuntamiento de San Sebastián entre enero y mayo de 2014. Finalmente, se estudiará como metodología alternativa las observaciones RTK en Red (NRTK), con el fin de validar el método para trabajos de observación de Redes Urbanas de Referencias Topográficas.

Direito à moradia, políticas públicas em habitação e o enfrentamento do déficit habitacional: os desafios do Programa Minha Casa, Minha Vida

A presente dissertação tem por objetivo a análise do Programa Minha Casa, Minha Vida no sentido de verificar se o mesmo é passível de ser aplicado em municípios com características diversas, tornando-se um instrumento útil para esses entes federativos, combatendo o déficit habitacional urbano. Inicialmente, é desenvolvida uma abordagem sobre a moradia e o reconhecido direito a esta, que tem residência nas ideias de direitos fundamentais e direitos humanos, buscando definir sua utilização como instrumento para alcançar um status de dignidade humana. A questão do déficit habitacional, de longa data como objeto de políticas públicas em habitação no país, é também abordada, coligindo-se a teoria do direito à moradia com a realidade do referido déficit, utilizando-se como exemplo histórico a cidade do Rio de Janeiro e procurando abordar o porquê da dificuldade em solucionar a questão da moradia para a população de baixa renda, abordando também a natureza da propriedade imobiliária e a influência do setor imobiliário. Continua-se com a abordagem do programa em bases teórica e técnica, descendo-se após a alguma análise de sua legislação, sem esquecer das bases legislativas e programáticas que o antecederam e com ele relacionados. O trabalho finaliza com três estudos de caso nos Municípios de Silva Jardim, Petrópolis e Rio de Janeiro, onde, pelos dados coligidos, verifica-se que nem todos conseguem a contento implementar o programa em seu território, mormente para a faixa de menor renda, bem como que o programa não deixa de sofrer a influência do setor imobiliário, influência esta que pode acabar determinando para onde a cidade crescerá. Também se verifica que a efetiva atuação do poder público municipal é imprescindível para que o programa se torne um instrumento útil no território da cidade.